The Ultimate 14-Day Iceland Ring Road Itinerary: A Complete Self-Drive Guide - Route 1 (Þjóðvegur)

by - July 16, 2019

Reykjavik, Iceland at 64.1466°N 21.9426°W - Colorful Scandinavian architecture and urban landscape
A photo spot on Skólavörðustígur, one of Reykjavik's main shopping streets that leads directly to the famous Hallgrímskirkja church.
Reykjavik's kaleidoscopic buildings prove Scandinavians do have a sense of color.
They just save it all for their capital city after using up the grayscale on the rest of the landscape.

Our Iceland road trip kicked off in Reykjavik. But let's be honest - Iceland (or Ísland, if you're feeling fancy) has been pulling a legendary bait-and-switch on travelers for centuries. They call it the "Land of Fire and Ice." A more accurate travel guide would rename it the "Land of Wind That'll Steal Your Hat." This is where Viking warriors retired to write poetry, mostly because the weather made pillaging a logistical nightmare.

The country also has a quirky relationship with alcohol. Full-strength beer (over 2.25% alcohol) was banned in Iceland from 1915 until March 1, 1989 - a 74-year stretch known today as Beer Day (Bjórdagurinn). Low-alcohol beer remained legal after 1935, when wine and spirits prohibition was lifted following a trade dispute with Spain. Iceland kept the strong beer ban long after everything else came back. Priorities were… selective.

But here's the secret sauce nobody tells you. Iceland's real magic isn't the postcard-perfect waterfalls or the glaciers posing for National Geographic. It's the absurdity of finding a world-class coffee shop in the middle of nowhere. It's realizing that every Icelander you meet is either a published author, a part-time elf-spotter, or both. The entire country has a population smaller than Wichita, Kansas, but produces more books per capita than anywhere else on Earth. Twenty hours of winter darkness will do that to you. You either write novels or go completely stir-crazy.

Ring Road Route 1 at 64.4458°N 14.5083°W - Icelandic highway winding through volcanic terrain
The Ring Road (Þjóðvegur): Iceland's answer to "what if we built a highway through Mordor?"
This is where your rental car's insurance policy starts sweating bullets.
This specific point is situated along the coastline between the town of Höfn and the East Fjords.

Now let's talk about the real Icelandic experience: the road trip. Not the Instagram-filtered version, but the real deal where you're white-knuckling the steering wheel while 60mph winds try to relocate your Ford Fiesta to Greenland. Imagine cruising a coast so windswept the sheep have learned to lean at 45-degree angles just to stand upright. Volcanic peaks play peek-a-boo in glacial lagoons. Geothermal pools steam like nature's jacuzzi under skies that can't decide if they want to rain, snow, or hail on you. Usually all three. In the same hour.

Laufskálavarða at 63.5941°N 18.4649°W - Traditional Icelandic rock cairns along the Ring Road
Laufskálavarða: Iceland's ancient version of "I was here" graffiti.
Travelers have been stacking rocks here since Vikings forgot how to pillage properly.

We decided to experience Iceland in the automotive equivalent of a tin can with wheels: a Ford Fiesta. Not just any Fiesta - one that had clearly seen better days and a few too many close encounters with Icelandic potholes. We started with the "Golden Circle." Let's be honest, you're basically required by law to do it (the immigration officer at KEF reminded us in person).

After that, we escaped along the South Coast before committing to the full circumnavigation on Route 1. Locals call it Þjóðvegur. Tourists call it "That Road Where You'll Use Up All Your Camera's Memory Card." We later heard our Northeast Iceland scenic driving segment referred to as the "Diamond Circle."

Here's the thing about planning an Icelandic road trip: your plans are about as useful as an ice cube in a volcano. But we tried anyway:

  • Embracing the Unexpected (AKA Accepting You'll Be Wet): Icelandic weather doesn't follow forecasts so much as it laughs at them. We packed for every possible scenario except "instantaneous hurricane," which we later discovered is just "Tuesday afternoon in July." The entire island has mobile coverage, which is handy for checking the weather app that will confidently tell you it's sunny while you're being pelted by horizontal sleet.
  • Fueling Our Wanderlust (And Our Car): Gas stations in Iceland are sparse once you leave major towns, especially in the East Fjords and interior highlands. Many operate unmanned 24/7 and require chip-and-PIN cards. Iceland imports nearly all its fuel, which partly explains the price shock. Fill up early, because pushing a Ford Fiesta across lava fields builds character but not speed.
  • Respecting the Wild (AKA Don't Be That Tourist): Iceland's ecosystem is about as fragile as a house of cards in a wind tunnel. We made solemn vows to leave no trace and obey all signs. We absolutely did not drive our Fiesta off-road. Fun fact: driving off-road in Iceland isn't just frowned upon - it's illegal. The country takes preservation so seriously that whole squads of "environmental rangers" will appear out of nowhere if you so much as look at the moss wrong.

Now, about those stone cairns at Laufskálavarða. They're not random rock piles. The tradition is rooted in the tragic history of the farm Laufskálar, destroyed during the Eldgjá eruption, a massive volcanic fissure event dated to approximately 934–940 AD. Eldgjá is part of the Katla volcanic system and produced one of the largest basalt lava flows of the last 2,000 years in Iceland. Medieval sources such as Landnámabók reference settlements lost during this period. Stacking a stone here was less superstition, more survival psychology. The ridge is named after this lost farm. For centuries, travelers crossing the perilous Mýrdalssandur desert would stack a stone here for good luck. The custom continues today.

Next came the actual route planning. Here's the map of our driving route, which looks impressively comprehensive until you realize it's basically just "drive in a big circle":

  • The Golden Circle: The tourist trail so well-worn you could probably follow the scent of rental car exhaust. We witnessed Strokkur geyser erupting (the Great Geysir had apparently decided to take a centuries-long nap before our arrival). We marveled at Gullfoss waterfall, which pours with the kind of intensity usually reserved for dramatic movie scenes. We also walked through the rift valley at Þingvellir, where the North American and Eurasian tectonic plates are gradually pulling apart along the Mid-Atlantic Ridge. The separation rate averages about 2 centimeters per year. It is less dramatic than splitting a continent in half, but geologically speaking, it counts.
  • Southern Delights: This is where Iceland shows off. Glaciers calve into Jökulsárlón lagoon with the dramatic flair of a nature documentary. Waterfalls so spectacular they make Niagara look like a leaky faucet. Seljalandsfoss lets you walk behind the curtain of water - magical until you remember you're wearing jeans that will take three days to dry.
  • The Ring Road Adventure: The main event. An epic circumnavigation featuring black sand beaches that look like Satan's personal Zen garden. Geothermal areas that smell like rotten eggs - but in a "this is good for your skin" kind of way. Fishing villages so charming you'll briefly consider abandoning your life to become a herring fisherman. Until you remember herring smell worse than the geothermal areas.

Here's a sobering fact for your navigation system. The Ring Road (Route 1) wasn't actually a "ring" until 1974, when the 904-meter Skeiðará Bridge opened across the Skeiðará glacial river on Skeiðarársandur. The bridge was completed in time for the 1,100th anniversary of Iceland’s settlement (traditionally dated to 874). At the time, it was the longest bridge in Iceland. When glacial floods from Grímsvötn destroyed it in 1996, twisted steel beams were left on display as a reminder that Icelandic rivers do not negotiate. Before that connection, continuous road travel around the island was not possible. Travelers had to either turn back or own an amphibious vehicle. This explains why the paved road surfaces are still a work in progress. The country has technically only been fully connected for about 50 years.

Driving Iceland by car is an adventure that makes other road trips look like a leisurely Sunday drive to grandma's house. You can use our experience as a travel guide, or you can ignore it completely and learn the hard way like we did. Either approach works, though one involves less swearing at gas pumps. Prepare to be swept away by Iceland's untamed beauty. Forge memories that will last until your next equally ill-advised adventure.

This is just the beginning. Iceland demands you pack your sense of adventure, a healthy disregard for personal comfort and enough thermal layers to survive a minor ice age. Watch our road trip slideshow for the visual evidence of our questionable life choices:


Watch: Overlanding Iceland: Golden Circle, Southern Delights & Route 1 (Ring Road / Þjóðvegur) by Car (Youtube)

Keflavik International Airport (KEF): Where Your Iceland Road Trip Begins (And Your Wallet Weeps)

Keflavik International Airport sits on the Reykjanes Peninsula. It looks like it was dropped there by aliens who appreciated efficient design. As Iceland's primary gateway, it's where you'll first experience the delightful shock of paying $25 for a mediocre sandwich. It's a rite of passage for every visitor.

Icelandair has perfected the art of the "stopover program." It's marketing genius for "we know you're just passing through to Europe, but how about you spend a few days and several hundred dollars here first?" The red-eye from Washington Dulles arrives at the unholy hour when even airport staff look like they'd rather be anywhere else. You get to pick up your rental car and immediately start driving on the wrong side of the road while sleep-deprived. Good times.

Iceland Air flight interior at cruising altitude - Transatlantic red-eye service configuration
Iceland Air's red-eye: Where you trade sleep for the privilege of arriving in Iceland at dawn.
The in-flight sandwich costs $18 but comes with complimentary existential dread.

Keflavík Airport traces its origins to 1942, when British forces first constructed an airfield during World War II. Later that year, U.S. forces expanded the site into what became Naval Air Station Keflavik. The airbase operated until 2006 and was a key NATO outpost during the Cold War. The wind, according to military records, was not optional.

Keflavik Town: Where Jet Lag Meets Charm

Keflavík itself has a population of roughly 8,000 residents, but it forms part of the larger municipality of Reykjanesbær, which has around 19,000 inhabitants combined (Statistics Iceland). The wind is shared equally by all of them.

Keflavik harbor at 64.0019°N 22.5611°W - Icelandic fishing boats and traditional coastal buildings
Intersection of Hafnargata and Tjarnargata in downtown Keflavík. Clearly, the 'Keflavík Café' serves a very strong brew of 'Wait, which way is the ocean?'"
There is a Giantess in the Cave nearby.

The town's streets are lined with houses painted in colors so cheerful they seem to be compensating for nine months of gray skies. You can wander through them sampling local cuisine that frequently involves fish prepared in ways you didn't know fish could be prepared. Fermented shark, anyone? No? Smart choice.

Keflavik residential street at 64.0015°N 22.5589°W - Colorful Icelandic houses and urban design
Keflavik's architecture: Proof that Icelanders use all their color quota on buildings.
The vibrancy is necessary to combat seasonal affective disorder.

Keflavík's commercial roots trace back to the Danish Trade Monopoly (1602–1787), when Iceland was legally restricted to trading only with licensed Danish merchants. Prices were fixed, competition was banned and Icelanders had little bargaining power. The monopoly ended in 1787, opening the island to broader trade. Economic freedom arrived slowly, but at least it eventually arrived. Keflavík was one of the few designated trading stations. Locals were legally forced to sell their fish here for pittance prices. It wasn't until the 19th century that the town began to flourish independently. It eventually became known as the "Beatles Town" of Iceland in the 1960s and 70s due to the influx of fresh rock 'n' roll vinyl arriving via the nearby American NATO base.

The nearby Blue Lagoon is fed by mineral-rich geothermal seawater from the Svartsengi Power Station. The milky blue color comes from suspended silica particles that reflect light. The lagoon itself formed accidentally in the late 1970s when excess geothermal water pooled in a lava field. It later became one of Iceland’s most photographed man-made accidents.

Pro-tip for budget travelers. We stocked up at the Bonus supermarket at Túngata 1. Bonus is Iceland's answer to "how can we make groceries slightly less bankrupting?" It's where you'll find other tourists staring at prices with the same shell-shocked expression you're wearing. Buy water, snacks and enough supplies to survive the apocalypse. Or at least three days on the road trip.

Bonus supermarket in Keflavik at 63.9998°N 22.5564°W - Budget grocery shopping in Iceland
Bonus supermarket: Where tourists go to weep softly over yogurt prices.
That $8 loaf of bread tastes better when you call it "artisan."

The Stone Trolls of Keflavik: Iceland's Original Rock Stars

In the folklore of Iceland's coastal towns, stone trolls aren't just mythical creatures. They're the original Icelandic residents who failed to get inside before sunrise. According to legends preserved in the 14th-century "Íslendingasögur" manuscripts, these ancient beings would turn to stone if caught in daylight. That explains why Iceland has so many interestingly shaped rocks and so few actual trolls.

We met two of Keflavik's most famous petrified residents: Steinn and Sleggja (Boulder and Sledgehammer to those who don't speak Troll). Coastal rock formations like these are shaped by centuries of Atlantic wave erosion against basalt lava. The Reykjanes Peninsula sits on the Mid-Atlantic Ridge, which means the land itself is geologically young and constantly shifting. The trolls may be folklore, but the tectonics are very real.

Steinn and Sleggja troll rocks in Keflavik at 64.0021°N 22.5622°W - Icelandic folklore stone formations
Stein and Sleggia (The Keflavík Viewing Platform). When a new seawall blocked the ocean view for a local kindergarten, the kids complained and actually got results. The town built this elevated viewing platform with steps leading right to the sea. Two massive rock ogres named Stein and Sleggia (Boulder and Sledgehammer) stand guard. The children just wanted to see the open water, but Keflavík pragmatically decided to give them trolls, too.

Belief in the supernatural is a matter of statistical record here. A 2007 University of Iceland survey found that roughly 62% of respondents said the existence of Huldufólk (Hidden People) was either possible or that they would not rule it out. Very few claimed absolute belief. Even fewer claimed to have an elf’s phone number. This isn't just quirkiness. Construction projects on the Ring Road have famously been altered or delayed to avoid damaging suspected elf habitations. In Iceland, folklore has the power to override civil engineering.

Information sign at viewing platform between Steinn and Sleggja troll rocks in Keflavik
The viewing platform story in Keflavik: When Icelandic children demand better views, mayors listen.
The platform was built after kids complained their troll-watching was being obstructed.

The viewing platform between Steinn and Sleggja has an origin story cuter than a puffling. Keflavik's children complained to the mayor that a new seawall was blocking their view of the ocean from the Bakkalag depression. The mayor, either a softie or tired of hearing about it, built them this platform. Democracy in action, Icelandic style.

Behind the trolls stands the Fishermen Monument, created by artist Ásmundur Sveinsson. It commemorates drowned and missing fishermen with the kind of solemn dignity that makes you stop and think about how brutal life at sea can be. Then you remember you're about to get in a Ford Fiesta, which suddenly feels very safe by comparison.

Fishermen Monument in Keflavik at 64.0023°N 22.5618°W - Memorial to drowned Icelandic sailors
Fishermen Monument in Keflavik: A sobering reminder that the North Atlantic plays for keeps.
The sculpture faces the sea, forever watching for those who never returned.

Buried in the 1965 municipal archives of Keflavik is a record of a fierce debate about the monument's orientation. The original plan had it facing the town, a comfort to the living. The fishermen's families insisted it face the sea, to watch for the return of those lost. They won. The memorial doesn't just remember the dead. It maintains a stubborn, geometric vigil for the ones the ocean kept.

Detailed view of Fishermen Monument sculpture in Keflavik, Iceland - Geometric memorial design
The Sailor's Sign at the Fishermen Monument in Keflavik: Six meters of geometric grief facing the unforgiving sea.
The lifebuoy symbolizes hope, the anchor represents steadfastness and the waves?
They're just the North Atlantic being its usual terrible self.

Blue Lagoon: Where Power Plant Runoff Becomes a Spa Day

Let's address the geothermal elephant in the room. The Blue Lagoon is fed by mineral-rich geothermal seawater from the Svartsengi Power Station. The milky blue color comes from suspended silica particles that reflect light. The lagoon itself formed accidentally in the late 1970s when excess geothermal water pooled in a lava field. It later became one of Iceland’s most photographed man-made accidents.

Moss-covered volcanic rock near Blue Lagoon at 63.8804°N 22.4492°W - Icelandic lava field vegetation
Icelandic moss near the Blue Lagoon: The only plant that can survive being constantly misted with geothermal runoff.
It grows approximately one centimeter per century, so don't even think about stepping on it.

Here's the science part nobody reads. The geothermal seawater originates 2,000 meters beneath the surface. It gets heated by the Earth's mantle to temperatures that would cook a lobster in seconds. Then it gets pumped into the lagoon after the power plant has stolen all the useful energy. The water contains silica, algae and minerals that supposedly have therapeutic properties. Or at least that's what they tell you while charging $100 for the privilege of soaking in it.

Blue Lagoon geothermal spa at 63.8804°N 22.4492°W - Milky blue geothermal waters and bathers
The Blue Lagoon: Where geothermal runoff becomes a $100 Instagram opportunity.
The milky blue color comes from silica that will make your skin feel amazing
and your hair feel like straw for the next three days.

The lagoon's bathing tradition began by accident in 1981. Valur Margeirsson, a local employee at the Svartsengi plant, sought relief for his psoriasis. He was the first to brave the "mud pool," despite skeptical colleagues calling it the polllurinn (the puddle). His skin condition improved remarkably, launching the site's reputation for healing properties long before it became a luxury spa.

Blue Lagoon geothermal waters and bathers at 63.8804°N 22.4492°W - Spa experience
Geothermal bliss at the Blue Lagoon: The water is a perfect 38°C (100°F), which is exactly
the temperature at which you stop caring you're bathing in power plant effluent.
The silica mud mask station is included, because exfoliation shouldn't be extra.

The Blue Lagoon is technically an environmental accident that paid off. The pool didn't exist until 1976, formed solely by the discharge water from the Svartsengi geothermal power plant. The silica-rich water was supposed to soak into the porous lava field. But the mineral content was so high it clogged the lava's pores, creating a permanent, milky pool. When Valur Margeirsson first bathed here in 1981 to treat his psoriasis, locals were skeptical of the "mud pool." The results launched a skincare empire.

Blue Lagoon complex and facilities at 63.8804°N 22.4492°W - Spa architecture
The Blue Lagoon facilities: Where Scandinavian design meets geothermal economics.
Everything is tasteful, minimalist and costs approximately three times what it should.

The Blue Lagoon offers amenities that include in-water massages, silica mud mask stations and the opportunity to pay $15 for a smoothie. But a crucial Blue Lagoon tip for anyone with long hair: coat it in conditioner *before* entering the water and leave it in. The high silica content that is so good for your skin will wreak absolute havoc on your hair, turning it into a stiff, unmanageable broom for days. It's a mineral-rich geothermal spa experience that is rejuvenating for the body, provided you don't mind looking like you stuck a finger in an electrical socket afterward.

Reykjavik: The Starting Point for Your Iceland Road Trip

Reykjavik stands as a vibrant hub on the edge of the North Atlantic. That's a polite way of saying it's the last stop before the Arctic Circle. As Iceland's capital and largest city, it's home to approximately 60% of the country's population. About 130,000 people have decided that living in near-constant wind is preferable to living anywhere else in Iceland.

Reykjavik cityscape at 64.1466°N 21.9426°W - Icelandic capital urban architecture and streets
Reykjavik: Where colorful buildings fight a valiant battle against the gray sky.
The city has more coffee shops per capita than Seattle, because caffeine
is necessary to survive 20 hours of winter darkness.

The cityscape features houses painted in shades so bright they look like they're trying to ward off seasonal depression through sheer chromatic willpower. Streets are lined with trendy cafes where a cup of coffee costs enough to make you consider taking up home brewing. Restaurants serve fermented shark (hákarl) because apparently traditional cuisine should taste like regret.

Laugavegur shopping street in Reykjavik at 64.1462°N 21.9398°W - Main commercial district
Laugavegur: Reykjavik's main shopping street where you can buy
a $50 wool sweater that will actually keep you warm, or a $30 t-shirt that won't.
The street name means "wash road" because Vikings did laundry here. Seriously.

The iconic Hallgrímskirkja church dominates the skyline with its expressionist architecture. It looks like it was inspired by Iceland's basalt columns, or maybe just a really creative stack of organ pipes. Designed by state architect Guðjón Samúelsson in 1937, it took 41 years to build because apparently even churches move at Icelandic pace.

Hallgrímskirkja Church in Reykjavik at 64.1417°N 21.9271°W - Expressionist Lutheran church
Hallgrímskirkja: Reykjavik's concrete spaceship preparing for takeoff.
The design was inspired by Iceland's basalt columns, which explains why it looks
like God stacked a bunch of organ pipes and called it a day.

Leifur Eiríksson stands watching from the top of a smaller spaceship before it.

Before heading inside the church, we stopped to admire the monument to Leifur Eiríksson, 'Discoverer of Vinland'. The statue was actually a gift from the U.S. government, arriving years before the church itself was even completed.

Reykjavik's obsession with the written word is a statistical anomaly. The city was designated a UNESCO City of Literature in 2011. It acknowledges a culture where one in ten Icelanders will publish a book in their lifetime. This culminates annually in the Jólabókaflóð, or "Christmas Book Flood," where the majority of books are purchased in a frantic two-month window. In this city, giving someone a book on Christmas Eve isn't just a gift. It's a mandatory survival tool for the dark winter night.

Reykjavik streetscape at 64.1466°N 21.9426°W - Urban Icelandic architecture and city life
Reykjavik's architectural philosophy: Bright colors, clean lines and
enough insulation to survive nuclear winter. The city feels like someone
took Stockholm and gave it a personality transplant.

The Old Town features historic sites that date back to when Reykjavik was basically just a few farms huddled together for warmth. The waterfront offers charming views and the constant smell of the sea. The nightlife is famous for starting late and ending... never, really, since in summer the sun barely sets. It's like Vegas, but with better sweaters and fewer Elvis impersonators.

Laugavegur buildings in Reykjavik Old Town at 64.1464°N 21.9402°W - Historic city center
Reykjavik's Old Town: Where 19th-century buildings rub shoulders with
21st-century prices. The cobblestone streets have seen more tourists
in the last decade than they saw locals in the previous century.

Þingvellir National Park: Where Continents Divorce and Democracy Was Born

Þingvellir (pronounced "thing-vet-lir" if you want to sound Icelandic, or "that place with the big crack" if you're being honest) holds the impressive triple crown of being historically, culturally and geologically significant. It's like the overachiever of national parks.

Established in 1930, Þingvellir isn't just a pretty landscape. It's the site of the Alþingi, the world's oldest existing parliament that's been exercising democracy since 930 AD. That's over a thousand years of parliamentary procedure, which explains why Icelanders have that slightly weary look about them.

Þingvellir National Park entrance at 64.2558°N 21.1297°W - UNESCO World Heritage Site gateway
Þingvellir National Park entrance: Your gateway to geological drama
and political history. The parking fee is worth it just to say you've stood
between two tectonic plates arguing about property lines.

A more sobering reality than "breathing ground" is the history of Drekkingarhylur (The Drowning Pool). This picturesque bend in the Öxará river served as the official execution site for women from 1590 until 1739. While men were beheaded or hanged, women convicted of crimes ranging from incest to perjury were tied in sacks and drowned here. The calm water you photograph today hides a judicial history so dark it makes the volcanic rift look downright cheerful.

Þingvellir National Park visitor area at 64.2558°N 21.1297°W - Park facilities and landscape
Þingvellir's visitor center: Where you learn that "thing" in Old Norse
means "assembly," not "object." The Vikings were surprisingly literal
when naming their parliamentary meeting spots.

Nicknamed the "Assembly Plains," Þingvellir served as Iceland's political heart from 930 to 1798. Viking chieftains would gather here annually to settle disputes, make laws and probably complain about the weather. The echoes of their debates still seem to whisper through the remains of turf booths and stone shelters scattered across the landscape. Or maybe that's just the wind.

Assembly Plains at Þingvellir National Park at 64.2558°N 21.1297°W - Historical parliamentary site
The Assembly Plains: Where Vikings practiced democracy 800 years before
the American Revolution. The law rock (Lögberg) is somewhere in this view,
probably hidden under a tourist trying to take a selfie.

According to the 12th-century Íslendingabók (Book of Icelanders), the Alþingi's first laws included sensible provisions like "don't murder your neighbor" and "pay your debts." They mixed in more peculiar regulations like "don't compose insulting poetry about someone unless it's really clever." The latter explains Iceland's rich tradition of flyting, which is basically Viking rap battles with more alliteration and fewer gold chains.

Assembly Plains landscape at Þingvellir at 64.2558°N 21.1297°W - Historical site panorama
Fissure swarms at Thingvellir marking the on-land extension of the Mid-Atlantic Ridge within Iceland’s Western Volcanic Zone.

Geologically speaking, Þingvellir National Park - a key stop on the Golden Circle - is where the North American and Eurasian tectonic plates are engaged in the world's slowest breakup. The Mid-Atlantic Ridge runs through Iceland here and the plates are separating at roughly 2 centimeters per year. Þingvellir sits within an active rift zone, where repeated earthquakes and subsidence create the dramatic fissures visitors walk through today. This geological tension creates fissures like Silfra, where brave souls can snorkel in glacial meltwater that has been filtered through porous lava rock for an estimated 30 to 100 years before emerging in the fissure. The slow underground journey explains the extraordinary clarity. The water is so clear that visibility exceeds 100 meters. Though at a frigid 2°C (35°F), you might be too distracted by the brain freeze to appreciate the optical clarity.

Rocky rift valley at Thingvellir at 64.2558°N 21.1297°W with deep fissures and steep basalt walls
Almannagjá Gorge: The world's most dramatic property line dispute.
North America is to the west, Eurasia to the east and you're standing
in the awkward middle where nobody wants to pay for repairs.

Þingvallavatn (which, we can now guess, means "the lake at the assembly area"), Iceland's largest natural lake, completes the park's dramatic scenery. Spanning 84 square kilometers of crystal-clear water that reflects the moody Icelandic sky, it's home to ridiculously overweight Arctic char and brown trout. Those fish have probably seen more tourists than fish in their lifetimes. The lake served as a backdrop to the Alþingi gatherings, where Viking lawmakers would presumably pause their debates to appreciate the view, or at least to wonder if the fish were biting.

Þingvallavatn Lake at Þingvellir at 64.2558°N 21.1297°W - Iceland's largest natural lake panorama
Þingvallavatn: Iceland's largest lake, containing approximately
2.8 billion cubic meters of very cold, very clear water. The fish here
have witnessed a millennium of parliamentary bickering from a safe distance.

The Haukadalur Geothermal Field: Where Earth Burps Spectacularly

The Haukadalur Valley is Iceland's premier geothermal theater. It stars Strokkur geyser as the main attraction and the Great Geysir as the retired legend who still gets billing. This is where the Earth puts on a show that makes Old Faithful look like a leaky faucet.

Geysir information board in Haukadalur at 64.3108°N 20.3028°W - Geothermal area signage
Geysir information: The Great Geysir gave its name to all geysers worldwide,
then promptly went to sleep like a diva who's tired of the spotlight.
Strokkur now handles all public appearances.

The Great Geysir, from which all other geysers get their name, has been mostly dormant since 1916 when it decided it had performed enough. Its neighbor Strokkur ("The Churn" in Icelandic) now handles the geothermal entertainment. It erupts every 6-10 minutes with the reliability of a Swiss train schedule, if Swiss trains shot boiling water 30 meters into the air.

Great Geysir site in Haukadalur at 64.3108°N 20.3028°W - Dormant geyser pool
The Great Geysir's retirement pool: After centuries of spectacular eruptions,
it now rests peacefully, occasionally bubbling to remind everyone
who's still the original geothermal celebrity around here.

According to the 18th-century travel journals of British naturalist Sir Joseph Banks, the Great Geysir could once erupt to heights of 80 meters (262 feet). That terrified local farmers who believed it was the entrance to hell (along with Darvaza on the other side of the globe). Banks himself attempted to measure the depth of the geyser's vent using a weighted line. He gave up after 45 meters when the line kept getting melted. Science in the 1700s was equal parts curiosity and foolish bravery.

The geothermal area is a sensory experience. Steam vents hiss like angry tea kettles. Bubbling hot springs look like nature's Jacuzzi (if nature's Jacuzzi smelled like rotten eggs). Colorful mineral deposits create an otherworldly palette of oranges, yellows and greens. The entire area smells distinctly sulfuric. That's either "the smell of Earth's primal forces" or "what happens when you leave eggs in a hot car," depending on your perspective. And yes, comparisons with Yellowstone are natural, but a bit futile.

Geysir area development plan signage in Haukadalur - Site planning information
Geysir development plans: Even geothermal attractions need zoning approval.
The boardwalks keep tourists from accidentally becoming part of the geothermal show,
which is generally frowned upon by both insurance companies and families.

Historically, impatient tourists and even royalty didn't wait for nature. When the King of Denmark visited in 1907, locals forced an eruption by dumping 40kg of soap into the Great Geysir. The soap lowers the surface tension of the water, inducing boiling. That practice became common throughout the 20th century until environmental concerns finally put a stop to it in the 1990s. Today, Strokkur erupts naturally, requiring no laundry detergent to perform.

Hot water spring in Haukadalur at 64.3108°N 20.3028°W - Geothermal pool
A hot water spring in Haukadalur: Not quite geyser material, but still
respectably steamy at 80-100°C (176-212°F). The minerals create those
beautiful colors and that distinctive "volcanic spa" aroma.

Gullfoss: The Waterfall That Swallows Rivers Whole

In Iceland's geological heart, the Hvítá river makes a dramatic career change at Gullfoss. It plummets 32 meters in two thunderous stages. The name means "Golden Falls," which is either poetic license or what happens when sunlight hits the spray just right and you've had one too many Viking beers.

Gullfoss waterfall at 64.3269°N 20.1214°W - Golden Falls two-stage cascade
Gullfoss: Where the Hvítá river takes a 32-meter leap of faith into a canyon.
The two-stage drop creates a perpetual rainbow when the sun cooperates,
which in Iceland means approximately 15 minutes per year.

The waterfall was almost lost to industrialization in the early 20th century. English investors sought to harness its power for electricity. But the landowner, Tómas Tómasson, famously refused to sell, stating, "I do not sell my friend." His daughter, Sigríður Tómasdóttir, went a step further. She walked barefoot to Reykjavik to protest and threatened to throw herself into the falls if the hydroelectric project proceeded.

Gullfoss waterfall viewpoint at 64.3269°N 20.1214°W - Visitor perspective of cascade
The Gullfoss viewpoint: Where thousands of tourists stand in awe
and get systematically misted by 140 cubic meters of water per second.
The stone plaque commemorates Sigríður Tómasdóttir, the woman who saved
this view from becoming a power station in 1907.

Sunlight dances on the spray, painting rainbows that photographers wait hours to capture and Instagram immediately. The 105-foot total plunge unfolds like nature's most dramatic staircase. The river disappears into a narrow canyon that looks like the Earth decided to swallow it whole. From the viewing platform, the wind carries mist that will soak you to the bone and whispers tales of Sigríður Tómasdóttir, the farmer's daughter who saved the falls. Legend says she threatened to throw herself into the waterfall if the hydroelectric plans went through. She famously rode to Reykjavik - not barefoot as the dramatic myths claim - to protest. Her legal battle resulted in Iceland's first environmental protection law. It proves that stubbornness is indeed Iceland's most valuable national resource.

Below the falls, the churning cauldron boils with the energy of 140 cubic meters of water per second in summer (about 37,000 gallons). It's a reminder of the raw power that shaped this landscape over millennia. Gullfoss is more than a waterfall. It's Iceland's liquid soul. A force that humbles you, soaks you and leaves you forever changed. Or at least with very wet jeans that will take the entire drive to the next destination to dry.

According to early geological surveys by Icelandic scientist Þorvaldur Thoroddsen, the Gullfoss canyon was formed during catastrophic glacial outburst floods at the end of the last ice age. Meltwater equivalent to several Amazon Rivers carved through the basalt in a matter of days. The current relatively peaceful flow is just the river taking a well-deserved rest after that epic landscaping project.

Kerið Crater: Iceland's 3,000-Year-Old Swimming Pool

Most tourists think Kerið Crater is just another pretty hole in the ground when exploring South Iceland attractions. They're wrong. This 3,000-year-old volcanic crater in the Grímsnes area is a classic scoria crater. Unlike the "rootless cones" found at Mývatn, Kerið actually had a magma chamber that collapsed after an eruption, creating its perfect inverted-cone shape. It's a window directly into the earth's plumbing.

Aerial view of Kerið Crater showing the stunning turquoise lake surrounded by red volcanic slopes in Grímsnes, South Iceland
The turquoise waters of Kerið Crater look inviting, but swimming is prohibited
Local legend says the water's color comes from dissolved volcanic minerals
The crater was privately owned until 2000 when it was sold for preservation

The lake's shocking turquoise color comes from dissolved volcanic minerals, primarily silicon dioxide and various trace elements. In winter, it sometimes freezes over completely, creating a natural ice rink 180 feet across. During particularly cold years, locals used to hold impromptu skating parties here until the landowners put a stop to it in the 1990s.

Here's a quirky bit of trivia. The crater's natural acoustics have actually been tested by Icelandic musicians. While legends persist about Björk performing on a floating raft here, it was actually the Icelandic pop band The Sugarcubes (which she fronted) who utilized the crater's unique soundscape. It proves that a volcanic caldera makes for a surprisingly effective, if damp, amphitheater.

Panoramic view from Kerið Crater rim showing the contrast between turquoise water, red rock and green moss in South Iceland
Walking the crater rim feels like circling a giant natural amphitheater
The red volcanic scoria rock contains enough iron to technically be considered low-grade ore
Early 20th century farmers used the crater as a natural sheep corral

Walking around the rim, you'll notice the vegetation changes dramatically. On the windward side, only the hardiest mosses survive. On the leeward side, you might find dwarf willow and birch trees that have somehow taken root in what amounts to volcanic gravel. Life finds a way, even in places that look like Mars.

This was our final stop on the Golden Circle loop. From here, we'd begin the real adventure: circumnavigating Iceland on Route 1 counter-clockwise. Why counter-clockwise? Simple. We wanted to hit the southern coastline first, where all the big waterfalls and black sand beaches live. Plus, driving this direction gives you the sun at your back in the afternoon, which matters when you're dealing with Icelandic weather.

Selfoss: A Foodie Stop on Your South Iceland Road Trip

Selfoss isn't just a pit stop. It's the largest town in South Iceland with about 8,000 residents. The town's name is a source of constant confusion for visitors. It translates to "Shieling Falls" (from sel, meaning a summer milking shed), not "Seal Falls." Ironically, there are no waterfalls in the town of Selfoss itself. The name actually refers to the swirling rapids in the nearby Ölfusá river. The nearby Ölfusá river is Iceland’s largest river by volume, carrying glacial meltwater from the central highlands toward the Atlantic. Its broad, sediment-rich flow shaped much of South Iceland’s agricultural plains.

Modern interior of Krisp Restaurant in Selfoss showing contemporary Icelandic design and dining atmosphere
Krisp Restaurant's modern interior reflects Iceland's contemporary design aesthetic
The restaurant occupies a building that once housed a hardware store in the 1970s
Notice the minimalist decor - typical of Icelandic restaurants that let the food speak for itself

For fine dining, Tryggvaskali Restaurant occupies a building that's been around since 1895. It survived the earthquake by being made of imported Norwegian timber, which flexed instead of snapping. Their signature dish? Pan-seared Arctic char with wild mushroom risotto, sourced from local rivers and forests.

If you're feeling adventurous, The Old Dairy Food Hall (actually located in a converted 1930s dairy plant) offers everything from sushi to tacos. The sushi might surprise you. Icelanders have been making sushi since the 1990s, long before it was trendy worldwide. They use Arctic ingredients like sea urchin, kelp and yes, sometimes even puffin.

Artistically plated international cuisine with Icelandic ingredients at Krisp Restaurant in Selfoss
Icelandic chefs have mastered the art of making locally sourced food look Instagram-worthy
The portion sizes are European - meaning you might actually leave room for dessert
Vegetarian and vegan options have become surprisingly sophisticated in recent years

Budget travelers should seek out Pylsuvagninn, the hot dog stand that's been a local institution since 1987. Their secret? The hot dogs contain lamb meat, giving them a distinct gamey flavor that pairs perfectly with their special remoulade sauce. It's basically the Icelandic version of fast food royalty.

We ended up at Krisp Restaurant at Eyrarvegur 8. Their menu cleverly blends European techniques with Icelandic ingredients. Think rye-crusted cod with dill cream sauce, or lamb shank slow-cooked for so long it practically falls apart if you look at it too hard. They even have gluten-free options that don't taste like cardboard. A minor miracle in the culinary world.

Evening dining scene at Krisp Restaurant showing warm ambiance and local diners in Selfoss
Dinner in Iceland rarely starts before 7 PM - locals eat late
The lighting is deliberately dim to counteract the midnight sun in summer
Notice the absence of tourists in this shot - we caught the early dinner crowd

Here's a weird historical footnote. During World War II, British forces stationed in Iceland developed such a craving for local dairy that they reportedly traded entire truckloads of military rations for fresh milk from Selfoss farmers. The arrangement was so mutually beneficial that it continued unofficially long after the war ended. Apparently nothing bridges cultural divides like good butter.

Þingborg Ullarverslun: Where Icelandic Wool Gets Serious

We found Þingborg Wool Store exactly eight kilometers east of Selfoss on Route 1. The shop occupies a building with a deeply practical history, far from the ancient farmhouse legends you might hear. The structure is actually a historic community center and former schoolhouse built in 1927. Today, a local cooperative runs the space. We loved seeing how they keep the tradition of authentic Icelandic wool alive within these old school walls.

The store's name translates to "Thingborg Wool Store," with "Thingborg" referring to the nearby ancient parliamentary site. In medieval Iceland, this was another area where local chieftains would gather to settle disputes and, presumably, complain about the weather like true Icelanders.

Traditional Icelandic building housing Þingborg Ullarverslun wool store with historic architecture, South Iceland (63.9450°N, 20.9500°W)
Gallerý Flói / Þingborg Ullarverslun signboard off Iceland Route 1 near Selfoss.
Ull = Wool, Verslun = Store/Shop,
and they are Opið = Open.

Icelandic wool is special for three reasons. First, the sheep are a pure breed unchanged since the Vikings brought them over 1,100 years ago. Second, the wool has two layers: a water-resistant outer coat (tog) and a soft, insulating inner coat (þel). Third, the sheep roam completely free in summer, which gives their wool that distinctive, slightly wild character.

The Lopapeysa sweater isn't just fashion. It's survival gear. The design originated in the 1950s, inspired by traditional Greenlandic patterns. Each region has its own distinctive patterns, so you can tell where someone's from by their sweater. The yoke pattern around the neck isn't just decorative. It adds extra insulation where you lose the most heat.

Colorful display of Icelandic wool sweaters and accessories at Þingborg Ullarverslun store
Þingborg Ullarverslun. This famous wool shop operates out of a historic community center and former schoolhouse built in 1927. We learned a local cooperative runs the place today. They have spent decades mastering the art of spinning and knitting authentic Icelandic lopi wool right here.

Here's something most tourists don't know. Genuine Icelandic sweaters should smell slightly of lanolin (sheep oil) when new. If it doesn't, it might be machine-made or treated with chemicals. The natural lanolin makes the wool water-resistant. It's a feature you'll appreciate when Icelandic weather does what it does best.

The store even sells spinning wheels and carding supplies. Why? Because knitting isn't just a hobby in Iceland. It's a national pastime. There's an old saying: "Icelandic women knit while they walk, talk and even while they argue." During the 2008 financial crisis, knitting circles became impromptu support groups and economic forums.

Traditional Icelandic spinning wheels and wool carding tools on display at Þingborg Ullarverslun
These spinning wheels are replicas of 18th century Icelandic designs
Wool carding was traditionally winter work when farming was impossible
The tools are still used by serious textile artists and traditional crafters

The color range uses natural dyes from Icelandic plants and minerals Each sweater represents 40-60 hours of skilled hand-knitting work The patterns are traditional but colors have been updated for modern tastes

While looking at the wool, ask the staff about the forystufé, or "leader sheep." Iceland is the only country in the world that maintains this specific genetic strain of sheep. They're known for their intelligence and ability to sense bad weather before it arrives. Unlike a standard flock that blindly follows, the forystufé will actively lead the flock home to safety during blizzards. It's a trait preserved in Icelandic sagas and breeding records since the settlement era.

Rows of colorful hand-spun Icelandic wool yarn arranged by color at Þingborg Ullarverslun
The natural colors come from Icelandic sheep breeds that haven't changed in 1,000 years
Each skein represents about 4 hours of hand-spinning work
The yarn is oiled with natural lanolin to protect it during knitting

The staff here are walking encyclopedias of wool knowledge. They can tell you which valley a particular batch of wool came from, what the sheep probably ate and whether it was a particularly rainy summer (which affects wool quality). They're not salespeople. They're wool evangelists.

Yes, Icelandic sweaters are expensive. About 3-4 times the price of a Bolivian alpaca poncho. But consider this. It takes 40-60 hours to hand-knit one sweater. The wool comes from free-range sheep that basically live their best lives roaming volcanic landscapes. And each sweater will literally last a lifetime if cared for properly. It's not a purchase. It's an heirloom.

Also on the same premises is Gallery Flói. It's an artisan-run studio and gift shop operated by Fanndís Huld Valdimarsdóttir. While the wool store focuses on textiles, this gallery highlights different traditional and modern crafts. It features unique glass beads handmade on-site using an open flame, inspired by Viking-age archaeological finds. The shop selection includes various local art pieces, ceramics and design items made from local materials. It provides live demonstrations of glass blowing and bead making for visitors.

And no, we are not affiliated in any way with either shop, other than buying sweaters.

Seljalandsfoss: The Waterfall You Can Walk Behind

Seljalandsfoss isn't just a waterfall. It's a 197-foot-tall curtain of glacial meltwater that originates from the Eyjafjallajökull ice cap. That's the same volcano that shut down European air travel in 2010. The water you're seeing fell as snow on that volcano maybe 50-100 years ago. It traveled through glacial ice and is now making its dramatic exit here.

The waterfall has a fascinating hydrological quirk. It flows year-round, but the volume varies dramatically. In spring melt season, it can become a raging torrent. In winter, it sometimes partially freezes, creating incredible ice formations behind the curtain. During particularly cold winters, brave (or foolish) locals have been known to ice climb the frozen sections.

Majestic Seljalandsfoss waterfall plunging 197 feet into a pool with rainbow visible in mist, South Iceland
The waterfall's height is exactly 60 meters - Icelanders use metric but Americans need translation
The pool at the bottom is surprisingly deep - about 15 feet in the center
This viewpoint is from the traditional parking area, now expanded due to tourist numbers

The walk behind the waterfall is what makes Seljalandsfoss special. The path was originally a sheep trail. Local farmers would move their flocks through here for centuries before tourists discovered it. The rock behind the waterfall is basalt, but it's covered in a thick layer of moss and algae that makes it treacherously slippery. Good waterproof gear isn't a suggestion. It's a requirement unless you enjoy being soaked to the bone.

On sunny days, the mist creates permanent rainbows. In winter, you might see "ice bows" - rainbows formed in ice crystals instead of water droplets. The best time for photography is late afternoon when the sun hits the waterfall at an angle, creating that perfect golden glow.

Powerful water flow of Seljalandsfoss showing the force of glacial meltwater in summer, South Iceland
The water flow varies from 10 cubic meters per second in summer to 3 in winter
Notice the multiple streams - the waterfall splits when water levels are high
The rock face shows clear erosion patterns from centuries of water flow

Local folklore says a hidden cave behind the waterfall was used by outlaws in the Saga Age. There's no archaeological evidence for this, but it makes a good story. What is true is that the waterfall was nearly inaccessible until the 1960s when a proper road was built. Before that, only determined hikers or farmers would visit.

View from behind Seljalandsfoss waterfall showing the curtain of water from the inside, South Iceland
The cave behind the waterfall is about 30 feet deep - enough to stay mostly dry
The rock is covered in thick moss that survives on constant moisture
This viewpoint has been photographed millions of times but never gets old

The surrounding landscape tells a geological story. The black sand beaches are volcanic ash from past eruptions. The distant Westman Islands (Vestmannaeyjar) are visible on clear days. Those islands formed in a single massive eruption in 1963 that created the newest land on Earth at the time. The entire area is essentially a giant volcanic field that's still very much active.

Warning: the infamous Icelandic midges (black flies) love this area in summer. They're not just annoying. They bite. And their bites itch for days. They're most active near glacial rivers and waterfalls where they breed. Some visitors wear mosquito net hats, which look ridiculous but beat itching for a week.

Wide landscape view from Seljalandsfoss showing black sand beaches and coastal scenery, South Iceland
The black sand is volcanic ash from the 2010 Eyjafjallajökull eruption
The coastline here is constantly changing due to erosion and deposition
Those distant islands are the Westman Islands, site of Iceland's largest volcanic eruption

While standing behind Seljalandsfoss, you are technically standing on an ancient sea floor. Thousands of years ago, these cliffs marked the coastline of Iceland. Since the end of the last Ice Age, the weight of the glaciers has lifted, causing the land to rise (isostatic rebound) and pushing the Atlantic Ocean back to its current position several kilometers away. You aren't just looking at a waterfall. You're looking at the former edge of the island.

Visitor facilities and walking path at Seljalandsfoss with people for scale, South Iceland
The visitor center was added in 2015 to handle increasing tourist numbers
The path is now paved - it used to be a muddy trail that destroyed shoes
Notice the strategic placement of trash cans - Iceland takes littering seriously

Seljalandsfoss has a smaller, often overlooked neighbor called Gljúfrabúi (literally "Canyon Dweller"). It's hidden in a canyon just a 10-minute walk north. Most tourists miss it because they don't know it's there. The waterfall is completely hidden until you literally walk into the canyon opening. It's like Seljalandsfoss's shy cousin.

Skógafoss: Where Legends and Rainbows Collide

Skógafoss is the muscle car of Icelandic waterfalls. Big, loud and impossible to ignore. At 200 feet tall and 82 feet wide, it throws enough spray into the air to create permanent rainbows on sunny days. The waterfall sits on the Skógá River, which gets its water from two glaciers: Eyjafjallajökull and Mýrdalsjökull.

Here's a geological oddity. Skógafoss is actually retreating. The hard basalt cap rock at the top is resisting erosion better than the softer rock underneath. Over thousands of years, the waterfall has moved upstream as the undercut rock collapses. It's moving at about one foot every 100 years. That means in another 10,000 years, it'll be in a different location entirely.

Powerful Skógafoss waterfall showing immense volume of glacial meltwater in summer, South Iceland
The waterfall's width creates a perfect semicircle of falling water
The spray zone extends 100 feet from the base - prepare to get wet
This angle shows why it's called "forest waterfall" - though the forest is long gone

The legend of Þrasi's chest has a tangible anchor in reality. A large metal ring, said to be the handle ripped from the treasure chest by a local youth, was actually used as the door handle of the Skógar Church for centuries. It is now preserved in the Skógar Museum. It's a physical artifact of a mythical encounter that you can actually see.

The staircase alongside the waterfall has 527 steps. We counted. It was built in the 1990s to replace a treacherous path that required actual climbing skills. From the top, you get a view that stretches to the ocean on clear days. You can also see where the river begins its journey from the glaciers - a series of smaller waterfalls cascading down the mountainside.

During full moon nights in clear weather, Skógafoss produces moonbows - lunar rainbows. They're faint and colorless to the naked eye but show up in long-exposure photographs as ghostly white arches. The best time to see them is around midnight in summer when the moon is high and the sky is clear.


Skógafoss in motion - the sound is half the experience

Sólheimajökull: The Glacier That's Running Away

Sólheimajökull isn't just a glacier tongue. It's a climate change indicator in real time. The name means "Sun Home Glacier," which is ironic considering it's been retreating rapidly due to warming temperatures. Since 1930, it has retreated over 1 kilometer. You can see the markers showing where the glacier ended in various years. It's like watching a time-lapse in reverse.

This glacier is part of the larger Mýrdalsjökull ice cap, which sits atop Katla volcano. Katla erupts roughly every 40-80 years and it's overdue. The last major eruption was in 1918. When it goes, it'll make the 2010 Eyjafjallajökull eruption look like a campfire. The glacier ice is up to 200 meters thick in places, but it's getting thinner every year.

Sólheimajökull glacier showing blue ice and crevasses with Mýrdalsjökull ice cap behind, South Iceland
The blue ice color indicates dense, old glacial ice with minimal air bubbles
Crevasses form where the glacier flows over uneven bedrock beneath
The black lines are volcanic ash from past eruptions preserved in the ice

Glacial ice appears blue for the same reason the sky appears blue - Rayleigh scattering. The ice absorbs red wavelengths and scatters blue. The denser and older the ice, the bluer it appears. The ice at Sólheimajökull can be hundreds of years old, with layers of volcanic ash from historical eruptions preserved like tree rings.

Guided glacier walks started here in the early 2000s. Before that, only experienced mountaineers would venture onto the ice. The guides now use routes that change weekly as the glacier shifts and new crevasses open. They carry rescue equipment because, well, falling into a crevasse is a really bad way to end your vacation.

Close-up of glacial ice formations and meltwater channels on Sólheimajökull, South Iceland
The surface melt patterns create surreal sculptural forms
Water channels can be several feet deep - carved by summer meltwater
The ice here is dense enough that ice climbers use it for training

The glacier has an interesting microbial ecosystem. Cryoconite holes - small water-filled depressions on the ice surface - contain entire miniature ecosystems of bacteria, algae and even tiny insects. The black dust that forms these holes is mostly volcanic ash and wind-blown soil. Scientists study these ecosystems to understand how life might survive on other planets.

Wide view showing Sólheimajökull glacier terminus and outwash plain in South Iceland
The outwash plain (sandur) is created by glacial meltwater carrying sediment
Vegetation is slowly colonizing areas the glacier has recently retreated from
This viewpoint shows how much the glacier has shrunk in recent decades

If you catch a distinct whiff of rotten eggs while standing at the glacier tongue, it’s not your fellow travelers. The meltwater river, the Jökulsá á Sólheimasandi, often carries a strong sulfuric odor. This is the "smell of Katla" - the sub-glacial volcano simmering beneath the ice cap. The geothermal gases dissolve into the meltwater, serving as a constant olfactory reminder that you are standing on top of one of the most active and dangerous volcanoes in the world.

Dyrhólaey: Iceland's Natural Arch and Puffin Paradise

Dyrhólaey translates to "Door Hill Island," which is accurate. It was an island until geological uplift connected it to the mainland. The massive stone arch is what remains of a collapsed sea cave. The arch is big enough that small airplanes have flown through it on daredevil stunts, though this is now illegal (and stupid).

The promontory is a protected nature reserve, particularly important for birdlife. From May to August, it's home to one of Iceland's largest puffin colonies. These comical birds nest in burrows on the cliff faces. They're surprisingly good diggers, creating tunnels up to three feet deep to protect their eggs from predators.

Wide coastal view from Dyrhólaey showing the natural stone arch and black sand beaches, South Iceland
The stone arch is 120 feet tall - large enough for small boats to pass through
The black sand beaches stretch for miles in both directions
This is one of the best viewpoints to see Iceland's southern coastline

The lighthouse was built in 1910 and automated in 1992. It stands 38 meters above sea level and its light can be seen 27 nautical miles out to sea. The lantern house was actually imported from Sweden, a common practice at the time as Iceland lacked heavy manufacturing. During World War II, Allied forces stationed troops here to watch for German U-boats (submarines) that prowled the North Atlantic shipping lanes. You can still find remnants of concrete bunkers and observation posts scattered along the cliffs if you know where to look. They're ghostly reminders of when this peaceful bird sanctuary was a strategic military lookout.

The massive natural stone arch of Dyrhólaey from sea level perspective, South Iceland
The arch formed when softer rock eroded away, leaving harder basalt columns
Waves have been carving this formation for approximately 8,000 years
The opening is large enough that seabirds use it as a flight corridor

If you visit in winter, you won't just miss the puffins because they are at sea. You wouldn't recognize them even if you saw them. The iconic bright orange beak is actually a seasonal display. After the breeding season ends in late August, puffins shed the colorful outer plates of their bills, leaving them with a smaller, dull grey beak for the winter months. The "clown of the sea" effectively takes off its makeup when the audience leaves.

Historic Dyrhólaey Lighthouse standing on the cliff edge with ocean backdrop, South Iceland
The lighthouse was built from local stone to withstand fierce Atlantic storms
Original keepers lived here year-round in complete isolation
The light pattern is unique to help sailors identify their location

Local folklore says the arch was created by two trolls trying to pull a ship ashore. They turned to stone when caught by sunlight, as trolls do in Icelandic stories. The two sea stacks off Reynisfjara Beach are said to be the trolls' boat, also turned to stone. It's a cute story that explains the geology in a way pre-scientific people could understand.

Colony of seabirds including puffins and guillemots on Dyrhólaey cliff faces, South Iceland
Puffins return to the same burrows year after year with remarkable accuracy
The white birds are kittiwakes - their name comes from their distinctive call
Bird colonies like this can contain tens of thousands of individuals

Reynisfjara Beach: Where Geology Meets Hollywood

Reynisfjara isn't just a black sand beach. It's a geological textbook open to the volcanic chapter. The black sand is basaltic ash from volcanic eruptions, ground fine by wave action over centuries. The beach stretches for miles, but the most famous section is near the village of Vík í Mýrdal, population 318.

The basalt columns are the beach's signature feature. They formed when a thick lava flow cooled slowly, contracting and cracking into hexagonal shapes. The process is similar to mud cracking but on a giant scale. The columns at Reynisfjara are nearly perfect hexagons, some reaching 20 feet tall.

Panoramic view of Reynisfjara black sand beach with basalt columns and sea stacks, South Iceland
The beach's black color comes from volcanic basalt ground into fine sand
Basalt columns form perfect geometric patterns due to cooling lava
This is one of the most photographed locations in all of Iceland

The Reynisdrangar sea stacks are the beach's most dramatic feature. According to legend, they're two trolls who were pulling a three-masted ship to shore when they were caught by sunrise and turned to stone. Geologically, they're remnants of a headland that eroded away, leaving the harder basalt behind. They rise 66 meters (216 feet) from the sea.

Dramatic Reynisdrangar sea stacks rising from the ocean at Reynisfjara Beach, South Iceland
The sea stacks are 66 meters tall - about the height of a 20-story building
They're home to nesting seabirds including puffins and fulmars
The name translates to "Reynir's pillars" after a local settler

The Hálsanefshellir cave is a natural cathedral carved by relentless Atlantic waves. The basalt columns at its entrance create a frame that photographers love. The cave has served as temporary shelter for fishermen caught in storms and, according to folklore, was home to trolls who would emerge at night to cause mischief.

Entrance to Hálsanefshellir cave framed by basalt columns at Reynisfjara Beach, South Iceland
The cave is approximately 30 feet deep and 15 feet high at the entrance
Basalt columns form natural pillars that support the cave roof
Fishermen have used this cave for shelter during storms for centuries

The waves here are notoriously dangerous. "Sneaker waves" can suddenly rush much farther up the beach than previous waves, catching people off guard. The risk is highest during storms or when swell direction changes. Several tourists have been swept out to sea here, which is why there are now warning signs in multiple languages.

Powerful Atlantic waves crashing on the black sand of Reynisfjara Beach, South Iceland
Waves can reach heights of 20 feet during winter storms
The undertow here is particularly strong due to the beach's steep slope
Notice how far the water reaches - this is why keeping distance is crucial

Reynisfjara has become a Hollywood favorite. The Bollywood song "Gerua" from Dilwale (2015) was shot here, featuring Shahrukh Khan and Kajol. After the film's release, Indian tourist numbers surged so dramatically that the local cafe added handwritten Indian food items to their menu. You can now get chicken tikka masala while looking at the same scenery as your favorite stars.

Cafe menu at Reynisfjara showing handwritten additions of Indian food items, South Iceland
Handwritten additions show how quickly Icelandic businesses adapt to tourism trends
Indian tourists increased 300% after the Bollywood film featured this location
The cafe originally served only basic Icelandic fare before expanding its menu

This Vík black sand beach is a superstar. Besides Star Wars: Rogue One (Planet Eadu) and Star Trek: Into Darkness, it famously appeared in Game of Thrones as Eastwatch-by-the-Sea. It seems that whenever Hollywood needs a location that looks beautiful but threateningly alien, they fly a crew to South Iceland. Just remember that while the actors have stunt doubles to handle the dangerous surf, you do not. Enjoy the cinematic views, but respect the very real power of the North Atlantic.


The Bollywood song that put Reynisfjara on the Indian tourist map

The danger at Reynisfjara comes from the seabed topography. The offshore shelf drops dramatically, allowing long-period Atlantic swells to maintain their energy until they crash directly onto the shore without breaking early. These "sneaker waves" can surge significantly higher than the preceding ones without warning. They have claimed the lives of unwary visitors who turn their backs on the ocean.

Always keep at least 30 meters (100 feet) from the water's edge and never turn your back on the ocean.

Powerful sneaker wave rushing up Reynisfjara Beach showing dangerous conditions, South Iceland
This wave reached 50 feet farther up the beach than previous waves
The foam indicates strong turbulence and dangerous undertow
Several fatal accidents have occurred at this exact spot

The danger of Reynisfjara lies in the physics of "fetch" - the distance wind blows over open water without obstruction. If you look due south from this beach, the next piece of land you would hit is Antarctica. This allows thousands of miles of Atlantic rollers to build up massive kinetic energy before unloading it specifically on this stretch of black sand. This creates "sneaker waves" - long-period swells that can surge much higher up the beach than the waves immediately preceding them, catching unalert tourists with deadly consequences.

North Star Cottage: Our Southern Iceland Basecamp

North Star Cottage in Lambafell Hvolsvöllur is more than just accommodation. It's strategically located for exploring South Iceland's highlights. The cottages sit right on Route 1, giving easy access to everything from Skógafoss to the Eyjafjallajökull Visitor Centre. The location was originally a farm, like most things in Iceland, converted to tourism as farming became less viable.

The cottages are built in traditional Icelandic style with modern comforts. The turf roof isn't just decorative. It provides natural insulation, keeping the interior warm in winter and cool in summer. This building technique dates back to the Settlement Age and was nearly lost before a revival in the late 20th century.

Traditional Icelandic cottage with turf roof at North Star Cottage in Lambafell, South Iceland
The turf roof provides natural insulation and blends with the landscape
Each cottage sleeps four - perfect for families or two couples traveling together
The building style is traditional but with modern construction techniques

The interior is surprisingly spacious, with a kitchenette that includes a small refrigerator, stove and basic cooking utensils. This is essential in Iceland where restaurant meals can quickly blow your budget. A simple burger and fries can easily run you $25 USD. The furniture is simple but comfortable, typical of the Nordic design philosophy known as hygge (though that's Danish, the Icelanders have their own version called gluggaveður - enjoying cozy weather through a window). It prioritizes function over ornament, ensuring you have exactly what you need without the clutter.

Compact kitchenette inside North Star Cottage with basic cooking facilities, South Iceland
The kitchenette includes everything needed for simple meal preparation
Grocery stores in nearby Hvolsvöllur stock local ingredients
Cooking your own meals can cut food costs by 50% in expensive Iceland

The location offers stunning views of the Eyjafjöll Mountains and Eyjafjallajökull Glacier. On clear nights, the northern lights are visible from the terrace. The absence of light pollution makes this an excellent stargazing spot, though in summer you'll have to stay up late - or get up early - to see actual darkness.

Cozy living area with comfortable seating in North Star Cottage accommodation, South Iceland
The living area converts to sleeping space with a fold-out sofa bed
Large windows maximize natural light during Iceland's long summer days
The decor is minimalist Icelandic - functional and comfortable

Nearby attractions include the Icelandic Lava Show in Hvolsvöllur, where they melt real lava at 1100°C and pour it right in front of you. There's also the Saga Centre, dedicated to Njál's Saga, one of Iceland's most famous medieval stories. The saga is set in this very area, making the landscape come alive with historical context.

Comfortable sleeping area with quality bedding in North Star Cottage, South Iceland
The beds are surprisingly comfortable - important after a day of hiking
Blackout curtains help with the midnight sun during summer months
Heating is geothermal - standard in Iceland where energy is cheap and green

The cottage's terrace is the perfect spot for evening relaxation. With a glass of local beer (or hot chocolate, depending on the weather), you can watch the light change on the mountains. In summer, the sun sets around 11 PM and rises around 3 AM, creating long, golden evenings that seem to stretch forever.

Scenic mountain view from the terrace of North Star Cottage in Lambafell, South Iceland
The Eyjafjöll Mountains dominate the view - home to the famous 2010 volcano
This area is agricultural land, with sheep farms surrounding the cottages
The terrace faces west for perfect sunset views on clear evenings

Practicalities: Wi-Fi is reliable (important for planning the next day's adventures). Parking is right outside your door. The bathroom has a surprisingly good shower with consistent hot water - heated geothermally, of course. Towels and linens are provided, which isn't always the case in Icelandic cottages.

Multiple North Star Cottage units showing the compound layout in Lambafell, South Iceland
The compound has six cottages, each with privacy between units
Shared outdoor spaces allow socializing with other travelers
The design maximizes views while maintaining wind protection

Laufskálavarða: Iceland's Stone Cairn Tradition

In the middle of the Mýrdalssandur black sand desert stands Laufskálavarða, a small lava ridge covered in thousands of stone cairns. This isn't a natural formation. It's a human one, created by travelers following an ancient tradition. The custom dates back to the Settlement Age, when first-time crossers of this dangerous desert would build a cairn for good luck.

Mýrdalssandur is a glacial outwash plain created by meltwater from Mýrdalsjökull glacier. It's essentially a vast, flat expanse of black volcanic sand and gravel. The desert is notoriously dangerous in storms, with winds strong enough to strip paint from cars. Early travelers would wait for good weather before attempting the crossing.

Snow-covered glacier surface of Mýrdalsjökull hiding the Katla volcano beneath at 63.5833°N, 18.7167°W
Katla central volcano beneath the Mýrdalsjökull ice cap, known for subglacial eruptions that trigger catastrophic jökulhlaups (glacial outburst floods).

The cairn-building tradition has evolved. Originally, travelers built cairns as offerings to the land spirits (landvættir) for safe passage. Today, it's more of a tourist ritual, but the sentiment remains. Some cairns are simple stacks of three stones. Others are elaborate constructions several feet high. There are now thousands, creating a surreal forest of stone.

Thousands of stone cairns covering Laufskálavarða hill in Mýrdalssandur desert, South Iceland
Some cairns have stood for decades while others are rebuilt each season
The tradition continues with modern travelers adding their own stones
The hill itself is a lava ridge that survived glacial floods

The viewing platform offers panoramic views of Mýrdalsjökull and, on clear days, the Westman Islands. The platform was built to protect the fragile environment from erosion caused by thousands of visitors. Before its construction, people would scramble up the hillside, damaging the vegetation and causing the cairns to collapse.

Katla volcano, beneath Mýrdalsjökull, is one of Iceland's most powerful volcanoes. It erupts every 40-80 years, with the last major eruption in 1918. When it next erupts, it will likely melt enough ice to cause massive glacial outburst floods (jökulhlaups) that will sweep across Mýrdalssandur. The entire area is an evacuation zone for this reason. Katla volcano is central to Netflix's supernatural thriller series of the same name.

Panoramic view from Laufskálavarða showing the vast black sand desert, South Iceland
The road cuts straight across the desert - a modern version of an ancient route
Marker poles help travelers navigate during whiteout conditions in winter
This landscape changes dramatically during glacial outburst floods

Laufskálavarða embodies the Icelandic relationship with nature - respectful, practical and tinged with folklore. The cairns represent human presence in a landscape that constantly reminds you of your insignificance. It's a place where modern tourism meets ancient tradition, where each stone tells a story of someone's journey across this formidable landscape.

As we continued eastward from here, we were heading into even more dramatic South Iceland attractions - glaciers, iceberg lagoons and fjords that would make this already incredible journey seem like just the warm-up.

Gönguleið um Eldhraun - The Lava Field That Fooled NASA

While often cited as a training ground for NASA, the Eldhraun lava field was actually too fragile for astronaut boots. The Apollo crews mostly trained in the barren, rocky highlands near Askja and Mývatn. However, Eldhraun holds a darker title. It was created by the Laki eruption (1783–1784), an event so catastrophic it killed 20% of Iceland's population and released 120 million tons of sulfur dioxide. The resulting "Haze Famine" lowered global temperatures and caused crop failures as far away as Egypt. It proves that when Iceland burps, the world shivers.

Gönguleið um Eldhraun hiking trail through Eldhraun lava field in South Iceland, showing black volcanic rock covered with vibrant green moss (63.7911°N, 18.2154°W)
The trail through Eldhraun lava field looks extraterrestrial for good reason.
Contrary to popular myth, NASA astronauts didn't train here (they used the vegetation-free Askja highlands), but the landscape is still otherworldly.

The field was born from the Laki fissure eruption of 1783-1784, which was arguably the most devastating volcanic event in human history. Forget Pompeii. This one killed 20% of Iceland's population and triggered famines across Europe. Benjamin Franklin, then in Paris, noticed the "dry fog" and correctly deduced it came from Iceland. That made him possibly the first person to link volcanism with climate change.

What's hilarious is that the lava here isn't just black. Certain iron-rich sections oxidize to rust-red colors, creating natural abstract art that would make Jackson Pollock jealous. The moss (mostly Racomitrium lanuginosum, if you're into that sort of thing) grows exactly one millimeter per year. That lush carpet you're walking on? Some of it started growing when George Washington was president.

Close-up view of green moss covering Eldhraun lava field in Iceland showing intricate patterns of Racomitrium lanuginosum that grows 1mm per year (63.7923°N, 18.2178°W)
This moss grows slower than government bureaucracy.
Each green puff represents decades of patient survival on nutrient-less rock at Eldhraun.

Local folklore says hidden people (Icelandic elves) love Eldhraun because the lava tubes make perfect subterranean real estate. There's even a story about road construction being halted when workers refused to disturb a particular moss-covered rock formation said to be an elf church. We didn't see any elves, but we did notice the moss seems to grow in suspiciously geometric patterns in places.

Long row of volcanic craters and moss-covered lava fields at Laki at 63.7945°N, 18.2201°W
Nature's ultimate comeback story: life reclaiming destruction at Eldhraun.
The green isn't just moss - it's 200+ years of botanical persistence.

The Laki eruption that created this field was a global catastrophe. It released roughly 120 million tons of sulfur dioxide, creating a "Haze Famine" that killed livestock across Europe and caused temperature drops in North America. The Mississippi River reportedly froze in New Orleans during the subsequent winter of 1784. It shows how a fissure in Iceland can alter the fate of the world.

The N1 Gas Station and Skaftárskáli Grill: Iceland's Most Informative Pit Stop

Driving through Skaftárhreppur municipality feels like navigating a giant's sandbox after a tantrum. The glacial wash plains stretch to infinity. Just when you're convinced you've entered a monochromatic purgatory, Kirkjubæjarklaustur appears like a mirage. The name means "church farm cloister," which sounds medieval because it is. This settlement dates back to the 12th century when Irish monks apparently thought this was a good place for quiet contemplation.

What they didn't have was the N1 gas station with its adjacent Skaftárskáli Grill. It might be the most important building in southern Iceland. In a country where services are separated by hours of driving, this place is an oasis. The real magic happens inside, where they serve lamb that tastes like the sheep spent their lives doing yoga on herb-covered hillsides.

Exterior view of Skaftárskáli Grill restaurant at Kirkjubæjarklaustur in Skaftárhreppur municipality, Iceland with N1 gas station signage (63.7804°N, 18.0655°W)
The Skaftárskáli Grill at Kirkjubæjarklaustur: where highway hunger meets heavenly lamb.
This place has saved more road trips than AAA.

We had to skip the nearby Kirkjugólf ("Church Floor"), which isn't a floor at all but natural basalt columns that look suspiciously like man-made tiles. Spanning about 80 square meters, these honeycomb-like hexagonal stones were formed when lava cooled and contracted, cracking into perfect geometric pillars. They were smoothed down by centuries of glacial erosion and sea tides when the ocean level was higher. It creates the illusion of a paved floor where no church ever actually stood.

KirkjubaejarklausturFloor
Kirkjugólf
Photo: Andreas Tille, CC BY-SA 4.0

Local legend says Kirkjugólf is the remnant of a church buried by lava. Geologists say it's just columnar jointing doing its best impression of interior design. The columns are so perfectly hexagonal that early settlers were convinced supernatural forces were involved.

Landscape view of Kirkjubæjarklaustur village in Skaftárhreppur, Iceland showing traditional houses against dramatic mountain backdrop (63.7812°N, 18.0678°W)
Kirkjubæjarklaustur: population 120, scenery value: priceless.
Those mountains have seen more weather than a meteorologist's nightmare.

Kirkjubæjarklaustur's history has a grim chapter regarding the "Systrastapi" (Sisters' Rock), a rocky hill west of the village. According to local folklore (though historical records are silent on the actual execution), two nuns from the local convent were burned at the stake here in the 14th century for violating their vows. One for selling her soul to the devil and the other for speaking blasphemy against the Pope. It is said that after the Reformation, good flowers grew on the grave of the second nun, but nothing ever grew on the grave of the nun who dealt with the devil.

Interior of Skaftárskáli Grill restaurant at Kirkjubæjarklaustur showing traditional Icelandic dishes including grilled lamb and seafood (63.7806°N, 18.0658°W)
Icelandic comfort food at its finest: lamb that probably had a name.
The seafood here at Skaftárskáli Grill is so fresh it might still be considering escape options.

The village is most famous for the "Eldmessan" (Fire Sermon) of July 20, 1783. As the Laki lava flow threatened to destroy the church and the town, the local pastor Jón Steingrímsson gathered the terrified congregation inside the church. He delivered a sermon of such intensity that it is credited with stopping the lava flow just meters from the building. Geologists now know the lava stopped because it hit a specific topographical cooling point. But to the locals, it was divine intervention.

Extremely detailed road information sign at Kirkjubæjarklaustur in Iceland showing directions to multiple glaciers, waterfalls, canyons and tourist attractions (63.7809°N, 18.0661°W)
This road sign at Kirkjubæjarklaustur contains more information than some travel guides.
If you read the fine print, it probably includes tomorrow's weather and a philosophical quote.

Haoldukvisl Glacier: The Shy Cousin of Vatnajökull

Most glaciers scream for attention. Haoldukvisl whispers. This unassuming tongue of Vatnajökull doesn't have a fancy visitor center or Instagram-famous ice caves. What it does have is raw, unfiltered glacial presence without the crowds. The name roughly translates to "Hay River Glacier," which is either charmingly pastoral or someone really lacked imagination.

Aerial view of Haoldukvisl, Skaftafell and Svínafellsjökull Glaciers in Vatnajökull National Park, Iceland showing multiple glacial tongues flowing from ice cap (64.0155°N, 16.9655°W)
Haoldukvisl Glacier doing its best impression of a frozen river.
The black streaks aren't dirt - they're volcanic ash layers from eruptions past.

Geologically speaking, Haoldukvisl is interesting because it flows over the summit of Öræfajökull, Iceland's tallest volcano and only active stratovolcano. Yes, there's an active volcano under this glacier. The last eruption was in 1727, but it's considered overdue. The ice here is literally sitting on a ticking geological time bomb.

Detailed close-up view of Haoldukvisl Glacier surface in Iceland showing deep crevasses, pressure ridges and layers of volcanic ash trapped in ice (64.0172°N, 16.9688°W)
Each crevasse tells a story of ice under stress on Haoldukvisl.
The darker layers are volcanic ash deposits - nature's own geological calendar.

What few visitors realize is that Haoldukvisl's meltwater eventually feeds into the Jökulsá á Dal river, which has the distinction of being one of Iceland's best salmon fishing rivers. The glacial flour (rock particles ground to fine powder) gives the water its milky turquoise color and, apparently, makes salmon exceptionally happy.

Wide panoramic view showing Haoldukvisl, Skaftafell and Svínafellsjökull Glaciers flowing from Vatnajökull ice cap in Iceland with black sand plains in foreground (64.0198°N, 16.9723°W)
Three glaciers in one frame: Haoldukvisl, Skaftafell and Svínafellsjökull.
It's like a glacial family portrait, but with more crevasses and less smiling.

Standing before Haoldukvisl, you get a sense of geological time that's humbling. The ice at the terminus might have fallen as snow when Vikings first settled Iceland. It's been compacting and flowing downhill ever since, only to melt in moments before your eyes. Poetic, until you realize your feet are getting wet.

Skaftafell and Svínafellsjökull: Iceland's Glacial Sibling Rivalry

These two glaciers are like brothers with very different personalities. Skaftafell is the older, more reserved sibling. Vast, majestic and somewhat aloof. The Athabasca of Iceland. Svínafellsjökull is the adventurous younger brother. Dramatic, accessible and full of personality. The Stutfield of Iceland. Both flow from Vatnajökull, Europe's largest ice cap, but they couldn't be more different in character.

Meeting point of Skaftafell and Svínafellsjökull Glaciers in Vatnajökull National Park, Iceland showing distinct ice formations and colors (64.0234°N, 16.9765°W)
Skaftafell (left) and Svínafellsjökull (right) sharing an ice field.
They're like glacial conjoined twins with different fashion senses.

The relationship between these glaciers and the local farmers has historically been terrifying. During the "Little Ice Age" (roughly 1450–1850), the outlet glaciers of Vatnajökull advanced so aggressively that they consumed valuable farmland. Historical tax records from the 18th century confirm that the King of Denmark had to lower taxes for the Skaftafell farms because the glacier had physically eaten their grazing fields.

Detailed view of Skaftafell Glacier ice formations showing deep blue ice, crevasses and meltwater channels in Vatnajökull National Park, Iceland (64.0251°N, 16.9792°W)
Skaftafell's blue ice: nature's stained glass window.
The deeper the blue, the older and more compressed the ice.

Other than a shooting location for numerous films (27 and counting!), the neighboring Svínafellsjökull has a dark history found in Njál's Saga. The glacier is named after the farm Svínafell, which was the home of Flosi Þórðarson, the chieftain who burned Njáll Þorgeirsson and his family to death in the saga's climax. The "Pig Mountain" name likely refers to the settlement era when pigs were grazed here before the climate cooled and the glaciers advanced.

Svínafellsjökull Glacier ice cave and formations showing surreal blue hues and intricate ice structures in Iceland (64.0268°N, 16.9821°W)
Svínafellsjökull's blue ice caves: nature's avant-garde art installation.
These colors occur when ice absorbs all light spectrum except blue.

Locals often refer to Svínafellsjökull as the "Hollywood Glacier" because its jagged crevasses are so accessible they have become the go-to stand-in for alien planets. This is the exact ice where Matthew McConaughey walked on "Dr. Mann's planet" in Interstellar and where Christian Bale fought Liam Neeson in Batman Begins. The ice here is so distinctively blue and compressed that production crews rarely need to use CGI to enhance the color.

Alternate angle view of Skaftafell and Svínafellsjökull Glaciers showing immense scale against mountain backdrop in Iceland (64.0285°N, 16.9853°W)
The scale is deceptive - what looks like small ridges are house-sized ice formations on Skaftafell and Svínafellsjökull.
Everything is bigger in glacial terms, including the potential for embarrassment if you fall in.

If you look closely at the surface of Svínafellsjökull from above, you might see curved, alternating bands of light and dark ice known as "ogives" or "Forbes bands." These form at the base of the icefall where the glacier flows over a steep drop. Like tree rings, each pair of light and dark bands represents one year of movement. The dark ice forms in summer when dust and debris collect in the melt and the light ice forms in winter.

Composite panoramic stitch of Skaftafell and Svínafellsjökull Glaciers showing full extent of glacial tongues in Vatnajökull National Park, Iceland (64.0302°N, 16.9886°W)
A panoramic view of Skaftafell and Svínafellsjökull that still doesn't capture the full scale.
These glaciers are so large they have their own weather systems.

Both glaciers have retreated significantly in recent decades. Skaftafell has pulled back over a kilometer since 1930, while Svínafellsjökull has retreated even faster. Old photographs show ice where there's now vegetation. Standing at the terminus, you're literally watching climate change in real time. It's a sobering experience that no amount of glacial beauty can fully offset.

Final view of Skaftafell and Svínafellsjökull Glaciers with meltwater river flowing from terminus in Iceland (64.0319°N, 16.9918°W)
The Skaftafell and Svínafellsjökull glaciers' gift to the lowlands: pure meltwater rivers.
This water is older than your grandparents and probably tastes better too.

Fjallsjökull: The Glacier That Prefers Privacy

While Jökulsárlón gets all the press, its neighbor Fjallsjökull maintains a dignified distance from the tourist circus. This outlet glacier terminates in Heinabergslón lagoon, a proglacial lake formed by the retreat of Heinabergsjökull, an arm of the larger Vatnajökull ice cap. Unlike Jökulsárlón, Heinabergslón remains less developed for tourism, offering a quieter view of active glacier retreat. The name means "Mountain Glacier," which is accurate if somewhat unimaginative.

Fjallsjökull Glacier terminus meeting Fjallsárlón lagoon in Iceland with icebergs floating in calm waters against mountain backdrop (64.0150°N, 16.3835°W)
Fjallsjökull: the introverted cousin of Jökulsárlón.
Same family of ice, different personality entirely.

What makes Fjallsjökull special is its geology. The glacier flows over the Bárðarbunga volcanic system, one of Iceland's most powerful and active volcanoes. The 2014-2015 Holuhraun eruption occurred in this system, producing the largest lava field since the 1783 Laki eruption. That lava field is visible from certain angles near Fjallsjökull.

Panoramic view of Fjallsjökull Glacier from Iceland's Ring Road showing full extent of glacial tongue flowing into lagoon (64.0167°N, 16.3862°W)
Fjallsjökull from a distance: ice meeting water meeting sky.
The scale only becomes apparent when you notice the dots for kayaks.

The lagoon at Fjallsjökull's base has an interesting characteristic. Its water level fluctuates dramatically based on subglacial water pressure. During summer melt or after volcanic activity, the lagoon can rise several meters overnight. Local kayak guides have stories of arriving to find their usual launch spots underwater - or high and dry.

Detailed view of Fjallsjökull Glacier ice formations and Fjallsárlón lagoon with floating icebergs in Iceland (64.0184°N, 16.3895°W)
Icebergs in Fjallsárlón lagoon: nature's ice sculpture garden.
Each one is a unique masterpiece that will never be duplicated.

Fjallsjökull is technically an outlet of the larger Breiðamerkurjökull, which is known for its "surging" behavior. During the 19th century, this glacier advanced so far that it almost reached the ocean, cutting off the coastal route entirely. Travelers were forced to trek dangerously across the high ice cap to pass. The strip of sand we now drive on (Route 1) was completely buried under glacial ice as recently as 100 years ago.

Close-up view of icebergs floating in Fjallsárlón glacial lagoon at base of Fjallsjökull Glacier in Iceland (64.0201°N, 16.3928°W)
Fjallsárlón's icebergs: fewer tourists, more tranquility.
This is where glaciers go to retire from the Instagram spotlight.

When standing at the edge of the lagoon, you are standing on land that didn't exist a century ago. Detailed maps from 1904 show that the glacier edge extended all the way to the prominent moraine ridges (hills of gravel) that you now park your car behind. The entire lagoon has formed in the brief geological blink of an eye since the glacier began its rapid retreat in the 1930s.

Fjallsjökull glacial lake with calm waters reflecting mountains and sky in Vatnajökull National Park, Iceland (64.0218°N, 16.3961°W)
Perfect reflections in Fjallsárlón: when nature becomes symmetrical.
The water is so still it feels like you're looking at a painting.

During winter, Fjallsjökull becomes a different world entirely. The lagoon freezes over, trapping icebergs in place like insects in amber. The ice takes on surreal shapes as wind sculpts the surface, creating formations that look more like modern art than natural phenomena. Local photographers prize winter shots here precisely because so few bother to visit.

Jökulsárlón: Where Icebergs Go to Socialize

If glaciers had social lives, Jökulsárlón would be the nightclub. This is Iceland's most famous glacial lagoon and for good reason. It's where icebergs from Breiðamerkurjökull come to hang out before heading to the Atlantic. The lagoon is essentially a glacial retirement home where ice gets to live its best life before melting into oblivion.

Panoramic view of Jökulsárlón glacial lagoon in Iceland with numerous icebergs floating in milky blue waters against glacier backdrop (64.0476°N, 16.1789°W)
Jökulsárlón: nature's ice cube tray on a monumental scale.
Each iceberg here is older than your last relationship.

While it looks like a shallow lagoon, Jökulsárlón is actually a geological gouge of immense proportion. As the glacier has retreated, it has carved out the earth so deeply that the lagoon recently became the deepest lake in Iceland, reaching depths of over 248 meters (814 feet). That innocent-looking iceberg floating near the shore could be sitting in water deeper than two Statues of Liberty stacked on top of each other.

High resolution stitched panorama of Jökulsárlón glacial lagoon showing full extent with Breiðamerkurjökull glacier in background, Iceland (64.0493°N, 16.1822°W)
A panoramic view of Jökulsárlón that still doesn't do justice to the scale.
This lagoon is so large it has its own currents and microclimate.

The lagoon formed relatively recently. It didn't exist in 1935. Breiðamerkurjökull glacier has retreated so dramatically that what was once solid ice is now a 248-meter-deep lake. That's deeper than most skyscrapers are tall. If you dropped the Eiffel Tower into Jökulsárlón, only the very tip would poke above water.

Here's something most visitors miss. The icebergs' colors indicate their age and composition. Bright white ice is younger and full of air bubbles. Deep blue ice is older, denser and has fewer bubbles. Black streaks are volcanic ash from ancient eruptions. Some icebergs have all three, creating natural layered cakes of geological history.

Close-up view of iceberg in Jökulsárlón glacial lagoon showing blue ice, white air bubbles and black volcanic ash layers in Iceland (64.0510°N, 16.1855°W)
Jökulsárlón iceberg geology lesson in one photo: white = young, blue = old, black = volcanic.
Nature doesn't need labels when it's this obvious.

Jökulsárlón isn't just a natural wonder. It's a paid actor. The lagoon was frozen over specifically to film the car chase scene in the James Bond movie Die Another Day. The filmmakers dammed the river outlet to prevent saltwater from entering (saltwater doesn't freeze easily), allowing the fresh water to freeze into a thick enough sheet for Aston Martins to drift on. Once filming wrapped, they broke the dam and the lagoon returned to its natural, iceberg-filled state, leaving no trace of 007 except on celluloid.

Seals resting on icebergs in Jökulsárlón glacial lagoon with Breiðamerkurjökull glacier in background, Iceland (64.0527°N, 16.1888°W)
Seals using Jökulsárlón icebergs as floating loungers.
They've figured out the whole "work-life balance" thing better than we have.

The seals you see are likely Harbor Seals (Phoca vitulina), which flock to Jökulsárlón and the Diamond Beach for a very specific strategic reason: safety. While the open Atlantic is patrolled by Orcas (Killer Whales), the lagoon offers a sanctuary. The shallow river outlet acts as a natural barrier. The seals can easily swim through it, but the large Orcas cannot enter the lagoon to hunt them.

Amphibious boat tour among icebergs in Jökulsárlón glacial lagoon with tourists viewing ice formations up close, Iceland (64.0544°N, 16.1921°W)
Boat tours get you close enough to hear the ice crack at Jökulsárlón.
The sound is like giant bubble wrap popping underwater.

The river connecting the lagoon to the ocean, Jökulsá, was a terrifying obstacle for centuries. Before the first single-lane suspension bridge was built in 1967, travelers had to cross the treacherous glacial waters by boat, while their horses were forced to swim. Many drowned. The construction of the bridge was a national milestone, finally completing the Ring Road and permanently connecting the southeastern settlements to the rest of the country.

Jökulsárlón glacial lagoon outlet channel where icebergs float toward Atlantic Ocean through short river, Iceland (64.0561°N, 16.1954°W)
The short river connecting Jökulsárlón to the Atlantic.
Icebergs make their final journey here before becoming ocean water.

The lagoon is teeming with life. Harbor seals are frequently seen swimming among the icebergs or lounging on the ice to escape the killer whales that patrol the open ocean. If you take a Glacier Lagoon boat tour, you'll likely spot them curious about the boats. They flock here to feed on the capelin and herring brought in by the tides. Jökulsárlón is the crown jewel of Vatnajökull National Park, a protected wilderness area that encompasses 14% of Iceland.

Collection of icebergs at Jökulsárlón glacial lagoon showing diverse shapes, sizes and colors including blue, white and black ice formations (64.0578°N, 16.1987°W)
Iceberg diversity on display at Jökulsárlón: no two are alike.
Nature's sculpture garden, admission free, melting fast.

Climate change has accelerated Jökulsárlón's expansion dramatically. Since the 1930s, the lagoon has grown from a small proglacial lake into Iceland’s deepest lake - now over 248 meters (814 feet) deep. Its surface area has expanded several-fold as Breiðamerkurjökull has retreated and in 1967 the lagoon finally breached the coastal barrier and connected permanently to the Atlantic. What’s happening here isn’t just a tourist attraction. It’s one of Europe’s most visible examples of glacier retreat.

Breiðamerkursandur (Diamond Beach): Where Ice Meets Sand Meets Poetry

If Jökulsárlón is the nightclub, Diamond Beach is the afterparty. The beach sits directly across the narrow tidal channel from the lagoon, where outgoing tides sweep freshly calved icebergs into the North Atlantic. Some pieces wash back ashore within hours, reshaped by waves and sand into translucent sculptures that rarely survive more than a few tide cycles.

Panoramic view of Diamond Beach (Breiðamerkursandur) in Iceland showing icebergs washed up on black volcanic sand against ocean backdrop (64.0432°N, 16.1765°W)
Diamond Beach (Breiðamerkursandur): where glaciers go to retire in style.
The black sand makes the ice look like it's glowing.

The black sand comes from volcanic basalt ground to powder by glacial action. Each grain has likely been through multiple cycles of eruption, glaciation, erosion and deposition. Some of these sand particles are older than human civilization. They've seen ice ages come and go.

Clear and blue icebergs resting on black sand at Diamond Beach at 64.0449°N, 16.1798°W
Ice meets sand: the ultimate contrast in textures at Diamond Beach.
Smooth ice against gritty volcanic sand creates a tactile wonderland.

The "diamonds" on Diamond Beach are fleeting masterpieces. These ice chunks are polished by the Atlantic waves, which remove air bubbles and carve the ice into gem-like clarity. The ice in these blocks originally fell as snow on Vatnajökull, Europe’s largest glacier by volume. Some of the compressed ice now calving into Jökulsárlón began as snowfall centuries ago, slowly compacted under immense pressure into dense glacial ice before finally breaking free at the glacier’s terminus.

Iceberg floating from Jökulsárlón toward Diamond Beach through short river channel in Iceland (64.0466°N, 16.1831°W)
Icebergs calved from Breiðamerkurjökull (an outlet glacier of Vatnajökull) drifting from Jökulsárlón onto Diamond Beach.

What visitors rarely consider: the icebergs on Diamond Beach are temporary artworks. A particularly beautiful ice sculpture might form overnight and be gone by afternoon. Photographers have learned to work quickly here. The scene changes with the tides, wind and melting rates. Some icebergs literally disappear while you're watching.

Seals sunbathing on icebergs washed up on Diamond Beach (Breiðamerkursandur) in Iceland with ocean in background (64.0483°N, 16.1864°W)
Seals have discovered the best sunbathing spots at Diamond Beach.
They look more relaxed than most people on vacation.

It is worth noting that "Diamond Beach" is purely a tourism marketing moniker. You won't find it on older Icelandic maps. The correct geographical name is Breiðamerkursandur ("Broad Mark Sands"). Locals never used the gem-related name until tourists started flocking here in the 2010s to photograph the ice, prompting the travel industry to adopt the catchier title.

Multiple seals resting on icebergs at Diamond Beach (Breiðamerkursandur) in Iceland showing colony behavior on ice platforms (64.0500°N, 16.1897°W)
Seal social hour on ice platforms at Diamond Beach.
This is their version of meeting friends for drinks, minus the drinks.

Climate scientists monitor the glacier that feeds Jökulsárlón rather than counting icebergs on the beach itself. Breiðamerkurjökull has been retreating steadily since the end of the Little Ice Age in the late 19th century, exposing new lagoon area year by year. The icebergs that wash ashore at Breiðamerkursandur are fragments calved from this retreating outlet glacier. Their presence reflects ongoing glacier loss, not a predictable seasonal “increase” in beach ice.

Diamond Beach (Breiðamerkursandur) with Atlantic Ocean waves washing around grounded icebergs on black sand in Iceland (64.0517°N, 16.1930°W)
The Atlantic's constant reshaping of Diamond Beach.
Every wave changes the arrangement of ice and sand.

Heinaberg Glacier: The Quiet One at the End of the Road

While everyone crowds around Jökulsárlón, Heinaberg Glacier sits quietly further east, feeling somewhat neglected. This outlet glacier terminates in Heinabergslón lagoon, a proglacial lake formed by the retreat of Heinabergsjökull, an arm of the larger Vatnajökull ice cap. Unlike Jökulsárlón, Heinabergslón remains less developed for tourism, offering a quieter view of active glacier retreat. The name derives from hein (whetstone), referring to the fine-grained basalt in the surrounding cliffs once used to sharpen tools.

View of Heinaberg Glacier from Iceland's Ring Road (Route 1) showing glacial tongue flowing into Heinabergslón lagoon (64.2543°N, 15.2132°W)
Heinaberg Glacier from the road: distant but imposing.
This is what glaciers looked like before Instagram discovered them.

Heinaberg has a unique characteristic. It was once a staging ground for early glaciological expeditions. In the 19th century, the lagoon didn't exist. The glacier extended far further down the valley. The lagoon only began forming in the mid-20th century as the ice retreated, leaving behind "dead ice" buried in the moraines that slowly melts and creates kettle holes.

Heinaberg Glacier terminus meeting Heinabergslón lagoon with floating icebergs and mountain backdrop in Iceland (64.2560°N, 15.2165°W)
Heinabergslón: Jökulsárlón's quieter, more introverted sibling.
Same family DNA, different personality entirely.

The lagoon at Heinaberg's base is particularly rich in wildlife. Arctic terns nest along its shores and their aggressive defense of territory is legendary. Visitors quickly learn to wear hats. Terns dive-bomb anything that comes near their nests. It's like nature's version of "No Trespassing" signs, but with more screaming and pecking.

Panoramic view of Heinaberg Glacier from distance showing full glacial tongue flowing from Vatnajökull ice cap in Iceland (64.2577°N, 15.2198°W)
Heinaberg's final panoramic: ice, water, sky in perfect harmony.
A fitting end to Iceland's glacial parade along the southern coast.

What Heinaberg lacks in fame, it makes up for in raw, undisturbed beauty. This is where you come when you want to experience a glacial lagoon without the soundtrack of tourist chatter. The silence here is profound, broken only by the occasional crack of ice or call of a bird. It's a reminder that not everything in Iceland needs to be shared with hundreds of others.

Þveit: Where Icelandic Serenity Meets Spooky Horse Tales

This historic farmstead and lake sits just a hop, skip and jump from Höfn in Hornafjörður. It boasts scenery so pretty it should be illegal. Snow-capped mountains play peek-a-boo with the Atlantic Ocean's vast expanse. The area's heart beats around shallow Lake Þveit, a magnet for bird nerds and fishing enthusiasts. The name comes from the Old Norse þveit, meaning a "cut" or piece of land separated from a larger estate. It's a term linguistically cognate with the English suffix "thwaite" found in Yorkshire place names.

Lake Þveit, Iceland - Serene glacial lake surrounded by mountains in southeastern Iceland (64.2536°N, 15.2078°W)
Lake Þveit, Iceland, on a calm day - so peaceful you can hear your own thoughts, which is terrifying for some of us.
The water teems with Arctic char that have never heard of personal space, plus brown trout and their fancy cousin, the sea trout.

The lake's fishing reputation isn't just local gossip. Back in the 1930s, British anglers would haul their tweed jackets here specifically for the sea-run brown trout, which grow to ridiculous sizes thanks to a diet of crustaceans that turn their flesh salmon-pink. It's like nature's version of fancy koi fish, but tastier.

Lake Þveit shoreline, Iceland - Rocky shoreline with mountain backdrop in East Iceland (64.2536°N, 15.2078°W)
Another angle of Lake Þveit, Iceland, where the mountains look like they're judging your life choices.
Winter transforms this place into a snowmobiling paradise - Iceland's version of a Disney ride, but with more layers.

Beyond the outdoor activities, Þveit's real charm lies in its folklore. The legend of the horse-shaped creature with backwards hooves isn't just campfire talk. It dates to settlement-era tales of nykur, water spirits that drown victims by offering them rides. Locals swear the creature haunts the lake on dark autumn evenings, which explains why fishing trips end early when the mist rolls in.

Nearby farms offer glimpses into Iceland's agricultural past, where sheep outnumbered people 3-to-1 until recently. You can sample homemade skyr (Icelandic yogurt that puts Greek yogurt to shame) and hear stories about the 1970s when farmers used World War II surplus jeeps to herd sheep. Talk about resourceful.

Höfn: Where Lobster Reigns Supreme and Soup is a Meal

Höfn (pronounced like you're clearing your throat) marks the geographical pivot point of Iceland's Ring Road. For us counter-clockwise circumnavigators, it's where the south coast's drama gives way to the east coast's rugged charm - the eastfjords. This fishing town doesn't just hug the coast. It practically marries it, with snow-capped mountains as wedding guests.

Höfn harbor, Iceland - Fishing port with boats and mountain backdrop in southeast Iceland (64.2539°N, 15.2083°W)
Höfn's working harbor, Iceland - where fishing boats coexist with tourist cameras in uneasy harmony.
The town processes 40% of Iceland's langoustine catch, which explains why every restaurant smells like butter and ocean.

Höfn's "lobster capital" title isn't just marketing. The local hummer (langoustine) fishery dates to the 1950s when Norwegian fishermen introduced the techniques. Today, the town's boats haul in about 2,000 tons annually, mostly exported to France where they pretend it's theirs. The secret? The cold, nutrient-rich waters make these crustaceans grow slower, developing more intense flavor. Science says so.

Fiskisúpa: Iceland's Hug in a Bowl

We lunched at Pakkhús Restaurant, a converted warehouse that somehow makes fish smell chic. The menu offered many choices, but only one called to us: Iceland's iconic fiskisúpa. This isn't soup. It's a culinary conspiracy to redefine what soup can be.

Fiskisúpa - Icelandic fish soup at Pakkhús Restaurant, Höfn, Iceland (64.2539°N, 15.2083°W)
Icelandic fish soup that laughs in the face of portion control.
Contains enough fish to qualify as an aquarium, plus vegetables for plausible deniability about health.

Chatting with the chef revealed the soup's backstory. During Iceland's Þorri midwinter festival, families would make "cleanout soup" using whatever fish remained in storage. The addition of sherry came from 19th-century Danish traders who used it as currency. Today's version uses cod caught within sight of the restaurant. It's the ultimate locavore flex.

The soup's cream base often includes rjómi (Icelandic cream) with 38% fat content because when you live where winter lasts eight months, calories are survival. The dill isn't just garnish. It grows wild in Icelandic meadows and contains more vitamin C than oranges. Vikings used it to prevent scurvy, though they probably didn't call it that.

The North Sea Viewpoint at Múlaþing: Where Wind Gets Philosophical

Driving Iceland's rugged eastern coastline requires frequent stops. Not for restrooms, but because the views literally demand it. The dramatic cliffs at Stapavík are one such spot where the Atlantic seems to whisper, "Look at me, I'm fabulous."

Múlaþing North Sea panorama, Iceland - Panoramic view of North Atlantic coastline in East Iceland (64.9123°N, 13.8765°W)
Múlaþing's panoramic drama, Iceland - where the horizon line gets confused about its job.
This stitched panorama captures approximately 140 degrees of coastline real estate.

Múlaþing, formed by merging four municipalities in 2020, became Iceland's largest municipality by area. It's like the Amazon of Icelandic regions, minus the two-day shipping. The coastline features fjords with names like Seyðisfjörður (say that five times fast). Although early Norse pioneers claimed the fjord back in the 9th century, the town's real claim to fame hit in the mid-1800s. That’s when Norwegian sailors showed up, established a booming commercial port and realized the local herring were basically jumping directly into their boats.

Múlaþing coastal cliffs, Iceland - Dramatic cliffs meeting North Atlantic waves in East Iceland (64.9123°N, 13.8765°W)
Cliffs so dramatic they should have their own soundtrack.
The basalt columns formed during the Miocene epoch when Iceland was still figuring out its landscape.

Seyðisfjörður's colorful houses aren't just for Instagram. The tradition dates to the 19th century when fishermen used mineral-based paints from Germany. Ochre from yellow, copper from green and iron oxide from red. The bright colors helped boats identify home port through fog thicker than Icelandic wool.

Múlaþing coastline view, Iceland - Coastal vista with distant fjords in East Iceland (64.9123°N, 13.8765°W)
The view that convinced us to postpone lunch for another hour.
Each fjord in the distance has its own microclimate - nature's way of showing off.

From our vantage point, we witnessed waves performing their eternal battle with basalt. The raw power here isn't just poetic. It's measurable. Winter storms generate waves over 20 meters high, which explains why coastal roads occasionally go on unplanned vacations.

Múlaþing sea stacks, Iceland - Sea stacks and rock formations in North Atlantic (64.9123°N, 13.8765°W)
Sea stacks that have weathered more storms than a Icelandic fisherman's sweater.
These basalt formations erode at about 1 centimeter per century - glacial pace, literally.

The wind here doesn't blow. It debates. At 15 meters per second average, it sculpts everything from dwarf birch trees to tourist hairstyles. Early settlers called this area Fjallabyggð (mountain settlement) but quickly learned to build homes half-buried for protection. Smart people.

Múlaþing wave action, Iceland - Waves crashing against Icelandic coastline (64.9123°N, 13.8765°W)
The Atlantic demonstrating its disapproval of coastline.
This wide-angle shot captures about 200 meters of shoreline drama.

Berufjörður and Iceland's Austfirðir: Where Fjords Have Identity Crises

Berufjörður (not to be confused with its two Borgarfjörður doppelgangers) sits in Iceland's Eastfjords region like that quiet middle child who turns out most interesting. Located between Djúpivogur and Eskifjörður, this fjord's name derives from the saga-age settler Bera, though folklore claims it is named after a cow that dragged a rock slab from the sea.

Berufjörður fjord, Iceland - Steep mountains rising from fjord waters in East Iceland (64.6531°N, 14.2794°W)
Berufjörður, Iceland, showing off its vertical real estate.
The mountains rise 800 meters straight from sea level - nature's skyscrapers.

The Berufjörður-Djúpivogur area hosts the Langabúð museum, housed in Iceland's oldest commercial building (built 1790). It displays fishing gear so ancient it makes your grandfather's tackle box look space-age. The museum's prize exhibit? A 19th-century shark liver oil press that produced oil so pungent it was used both as lamp fuel and as punishment for misbehaving children.

Berufjörður mountains, Iceland - Mountain peaks surrounding Icelandic fjord (64.6531°N, 14.2794°W)
Búlandstindur mountain, Iceland, playing hide-and-seek with clouds.
The pyramid-shaped peak is 1,069 meters tall and notoriously difficult to climb.

Djúpivogur's most famous resident isn't human. It's Búlandstindur mountain, a pyramid-shaped peak that looks like Iceland's attempt at geometry. Local legend claims the mountain contains a hidden church where elves worship, which explains why construction projects nearby often encounter "delays."

Fog is Berufjörður's favorite accessory. The fjord experiences 150 foggy days annually because the East Greenland Current collides with the warmer Irminger Current right here. The resulting fog bank can linger for weeks, giving the area a permanent mystery novel atmosphere.

Berufjörður fog, Iceland - Misty conditions over East Iceland fjord (64.6531°N, 14.2794°W)
Berufjörður fog, Iceland, doing its best impression of solid ground.
Visibility drops to 50 meters on days like this, which explains why Vikings stayed home.

The Berufjörður area is geologically world-famous for zeolites - crystal minerals that form in the cavities of basalt rock. The nearby farm, Teigarhorn, is a protected natural monument because its zeolite yield is among the finest on Earth. In the 19th century, these crystals were so abundant they were simply used as road gravel until mineralogists realized locals were essentially paving their driveways with museum-grade gemstones.

Berufjörður coastal landscape, Iceland - Rocky coastline with vegetation in Eastfjords (64.6531°N, 14.2794°W)
Berufjörður coastal terrain, Iceland, where sheep outnumber people 20-to-1.
The green vegetation is mostly moss and hardy grasses that survive salt spray.

Djúpivogur village houses the famous Eggin í Gleðivík (Eggs of Merry Bay) - 34 granite eggs representing local bird species. Artist Sigurður Guðmundsson installed them in 2009, but locals still debate whether they're art or really confused birds' nests. Each egg weighs between 1 and 2 tons, because subtlety is overrated.

Berufjörður tranquility, Iceland - Peaceful fjord waters reflecting mountains (64.6531°N, 14.2794°W)
Berufjörður, Iceland, on its best behavior - calm waters and zero drama.
The fjord reaches depths of 75 meters, hiding shipwrecks from the 19th century.

Before the Eggs of Merry Bay, there were the Stones of Sorrow. In the 18th century, a local farmer placed 34 regular stones along the shore to count the days until his fishing boat returned. The boat sank, the stones remained and now we have granite eggs. Progress, we guess.

Eggin í Gleðivík sculpture, Djúpivogur, Iceland - 34 stone eggs on coastline art installation (64.6578°N, 14.2856°W)
Eggin í Gleðivík (The Eggs of Merry Bay), Djúpivogur, Iceland
Either profound art or nature's weirdest Easter.
Icelandic artist Sigurður Guðmundsson installed these 34 massive granite eggs in 2009.
They perfectly replicate the exact shape and colors of eggs from 34 different bird species that nest locally in the Eastfjords region
Photo credit: Ira Goldstein

Driving Berufjörður's northern side, we discovered Havari Cafe, a coffee shop with views so stunning they should charge admission. The name means "wreck" in Icelandic, referencing a 19th-century shipwreck whose timbers were used to build the original structure. Nothing says cozy like drinking coffee surrounded by maritime tragedy.

Havari Cafe, Berufjörður, Iceland - Cozy cafe with fjord views in East Iceland (64.6601°N, 14.2902°W)
Havari Cafe, Berufjörður, Iceland - where the coffee is hot and the views are illegally beautiful.
The building incorporates timber from a 19th-century Norwegian schooner wreck.

We sipped excellent kaffi (Icelandic for coffee strong enough to restart a heart) while absorbing the view. The cafe's owner told us the area's population peaks at 12 in summer and drops to 3 in winter. That's not a village. That's a stubborn family reunion.

Berufjörður from Havari Cafe, Iceland - Fjord view from cafe terrace in Eastfjords (64.6601°N, 14.2902°W)
The view from Havari Cafe, Berufjörður, that makes you reconsider your career choices.
The fjord's water stays around 4°C year-round - refreshing for polar bears.

The Berufjörður area is historic for the Gautavík trading post, which operated from the 10th to the 15th century. Archaeologists have excavated thousands of objects there, including German pottery and combs, proving international trade thrived here 500 years before Columbus sailed.

Berufjörður misty conditions, Iceland - Low fog over East Iceland fjord landscape (64.6531°N, 14.2794°W)
Berufjörður fog, Iceland, so thick you could carve it with a spoon.
These conditions reduce traffic to one car per hour - Iceland's version of rush hour.

Iceland's Austfirðir (Eastfjords) region contains more coastline than the entire country of Belgium, which seems excessive but who's counting? The fjords were carved by glaciers during the last ice age, then flooded when sea levels rose 10,000 years ago. Basically, nature's version of "Oops, my bad."

Egilsstaðir: East Iceland's Beating Heart (Population: 2,500 and One Monster)

Egilsstaðir reigns as East Iceland's hub with the confidence of a town that knows it's the only game for 200 kilometers. Located on Lagarfljót river's shores, this settlement of 2,500 feels bigger because everyone has three jobs. The town's name means "Egill's farmstead," named after a 15th-century farmer who probably never imagined his homestead would one day host a Subway.

Subway restaurant, Egilsstaðir, Iceland - American fast food chain in East Iceland town (65.2653°N, 14.3948°W)
Subway in Egilsstaðir, Iceland - where "eat fresh" meets "it's freezing outside."
The most American thing for 300 kilometers in any direction.

We grabbed dinner at Egilsstaðir's Subway, because sometimes you need a break from fermented shark (hákarl). The fermentation isn't just for flavor. It's a chemical necessity. Greenland shark meat contains high levels of urea and trimethylamine oxide, which acts as a natural antifreeze but is toxic to humans. The fermentation process breaks these toxins down, making the meat edible, if not exactly palatable. The sandwich artist was a philosophy student from Reykjavik working his summer job. Proof that existential crises and footlongs aren't mutually exclusive.

Egilsstaðir's real claim to fame is Hallormsstaðaskógur, Iceland's largest forest. "Forest" here means "trees that reach your shoulder," but after centuries of Viking deforestation, it's impressive. The woods contain 85 tree species, including Siberian larch planted in 1949 that now stand 20 meters tall. Iceland's version of skyscrapers.

Then there's the Lagarfljót monster, Iceland's answer to the Loch Ness monster. First sighted in 1345, the creature allegedly resembles a giant worm with humps. In 2012, a local farmer filmed a serpentine shape in the ice-covered river. A dedicated 13-member "Truth Commission" established by the local council officially ruled in 2014 (by a 7-6 vote) that the video was authentic footage of the worm, entitling the cameraman to a 500,000 ISK prize. The monster even has its own Wikipedia page, which is now backed by a municipal decree.

Mjóanes Accommodation: Where Toilets Become Art

Our night halt west of Egilsstaðir was Mjóanes Accommodation, a B&B that proves Icelanders have a unique relationship with plumbing. The largest cottage promised "rustic charm," which in Icelandic means "the WiFi works sometimes."

Mjóanes Accommodation cottage, Egilsstaðir, Iceland - Rustic cottage with mountain views in East Iceland (65.2801°N, 14.4102°W)
Our cottage at Mjóanes, Iceland - where "rustic" means "the door doesn't squeak much."
The structure dates to the 1960s but has been updated with electricity and everything.

Staying in East Iceland offers a unique wildlife opportunity found nowhere else in the country: wild reindeer. Originally imported from Norway in the late 18th century for farming, the experiment failed miserably when the Icelanders realized they had no interest in herding them. The animals were released into the wild and today a population of roughly 6,000-7,000 roams the East Fjords. If you see a "sheep" with antlers near your cottage, it's not a mutant. It's a descendant of that failed agricultural experiment.

Mjóanes cottage interior, Egilsstaðir, Iceland - Cozy interior of Icelandic rural cottage (65.2801°N, 14.4102°W)
Mjóanes Accommodation - where wood paneling makes a bold comeback.
The main farm house fireplace burned birch logs, Iceland's primary tree species that isn't imported.

Mjóanes' most striking feature wasn't the views (though spectacular) but a discarded toilet repurposed as garden art. This represents peak Icelandic pragmatism. When your toilet breaks, plant flowers in it. The owner told us it was a 1970s model too historic to trash but too ugly for indoors. Compromise!

Mjóanes Accommodation grounds, Egilsstaðir, Iceland - Rural guesthouse with mountain backdrop (65.2801°N, 14.4102°W)
Mjóanes Accommodation grounds, Iceland - where simplicity meets stunning scenery.
The property spans 20 hectares, which is about 40 American football fields for reference.

The property has been in the same family since the 10th century and the family crest features a Viking who allegedly killed a troll with a piece of dried fish. The current owner tried to register the crest officially but was denied because "fish-based troll combat" isn't recognized as heraldic. The rejection letter is framed in the bathroom.

Mjóanes Accommodation view, Egilsstaðir, Iceland - Panoramic view from guesthouse in East Iceland (65.2801°N, 14.4102°W)
The view from Mjóanes, Iceland, that made us forget about the toilet garden decoration.
Distant mountains still had snow in July - Iceland's version of air conditioning.

That stunning view almost caused an international incident in 1973 when a German cartographer tried to claim the land was actually in Norway. He spent three weeks taking measurements before a local farmer pointed out he was using a tourist map from 1952. The cartographer left in shame, but not before buying two sweaters.

Toilet garden decoration, Mjóanes Accommodation, Iceland - Repurposed toilet as flower planter (65.2801°N, 14.4102°W)
The toilet that found its true calling as art at Mjóanes, Iceland.
Petunias seem to thrive in porcelain - botany's unexplored frontier.

The toilet isn't the only repurposed fixture. The owner also uses an old bathtub as a potato planter, claiming the porcelain keeps slugs away. We're not sure if that's true, but the potatoes are delicious and slightly haunted by the ghosts of past baths.

Toilet garden art closeup, Mjóanes Accommodation, Iceland - Creative recycling in Icelandic countryside (65.2801°N, 14.4102°W)
Closeup of floral toilet at Mjóanes, Iceland - proof that everything can be repurposed with enough creativity.
The 1970s-era toilet still had its original manufacturer's stamp underneath.

Mjóanes offers the quintessential Icelandic countryside experience. Tranquility so profound you can hear sheep contemplating their life choices. The guesthouse sits on land farmed since the 10th century, though today's sheep seem less interested in Viking heritage than in finding the greenest patch of grass.

Mjóanes rural landscape, Egilsstaðir, Iceland - Pastoral scenery with mountains in East Iceland (65.2801°N, 14.4102°W)
Mjóanes Accommodation Main Farm Building, Iceland
Outside: Sheep-dotted landscape that hasn't changed much in 1,000 years.
Icelandic sheep roam freely from May to September, becoming temporary landscape features.

The sheep here produce such soft wool that in the 1930s, a French fashion house tried to buy the entire flock. The farmers refused because the sheep were also expert lawnmowers. The French sent angry telegrams, but the sheep just kept chewing, unaware of their haute couture potential.

Mjóanes Accommodation surroundings, Egilsstaðir, Iceland - Countryside views from Icelandic guesthouse (65.2801°N, 14.4102°W)
Mjóanes Accommodation game room in main farm building, Iceland
More views outside that make you want to quit your job and raise sheep.
The distant river is part of the Lagarfljót system, home to Iceland's less famous monster.

The game room features a 1950s Icelandic version of Monopoly where the most expensive property is the geothermal power plant. It's surprisingly cutthroat and the thimble piece is actually a tiny sheep. The game was banned in 1978 for causing family arguments but was brought back by popular demand.

Mjóanes Accommodation facilities, Egilsstaðir, Iceland - Guesthouse buildings in rural setting (65.2801°N, 14.4102°W)
The main building at Mjóanes, Iceland - with its own character and creaky floorboards.

The red roofs in East Iceland are painted with iron oxide from a mine that closed in 1974. The mine was so remote the workers lived there year-round and developed their own dialect. The last speaker died in 2001, but you can still see the mine's rusty tracks disappearing into the hills like a geological mystery.

Mjóanes Accommodation final view, Egilsstaðir, Iceland - Last look at Icelandic countryside guesthouse (65.2801°N, 14.4102°W)
Old farm buildings, Mjóanes, Iceland.
Red roofs are traditional in East Iceland, painted with iron oxide-based paint.
One last view before continuing our journey west.
The clouds are moving at approximately 40 km/h - standard Icelandic breeze.

Note: We're not affiliated with Mjóanes Accommodation. This isn't a paid promotion, though we'd accept payment in hot coffee and more toilet art.

Iceland's Highland Deserts, Dark Lava Fields & Grímstunga Guesthouse

Leaving Egilsstaðir marked our turn westward along Iceland's northern coastline. The landscape shifted from fjords to highland deserts with the subtlety of a sledgehammer. Suddenly, we were in Hálendið (the highlands), where vegetation takes one look at the conditions and says, "I'm out."

Möðrudalsöræfi highland desert, Iceland - Volcanic desert landscape in Icelandic interior (65.5123°N, 15.8765°W)
Möðrudalsöræfi's highland desert, Iceland - where Mars volunteers for landscaping duty.
The dark lava fields absorb so much heat the ground feels warm even at 10°C air temperature.
The prominent mountain rising behind the Möðrudalsöræfi plateau is Mount Herðubreið.

Möðrudalsöræfi (try saying that after coffee) is a vast highland plateau covered in lava flows primarily from the shield volcanoes of the Askja and Kverkfjöll systems, not the southern Laki fires. The horizon is dominated by the "Queen of Icelandic Mountains," Herðubreið, a tuya (table mountain) formed by a sub-glacial eruption during the last Ice Age.

We took a coffee break 150 kilometers west at Grímstunga Guesthouse, located at the highlands' eastern edge like a sentry guarding civilization. The guesthouse dates to the 1940s when it served as a coaching inn for farmers traveling to seasonal markets. Today, it serves coffee strong enough to make your eyebrows vibrate.

Grímstunga Guesthouse, Iceland - Remote guesthouse in Icelandic highlands (65.6123°N, 16.4765°W)
Grímstunga Guesthouse, Iceland - where the nearest neighbor is 20 kilometers away.
The building's turf roof provides natural insulation, a Viking-era technology still in use.

Grímstunga sits along the ancient Möðrudalsleið route, historically one of the most dangerous crossings in Iceland due to sudden blizzards. In the 19th century, the farm was a critical emergency shelter. Local folklore tells of the "Mountain Postman" who survived this route in winter by burying himself in the snow with his horse for warmth.

Grímstunga Guesthouse interior, Iceland - Cozy common area in highland accommodation (65.6123°N, 16.4765°W)
Inside Grímstunga Guesthouse, Iceland - where every piece of furniture has a story and probably a name.
The guestbook contained entries in 14 languages, including one in Elvish.

Grímstunga sits 40 kilometers southeast of Dettifoss, which in Icelandic distance terms means "around the corner." The guesthouse generates its own electricity via micro-hydro from a nearby stream, because when you're this remote, you become your own utility company.

Note: We're not affiliated with Grímstunga Guesthouse either. Though we'd consider affiliation in exchange for their coffee recipe.

The Magnificent Dettifoss: Where Water Gets Angry

Iceland saves its most dramatic waterfall for the northeast. Dettifoss isn't just a waterfall. It's Europe's most powerful waterfall having a perpetual tantrum. The water here doesn't fall. It declares war on the canyon below.

Dettifoss waterfall east view, Iceland - Europe's most powerful waterfall in Vatnajökull National Park (65.8143°N, 16.3855°W)
Dettifoss from the east bank, Iceland - where 193 cubic meters of water per second demonstrate gravity.
The waterfall's mist creates constant rainbows when the sun cooperates.

Located in Vatnajökull National Park, Dettifoss is accessible via Route 864 (Hólsfjallavegur) to the east side or Route 862 to the west. We took the east approach because it matched our counter-clockwise journey and because the gravel road looked more exciting for our Ford Fiesta, which has been remarkably capable so far.


Watch: Hólsfjallavegur gravel road and Dettifoss east view

The waterfall's statistics read like nature's resume: 44 meters (144 feet) drop, 100 meters (328 feet) width, average flow of 193 cubic meters per second. During spring melt, it reaches 500 cubic meters per second. Enough water to fill an Olympic swimming pool every five seconds. The milky-gray color comes from glacial flour, rock ground so fine it remains suspended. It's basically liquid geology.

Route 864 to Dettifoss, Iceland - Gravel road leading to Europe's most powerful waterfall (65.8143°N, 16.3855°W)
Iceland Route 864 - where gravel roads lead to geological wonders.
The road surface changes color with rainfall, from gray to reddish-brown.

Dettifoss formed during the last ice age when glacial outburst floods carved the Jökulsárgljúfur canyon. The waterfall continues to retreat upstream at about 1 meter per century. That means in 100,000 years it might be in Akureyri. Plan your visit accordingly.

Dettifoss waterfall power, Iceland - Close view of powerful waterfall cascade (65.8143°N, 16.3855°W)
Dettifoss, Iceland, showing off its horsepower - approximately 2.5 million theoretical horsepower.
The roar measures 90 decibels at the viewpoint, equivalent to a motorcycle at full throttle.

The east bank viewing platform puts you close enough to feel the vibration in your teeth. The mist creates permanent rainbows when sunlight hits at the right angle, which happens approximately three minutes per day in Iceland. We caught it, feeling briefly blessed by Norse weather gods.

Dettifoss canyon view, Iceland - Waterfall within Jökulsárgljúfur canyon (65.8143°N, 16.3855°W)
Dettifoss within its canyon context, Iceland - water versus basalt, the eternal struggle.
The canyon walls reveal volcanic layers dating back 2 million years.

Hiking trails connect Dettifoss to nearby waterfalls Selfoss (upstream) and Hafragilsfoss (downstream). The entire canyon trail covers 34 kilometers, but we opted for the sensible option: standing in one spot saying "wow" repeatedly.

Dettifoss geological features, Iceland - Basalt formations around powerful waterfall (65.8143°N, 16.3855°W)
Columnar basalt formations around Dettifoss, Iceland - nature's version of organ pipes.
These hexagonal columns form when lava cools slowly and contracts.

The waterfall's raw, primordial power made it the perfect stand-in for a prehistoric Earth in the opening scene of Ridley Scott's 2012 sci-fi epic Prometheus. The film crew had to transport equipment by helicopter to capture the sheer scale of the 193 cubic meters of water that thunder over the edge every second.

Dettifoss final perspective, Iceland - Last look at Europe's most powerful waterfall (65.8143°N, 16.3855°W)
Final view of Jökulsárgljúfur canyon (or Jökulsá River Canyon) at Dettifoss, Iceland. The canyon also houses Selfoss and Hafragilsfoss.
Dettifoss waterfall has appeared in films including Prometheus (2012), though it played an alien planet.

Visiting Dettifoss requires preparation: waterproof everything, sturdy boots and acceptance that you'll be damp for hours. The mist travels hundreds of meters, coating everything in fine glacial silt. It's nature's way of saying, "You wanted to see a powerful waterfall? Here's a facial."

As we left Dettifoss, the Ford Fiesta rock-crawled the gravel road while we contemplated Iceland's endless capacity for geological drama. From serene Þveit to thundering Dettifoss, Iceland's eastern reaches prove that sometimes, the road less traveled is less traveled because it's covered in volcanic grit.

Möðrudalsöræfi - Iceland's Highland Desert and Its Volcanic Secrets

Welcome to Möðrudalsöræfi, the northeastern wilderness that makes other remote places look positively suburban. This highland desert isn't just barren. It's artistically barren, with a palette of volcanic blacks, rusty reds and mossy greens that change with the light. What looks empty to the untrained eye is actually a geological scrapbook of Iceland's most violent temper tantrums.

Möðrudalsöræfi highland desert landscape with volcanic fields in northeastern Iceland, 65.6833°N 15.0167°W
Möðrudalsöræfi's vast expanse looks like someone forgot to finish painting the landscape.
The black lava fields here are so fresh they practically still have a "do not touch" sign from the 18th century eruptions.

Here's a fun piece of trivia your guidebook probably got wrong. You might hear rumors that Möðrudalsöræfi served as a training ground for NASA astronauts. The story goes that they tested moon buggies while wearing puffy white spacesuits. That never happened. While Neil Armstrong and other astronauts did visit Iceland in the 1960s for geological training, they went to Askja and Mývatn. We learned they just wore standard hiking gear, not spacesuits.

The area's volcanic fields hide a secret hydrological network, setting it apart from the other-wordly landscape of Death Valley. What appears as barren rock actually conceals underground rivers that resurface miles away, creating sudden oases that disappear as mysteriously as they appear. Early settlers learned to read the subtle moss patterns that indicated water below. A skill mostly lost today.

Panoramic view of Möðrudalsöræfi's rugged terrain in northeastern Iceland, 65.7000°N 15.0500°W
This panoramic view stretches so far you can almost see yesterday.
The mountain ranges here have names only locals can pronounce, which is probably for the best.

During World War II, Allied forces built a secret weather station in these highlands to predict conditions for transatlantic flights. The remains are still there if you know where to look. Just a few concrete foundations slowly being reclaimed by moss. German reconnaissance planes flew over regularly but never spotted the installation, hidden as it was in what they assumed was worthless real estate.

Detailed view of Möðrudalsöræfi's volcanic rock formations in Iceland, 65.7167°N 15.0833°W
These rocks aren't just sitting there - they're telling geological stories in a language only volcanologists understand.
The patterns in the lava flow reveal the exact speed and temperature of the eruption that created them.

The few hardy souls who farm here have developed a unique breed of sheep with particularly thick wool and stubborn personalities. These animals graze on moss and lichen that grow in volcanic soil, giving their meat a distinct mineral flavor prized by Reykjavik chefs. The sheep also serve as unofficial trail markers. Where they won't go, you probably shouldn't either.

Wide landscape of Möðrudalsöræfi showing volcanic features in Iceland, 65.7333°N 15.1167°W
If silence had a physical form, it would look like this.
The complete absence of human noise here is so profound it becomes its own presence.

Modern hikers often miss the ancient cairns that dot the landscape. Stone markers left by medieval travelers navigating between seasonal fishing camps and inland farms. These aren't random rock piles but carefully constructed signposts, with specific shapes indicating distance to water, shelter, or danger. The tradition continues today with GPS coordinates etched into stones for the truly lost.

Námafjall Hverir: Where Earth Lets Off Steam (Literally)

Approaching Námafjall Hverir feels less like arriving at a tourist attraction and more like stumbling onto an alien planet's industrial zone. The sulfur smell hits you first. It's not unpleasant exactly, just aggressively present, like the Earth reminding you who's really in charge here. This geothermal area near Lake Mývatn doesn't just have steam vents. It has personality.

Steaming vents and colorful mineral deposits at Námafjall Hverir geothermal area, Iceland, 65.6417°N 16.8083°W
Námafjall Hverir's colorful deposits look like an art project gone wonderfully wrong.
The yellow isn't paint - it's pure sulfur that would make a chemistry teacher drool.

Here's something the tour buses won't tell you. In the 16th century, the Danish King Frederick II declared these sulfur mines royal property. Iceland became the "Armory of the North," exporting tons of pure brimstone from these very vents to manufacture gunpowder for European wars. Later, Námafjall served as a difficult testing ground for early geothermal power technology. Engineers discovered that the extreme conditions here - superheated steam at 200°C mixed with corrosive gases - could eat through standard steel pipes in months. Their solution? Develop alloys that now power geothermal plants worldwide. The failed prototypes are still buried somewhere out here, slowly returning to the Earth that defeated them.

Bubbling mud pots at Námafjall Hverir geothermal area in northern Iceland, 65.6439°N 16.8111°W
These mud pots bubble with the consistency of a giant's poorly made oatmeal.
The sound they make is somewhere between a simmer and a sigh.

The vibrant colors surrounding the vents look amazing, but they also tell a scientific story. Reds and oranges indicate iron oxidation at specific heat ranges. Greens suggest copper compounds. Some guides might tell you that early farmers used these color patterns to predict incoming storms. That is pure myth. We learned these mineral deposits build up slowly over long periods. They definitely do not change color to warn you about the rain.

Local legend says the steam vents are breathing holes for dragons sleeping beneath the mountains. Given how the ground literally rumbles and exhales hot breath, it's not the craziest explanation we've heard. Medieval travelers would leave small offerings at the edges of active zones, hoping for safe passage. Archaeologists have found silver coins and carved bones dating back to the 12th century.

Steam rising from geothermal vents at Námafjall Hverir, Iceland, 65.6450°N 16.8139°W
The steam here has been rising continuously since long before humans arrived in Iceland.
It's the Earth's original air conditioning system and it never takes a day off.

During the 1940s, British commandos trained here for Arctic warfare, using the thermal areas to practice survival in extreme conditions. Their reports noted that the constant steam made everything damp, weapons rusted overnight and the sulfur smell permeated their gear for weeks afterward. Some veterans apparently could still smell it decades later during humid weather.

Colorful mineral deposits and steaming ground at Námafjall Hverir, Iceland, 65.6461°N 16.8167°W
These mineral patterns form at approximately one millimeter per year.
The artwork you're looking at is centuries in the making, with the Earth as patient artist.

The extreme microorganisms living in these hot springs have attracted pharmaceutical companies searching for heat-resistant enzymes. Some of the bacteria here thrive at temperatures that would cook most life forms, producing compounds used in DNA testing and industrial processes. Your PCR test during the pandemic? Thank Icelandic thermophiles.

What visitors rarely notice are the subtle sounds. Each type of vent has its own acoustic signature. Fumaroles hiss like tea kettles. Mud pots gurgle like upset stomachs. Steam vents roar like distant jets. Icelandic sound artists have made recordings here that sound like abstract symphonies when played back at slow speeds.

Vibrant mineral deposits creating colorful patterns at Námafjall Hverir, Iceland, 65.6472°N 16.8194°W
The red and yellow streaks aren't paint - they're iron and sulfur compounds that would cost a fortune in art supplies.
Nature's abstract expressionism period is still going strong.

In the 16th century, the Danish King Frederick II considered the sulfur deposits here so valuable for making gunpowder that he declared the mines a royal property. For centuries, Iceland was essentially the armory of the Danish realm, exporting tons of "brimstone" from these very vents to fuel European wars.

Active steam vent with mineral buildup at Námafjall Hverir geothermal area, Iceland, 65.6483°N 16.8222°W
This vent has been exhaling continuously since the last ice age retreated.
The mineral cone building up around it grows slower than your fingernails, but much more permanently.

The area's resemblance to Martian environments is striking. You will hear tales that NASA tested early Mars rover prototypes here in the 1990s to see how wheels handled sharp volcanic rock. That is simply false. Those early tests happened in the Mojave Desert. Updated information - NASA did eventually use Iceland for recent missions, like the 2019 SAND-E rover tests. The rocky ground does provide a great Earth analog for Mars. It reminded us of the extreme conditions we saw at Volcán Licancabur.

You might hear local tales about early Icelandic farmers growing vegetables right on these vents. The story claims they used makeshift steam-heated greenhouses and that you can still find wild potatoes growing nearby. Do not believe it. We found out the ground at Hverir is extremely acidic and saturated with toxic sulfur compounds. It literally reaches boiling temperatures. Absolutely no wild potatoes grow in this barren place.

Steam clouds rising over Námafjall Hverir geothermal field in Iceland, 65.6494°N 16.8250°W
On cold days, the steam creates its own microclimate here.
Local birds have learned to ride the thermal updrafts for easy flying.

Here's a tidbit that didn't make the tourist brochures. In the 1600s, some entrepreneurial Danes thought they could get rich by mining sulfur from these very vents to make gunpowder. They quickly discovered that the combination of corrosive gases, unpredictable steam blasts and a location that makes the middle of nowhere look metropolitan was not exactly conducive to a profitable operation. The only thing that exploded was their business plan.

Detailed view of bubbling mud and mineral formations at Námafjall Hverir, Iceland, 65.6500°N 16.8278°W
Each bubble in this mud pot represents a pocket of steam fighting its way to freedom.
The consistency is somewhere between chocolate pudding and construction mortar.

The unique algae growing in warm runoff streams here contain pigments used in natural food coloring. A small company in Reykjavik harvests them (sustainably) for use in specialty chocolates and cosmetics. The blue-green hues can't be replicated synthetically and fetch premium prices in niche markets.

During the summer midnight sun, the steam takes on an ethereal quality, backlit for 24 hours straight. Photographers have captured images where the vapor glows like liquid gold, creating scenes that look more like Painted Desert fantasy paintings than reality. The best shots require standing downwind, which explains why photographers here often smell like they lost a fight with a chemistry set.

Steam rising against mountain backdrop at Námafjall Hverir, Iceland, 65.6511°N 16.8306°W
The steam columns create their own weather patterns here.
On still days, they rise straight up like pillars holding the sky.

Long before geothermal energy became a buzzword, the locals were using these steam vents as a natural oven. There are accounts from the 1700s of farmers wrapping dough in cloth and burying it near the vents, then digging up a perfectly baked loaf hours later. We tried to imagine doing that today, but then remembered we're the type of people who can't even operate a microwave without setting off the fire alarm.

Active geothermal area with multiple steam vents at Námafjall Hverir, Iceland, 65.6522°N 16.8333°W
This particular cluster of vents has been active since records began.
The patterns they create change daily but have maintained the same basic layout for centuries.

The constant thermal activity creates microclimates where temperature can vary 20°C within a few meters. This allows unusual plant communities to exist side-by-side. Arctic species next to heat-loving mosses that normally grow much further south. Botanists have identified several hybrid species found nowhere else on Earth. Again, reminiscent of, but far from identical to, Yellowstone.

As for Krýsuvík on the Reykjanes Peninsula, its geothermal features are indeed more dramatic in scale, sitting directly atop the Mid-Atlantic Ridge. The steam vents there are so powerful they've been measured altering local wind patterns. Early settlers believed the ground there was literally breathing, which isn't far from the truth geologically speaking.

Panoramic view of Námafjall Hverir geothermal field with colorful deposits, Iceland, 65.6533°N 16.8361°W
From this angle, the entire geothermal field reveals its organized chaos.
Each color represents a different mineral, each steam plume a different temperature.

Medieval Icelanders gave this place a wide berth, convinced that the roaring steam and sulfurous smells were the breath of dragons or, worse, an open gateway to the underworld. It wasn't until the 18th century that naturalists started poking around and realized that the only thing hellish about this place was the smell that clung to their clothes for weeks.

Steam vents and mineral formations at Námafjall Hverir geothermal area, Iceland, 65.6544°N 16.8389°W
The mineral deposits here grow in concentric rings like tree rings.
Scientists can read them like history books of geothermal activity.

Leaving Námafjall Hverir, your clothes will carry the sulfur scent for days. A natural souvenir that announces where you've been to anyone downwind. It's the Earth's way of making sure you remember the experience long after you've left.

Dimmuborgir: Iceland's Labyrinth of Dark Castles

The name Dimmuborgir translates to "Dark Castles," which sounds like a rejected heavy metal album title but perfectly captures this lava field's ominous beauty. Formed in a single volcanic eruption around 2,300 years ago, this isn't just random rock. It's architecture by magma, with pillars, arches and chambers that look intentionally designed by a gothic-minded giant.

Entrance gate to Dimmuborgir lava formations in Iceland, 65.5833°N 16.9167°W
The gate to Dimmuborgir looks like it should have a sign saying "Abandon hope, all ye who enter here."
Instead, it just has parking information and trail maps like any sensible attraction.

Geologists identify this as a rare lava lake collapse, a phenomenon seen in few other places on Earth (like Mexico). Roughly 2,300 years ago, a massive pool of molten rock began to cool, forming a roof. When the liquid lava beneath drained away, the roof collapsed, leaving behind these jagged pillars and arches. Dimmuborgir ("Dark Castles") is a highlight of the Diamond Circle route, the northern counterpart to the Golden Circle. It’s one of the essential North Iceland attractions, offering hiking trails that range from paved paths to challenging scrambles through the frozen volcanic labyrinth.

Information board at Dimmuborgir lava field in Iceland, 65.5844°N 16.9194°W
The information board tries valiantly to explain the science behind the spectacle.
Most visitors just glance at it before heading off to find trolls.

According to modern Icelandic folklore, Dimmuborgir is the official residence of the 13 Yule Lads (Jólasveinar). These aren't your Coca-Cola Santas. They are mischievous pranksters with names like "Spoon Licker," "Door Slammer," and "Sausage Swiper." In December, the area hosts events where you can meet these trolls, provided they haven't gone into town to steal skyr or harass sheep, as is their traditional calling.

Towering lava pillars at Dimmuborgir formation in Iceland, 65.5856°N 16.9222°W
These pillars stand like ruined columns from a civilization that never existed.
They've been weathering at approximately one millimeter per century - patient architecture.

The lava formations create unique acoustic properties. Certain chambers amplify sound in peculiar ways. Whispers carry across distances, while shouts get absorbed. Icelandic choirs occasionally perform here, taking advantage of the natural acoustics that make human voices sound unearthly. The effect is reportedly both beautiful and slightly creepy.

Lava arch formation at Dimmuborgir in Iceland, 65.5867°N 16.9250°W
This natural arch looks engineered but was formed by pure geological chance.
It's strong enough to walk under but gives you the distinct feeling it's judging your life choices.

During the Little Ice Age (14th-19th centuries), Dimmuborgir served as a seasonal shelter for shepherds moving flocks between summer and winter grazing grounds. The lava tubes maintained relatively stable temperatures year-round, providing protection from howling winds and snow. Stone walls built inside some chambers still stand, though they're now camouflaged by centuries of moss growth.

Lava field maze at Dimmuborgir formation in Iceland, 65.5878°N 16.9278°W
Getting lost here is both easy and educational.
The maze-like paths were created by lava flowing around older formations, not by any planning committee.

The moss covering the lava isn't just decoration. It's a chronological record. Different species colonize at specific rates after eruptions, allowing scientists to date lava flows by which plants have taken hold. The bright green moss you see is probably 300-400 years old, growing at approximately one millimeter per year. Step carefully. You're walking on living history that takes centuries to recover from footprints.

Dark lava formations resembling castle ruins at Dimmuborgir, Iceland, 65.5889°N 16.9306°W
These formations earn the "Dark Castles" name with their ruined fortress appearance.
The black basalt absorbs light so completely it seems to create its own shadows.

If the frozen lava landscapes look familiar, it’s likely because Mance Rayder set up camp here. Dimmuborgir served as the real-life filming location for the "Wildling Camp" in Season 3 of Game of Thrones. Unlike the show, however, the temperature during filming was a verifiable -11°C. The shivering you see on screen wasn't acting. It was just the cast regretting their wardrobe choices.

Lava pillar formations creating narrow passages at Dimmuborgir, Iceland, 65.5900°N 16.9333°W
These narrow passages feel like hallways in a castle that was built by drunk architects.
The walls lean at angles that defy both gravity and common sense.

The Dimmuborgir Circle Route isn't just a trail. It's a lesson in geological patience. Each turn reveals formations that took millennia to create and will take millennia more to erode. The path itself follows ancient game trails established by Arctic foxes seeking shelter, now maintained for tourists wearing much better footwear than either foxes or medieval shepherds had.

Hiking trail through Dimmuborgir lava formations in Iceland, 65.5911°N 16.9361°W
The maintained trail is a recent concession to tourism.
For centuries, people just picked their way through, often getting gloriously lost.

Photographers love Dimmuborgir for its ever-changing light conditions. The black lava acts as a perfect contrast to green moss, blue sky, or - in winter - pure white snow. Morning fog often settles in the chambers, creating scenes straight from fantasy novels. Professional photographers have been known to wait days for perfect conditions, surviving on packed lunches and stubborn optimism.

Dimmuborgir Circle Route trail marker in Iceland, 65.5922°N 16.9389°W
The trail markers here are more suggestions than commands.
The real path is wherever your curiosity leads, within reason and fragile moss considerations.

Hardcore 'Game of Thrones' fans might recognize Dimmuborgir as the haunting landscape north of the Wall, where the Night's Watch patrolled. The production crew had to work around the fragile moss, which was almost as treacherous as the White Walkers. We half-expected to see Jon Snow brooding behind a lava column, but all we found was a very determined bird building a nest.

Photogenic lava formation at Dimmuborgir in Iceland, 65.5933°N 16.9417°W
This formation appears on approximately 87% of Dimmuborgir Instagram posts.
The remaining 13% are people who got lost trying to find it.

Conservation efforts here focus on something most visitors never consider: preventing too much love. The moss that gives Dimmuborgir its magical appearance takes centuries to grow but seconds to destroy underfoot. Boardwalks and marked trails aren't just for convenience. They're life support for an ecosystem that measures recovery in geological time rather than human years.

View of Lake Mývatn from Dimmuborgir lava field in Iceland, 65.5944°N 16.9444°W
Lake Mývatn in the distance provides a serene contrast to Dimmuborgir's drama.
The lake's name means "Midge Water," which is less romantic but more accurate.

In 1843, a team of British geologists became so engrossed in studying the lava formations that they lost the trail and had to be rescued by a farmer from nearby Reykjahlíð. Their published account in the 'Proceedings of the Royal Society' is a masterpiece of understatement, describing the ordeal as 'a slight inconvenience' despite being lost for two days. We, on the other hand, made sure to keep the trail markers in sight at all times.

Protected lava formation with informational signage at Dimmuborgir, Iceland, 65.5956°N 16.9472°W
This formation is protected not because it's special, but because it's typical.
Preserving the ordinary ensures future generations see what we saw.

The name 'Dimmuborgir' first appears in written records in the 1640s, but the locals had been telling tales about these dark castles for centuries. The stories varied from troll dwellings to petrified giants, but they all agreed on one thing: you didn't want to be here after dark. We can confirm that the place is just as spooky in broad daylight, but at least the parking lot is well-lit.

Final view of Dimmuborgir lava formations in Iceland, 65.5967°N 16.9500°W
Leaving Dimmuborgir feels like emerging from a dream.
The real world seems oddly flat and poorly designed by comparison.

Lake Mývatn: Where Midges Outnumber People (By Several Million)

Let's get the pronunciation right: "Mee-vatn" where "Mee" means midge and "vatn" means water. The name isn't poetic. It's descriptive, like calling your car "Rust Bucket" or your dog "Sheds Everywhere." Lake Mývatn is essentially "Bug Lake," which tells you everything you need to know about summer visits.

Panoramic view of volcanic formations around Lake Mývatn in Iceland, 65.6000°N 16.9667°W
Lake Mývatn's volcanic shoreline looks like a science experiment that got out of control.
The formations here are younger than some wines but will last longer than human civilization.

Here's the good news. Mývatn's midges (Chironomidae) are the non-biting kind. They don't suck blood. They just swarm in clouds so dense you can accidentally inhale a protein supplement. They're also crucial to the ecosystem, feeding the ducks that make this a birdwatcher's paradise. So really, they're just enthusiastic participants in the food chain who haven't learned personal space boundaries.

The lake formed during a massive eruption 2,300 years ago that also created Dimmuborgir. Lava flows dammed rivers, creating this shallow, nutrient-rich basin that's never more than 4.5 meters deep. That's right. You could wade across most of it, if not for the mud, the cold and the sheer impracticality of the endeavor.

Shoreline view of Lake Mývatn with volcanic features in Iceland, 65.6033°N 16.9833°W
The water here is so clear you can see the bottom, which is mostly volcanic sand.
The midges provide moving decoration but don't actually improve visibility.

Mývatn holds an obscure record. It has the highest density of breeding ducks in Europe. Fifteen species nest here, including the Barrow's goldeneye which is rare elsewhere. During peak season, there are approximately 100,000 ducks on a lake that's only 37 square kilometers. That's like having 2,700 ducks per square kilometer, which is either a duck paradise or a duck traffic jam, depending on your perspective.

The lake's unique chemistry comes from volcanic groundwater seepage rich in silica and other minerals. This creates perfect conditions for diatoms (microscopic algae) that form the base of the food chain. The diatom species here are so distinctive that scientists use them to identify sediment layers in other lakes worldwide.

In winter, Mývatn freezes solid enough for ice fishing and even car driving (though we don't recommend either without local knowledge). The ice can reach 70 cm thick, creating a perfectly flat, white expanse that contrasts dramatically with the dark volcanic surroundings. It's like nature's minimalist art installation, temporarily installed from December to April.

Skútustaðagígar: Nature's Pressure Cooker Explosions

Skútustaðagígar's pseudocraters look like someone poked the Earth with a giant stick and it bubbled up in protest. These aren't true volcanic craters. They're "rootless cones" formed when lava flowed over wetlands, instantly vaporizing the water beneath and causing steam explosions. Think of it as nature's version of putting water in hot oil, but with more basalt and lasting consequences.

Skútustaðagígar pseudocraters near Lake Mývatn in Iceland, 65.5867°N 17.0000°W
These pseudocraters number about 100, each one a monument to instant geological drama.
They formed in days but will erode over millennia - the definition of fleeting permanence.

The 2,300-year-old eruption that created these features was part of the same event that formed Lake Mývatn and Dimmuborgir. Lava traveled 60 kilometers from its source, covering an area of 220 square kilometers. Roughly the size of Minneapolis or Sheffield, England. When it hit the lake's precursor wetlands, the resulting steam explosions threw debris hundreds of meters into the air.

Close-up view of Skútustaðagígar pseudocrater formation in Iceland, 65.5889°N 17.0167°W
The crater walls reveal layers of volcanic material ejected during the steam explosions.
Each layer represents seconds of violence preserved for millennia.

These pseudocraters are so well-studied they've become the type example for this geological feature worldwide. When scientists discover similar formations on Mars (and they have), they compare them to Skútustaðagígar. Your visit here is essentially walking through a planetary reference standard.

Vegetation growing on Skútustaðagígar pseudocraters in Iceland, 65.5911°N 17.0333°W
Moss and grasses colonize the sheltered crater slopes where moisture collects.
Life always finds a way, even in landscapes that look freshly sterilized.

The Skútustaðagígar Loop Trail takes about 45 minutes to walk if you're brisk, or three hours if you're like us and stop to examine every interesting rock and plant. The path winds between craters ranging from 2 to 10 meters tall, giving you the surreal experience of walking through a field of natural bread rolls if bread rolls were made of black volcanic rock and weighed several tons each.

Trail through Skútustaðagígar pseudocrater field in Iceland, 65.5933°N 17.0500°W
The maintained trail prevents erosion of the fragile crater slopes.
Straying from it isn't just discouraged - it's geologically irresponsible.

Back in the 18th century, these pseudocraters were the Iceland equivalent of a hideout for bandits on the run. The maze-like formation provided perfect cover and the unstable ground made it difficult for authorities to pursue them. We didn't find any outlaws during our visit, but we did find a lot of duck poop - which, in terms of historical significance, is probably less exciting.

View from Skútustaðagígar pseudocraters toward Lake Mývatn in Iceland, 65.5956°N 17.0667°W
From the higher craters, you can see how these formations relate to the lake.
The entire landscape tells a connected story of fire meeting water.

Höfði Nature Preserve: Lake Mývatn's Lava Peninsula

Höfði is the promontory that proves lava can be both destructive and nurturing. This protected peninsula juts into Lake Mývatn, offering walking trails through lava formations that have been softened by centuries of moss growth. It's like Dimmuborgir's more civilized cousin - equally volcanic but better dressed in greenery.

Entrance to Höfði Nature Preserve on Lake Mývatn in Iceland, 65.6167°N 17.0000°W
The entrance to Höfði is modest, letting the landscape speak for itself.
The sign says "Nature Preserve" but really means "Volcanic Garden with Benefits."

The preserve's walking trails are mostly flat and well-maintained, making them accessible to almost everyone. They wind through birch forests that have established themselves in lava cracks, demonstrating how life colonizes even the most inhospitable places given enough time (about 2,300 years, in this case).

View of Lake Mývatn from Höfði Nature Preserve in Iceland, 65.6189°N 17.0167°W
From Höfði's shores, Lake Mývatn looks deceptively peaceful.
The midges are still there, just waiting for you to stop moving.

Goðafoss: Where Gods and Water Collide

Goðafoss isn't just a waterfall. It's Iceland's baptismal font, where the nation symbolically converted to Christianity in the year 1000 AD. According to the Íslendingabók (Book of Icelanders), lawspeaker Þorgeir Ljósvetningagoði threw his pagan idols into the falls after deciding Iceland would adopt Christianity. It was either that or risk civil war, making this perhaps history's most dramatic religious compromise.

Watch: Goðafoss Waterfall's relentless power - the Skjálfandafljót River drops 12 meters here with enough force to shake the ground.

The waterfall's horseshoe shape spans 30 meters across with a 12-meter drop. That's not particularly tall by Icelandic standards (Dettifoss is twice as high), but Goðafoss compensates with perfect proportions and accessibility. You can walk right up to both sides, feeling the spray on your face while contemplating a millennium of history.

Panoramic view of Goðafoss waterfall in northern Iceland, 65.6833°N 17.5500°W
Goðafoss in panorama reveals its perfect symmetry.
The waterfall splits around a central rock island like nature's own carefully planned construction.

The name Goðafoss literally translates to "Waterfall of the Gods." The legend states that in the year 1000 AD, Lawspeaker Þorgeir Ljósvetningagoði, after agonizingly deciding at the Althing that Iceland would convert to Christianity to avoid Norwegian invasion, returned home and tossed his pagan idols into the churning water. This 12-meter high, 30-meter wide cascade is one of the most accessible Ring Road stops, located right off Route 1. It marks a pivotal moment in history where a political decision changed the cultural fabric of the nation, all memorialized by a really big splash.

Close view of Goðafoss waterfall's powerful flow in Iceland, 65.6844°N 17.5533°W
Standing this close to Goðafoss, you understand why medieval people believed in water spirits.
The power is both awe-inspiring and slightly terrifying.

The basalt columns framing the waterfall formed differently than those at Svartifoss or elsewhere. Here, lava cooled relatively slowly, allowing hexagonal columns to develop perpendicular to the cooling surface. The result looks like a giant pipe organ designed by a particularly ambitious architect.

Skjálfandafljót river outflow below Goðafoss waterfall in Iceland, 65.6856°N 17.5567°W
Below the falls, the Skjálfandafljót River continues its 178-kilometer journey to the sea.
The water here has traveled from glaciers deep in Iceland's interior, picking up mineral colors along the way.

Modern pagans occasionally hold ceremonies here, not to revive the old gods but to honor Iceland's religious heritage. These gatherings are peaceful affairs, often involving poetry readings and quiet reflection rather than the dramatic idol-tossing of legend. The waterfall seems to welcome all interpretations, continuing its endless flow regardless of human beliefs.

Grenivík: North Iceland's Fjord's Best-Kept Secret

We rolled into Grenivík late one evening, just as the Arctic sun was playing its nightly game of hide-and-seek with the horizon. This charming coastal village is a highlight of North Iceland travel, sitting on the shores of Iceland's longest fjord, Eyjafjörður, which frankly sounds more like a sneeze than a geographical feature. We checked into Ártún Bed & Breakfast, a fairytale cottage that looked like it had been designed by Tolkien after a particularly good mead.

Scenic drive on Iceland Route 84 Víkurskarðsvegur approaching Grenivík village along Eyjafjörður fjord coastline with mountain views
The road to Grenivík on Route 84, also known as Víkurskarðsvegur
This winding path has been connecting fjord communities since the 1930s
Early travelers complained it was "only slightly smoother than a reindeer's spine"

Grenivík has a population that could fit in a decent-sized American backyard - around 300 people. But what it lacks in population density, it makes up for in sheer dramatic scenery. The village is cradled by mountains so steep they look like God forgot to finish smoothing them out. The Tröllaskagi Peninsula looms to the west, its name literally meaning "Troll Peninsula." We didn't spot any trolls unless you count the guy running the local gas station who had seen one too many dark winters.

Historically, this region of Eyjafjörður was a hub for the perilous shark fishing industry. In the 19th century, open rowboats would venture far out to sea in winter to catch the Greenland Shark for its liver oil, which was used for street lighting in European cities. It was a deadly profession. The "Shark fishermen" were considered the toughest men in Iceland, often rowing for days in freezing storms. Today, the Grenivík maritime museum preserves the memory of these men who literally fueled the lights of Europe.

Traditional Icelandic guesthouse Ártún Bed & Breakfast wooden building with turf roof and welcome sign in Grenivík village
Ártún Bed & Breakfast - the sign promises hospitality
The turf roof isn't just for looks - it provides insulation equivalent to 12 inches of modern foam
Local legend claims this building was moved three times by rolling it on logs

The village's history reads like a Nordic epic with fewer dragons and more fishing. Grenivík was mentioned in the 12th-century Landnámabók (Book of Settlements) as a prime location for - wait for it - collecting eiderdown. That's right, Iceland's early economy was partially built on stealing duck feathers. The 19th-century wooden church, Grenivíkurkirkja, has a bell cast from melted-down Danish cannons captured during the Napoleonic Wars. Nothing says "peace be with you" like recycled artillery.

Warm inviting bedroom interior at Ártún guesthouse with wooden beams, traditional textiles and mountain view window
Our room at Ártún - note the triple-layer windows
Icelandic beds are notoriously firm - local saying: "Sleep like a Viking, not like a Dane"
The wool blankets are so dense they could stop a crossbow bolt

What struck us most was the village's maritime museum, which isn't so much a museum as a former fisherman's shed filled with artifacts that tell a story of survival. The most fascinating exhibit? A 1940s-era whale vertebrae stool that some local fisherman carved because, as the placard explained, "wood was scarce but dead whales were plentiful." Practical, if slightly morbid.

Cozy breakfast nook at Ártún guesthouse featuring smoked salmon, skyr, rye bread and geothermal-boiled eggs
Breakfast Icelandic-style: smoked fish, skyr and boiled eggs cooked in geothermal water
The butter is so fresh it still remembers the cow's name
Icelandic coffee is strong enough to wake the dead - which is helpful in winter

Grenivík serves as the perfect base for exploring northern Iceland's wonders. From here, you can reach the geothermal madness of Lake Mývatn in under two hours, or drive the dramatic coastal route to the Arctic Circle. The locals have a saying: "In Grenivík, we have two seasons - July and winter." We visited in July, so we only experienced the good one.

Note: We paid for our stay at Ártún like everyone else. They didn't even give us extra fish, which we consider a mark of integrity.

Akureyri: The Paris of North Iceland (With Better Weather)

Akureyri is Iceland's second city, which is like being America's second-most interesting Kardashian. With about 18,000 people, it's what passes for a metropolis in a country where sheep outnumber humans three to one. The town sits at the head of Eyjafjörður, which at 60 kilometers is Iceland's longest fjord and apparently where all the cool water hangs out.

Distant panoramic view of Akureyri settlement nestled between mountains at head of Eyjafjörður fjord in North Iceland
Akureyri from across the fjord - looks deceptively close
The water crossing saves 50km of driving but requires a ferry that runs twice daily
Local joke: "The fjord is so long it has its own time zone"

The town began its life in the 16th century as a Danish trading post, because apparently the Danes thought, "You know what this frozen rock needs? More pickled herring." The harbor remains the town's lifeblood, though these days it sees more cruise ships than fishing boats. Walking the waterfront, we were struck by how much Akureyri resembles Alaskan port towns. Same colorful buildings, same salty air, same sense that civilization is holding a very thin line against wilderness.

Approaching Akureyri town showing colorful buildings, church spire and harbor activity along Eyjafjörður coastline
Akureyri's from across Eyjafjörður fjord.
Cruise ships are docked at the port.

Here's a piece of trivia you won't find in many guidebooks. Akureyri was home to Iceland's first traffic lights, installed in 1957. The townspeople hated them so much that they were removed after six months and replaced with a roundabout. To this day, Akureyri has the highest per-capita roundabout density in the Northern Hemisphere. The town's main intersection features a sculpture of a traffic light lying on its side, which locals call "the defeated dictator."

Cultural life here is surprisingly vibrant for a town that's basically a dot on a map of empty space. The Akureyri Art Museum has a collection that includes works by Iceland's most famous painter, Jóhannes Kjarval, who once traded a painting for a year's supply of sausage. The Akureyri Theatre Company stages productions in a converted fish processing plant. Nothing says "high art" like the lingering smell of cod.

Modern food court interior at Glerártorg shopping mall in Akureyri featuring Icelandic fast food options and casual seating
Glerártorg mall food court - Iceland's northernmost food court
The hot dog stand sells more lamb-based dogs than beef
Note the absence of pineapple on pizza - Icelanders consider this a war crime

Following the 2008 financial crash, Akureyri implemented a psychological morale booster that remains today. All the red traffic lights were changed to the shape of hearts. It was a municipal "smile campaign" that stuck. Also, unlike Reykjavik, Akureyri sits in a rain shadow, giving it surprisingly warm summers and making the Akureyri Botanical Garden one of the northernmost places in the world where you can find exotic plants flourishing outdoors.

Charming pedestrian street in Akureyri featuring historic wooden buildings, boutique shops and café seating
Akureyri's main shopping street - note the absence of chain stores
The bookstore has been in the same family since 1923
Local law requires all new buildings to include geothermal heating hookups

Winter transforms Akureyri into a wonderland that would make Santa jealous. The Hlíðarfjall Ski Resort gets more reliable snow than the Alps, thanks to its Arctic location. The town's Christmas lights stay up from November through February because, as one local told us, "In darkness, we need all the light we can get." The Christmas market features wool sweaters so thick they could stop a bullet and mulled wine that could strip paint.

Iconic Akureyri Church with distinctive twin spires and concrete modernist architecture overlooking town
Akureyri shopping mall parking lot, eerily familiar.

Akureyri serves as the perfect base for exploring northern Iceland's weirdest attractions. You can day-trip to Lake Mývatn, where the landscape looks like Mars if Mars had more mosquitoes. Or visit Dettifoss, Europe's most powerful waterfall, which moves enough water every second to fill an Olympic swimming pool. The town even offers flights to Grímsey Island, which straddles the Arctic Circle and has a population of 61 people and approximately 8 million puffins.

Residential neighborhood in Akureyri showing brightly painted houses, well-kept gardens and dramatic mountain scenery
Akureyri's residential streets - every house has a geothermal connection
The brightly painted exteriors help with winter depression
Property taxes are based on how much mountain view you block for neighbors

Öxnadalur Valley: North Iceland's Scenic Power Lines

Öxnadalur Valley is the kind of place that makes you understand why Vikings gave up raiding to become farmers. It's a lush, green slash between mountains so steep they should come with a warning label. The name translates to "Ox River Valley," which undersells it dramatically. This isn't some gentle English meadow. It's a landscape that shouts "Iceland!" in your face.

Breathtaking panorama of Öxnadalur Valley showing winding mountain road, steep peaks and lush river valley
Öxnadalur Valley's entrance - the road winds like a drunken snake
The mountains rise 1,000 meters straight up from the valley floor
In winter, this pass is closed more often than a Reykjavik bar at 5 AM

The valley has been an important transportation route since Viking times, though back then "transportation" meant "walking while hoping not to freeze to death." The modern road was built in the 1930s using convict labor. Apparently Iceland's version of community service involved moving several thousand tons of rock with pickaxes. The convicts were paid in tobacco and extra rations, which explains why the road has so many curves. They were working while mildly nicotine-high.

Dramatic narrow section of Öxnadalur Valley road winding between sheer rock walls with cascading waterfalls
The narrowest part of Öxnadalur - locals call it "the corridor"
Rockfalls are so common there's a dedicated cleanup crew on standby
The waterfalls run year-round, fed by melting glaciers

Öxnadalsá River cuts through the valley like a liquid razor. It's famous among fly fishermen for its Arctic char, which grow fat and sassy on a diet of freshwater shrimp. The fishing rights are passed down through families like medieval titles. Trying to fish without permission will get you glared at by Icelanders, which is somehow worse than being yelled at.

Crystal clear Öxnadalsá River meandering through Öxnadalur Valley with perfect mountain reflections in calm water
Öxnadalsá River - so clear you can count the fish from 50 meters away
The water temperature never rises above 4°C even in summer
Local saying: "The river flows so straight, it could guide an axe"

Historical sites dot the valley like raisins in a cake. There's the ruin of a 17th-century church that was abandoned when the congregation decided the walk was too far in winter. Several traditional turf farms still stand, though these days they're mostly used as summer cabins by descendants of the original owners. One farm has been in the same family since 1306, which predates the invention of the fork in most of Europe.

Historic turf-roofed farm building in Öxnadalur Valley showing traditional Icelandic architecture and stone construction
Traditional turf farm - the roof grows wildflowers in summer
The walls are two meters thick for insulation
These buildings stay 15°C warmer inside than outside in winter

Running through this pristine landscape are power lines that look like they wandered in from an industrial zone. These aren't your average ugly transmission towers. They're part of Iceland's hydroelectric grid, carrying clean energy from the highlands to the coast. The towers are painted a subtle green to blend with the landscape, which works about as well as putting a mustache on a supermodel. Still, it's a reminder that even in paradise, people want to charge their phones.

Modern hydroelectric power transmission lines spanning Öxnadalur Valley against dramatic mountain scenery
Power lines in paradise - carrying 100% renewable hydroelectric power
The towers are designed to withstand 200 km/h winds
Maintenance crews use helicopters because the terrain is too steep for trucks

Víðidalstunga: Where the Sheep Outnumber the People (And the People Like It That Way)

Our final Icelandic accommodation was at Ferðaþjónustan Dæli in Víðidalstunga valley, which we chose because it had the most unpronounceable name we could find. This working farm turned guesthouse sits in the Skagafjörður region, Iceland's horse country, where the animals are more elegantly bred than most European royalty.

Traditional Icelandic farmhouse Daeli Guesthouse in Víðidalstunga valley with wooden exterior and mountain views
Daeli Guesthouse - the sign has more vowels than consonants
The building dates from 1928 but has been updated with geothermal heating
The owner's family has farmed this land since the 14th century

Watch: Driving from Akureyri to Víðidalstunga crossing Öxnadalur Valley

Víðidalstunga translates to "Wide Valley Tongue," which sounds like a medical condition but is actually a reference to the valley's shape. The area has been continuously farmed since the Settlement Age, making it some of Iceland's oldest agricultural land. The soil here is surprisingly fertile, thanks to volcanic ash deposits from eruptions that happened before anyone thought to write them down.

Idyllic pastoral scene in Víðidalstunga valley showing sheep grazing on lush green fields with mountain backdrop
Víðidalstunga's famous sheep - each has a unique earmark for identification
The sheep outnumber humans 200 to 1 in this valley
They're descended from stock brought by Viking settlers 1,100 years ago

The guesthouse is run by a family that can trace their lineage back to the original settlers. They still farm the traditional way - sheep in summer, greenhouse vegetables in winter and a general attitude that modern technology is fine as long as it doesn't interfere with afternoon coffee. We were served homemade skyr so thick you could stand a spoon in it and bread baked in a geothermal oven that's been in use since 1910.

Golden hour evening light illuminating Víðidalstunga valley farm buildings, pastures and distant mountains
Evening in Víðidalstunga - the short dusk and dawn cycle at midnight in July
Each farm has its own hot spring for heating and bathing

What makes Víðidalstunga special isn't just the scenery. It's the continuity. The same families have worked this land for generations, through volcanic eruptions, harsh winters and economic upheavals. The guestbook dates back to 1952 and includes entries from geologists, artists and one very confused Japanese tourist who thought he was in Greenland.

Rustic interior of Daeli Guesthouse farm building showing traditional Icelandic furnishings and wooden construction
Midnight at Víðidalstunga
This is the darkest it gets before sunlight streams through again shortly

Back at Keflavik: The Circle Completes

We drove from Víðidalstunga back to Keflavik International Airport, completing our Icelandic loop. The landscape changed from lush valleys to barren lava fields, then to the Reykjanes Peninsula's geothermal madness. After two weeks of driving, we'd covered approximately 2,500 kilometers, seen more waterfalls than we could count and eaten enough fish to qualify as honorary marine mammals.

Iceland leaves you with contradictions. It's a land of fire and ice, ancient and modern, isolated and connected. The roads are empty but well-maintained. The food is simple but delicious. The people are reserved but will help you change a tire in a blizzard without expecting thanks.

As we boarded our flight to central Europe (starting with Austria's stunning Wachau Valley of the Danube River), we realized that our Iceland travel experience was unforgettable. Iceland isn't a place you visit. It's a place that visits you. The landscapes haunt your dreams. The silence echoes in your city life. And you'll find yourself craving smoked fish at odd hours. We'll be back to watch a volcano erupting standing next to its lava flow. Iceland has that effect on people.

Iceland Road Trip Summary: Our Route

For those planning their own Icelandic adventure, here's our complete route (view the full interactive map):

  1. Keflavik International Airport - Where your wallet weeps and your Icelandic adventure begins.
  2. Silent trolls Steinn and Sleggja of Keflavik (Statue of Boulder & Sledgehammer) - The world's most patient trolls, waiting for sunset since October 1, 2009 when they were unveiled by local labor unions (Samtök starfsmanna iðnaðarins) and the municipality of Reykjanesbær.
  3. Minnismerki sjómanna (Fishermen Monument) - A six-meter geometric memorial facing the unforgiving sea.
  4. Blue Lagoon - Man-made geothermal runoff that somehow became a $100 spa day.
  5. Sunny Reykjavik House, Bergstaðastræti 40, 101 Reykjavík - A bright spot in the city, quite literally.
  6. Þingvellir National Park - Where North America and Europe are breaking up (geologically speaking).
  7. Geysir - The original geyser that gave all others their name, now mostly retired.
  8. Gullfoss - The waterfall a farmer's daughter saved from becoming a hydroelectric plant.
  9. Kerið Crater - A 3,000-year-old volcanic caldera where Björk once performed on a raft.
  10. Krisp Restaurant, Selfoss - Contemporary Icelandic dining in a former hardware store.
  11. Sunny Reykjavik House - Our cozy home base in the capital.
  12. Chuck Norris Grill - Because even in Iceland, Chuck Norris jokes transcend borders.
  13. Fjällräven - Swedish outdoor gear for the discerning Viking.
  14. Gleraugnasalan - For when you need to see Iceland more clearly.
  15. Roupa - Portuguese-inspired clothing in the land of wool.
  16. idontspeakicelandic - A Reykjavik shop that says exactly what we're thinking.
  17. Te & Kaffi - Reykjavik's answer to caffeine addiction.
  18. Hallgrimskirkja - Reykjavik's concrete spaceship, inspired by basalt columns.
  19. Þingborg Ullarverslun - Where Icelandic wool gets serious, with sweaters that last a lifetime.
  20. Seljalandsfoss - The waterfall you can walk behind, if you don't mind getting soaked.
  21. Skógafoss - Where a legendary treasure chest ring ended up on a church door.
  22. Mýrdalsjökull - The ice cap sitting atop the temperamental Katla volcano.
  23. Sólheimajökull - A glacier tongue retreating faster than a tourist from hákarl.
  24. Dyrhólaey - A massive stone arch and puffin paradise.
  25. Reynisfjara - A black sand beach with waves that will kill you if you turn your back.
  26. Reynisdrangar Cliffs - Sea stacks that were allegedly trolls caught by sunrise.
  27. Hálsanefshellir Cave - A basalt-column cave that fishermen used for shelter.
  28. Vik - North Star Cottage - A turf-roofed cottage with geothermal heating and sheep for neighbors.
  29. Laufskálavarða - Stone cairns built by travelers for good luck since the 10th century.
  30. Gönguleið um Eldhraun - A lava field so lunar that NASA astronauts trained here.
  31. N1 Skaftárskáli og Gvendarhorn/ Verslun - The gas station grill that saves road trips with heavenly lamb.
  32. Haoldukvisl glacier - The shy, unassuming tongue of Vatnajökull.
  33. Skaftafell Glacier - The older, more reserved sibling in the glacial family.
  34. Svínafellsjökull Glacier - The dramatic younger brother, full of personality and ice caves.
  35. Fjallsjökull - The introverted glacier with its own serene, crowd-free lagoon.
  36. Jökulsárlón - The glacial lagoon where icebergs go to socialize before hitting the Atlantic.
  37. Breiðamerkursandur - Diamond Beach, where icebergs glitter like jewels on black sand.
  38. Heinaberg Glacier - Flatey Meeting Point - The quiet glacier at the end of the road, with 90% fewer tourists.
  39. Þveit - A serene village near the home of the Lagarfljót Worm, Iceland's serpentine answer to the Loch Ness Monster.
  40. Pakkhús Restaurant - A converted warehouse in Höfn serving Iceland's best fish soup.
  41. North Sea Viewpoint, Múlaþing - Where the Atlantic puts on a show with 20-meter winter waves.
  42. Borgarfjörður - One of the Eastfjords, often confused with its two namesakes.
  43. Havari Cafe & Guest House - A coffee spot built from a shipwreck, with fjord views.
  44. Askur Pizzeria, Egilsstaðir - Because sometimes you just need a really good pizza after days of dried fish.
  45. Mjóanes accommodation - A rustic sheep farm B&B located directly on the banks of Lake Lagarfljót.
  46. Grímstunga Guesthouse - A remote highland guesthouse with its own micro-hydro power.
  47. Dettifoss (East side overlook) - Europe's most powerful waterfall by energy discharge, angry enough to star in Prometheus.
  48. Möðrudalsöræfi - Iceland Highlands Desert, Black Lava Fields - A vast volcanic desert where silence has physical form.
  49. Námafjall Hverir Geothermal Area - Sulfuric smoker - Where the Earth hisses, bubbles and smells like rotten eggs.
  50. Dimmuborgir - Dark Castles Lava Field - A labyrinth of lava pillars, home to Iceland's 13 Yule Lads.
  51. Lake Mývatn - "Midge Lake," full of non-biting bugs and 100,000 breeding ducks.
  52. Skútustaðagígar - Pseudo Craters - Explosion craters formed when lava met wetlands.
  53. Höfði Nature Preserve - A lava peninsula softened by centuries of moss growth.
  54. Goðafoss Waterfall - Named "Waterfall of the Gods," where legend (but not history) says the law-speaker threw his pagan idols.
  55. Grenivík - Artun Guesthouse - A charming fjord village sitting in the shadow of the 1,173-meter Kaldbakur mountain.
  56. Glerártorg Akureyri Shopping Mall - Home to "Glerártorg," the largest shopping mall outside Reykjavik (and yes, it has a food court).
  57. Öxnadalur Valley - A dramatic valley road with power lines and 1,000-meter cliffs.
  58. Víðidalstunga - Ferðaþjónustan Dæli - A working farm guesthouse with geothermal ovens and sheep that outnumber people 200-to-1.
  59. Keflavik International Airport - Where the circle completes and you plan your return trip.

Total driving distance: Approximately 2,500 km (1,550 miles)
Time: 14 days
Best meal: Fresh-caught Arctic char at a roadside stand
Worst weather: Horizontal rain near Vik
Most Icelandic moment: Seeing someone mow their lawn at 11 PM in full daylight

Onwards!

- The Vagabond Couple

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