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| The Colorado River curling through layered canyons below Dead Horse Point at sunset |
Part 4 carried us from Colorado Springs across Hoosier Pass, through Breckenridge, Vail and Glenwood Canyon, and into Moab. With Shehzadi parked beneath Utah’s red rock, the next chapter stayed close to town but covered a surprising amount of vertical geology.
Our Moab base led to Arches National Park, Utah Route 313, Dead Horse Point, Canyonlands Island in the Sky and an unpaved drive in Sand Flats Recreation Area. US-191 was already familiar from our earlier Yellowstone and Glacier route. Around Moab, however, the road had acquired arches, mesas, canyon rims and a much stronger preference for red.
Trans-America Overland Part 5 — Post Summary
From our base in Moab, we drive Shehzadi through Arches National Park, follow Utah Route 313 to sunset at Dead Horse Point, visit Canyonlands Island in the Sky and finish on the unpaved roads of Sand Flats Recreation Area. Along the way, sandstone fins become arches, mesas fall into canyons and the Colorado River performs a very large U-turn far below the rim.
| What's Covered | |
| 🪨 | Arches National Park — Park Avenue, Courthouse Towers, Ham Rock and the scenic road |
| 🪟 | Windows Section — Balanced Rock, Turret Arch, North Window, Parade of Elephants and Double Arch |
| 🏚️ | Wolfe Ranch and Delicate Arch — historic cabin, trailhead and distant viewpoint |
| 🌅 | Dead Horse Point — Utah Route 313, Colorado River gooseneck and sunset from the rim |
| 🏜️ | Canyonlands Island in the Sky — Mesa Arch, Shafer Canyon, Grand View Point and Upheaval Dome |
| 🛻 | Sand Flats Recreation Area — graded dirt roads, slickrock country and Shehzadi’s Moab mileage check |
These Moab excursions began and ended in the same town, but the road never repeated itself. Arches put us among fins and openings. Dead Horse Point lifted us above the Colorado River. Canyonlands spread an entire drainage system below the mesa. Sand Flats finally handed the route to Shehzadi’s tires. The truck had found a place where geology came with parking lots, trails and occasional instructions not to drive over the interesting bits.
Base: Moab, Utah
Vehicle: Shehzadi, our Toyota Tundra
Main roads: US-191, Arches Scenic Drive, Utah Route 313 and local Sand Flats roads
Main experiences: Arches, Dead Horse Point sunset, Canyonlands Island in the Sky and an unpaved Sand Flats drive
Route character: Sandstone fins, arches, mesas, canyon rims and graded dirt roads
Route at a Glance
- Drive from Moab into Arches National Park for Park Avenue and Courthouse Towers.
- Continue through Balanced Rock and the Windows Section to Double Arch.
- Stop at Wolfe Ranch, the Delicate Arch trailhead and the distant viewpoint.
- Follow Utah Route 313 to sunset over the Colorado River at Dead Horse Point.
- Return along Route 313 for Canyonlands Island in the Sky.
- Take Shehzadi onto the graded roads of Sand Flats Recreation Area.
Arches National Park: Park Avenue and Courthouse Towers
Arches National Park begins only a few miles north of Moab, which makes the entrance seem almost suspiciously convenient. The road climbs quickly from the visitor area into a field of fins, towers and openings cut from sandstone. The National Park Service has documented more than 2,000 natural stone arches here. Their abundance comes from the right rock layers, deep salt movement, parallel fractures and enough water to keep erosion employed full time.
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| An NPS panel traces the work of fractures, sandstone fins, water and erosion |
The formation diagram made the sequence clearer. Buried salt pushed overlying rock upward and cracked it into long parallel lines. Water entered those joints. Softer material wore away, fins separated, and some fins eventually developed openings. It is an efficient process if one is willing to wait several million years and accept a considerable amount of debris.
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| Shehzadi among the red sandstone formations of Arches National Park |
Shehzadi climbed the entrance switchbacks and reached the main park road. The first pullouts appeared almost immediately, because Arches has correctly concluded that drivers confronted with giant sandstone walls should be given somewhere legal to stop staring.
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| The Arches National Park entrance sign beneath the first wall of red rock |
Park Avenue formed the first major corridor. Tall walls rose on both sides of the trail and road, while detached towers made the skyline look crowded without the inconvenience of an actual city. We walked into the opening section and then continued by road toward Courthouse Towers.
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| Park Avenue, where vertical sandstone walls form the park's opening corridor |
The Park Avenue walls are rock fins: long, narrow slabs created along parallel fractures. Some remain solid. Others develop weak zones that widen into arches. The park therefore contains both finished products and a large inventory of geological work in progress.
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| Courthouse Towers rising above the road through Arches National Park |
Courthouse Towers gathered several named formations close to the scenic drive. The names were visual shortcuts rather than scientific classifications, which helped. “Tall Jurassic sandstone monolith number four” would have been accurate but difficult to remember before lunch.
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| The Organ, named for the long vertical lines running down its sandstone face |
The Organ carried long vertical grooves down its face. From one angle, the resemblance was immediate. From another, it became a massive wall with shadows in the cracks. Rock names depend heavily on where one stands, much like arguments about furniture placement.
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| A second Courthouse Towers angle turns the rock into a broad wall of grooves and shadow |
A second angle flattened the same cluster into broader planes of stone. The shift was a useful warning: photographs identify viewpoints as much as objects, and sandstone is under no contractual obligation to look consistent.
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| The Three Gossips standing beside the Arches Scenic Drive |
The Three Gossips were easier to recognize. Three adjoining pinnacles rose beside the road, apparently engaged in a discussion that had lasted long enough for erosion to become involved.
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| Sheep Rock, a freestanding formation along the Courthouse Towers road |
Sheep Rock stood nearby as another freestanding form left behind while surrounding material wore away. The outline worked best from the signed viewpoint. Move too far, and the sheep returned to ordinary geology.
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| Tower of Babel rising from the desert floor at Courthouse Towers |
Tower of Babel completed the Courthouse Towers sequence with a broad vertical face and a name carrying more drama than the parking area. Its iron-stained sandstone shifted between red and orange as the angle of light changed.
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| Ham Rock, named by people who apparently reached the park before lunch |
Ham Rock required less interpretation. Its rounded top suggested a roast on a platter, proving that naming rights in the desert occasionally passed to hungry people.
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| A Ham Rock campervan parked in front of Ham Rock, with no advance planning by either rock |
The day’s best coincidence arrived when a Cruise America campervan carrying a photograph of Ham Rock parked directly in front of the real formation. Its occupants had not noticed. We pointed out the alignment, and the campervan briefly achieved the difficult state of being both transportation and a labeled field guide.
Balanced Rock, the Windows and Double Arch
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| Balanced Rock above its much narrower pedestal |
Balanced Rock came next. It invited comparison with the differently shaped Balanced Rock we had seen at Garden of the Gods, but the structure here follows its own rules. The upper mass is harder Entrada Sandstone. The pedestal includes softer rock that erodes faster. The name says “balanced,” while the geology says “still attached, for now.”
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| Balanced Rock from the road, where the pedestal becomes easier to see |
From the road, the narrowing pedestal became obvious. The caprock weighs heavily on a support that looks like it has already submitted a request for early retirement.
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| Balanced Rock standing alone against the open desert |
The open ground around the formation gave it the isolation required for proper theatrical effect. There were no ropes, braces or hidden steel beams. The only support system was stone and a very long schedule.
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| A closer view of the resistant caprock and softer pedestal below it |
A closer view showed the contact between the caprock and pedestal. Freeze-thaw cycles, rain and gravity continue to work on it. Balanced Rock is therefore a landmark and a reminder that “permanent” is a word humans use when geology is not listening.
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| The scenic road leaving Balanced Rock for the Windows Section |
The scenic drive continued toward the Windows Section. Red walls moved closer to the road, then opened into pullouts and broad slabs of bare rock.
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| A roadside pullout beneath sandstone towers on the way to the Windows |
Each turn changed the apparent shape of the fins. Some looked like towers from the front and thin walls from the side. The road was doing three-dimensional geometry without asking anyone to show their work.
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| Sunlight squeezing past a sandstone wall near the Windows Section |
Near the Windows, sunlight broke around a sandstone wall and briefly turned the parking area into a stage. The vehicles remained ungrateful and continued looking like vehicles.
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| Turret Arch, with its tall stone tower attached to the opening |
Turret Arch opened through a tall fin with a stone tower attached to one side. It introduced the Windows group with enough asymmetry to keep the camera busy.
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| Turret Arch seen across the open rock of the Windows Section |
Across the open rock, the arch changed again. Its opening widened, the tower separated visually from the wall, and the surrounding fins became part of the composition. The park had discovered multiple camera angles long before cameras arrived.
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| The rounded forms known as the Parade of Elephants |
The Parade of Elephants stood nearby as a row of rounded forms and gaps. The resemblance was strongest from the signed approach, where the “bodies” and “legs” aligned.
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| Elephant Butte and the Parade of Elephants near the Windows Section |
Elephant Butte added a larger mass behind the procession. The names are informal, but they help visitors keep their bearings in an area where every direction contains another sandstone object demanding attention.
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| North Window opening through a high sandstone wall |
North Window cut a broad opening through a high wall. In geologic terms, a “window” is still an arch; the name usually reflects size, position or the view framed beyond it.
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| The sandstone ceiling beneath North Window |
Under the opening, the ceiling revealed joints and rough surfaces that disappeared from the distant view. The arch felt less like a picture frame and more like a room that had misplaced most of its walls.
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| The opening of North Window framing the country beyond |
Looking outward through North Window reversed the scene. The surrounding country became the subject, and the arch became a dark border around it.
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| Double Arch, where two openings share the same mass of sandstone |
Double Arch formed differently from the side-cut openings nearby. Water entered from above and enlarged weak points downward, producing two openings that share the same body of rock. Standing beneath it made the structure easier to understand and the neck easier to tire.
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| The Colorado Plateau seen between sandstone walls in the Windows Section |
Between the walls, the Colorado Plateau spread beyond the Windows Section. A mesa is a broad, flat-topped highland with steep sides; a butte is the smaller remnant left after more erosion. The definitions were finally useful because the examples were no longer confined to a dictionary.
Wolfe Ranch and Delicate Arch Viewpoint
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| The surviving Wolfe Ranch cabin beside Salt Wash |
Wolfe Ranch shifted the scale from stone to human shelter. John Wesley Wolfe established the ranch near Salt Wash, and the surviving cabin records the practical limits of homesteading in a dry place. Nearby Ute petroglyphs predate the ranch and place the site within a much longer human history.
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| The Delicate Arch trailhead model and route display |
Our stop stayed with the trailhead and Delicate Arch Viewpoint. The full trail to the arch runs three miles round trip and climbs about 500 feet. The lower viewpoint instead offers a short walk and a distant view across the canyon. It is less intimate, but considerably kinder to a schedule already full of rocks.
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| An interpretive panel explains how Delicate Arch became Utah's best-known stone celebrity |
The trailhead display explained the route and Delicate Arch’s role as Utah’s most recognizable stone shape. The arch appears on a Utah license plate design, which is a demanding job for a piece of sandstone and still pays nothing.
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| Delicate Arch at the far left, seen across the canyon from the viewpoint |
From the viewpoint, Delicate Arch stood alone on a ridge at the far left. Rounded domes and eroded fins occupied the rest of the frame, showing the same processes at different stages.
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| A closer camera view of Delicate Arch from across the canyon |
A tighter camera view brought the arch closer without changing the canyon between us. The viewpoint was honest about the arrangement: good optics, no shortcut.
Utah Route 313 to Dead Horse Point
After Arches, we followed US-191 and Utah Route 313 toward Dead Horse Point. The byway climbs onto a mesa above the Colorado River and then divides between the state park and Canyonlands. We would use both branches. The road had designed an itinerary and was being unusually efficient about it.
Video: climbing Utah Route 313 toward Dead Horse Point, where the road leaves US-191 and gains the mesa.
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| Shehzadi beside the entrance sign at Dead Horse Point State Park |
At the park entrance, Shehzadi had reached the top of the climb. The overlook lies about 2,000 feet above a gooseneck in the Colorado River, a vertical difference large enough to turn a broad river into a thin green line.
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| The Colorado River bend below the rim at Dead Horse Point |
The Colorado River loops around a resistant bench of rock before continuing through the canyon. From above, the bend looks compact. The scale returns only when roads, vegetation and the water itself are compared against the walls.
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| An interpretive panel places the Colorado River, canyon walls and overlook in context |
An interpretive panel helped place the visible layers and the Colorado River’s course. It also made clear that the overlook was showing a working drainage system, not a static postcard.
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| Late sunlight crossing the canyon benches below Dead Horse Point |
Utah State Parks presents the place-name story as a legend. Cowboys once used the narrow neck of the point as a natural corral for wild horses. According to that account, some animals were left on the waterless mesa and died within sight of the Colorado River below. The legend is grim enough on its own. The water was visible; reaching it was another matter.
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| The Colorado River turning around a broad canyon bench below the overlook |
The Colorado River bend held the center of the view while the sun lowered. The canyon benches began losing detail from the bottom upward.
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| A wide view from the rim makes the Colorado River look much closer than it is |
A wide angle made the human scale almost disappear. The Colorado River was so far below that its movement was easier to infer than see.
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| Warm evening light reaching the Colorado River and lower canyon walls |
Warm light reached the lower walls and the Colorado River. Each band changed color at a different rate because each faced the sun at a different angle.
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| Sandstone at the rim above the deep Colorado River canyon |
The rim itself remained rough and immediate: broken sandstone, low shrubs and the drop beyond. The foreground kept the canyon from becoming an abstract map.
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| The Colorado River bend taking on the last orange light |
As the light softened, the gooseneck became more distinct against the orange walls. The Colorado River had spent millions of years cutting the bend. Sunset managed a respectable contribution in several minutes.
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| The final sunlight catching canyon cliffs beyond a juniper |
The final direct light touched the cliffs beyond a juniper. The lower canyon was already in shadow, dividing the view into illuminated walls and dark depth.
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| The sun reaching the canyon rim at Dead Horse Point |
The sun reached the rim. We sat in silence as the last light faded. Dead Horse Point had found the one reliable way to quiet a public viewpoint.
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| The Colorado River bend settling into blue evening light |
Blue evening light remained after the orange faded. The Colorado River bend was still visible, but the canyon had begun returning its details to the night.
Video: descending Utah Route 313 after sunset at Dead Horse Point and returning toward Moab.
We returned to Moab after dark. The road down Route 313 supplied the final chapter of the evening, mostly through headlights and the firm understanding that cliffs remain cliffs even when the sunset has clocked out.
Canyonlands Island in the Sky
The camera roll contributed one geographical prank before Canyonlands. Wilson Arch is beside US-191 south of Moab, roughly halfway toward Monticello. It was not on the northbound road to Island in the Sky. The photograph belongs to the same Moab stay, so it remains here with its coordinates returned to reality.
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| Wilson Arch beside US-191 south of Moab, a separate roadside stop from the Canyonlands route |
For Canyonlands, we drove north from Moab and returned to Utah Route 313. At the fork, the state-park road turned toward Dead Horse Point while the other branch continued into Island in the Sky.
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| The Canyonlands entrance sign on the road to Island in the Sky |
The Green and Colorado rivers divide Canyonlands into three major land districts: Island in the Sky, The Needles and The Maze. We visited Island in the Sky, the high mesa with a paved scenic road and overlooks along cliffs more than 1,000 feet above the surrounding terrain.
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| Shehzadi below the banded cliffs of Canyonlands |
Shehzadi moved between banded cliffs and open overlooks. The horizontal layers made the park’s erosion easy to read: resistant beds formed rims and benches, while softer beds retreated into slopes.
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| Mesa Arch framing the canyons below Island in the Sky |
Mesa Arch sat near the rim and framed the canyons below. It is a short walk from the road, but its placement makes the opening feel much larger. The arch borrows most of its drama from the drop immediately beyond it, a sound example of geological collaboration.
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| Layered canyon benches spreading below an Island in the Sky overlook |
The Island in the Sky mesa stayed high while the drainage network spread below. Canyons divided benches into smaller mesas and buttes, turning the definitions from the beginning of the post into visible anatomy.
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| Prickly pear cactus finding enough soil beside the trail |
A prickly pear beside the trail offered a smaller lesson in desert design. Water storage, shallow roots and defensive spines solve several problems at once. They also discourage casual touching, which is efficient public communication.
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| A sandy trail passing rounded sandstone domes |
Rounded domes and pale sandstone bordered the path. The heat remained direct, and shade arrived in fragments supplied by rock overhangs and juniper.
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| Shafer Canyon and the road dropping from the mesa rim |
Shafer Canyon opened below the rim, with switchbacks descending toward the lower benches. The road began as a route used by Indigenous people and later by ranchers and miners before becoming part of the modern backcountry network.
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| Shehzadi beneath the horizontal bands of Island in the Sky |
At a roadside stop, the cliff bands behind Shehzadi made the truck look briefly geological. She declined to become sediment and remained available for transportation.
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| Shafer Trail tracing a narrow bench below the mesa |
Shafer Trail wrapped around a narrow bench below the mesa. From above, its engineering looked tidy. At road level, the drop-offs would have offered a more detailed review.
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| Flat-topped mesas standing above the eroded canyon walls |
Flat-topped remnants stood above the lower canyons. A mesa becomes a butte as erosion narrows its summit, although no committee announces the moment of promotion or demotion.
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| A weathered juniper holding its ground above the canyon |
Juniper survived at the rim in shallow soil and steady exposure. Its twisted shape recorded wind and drought more clearly than any weather app.
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| A paved path threading through pale sandstone near an overlook |
The paved overlook paths kept the route accessible while leading through pale sandstone. Beyond the pavement, the country dropped away quickly and without guardrails supplied by nature.
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| Sandstone fins rising beside the walkway |
Fins beside the walkway repeated the Arches pattern at a different scale. Canyonlands had fewer openings in the photographed route, but no shortage of fractures waiting for future instructions.
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| Horizontal rock bands exposed above a long talus slope |
The exposed bands held more than 200 million years of geologic record. Rivers and runoff cut downward through those layers after uplift raised the Colorado Plateau, leaving cliffs where rock resisted and slopes where it did not.
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| Vertical cliff faces revealing stacked bands of rock |
Close views of the walls showed how sharply the resistant beds break. Talus collected below from pieces that had already lost the argument with gravity.
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| Pale caprock sitting above darker red sandstone |
Pale caprock protected darker layers beneath it. Once the cap breaks, the softer material retreats faster and the edge of the mesa moves backward. Geology does not hurry, but it is remarkably persistent.
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| The Green River bending among canyon benches far below the mesa |
The Green River appeared far below among the benches. Together, the Green and Colorado rivers do the large-scale cutting here, while storms and smaller channels extend the network into every side canyon.
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| An overhanging sandstone ledge beside the trail |
An overhanging ledge supplied temporary shade. In summer, even a narrow strip of shadow can develop a loyal following.
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| A sheer wall dropping to talus and lower benches |
The sheer wall below the rim exposed another full stack of layers. Loose material gathered at its base, waiting for water to move it farther downhill.
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| White Rim Road drawing a pale line across the lower bench |
White Rim Road traced the lower bench as a pale line. Its loops provided scale: a road wide enough for vehicles became a pencil mark in the canyon.
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| A trail cairn assembled from the park's layered sandstone |
A trail cairn brought the layers down to hand size. The stacked stones were useful for navigation and, unlike most roadside monuments, required no ribbon-cutting ceremony.
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| A sandstone outcrop above distant mesas and canyons |
Grand View Point opened across a maze of canyons and remnant mesas. The name was ambitious but difficult to dispute.
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| A wide panorama from Island in the Sky across the canyon country |
At Upheaval Dome, an older salt-dome explanation once competed with an impact origin. Geologic mapping, seismic evidence and shocked minerals now support a meteorite impact followed by collapse and erosion. The park kept the mystery for years; the rocks eventually submitted better paperwork.
The National Park Service identifies these southeastern Utah parks as ancestral homelands and sacred places associated with more than 30 Native nations. That broader statement is more accurate than reducing the region to three names or using artifacts we did not document as scenery. The canyons carry living cultural connections as well as ancient sites.
Sand Flats Recreation Area
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| Shehzadi on a graded Sand Flats road between sandstone walls |
Our final Moab drive took Shehzadi into Sand Flats Recreation Area, a high plain of slickrock domes, bowls and fins east of town. BLM and Grand County manage nearly 30 miles of jeep routes here, including highly technical named trails. Our route stayed on the graded roads visible in the photographs. Hell’s Revenge and Fins and Things existed nearby, but they were not promoted into our itinerary by wishful captioning.
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| Shehzadi's dashboard during the Moab stop |
The dashboard showed 8,742 miles. Compared with the 6,395-mile reading when we left home in Hyattsville at the beginning of Part 1, Shehzadi had covered 2,347 expedition miles.
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| Shehzadi at a gravel turnout above the Sand Flats road |
The first turnout overlooked the road and surrounding sandstone. The unpaved surface was firm and broad, with enough loose gravel to remind us that pavement had left the meeting.
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| The unpaved route narrowing between sandstone walls |
Farther in, the road narrowed between walls. Shehzadi’s width became more relevant than the distant view, which is a common effect of rock moving closer to the mirrors.
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| A graded road bending across the high plain of Sand Flats |
The graded track bent across the high plain. “Slickrock” is a general regional term for broad, exposed rock surfaces. Here it forms domes, bowls and fins, which is a practical description and a fairly ambitious road-design brief.
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| Shehzadi beneath a juniper on the Sand Flats road |
A juniper marked another canyon turn. The road remained manageable, but blind bends and rough patches kept the pace modest.
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| Shehzadi at a roadside stop among red sandstone |
We stopped beside red sandstone and let the truck cool. The photographs show a road-based outing rather than a technical obstacle course, which was entirely sufficient. Moab has no shortage of terrain willing to embarrass overconfidence.
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| A graded climb through the sandstone of Sand Flats |
A longer grade climbed through the rock. Shehzadi’s four-wheel-drive hardware was available, while restraint continued performing most of the useful work.
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| The road squeezing between tall red rock walls near Moab |
The route finished between tall walls before returning toward Moab. After arches, canyon rims and river bends, the narrow road brought the scale back to the truck’s hood and mirrors.
Moab turned the expedition into a vertical cross-section. Buried salt fractured the overlying rock at Arches, and water widened the breaks into fins and openings. The Colorado River curved below Dead Horse Point; the Colorado and Green rivers cut Canyonlands beneath Island in the Sky. Shehzadi linked paved park roads to Sand Flats dirt. This was our first sustained encounter with the Colorado Plateau, where erosion runs the design department.
Next Stop: Red Canyon, Kodachrome Basin and Kanab
Part 6 carries us from Moab to Kanab through the San Rafael Reef and Black Dragon Canyon, then into Red Canyon, Kodachrome Basin and Grosvenor Arch. Arches and canyon rims give way to I-70, Utah 12 and an unpaved Grand Staircase-Escalante detour. Shehzadi had finished her Moab geology course. The examination would be administered on dirt.
Reference route maps for our 9,000-mile USA and Mexico overland round trip: Map-1 and Map-2.
