Turret Arch

In the sun-scorched embrace of Arches National Park, where the desert weaves a tapestry of stone and sky, Turret Arch stands as a solitary sentinel, its rugged form a testament to nature’s sculptural prowess. Rising from the Windows Section, this singular sandstone arch evokes the silhouette of a medieval tower, its compact, sturdy span crowned with a blocky crest that seems to defy the erosive whims of time. Bathed in the molten gold of dawn or the fiery crimson of dusk, Turret Arch glows with hues of terracotta, ochre, and amber, its surface etched with the delicate tracery of wind and fleeting desert rains. The arch’s modest yet commanding presence frames a window to the vastness beyond, offering glimpses of distant mesas and a sky that stretches into eternity. Unlike its grander neighbors, Turret Arch exudes a quiet strength, its solitary grace a whispered ode to resilience in the heart of the desert.

A smoke fillled view of Turret Arch in 2025 during the North Rim Fires at the Grand Canyon.  Photo James L Rathbun
A smoke fillled view of Turret Arch in 2025 during the North Rim Fires at the Grand Canyon. Photo James L Rathbun

Set against a backdrop of jagged fins and scattered boulders, Turret Arch stands in close company with the North and South Window arches, forming a trio that feels like a sacred council of stone. Its weathered face, smoothed by eons, bears the marks of the desert’s patient artistry, inviting visitors to pause and listen to the silence that hums with the weight of geologic ages.

Geology and Formation of Turret Arch

Turret Arch is carved from the Entrada Sandstone, a formation deposited approximately 165 million years ago during the Jurassic period. Composed of fine quartz grains bound by calcium carbonate and iron oxides, this sandstone radiates the desert’s signature reds and oranges, its vibrant palette a gift of mineral oxidation. The arch’s creation is a chapter in a grand geologic narrative, shaped by deposition, uplift, and relentless erosion over millions of years.

In the Jurassic, vast dune fields blanketed the region, their sands compacting into the Entrada Sandstone. Around 70 million years ago, the uplift of the Colorado Plateau thrust these layers upward, exposing them to the elements. Beneath the surface, the Paradox Formation—a thick layer of salt laid down 300 million years ago—played a pivotal role. As the salt shifted and dissolved, it fractured the overlying sandstone, creating joints and fins. Water and wind, the desert’s master sculptors, exploited these weaknesses, eroding softer material to form thin sandstone fins. Turret Arch emerged as erosion widened a cavity within one such fin, eventually breaking through to create its distinctive opening. The arch’s compact, robust form and its namesake “turret” atop reflect variations in the sandstone’s resistance, where harder layers withstood erosion’s assault while softer ones yielded. This ongoing process of erosion continues to refine Turret Arch, a fleeting monument in the geologic saga of Arches National Park.

The Hike to Turret Arch and the Windows Arches

The South Window in Arches National Park does not seem to have as much traffic as the North Window.  Photo by James L Rathbun
The South Window in Arches National Park does not seem to have as much traffic as the North Window. Photo by James L Rathbun

The journey to Turret Arch and the nearby North and South Window arches is a captivating trek through the desert’s heart, accessible yet awe-inspiring. The trail begins at the Windows Section parking lot, approximately 9 miles from the entrance to Arches National Park. The Windows Loop Trail, a 1-mile round-trip hike, is rated easy to moderate, with a modest elevation gain of about 150 feet, making it welcoming for families and most hikers. The full loop, which includes Turret Arch and both Windows, takes 30-60 minutes, depending on pace and time spent marveling at the formations.

The trail, a blend of packed dirt, sand, and slickrock, winds through a starkly beautiful landscape of junipers, pinyon pines, and scattered sandstone boulders. As you approach, Turret Arch appears first, its sturdy, castle-like form standing slightly apart from the Windows, visible to the right of the trail. A short spur allows hikers to stand beneath its intimate span, where the arch’s solid frame contrasts with the delicate vistas it frames. Continuing along the main trail, the North and South Window arches emerge dramatically, their massive forms rising like twin portals against the horizon. The North Window’s broad, commanding span invites a closer scramble up slickrock to peer through its cavernous opening, while the South Window, slightly smaller, offers a serene frame for the desert beyond.

For a fuller experience, the primitive trail behind the arches completes the loop, offering quieter views and stunning perspectives of Turret Arch silhouetted against the Windows. This less-traveled path provides a panoramic appreciation of the Windows Section’s geologic splendor. The trail is exposed, with minimal shade, so hikers should bring water, sunscreen, and sturdy shoes, especially in the desert’s intense summer heat. Winter may bring icy patches, but the trail remains accessible year-round. Sunrise or sunset hikes are particularly enchanting, when the arches glow with ethereal light, casting long shadows across the desert floor. Interpretive signs along the path offer insights into the geology and ecology, enriching the journey to these iconic monuments. Together, Turret Arch and the Windows form a natural gallery, where the desert’s artistry invites wonder and reverence.

The Three Gossips

The Three Gossips located in Arches National Park, Utah. Photo by James L Rathbun
The Three Gossips located in Arches National Park, Utah. Photo by James L Rathbun

In the heart of Arches National Park, where the desert sun carves shadows into the rust-hued earth, the Three Gossips stand as silent sentinels of time, their towering forms whispering tales of ancient landscapes. These monolithic sandstone figures rise abruptly from the parched valley floor, their silhouettes evoking the image of three figures huddled in eternal conversation, their voices lost to the wind. Bathed in the golden glow of dawn or the fiery hues of sunset, their surfaces shimmer with a palette of ochre, crimson, and amber, as if the very spirit of the desert has been sculpted into their forms. The play of light and shadow accentuates their rugged contours, giving them an almost lifelike presence—stoic yet animated, as though caught mid-gossip, frozen in a moment of conspiratorial exchange.

Each spire, distinct yet unified, bears the marks of eons: smooth, wind-polished faces juxtaposed with jagged edges where the elements have gnawed away at their resolve. The tallest of the trio stretches skyward, its pinnacle sharp against the boundless blue, while its companions lean slightly, their forms softened by the relentless caress of wind and rare desert rains. Together, they form a natural cathedral, a place where the silence of the desert feels sacred, interrupted only by the occasional cry of a raven or the rustle of tumbleweeds skittering across the sands.

Geology and Formation of the Three Gossips

The Three Gossips stand proudly near Park Avenue, Arches National Park.  Photo by James L Rathbun
The Three Gossips stand proudly near Park Avenue, Arches National Park. Photo by James L Rathbun

The Three Gossips are a testament to the geologic artistry of the Colorado Plateau, sculpted from the Entrada Sandstone, a formation laid down approximately 165 million years ago during the Jurassic period. This sandstone, born from ancient desert dunes and intermittent shallow seas, is composed primarily of fine-grained quartz cemented by calcium carbonate and iron oxides, which lend the rock its vibrant red and orange tones. The monument’s creation is a story of deposition, uplift, and erosion—a slow dance of geologic forces spanning millions of years.

Initially, the Entrada Sandstone was deposited as vast dune fields in an arid environment, with grains of sand carried by wind and cemented over time into solid rock. Tectonic forces associated with the uplift of the Colorado Plateau, beginning around 70 million years ago, elevated these sedimentary layers, exposing them to the elements. Erosion, driven by wind, water, and temperature fluctuations, became the master sculptor. The Three Gossips owe their distinct forms to differential erosion, where softer, less resistant layers of sandstone were worn away faster than the more durable sections, leaving behind the towering spires we see today.

The monument’s location within Arches National Park, near the Courthouse Towers, places it in a landscape shaped by faulting and salt tectonics. Beneath the surface, a thick layer of Paradox Formation salt, deposited 300 million years ago, shifted and dissolved, causing the overlying rock to fracture and collapse. These fractures allowed water to seep in, further eroding the sandstone into isolated towers and fins. The Three Gossips, standing as erosional remnants, are part of this dynamic process, their shapes continually refined by the desert’s unrelenting forces.

Today, the Three Gossips remain a striking example of nature’s ability to craft beauty from endurance, their forms a fleeting moment in the geologic saga of Arches National Park, destined to evolve as the desert continues its patient work of creation and destruction.

The Three Gossips in the movies

The Three Gossips, a distinctive rock formation in Arches National Park’s Courthouse Towers area, has appeared in a few films, leveraging its striking silhouette for cinematic backdrops. Based on available information, here is a list of movies that feature or were filmed in the vicinity of the Three Gossips:

  • Indiana Jones and the Last Crusade (1989): The opening sequence, set in 1912, features young Indiana Jones (River Phoenix) in Arches National Park. The Three Gossips is visible from the main park road during scenes where the scout troop rides through the desert, near the Courthouse Towers and The Organ.
  • Thelma & Louise (1991): Several scenes were filmed in and around Arches National Park, including the Courthouse Towers area where the Three Gossips is located. A notable scene involves the protagonists locking a state trooper in his car’s trunk, with the Three Gossips and surrounding formations as a backdrop.

West Valley Jeep Road

Arches National Park is located in the south eastern corner of the state of Utah
Arches National Park is located in the south eastern corner of the state of Utah

West Valley Jeep Road, also known as West Valley 4×4 Road, offers a rugged and scenic off-road adventure in the northwestern backcountry of Arches National Park, connecting the Tower Arch 4×4 Road to Willow Springs Road. Spanning approximately 9.4 miles, this moderate trail is designed for high-clearance 4WD vehicles and experienced mountain bikers, with hiking possible but less common due to the trail’s length and exposure. The route traverses a stark desert landscape of sandy washes, sand dunes, and occasional rocky outcrops, offering sweeping views of sandstone fins, distant La Sal Mountains, and lesser-visited formations like the Eye of the Whale Arch. The trail is recommended for travel from north to south due to steep, sandy hills that are challenging to climb in the opposite direction. With an elevation change of about 45 feet (593 feet of climb and 638 feet of descent), the trail takes approximately 35-45 minutes by vehicle or 2-3 hours by bike, with hiking times varying based on pace.

The trail begins at the junction with Tower Arch 4×4 Road (accessible via Salt Valley Road from the park’s main entrance) and ends at Willow Springs Road, near its intersection with Highway 191 or further south at Balanced Rock. Key features include the Eye of the Whale Arch, accessible via a short detour, and the solitude of the park’s less-traveled backcountry. The trail’s technical sections, including deep sand and small rock ledges, require careful navigation, and conditions vary with weather, so checking with the Arches Visitor Center for road status is advised. Spring and fall are ideal seasons, as summer temperatures often exceed 100°F, and winter may bring snow or mud.

Trail Details

  • Length: 9.4 miles one-way.
  • Difficulty: Moderate for 4WD vehicles and mountain bikes; strenuous for hikers due to distance, exposure, and uneven terrain.
  • Elevation Change: 593 feet climb, 638 feet descent; altitude ranges from 4,775 to 5,083 feet.
  • Terrain: Sandy washes, sand dunes, rocky sections, and slickrock. High-clearance 4WD required; OHVs, ATVs, and UTVs are prohibited in the park.
  • Access: Start at the junction with Tower Arch 4×4 Road (38.701410, -109.580280) or access via Willow Springs Road from Highway 191. An Arches National Park entry fee ($30 per vehicle) is required, payable at the main entrance or online at recreation.gov. Timed entry reservations are required April 1–October 31, 2025, from 7 a.m. to 4 p.m.
  • Features: Access to Eye of the Whale Arch, views of sandstone formations, and a quiet backcountry experience. No dinosaur tracks are noted on this specific route, unlike Willow Springs Road.
  • Challenges: Steep sandy hills, deep sand, and rocky sections require technical driving or biking skills. No shade, limited cell coverage, and potential flash flooding in washes after rain. Pets are not allowed off roads, and motorcycles must be street-legal.
  • Amenities: No facilities on the trail. The closest are at the Willow Springs Road trailhead (porta-potties in UtahRaptor State Park) or Balanced Rock (picnic table, outhouses). Bring ample water and a detailed map (e.g., Trails Illustrated Moab North).

Trail Map

Hiking and Biking Notes

Hiking West Valley Jeep Road is uncommon due to its 9.4-mile length, lack of shade, and monotonous gravelly stretches, as noted by some trail users who found it dull for walking. For hikers, the trail is a long, exposed journey best suited for cooler months (March–May or September–November). The route follows the road, with firm footing on sand and slickrock but no dedicated path. Mountain bikers find the trail more rewarding, navigating sandy washes and rocky sections, though deep sand may require dismounting. Bikers should yield to vehicles and stay on designated roads to protect the fragile desert ecosystem, including cryptobiotic soil. A detour to the Eye of the Whale Arch, about 1.7 miles from the Tower Arch Road junction, adds a scenic highlight. Both hikers and bikers should carry ample water, sunscreen, and GPS navigation, as trail markers are minimal, and the route can be disorienting.

History and Significance

West Valley Jeep Road, like other backcountry routes in Arches National Park, has historical roots in the region’s early exploration and land use. While specific historical records for this road are sparse, its significance lies in its role as part of the park’s limited network of 4WD trails, offering access to remote areas rarely seen by casual visitors. The road traverses terrain shaped by geologic processes dating back 300 million years, when the Paradox Formation’s salt bed was deposited, later influencing the uplift and erosion that created the park’s iconic arches and fins. The Entrada Sandstone, visible along the trail, formed 165 million years ago from ancient dune fields, and the road’s path through sandy washes and slickrock reflects this geologic legacy.

Historically, the broader Moab region, including areas near West Valley Jeep Road, was inhabited by the Fremont and Ancestral Puebloan peoples until about 700 years ago, with evidence of their presence in nearby rock art and petroglyphs along routes like Potash Road. Spanish missionaries encountered Ute and Paiute tribes in 1775, and Mormon settlers attempted to establish the Elk Mountain Mission in 1855, abandoning it due to harsh conditions. Willow Springs Road, which West Valley Jeep Road connects to, was used by ranchers and early explorers, and its proximity to Native American migration routes adds cultural significance. The road’s integration into Arches National Park, established as a national monument in 1929 and a national park in 1971, reflects its role in providing access to the park’s geologic wonders, such as the Eye of the Whale Arch.

Today, West Valley Jeep Road is valued for its solitude and adventure, appealing to off-road enthusiasts and cyclists seeking to explore the park’s backcountry. Its designation as a National Park Service-managed route emphasizes responsible use to preserve the delicate desert ecosystem, with regulations prohibiting off-road travel and protecting features like cryptobiotic soil. The road’s connection to UtahRaptor State Park (formerly BLM land) and its proximity to dinosaur track sites on Willow Springs Road further enhance its significance as a gateway to the region’s paleontological and cultural heritage.

Potash Road

Potash Road, also known as Utah Scenic Byway 279 or the Lower Colorado River Scenic Byway, is a striking route that stretches approximately 17 miles along the Colorado River west of Moab, Utah, before transitioning into a dirt road that connects to the Shafer Trail in Canyonlands National Park. This road, running parallel to dramatic red rock cliffs and offering access to petroglyphs, arches, and dinosaur tracks, has a rich history tied to Native American use, industrial development, and modern recreation. Its proximity to the Shafer Trail makes it a critical segment of one of the most iconic backcountry driving routes in the American Southwest.

The deep blue potash evaporation pools capture from Google Earth
The deep blue potash evaporation pools capture from Google Earth

Native American and Early Use

Potash Road’s origins trace back to Native American pathways that followed the Colorado River through the deepening Wingate sandstone canyon. Indigenous peoples used these routes to access resources, hunt, and travel between seasonal locations. The corridor’s natural features, including the river and nearby cliffs, made it a vital passage for early inhabitants. Evidence of their presence persists in the form of petroglyphs, such as those visible along the road near the “Indian Writing” pullout, approximately 5 miles from Moab, where rock art panels adorn the cliffside.

Ranching and Early Development

In the early 20th century, the route that would become Potash Road was used by Mormon pioneer settlers and ranchers. While the nearby Shafer Trail was specifically improved by John “Sog” Shafer in 1917 to move cattle between summer pastures on the mesa top and winter grounds in the canyon, Potash Road served as a complementary route along the Colorado River, facilitating access to grazing areas and water sources. The road remained a rudimentary track during this period, suitable for livestock and limited vehicular traffic, with its path constrained by the river and towering sandstone cliffs.

Industrial Era and the Potash Mining Boom

The mid-20th century marked a significant transformation for Potash Road with the rise of potash mining in the Moab area. The road’s modern name derives from the Moab Salt Company (now Intrepid Potash, Inc.), located at the end of the paved section, approximately 17 miles from U.S. Highway 191. Established in the early 1960s, the potash mining operation extracted potassium chloride from deep underground deposits, using water from the Colorado River to dissolve the mineral, which was then pumped to vibrant blue evaporation ponds visible along the road. These man-made, rubber-lined ponds, dyed blue to speed evaporation, became a striking feature of the landscape, visible even from space.

To support the mining industry, the Atomic Energy Commission and mining companies improved Potash Road in the 1950s and early 1960s, paving the initial 15–17 miles from U.S. 191 to the potash plant. Beyond this point, the road transitions to a dirt track, historically used to transport uranium ore from mines in the Triassic Chinle Formation to processing facilities in Moab. This dirt section, which connects to the Shafer Trail, was widened and stabilized to accommodate heavy trucks, following the path of a natural rockfall that buried parts of the cliff-forming Wingate Sandstone. The construction of a single-track railway in 1964, paralleling the final six miles of the paved road and extending through Bootlegger Canyon to Moab, further supported the transport of potash and salt, reducing reliance on the road for industrial haulage.

Transition to a Scenic and Recreational Route

With the establishment of Canyonlands National Park in 1964, the region’s focus shifted from industrial activity to preservation and recreation. The dirt section of Potash Road, extending from the potash plant to the Shafer Trail, became integrated into the park’s backcountry road network. The National Park Service maintained the route for recreational use, requiring high-clearance 4WD vehicles due to its rugged terrain, including ruts, sand, and slickrock sections. The road’s connection to the Shafer Trail, which ascends 1,500 feet through dramatic switchbacks to the Island in the Sky district, made it a popular route for adventurers seeking to experience Canyonlands’ rugged beauty.

Potash Road’s paved section, designated as Utah Scenic Byway 279, became a draw for its accessibility and scenic attractions. Notable sites include “Wall Street,” a cliffside area popular with rock climbers, and the trailheads for Corona Arch and Jug Handle Arch, both located along the road. The Corona Arch trail, approximately 1.2 miles each way, leads to a 140-foot-wide arch, while Jug Handle Arch is visible from the road, offering easy access for photographers. Dinosaur footprints, reachable by a short scramble near the Poison Spider Trail, and petroglyphs along the river add historical and cultural depth to the drive. The road also passes by the Gooseneck Overlook, a remote viewpoint showcasing the Colorado River’s meanders, and Thelma and Louise Point, famous for its role in the 1991 film’s final scene, often mistaken for the Grand Canyon.

Modern-Day Significance

Today, Potash Road is a multifaceted route, blending paved accessibility with rugged backcountry adventure. The paved section is suitable for most vehicles, offering a scenic drive along the Colorado River with opportunities to stop at campsites, petroglyphs, and trailheads. The dirt section, connecting to the Shafer Trail, requires a high-clearance 4WD vehicle and is part of a 19-mile off-road route that enters Canyonlands National Park, where a fee is required. The road is prone to closure during wet or snowy conditions, as it becomes slippery and impassable, necessitating careful planning and checks with the National Park Service for current conditions.

The road’s recreational popularity has grown, attracting drivers, cyclists, and hikers. It is part of a larger loop from Moab to Canyonlands via Potash Road and the Shafer Trail, returning via U.S. 191 and SR-313, totaling approximately 66 miles. The route is celebrated for its stunning views of red rock formations, the Colorado River, and the dramatic Shafer switchbacks, though the narrow, steep sections demand caution, especially for those wary of heights. The road’s historical significance, from Native American trails to industrial transport and modern tourism, makes it a compelling journey through time and terrain.

Conclusion

Potash Road, from its origins as a Native American pathway to its role in the potash and uranium industries, has evolved into one of Utah’s most scenic and adventurous routes. Its paved section offers accessible beauty, while its dirt extension into the Shafer Trail provides a thrilling backcountry experience within Canyonlands National Park. With cultural landmarks like petroglyphs and natural wonders like Corona Arch, Potash Road remains a vital link in the region’s history and a must-visit for those exploring the Moab area’s rugged landscapes.

White Rim Trail

The White Rim Trail is Canyonlands National Park is a 100 mile back country 4×4 trail that follows an strata of white lime stone along the edge of Island in the Sky mesa Located in Canyonlands National Park, Utah.  Back country permits are required for this trail, and although it can easily be taken in one day, the wise traveler takes their time and runs the route in several days and nights.  There are several camp grounds offering star gazing opportunities, and the grand vistas and long light in the early morning and late afternoon will inspire the Ansel Adams within you.

Mesa Light taken from the White Rim Trail and Lathrop Canyon Road. Photograph by James L Rathbun
Mesa Light taken from the White Rim Trail and Lathrop Canyon Road. Photograph by James L Rathbun

The trailhead is reached by leaving the Islands in the Sky Mesa, using the steep and twisty Shafer Trail.  The Shafer Trail is a back county route that takes you back to Moab, UT and a fun way out at the end of your trip.  The Shafer trail drops quickly and about 700 feet using 6 switch backs.  The Shafer Trail and White Rim Trail are well maintained and not very narrow, but the elevation and views give the feeling the route is dangerous.

Sunset along the White Rim Trail in Canyonlands NP, Utah Photograph by James L Rathbun
Sunset along the White Rim Trail in Canyonlands NP, Utah Photograph by James L Rathbun

Once down on the bottom, the well marked Shafer Trail continues on, while the White Rim Trail branches right and to the south.  All along the backcountry dirt road there are numerous spur trails, vistas, and points of interest give you much to explore including Lathrop Canyon, Musselman Arch, Washer Woman Arch and the Monster Tower.  The entire route is easy to follow, well maintained, well traveled and pure joy to run.

The trail winds along a layer of erroded light colored sandstone called the White Rim which undulates around several smaller side canyons which lead down the the Colorado River.  

Available Campsites

There are several small primitive campsites throughout the route.

  • Shafer – Mile 7 – 1 site
  • Airport – Mile 19 – 4 sites
  • Gooseberry – Mile 30 – 2 sites
  • White Crack – Mile 39 – 1 site
  • Murphy Hogback – Mile 45 – 3 sites
  • Candlestick – Mile 55 – 1 sites
  • Potato Bottom – Mile 66 – 3 sites
  • Hardscrabble Bottom – Mile 70 – 2 sites
  • Labyrinth – Mile 72 – 2 sites
  • Taylor – Mile 77 – 1 site

White Rim Trail

The White Rim Trail is a renowned 100-mile loop through Canyonlands National Park’s Island in the Sky district, offering a bucket-list adventure for overlanders, mountain bikers, and 4×4 enthusiasts. This rugged, high-clearance 4×4 route circumnavigates the Island in the Sky mesa, winding along the “white rim” ledge between the mesa top and the Green and Colorado Rivers below. The trail showcases breathtaking vistas of red rock canyons, towering buttes (like Airport Tower, Monster Tower, and Junction Butte), and the rivers’ confluence, rivaling views from the Grand Canyon’s South Rim. Key highlights include Gooseneck Overlook, Musselman Arch, White Crack (with views of the Maze and Needles districts), and Murphy Hogback, which offers 360-degree panoramas.

The trail features a mix of wide dirt roads, sandy patches, and technical jeep trails with some cliff exposure, particularly at Shafer Trail, Lathrop Canyon Road, Murphy Hogback, Hardscrabble Hill, and Mineral Bottom switchbacks. It’s moderately difficult for vehicles and challenging for mountain bikes, with an elevation gain of approximately 9,160 feet. The route can be driven clockwise (starting at Shafer Trail) or counterclockwise (starting at Mineral Bottom Road), typically taking 2-3 days to complete, though hardcore cyclists may attempt it in one day. Permits are required for both day-use and overnight trips, with 20 designated campsites across 10 camping areas, including Airport Campground. No potable water is available, and high water on the Green River (May-June) can flood western sections, making a full loop impossible. The best seasons are spring (March-May) and fall (September-November) due to milder temperatures and more predictable weather, as summer is extremely hot and winter may bring closures.

Trail Map

White Rim Trail Campsites

Canyonlands National Park is located in the south eastern corner of the state of Utah

Airport Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Located in the heart of Canyonlands National Park’s Island in…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Gooseberry Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Gooseberry Campground is a remote backcountry camping area located along…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Hardscrabble Bottom Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Hardscrabble Bottom Campground is a remote backcountry camping area along…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Murphy Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Murphy Campground is a remote backcountry camping area along the…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Potato Bottom Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Potato Bottom Campground is a remote backcountry camping area along…
Canyonlands National Park is located in the south eastern corner of the state of Utah

White Crack Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah White Crack Campground is a remote backcountry camping area in…