Tag: Coconino County

Horseshoe Bend

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Horseshoe Bend is a stunning geological formation located on the Colorado River, just south of Page, Arizona. This iconic meander, carved over millennia by the river’s persistent flow, forms a dramatic, U-shaped loop that encircles a towering rock outcrop.

Horseshoe Bend is a stunning geological formation located on the Colorado River, just south of Page, Arizona. This iconic meander, carved over millennia by the river’s persistent flow, forms a dramatic, U-shaped loop that encircles a towering rock outcrop. Situated within the Glen Canyon National Recreation Area, it offers breathtaking views from a steep, 1,000-foot (300-meter) cliff overlooking the emerald-green waters below, framed by rugged, reddish desert cliffs. The overlook is accessible via a short, 1.5-mile round-trip hike from a parking area off U.S. Route 89, making it a popular destination for visitors to northern Arizona. The site is renowned for its striking beauty, especially at sunrise or sunset when the light enhances the vibrant colors of the canyon and river. Horseshoe Bend attracts photographers, nature enthusiasts, and tourists, drawing over two million visitors annually, though its popularity has led to increased management efforts to protect the fragile desert environment. Always stay on designated trails and respect safety barriers due to the sheer drop.

Horseshoe Bend, located near Page, Arizona, is a stunning example of a geological phenomenon known as a meander, where a river curves dramatically, creating a near-circular loop that resembles the shape of a horseshoe. This iconic feature along the Colorado River showcases the intricate interplay of geological processes, water flow, and time. Below is a detailed description of how rivers form bends like Horseshoe Bend, exploring the processes, conditions, and forces involved.

What is a Meander?

A meander is a sinuous, looping bend in a river’s course, often formed in relatively flat or gently sloping landscapes. Unlike straight river channels, which are rare in nature, meanders develop as a river seeks the path of least resistance across a landscape, eroding and depositing sediment in a dynamic process. Horseshoe Bend is an entrenched meander, meaning it is deeply incised into the bedrock, creating a dramatic, steep-walled canyon around the river’s curve.

Formation of Meanders

The formation of river bends like Horseshoe Bend involves several key processes, driven by the interaction of water flow, sediment transport, and the geological characteristics of the landscape.

Initial River Flow and Instability

Rivers naturally develop small irregularities in their channels due to variations in the terrain, such as slight depressions, obstacles like rocks or vegetation, or differences in soil and rock resistance. These irregularities disrupt the river’s flow, causing water to move faster on one side of the channel than the other. This differential flow sets the stage for meander development:

  • Faster Flow on the Outside: Water moves more quickly along the outer edge of a developing bend due to centrifugal force, much like a car taking a curve. This faster flow erodes the outer bank, carving it away.
  • Slower Flow on the Inside: On the inner side of the bend, water slows down, allowing sediment to settle and form a depositional feature called a point bar.

This erosion on the outer bank and deposition on the inner bank amplify the bend over time, causing the river to curve more dramatically.

Feedback Loop of Erosion and Deposition

As the river continues to flow, the meander grows through a self-reinforcing feedback loop:

  • The faster-moving water on the outer bank erodes material, deepening and widening the curve.
  • The eroded sediment is carried downstream and deposited on the inner bank, where the flow is slower, building up the point bar.
  • This process causes the meander to migrate laterally across the floodplain, with the bend becoming more pronounced.

Role of Sediment and Flow Dynamics

The type and amount of sediment a river carries influence meander formation. Rivers with a high sediment load, like the Colorado River, can deposit significant material on point bars, which helps stabilize the inner curve. Meanwhile, the river’s velocity and volume determine its erosive power. Seasonal variations, such as snowmelt or heavy rains, can increase the river’s flow, accelerating erosion and reshaping the meander.

Entrenched Meanders and Horseshoe Bend

The Colorado River Gorge cuts into the bedrock at the Horseshow Bend
The Colorado River Gorge cuts into the bedrock at the Horseshow Bend

Horseshoe Bend is not a typical meander found on a flat floodplain but an entrenched meander, which forms when a river cuts deeply into bedrock. This process is particularly pronounced in the Colorado Plateau, where Horseshoe Bend is located. Here’s how it happens:

Uplift of the Colorado Plateau

The Colorado Plateau, a region of relatively flat-lying sedimentary rocks, has been uplifted over millions of years due to tectonic forces. As the plateau rose, the Colorado River, which was already flowing across the region, began to incise downward into the bedrock to maintain its course. This process is called downcutting.

Preservation of Meander Shape

As the river cut downward, it retained the sinuous meander pattern it had developed on a flatter landscape millions of years ago. Instead of eroding laterally across a floodplain (as meanders typically do), the river eroded vertically into the resistant sandstone of the Navajo Formation, creating steep canyon walls. This results in an entrenched meander, where the river’s looping path is preserved but now confined within a deep, narrow canyon.

Geological Context of Horseshoe Bend

At Horseshoe Bend, the Colorado River has carved a canyon approximately 1,000 feet (300 meters) deep into the Glen Canyon Group, primarily composed of Navajo Sandstone. The river’s path forms a near-perfect U-shape, with the water flowing around a central rock promontory. The steep, vertical walls of the canyon highlight the river’s erosive power and the resistance of the surrounding rock, which prevents significant lateral migration of the meander.

Specific Features of Horseshoe Bend

Horseshoe Bend’s dramatic appearance is the result of several unique factors:

  • Geological Setting: The Navajo Sandstone, a thick layer of cross-bedded sandstone formed from ancient desert dunes, is highly resistant to erosion. This resistance allows the canyon walls to remain steep and well-defined, enhancing the visual impact of the bend.
  • River Dynamics: The Colorado River carries a significant sediment load, including sand and gravel, which aids in both erosion (by scouring the bedrock) and deposition (building point bars). The river’s high flow during spring snowmelt or after heavy rains increases its erosive capacity.
  • Time Scale: The formation of Horseshoe Bend has taken millions of years. The Colorado River began incising into the Colorado Plateau around 5–6 million years ago, following regional uplift. The meander itself likely began forming much earlier, when the river flowed across a flatter landscape, and was later entrenched as the plateau rose.

Ongoing Evolution of Meanders

Meanders like Horseshoe Bend are not static; they continue to evolve over time:

  • Meander Migration: Although entrenched meanders are constrained by bedrock, slow lateral erosion can still occur, causing the bend to shift slightly over geological time.
  • Neck Cutoff: In some cases, a meander can become so tight that the river erodes through the narrow neck of land separating two parts of the loop, forming a cutoff and abandoning the meander as an oxbow lake. However, at Horseshoe Bend, the resistant bedrock makes a cutoff unlikely in the near future.
  • Canyon Deepening: The Colorado River continues to downcut, deepening the canyon and making the walls of Horseshoe Bend even more dramatic over time.

Environmental and Human Factors

  • Climate and Water Flow: The arid climate of northern Arizona limits vegetation, which reduces bank stabilization and allows the river to erode the bedrock more freely. Human interventions, such as the construction of Glen Canyon Dam upstream, have altered the Colorado River’s flow and sediment transport, potentially affecting the rate of erosion at Horseshoe Bend.
  • Tourism and Preservation: Horseshoe Bend is a popular tourist destination, attracting millions of visitors annually. The overlook, perched 4,200 feet above sea level, offers a breathtaking view of the 270-degree river bend below. Efforts to manage tourism, such as designated trails and parking areas, help protect the fragile desert environment and prevent erosion of the canyon rim.

Why Horseshoe Bend is Unique

Horseshoe Bend stands out due to its combination of geological, hydrological, and aesthetic factors:

  • Scale and Symmetry: The near-perfect U-shape and the sheer scale of the canyon (1,000 feet deep and 0.6 miles wide at the bend) make it visually striking.
  • Contrast: The emerald-green waters of the Colorado River contrast vividly with the red and orange hues of the Navajo Sandstone, creating a photogenic landscape.
  • Geological Story: Horseshoe Bend tells a story of millions of years of uplift, erosion, and river dynamics, offering a window into the geological history of the Colorado Plateau.

Conclusion

The formation of river bends like Horseshoe Bend is a testament to the power of water, time, and geological processes. Starting as subtle curves in a river’s path, meanders grow through the interplay of erosion and deposition, amplified by the river’s flow and the landscape’s characteristics. At Horseshoe Bend, the Colorado River’s entrenched meander, carved into resistant Navajo Sandstone, creates a dramatic and iconic feature. This natural wonder continues to evolve, shaped by the relentless flow of the river and the geological forces of the Colorado Plateau, captivating visitors with its beauty and offering geologists a striking example of the Earth’s dynamic processes.

Lees Ferry Colorado River Crossing

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Lees Ferry, a remote site along the Colorado River in northern Arizona, holds a pivotal place in American history as a vital crossing point, a gateway to exploration, and a launchpad for modern river running. Situated at the confluence of the Paria and Colorado Rivers, just downstream from Glen Canyon and upstream from the Grand Canyon, Lees Ferry has served as a geographic and cultural hinge for centuries, bridging Native American trails, Mormon settlement, and modern adventure.

Historic photograph of ferryboat at Lees Ferry. The boat is relatively small. Five people and two horses or mules are on board. The ferry is guided by wires spanning the river. Historic photograph of ferryboat at Lees Ferry. John D. Lee established the first ferry at the confluence of the Colorado and Paria rivers in the 1870s. Ferries operated there until Navajo Bridge opened in 1929.
Historic photograph of ferryboat at Lees Ferry. The boat is relatively small. Five people and two horses or mules are on board. The ferry is guided by wires spanning the river. Historic photograph of ferryboat at Lees Ferry. John D. Lee established the first ferry at the confluence of the Colorado and Paria rivers in the 1870s. Ferries operated there until Navajo Bridge opened in 1929.

Early History and Native American Presence

Long before European settlers arrived, the area around Lees Ferry was a crossing point for Native American tribes, including the Ancestral Puebloans, Navajo, and Paiute. The site’s relatively calm waters and accessible riverbanks made it a natural ford for foot traffic and trade routes across the rugged Colorado Plateau. Archaeological evidence suggests human activity in the region dating back thousands of years, with petroglyphs and artifacts attesting to its significance.

The Colorado River, however, was a formidable barrier, with its steep canyons and turbulent rapids. Lees Ferry stood out as one of the few locations where the river could be crossed safely, earning it a place in the region’s cultural and economic landscape.

John D. Lee and the Mormon Era

John D Lee
John D Lee

Lees Ferry derives its name from John Doyle Lee, a prominent and controversial figure in the history of the Church of Jesus Christ of Latter-day Saints (LDS Church). Born in 1812, Lee was a devout Mormon pioneer who played a significant role in the church’s westward expansion. In 1871, following his excommunication for his involvement in the 1857 Mountain Meadows Massacre, Lee was sent by church leader Brigham Young to establish a ferry service at the site to facilitate Mormon settlement in Arizona.

Lee arrived with two of his wives, Emma and Ann, and several children, building a homestead known as Lonely Dell near the confluence of the Paria and Colorado Rivers. In 1872, he constructed a rudimentary ferry—a flatboat guided by ropes—capable of carrying wagons, livestock, and people across the river. The ferry became a critical link on the “Honeymoon Trail,” a route used by Mormon couples traveling from Arizona settlements to the temple in St. George, Utah, for marriage ceremonies. Lee operated the ferry until his arrest in 1874 for his role in the Mountain Meadows Massacre. He was executed in 1877, but his wife Emma continued running the ferry until 1879.

The ferry operation passed through several hands, including the LDS Church and private operators, until 1928, when it was rendered obsolete by the completion of the Navajo Bridge, located a few miles downstream. The bridge, opened in 1929, provided a more reliable crossing, marking the end of the ferry’s practical necessity.

Exploration and Scientific Significance

Lees Ferry’s strategic location made it a key staging point for early exploration of the Colorado River and the Grand Canyon. In 1869, John Wesley Powell, a one-armed Civil War veteran and geologist, launched his historic expedition down the Green and Colorado Rivers from Green River, Wyoming, passing through Lees Ferry en route to the Grand Canyon. Powell’s 1871–1872 expedition again used the site as a critical resupply point, cementing its role in the mapping and scientific study of the American Southwest.

First camp of the John Wesley Powell expedition, in the willows, Green River, Wyoming, 1871. - E. 0. Beaman - War Department. Office of the Chief of Engineers. Powell Survey. (1869 - ca. 1874)
First camp of the John Wesley Powell expedition, in the willows, Green River, Wyoming, 1871. – E. 0. Beaman – War Department. Office of the Chief of Engineers. Powell Survey. (1869 – ca. 1874)

The U.S. Geological Survey later designated Lees Ferry as the official division point between the Upper and Lower Colorado River Basins, a demarcation still used in water management today. The site’s consistent flow and accessibility made it ideal for gauging stations, which have monitored the river’s flow since the early 20th century, providing critical data for dam construction and water allocation in the arid West.

The Rise of River Running

In the 20th century, Lees Ferry transformed into the primary launch point for recreational and commercial river trips through the Grand Canyon. Its gentle waters and proximity to Marble Canyon make it an ideal starting point for navigating the Grand Canyon’s rapids. The site gained fame in the 1920s during the ill-fated honeymoon journey of Glen and Bessie Hyde, who launched their homemade scow from Lees Ferry in 1928, only to vanish downstream, leaving behind one of the canyon’s enduring mysteries.

By the mid-20th century, river running grew in popularity, spurred by figures like Norman Nevills, who pioneered commercial rafting trips, and Georgie Clark, who became a legendary river guide. Today, Lees Ferry is the starting point for thousands of annual river trips, ranging from half-day floats to multi-week expeditions through the Grand Canyon. The National Park Service tightly regulates these trips, with permits highly sought after due to the area’s scenic beauty and challenging rapids.

Lees Ferry Today

Now part of the Glen Canyon National Recreation Area, Lees Ferry is a designated historic site, with remnants of its past preserved for visitors. Lonely Dell, the original homestead, includes restored buildings, an orchard, and a small cemetery, offering a glimpse into the harsh life of early settlers. The ferry site itself features a boat launch, camping facilities, and interpretive displays about its history.

Lees Ferry also attracts anglers, drawn to its world-class trout fishery below Glen Canyon Dam, established after the dam’s completion in 1963 altered the river’s ecology. The clear, cold waters released from the dam create ideal conditions for rainbow trout, making the stretch between the dam and Lees Ferry a popular destination.

A Legacy of Connection

Lees Ferry’s significance lies in its role as a crossroads—geographic, cultural, and historical. From Native American trails to Mormon pioneers, from Powell’s daring expeditions to modern adventurers, the site has witnessed the unfolding of the American West. Its tranquil setting belies the challenges faced by those who crossed its waters or braved the canyons beyond. Today, as river runners launch from its shores and historians reflect on its past, Lees Ferry remains a testament to human resilience and the enduring allure of the Colorado River.

Upper Antelope Canyon

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Located just outside of Page, Arizona Upper Antelope Canyon is arguably the best known slot canyon on the planet, yet few people will know its name outside of desert enthusiasts.  For those unaware of these structures, slot canyons are extremely narrow canyons, carved by water, which are typically just a few feet wide, but may be just a few inches.  The typically arid dessert can instantly turn into raging torrent of water in just a few minutes with just a few inches of water.  This water picks up speed, and debris such as sand, which scours the landscape including rock.  Antelope Canyon is found on Navajo Tribal land, and access to the canyon is only allowed with a Navajo Guide.

Molten Wave - Located in Antelope Canyon near Page, Arizona Antelope Canyon is the best known slot canyon.
Molten Wave – Located in Antelope Canyon near Page, Arizona Antelope Canyon is the best known slot canyon.
Parallelism – The smooth canyon walls of Antelop Canyon offer amazing photographic images.

Antelope Canyon is actually two separate slot canyons located a short distance from each other on either side of US 98.  Upper Antelope Canyon is know as Tse’ bighanilini, which in Navajo means “the place where water runs through rocks.”  Travel to the Canyon is done via Navajo run transport and you are allowed about 2 hours for your visit.  The site is at about 4,000 feet elevation and the canyon walls rise 120 feet above a stream bed.

I would like to thank the LeChee Chapter of the Navajo Nation for keeping this location sacred and available to us.

James Rathbun, Destination4x4.com

Access into the upper canyon is simply a walking into a canyon.  The trail is flat and sandy and very easy to manage.  Upon entrance into the Upper Antelope Canyon you are immediately struck by the texture and color of this place.  Just inside the entrance, is a small chamber which seems to great you, and the pink and orange glow of the light bouncing off the walls force your eyes up.  The geography is such, that the narrow opening high above you lets in a small fraction of the available light, and that light bounces down towards the bottom of the canyon.

Relatively short, Upper Antelope Canyon may be traversed in just 5 minutes.  However, this is simply a waste of your time if you just rush through.  The only complaint of the canyon, are the other visitors.  As a photographer, I have many photographs ruined by people turning a corner and walking into my frame while I was making an exposure.  This does not mean they were rude or anything but patient, but rather an unfortunate side effect of composing photographs with long exposure times in a 18 inch wide slot Canyon.

French Curve - Upper Antelope Canyon
French Curve – Upper Antelope Canyon

As with all beautiful things, we must share this location and Antelope Canyon is a must stop location every time I visit the area.  There is a hidden danger, in that the very forces which sculpt a slot canyon are still very much in play and every few years a new story will appear about someone being killed in a slot canyon due to a sudden flash flood.

I would like to thank the LeChee Chapter of the Navajo Nation for keeping this location sacred and available to us.

Upper Antelope Canyon Map

John Doyle Lee

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John D Lee
John D Lee

John Doyle Lee is best known for establishing and operating Lees Ferry on the Colorado River in northern Arizona in 1871, under Brigham Young’s direction, to facilitate Mormon settlement in Arizona. The ferry, located at the confluence of the Paria and Colorado Rivers, became a vital crossing point for pioneers, including those traveling the “Honeymoon Trail” to the St. George Temple.

Early Life and Mormon Conversion

John Doyle Lee was born on September 6, 1812, in Kaskaskia, Illinois Territory. His early life was marked by hardship; his mother, Elizabeth, died when he was young, and his father, Ralph Lee, struggled with alcoholism. Lee was raised by his grandfather and later his uncle’s family. At age 20, he began working on steamboats and in business, eventually marrying Agatha Ann Woolsey in 1833. In 1838, at age 25, Lee joined the Church of Jesus Christ of Latter-day Saints (LDS Church), profoundly shaping his life. He became a dedicated member, serving as a missionary in Illinois, Ohio, Kentucky, and Tennessee, and a guard for Mormon prophet Joseph Smith. Lee embraced the LDS doctrine of plural marriage, ultimately marrying 19 wives and fathering 56 children, though 11 wives later left him.

Role in the Mormon Movement

Lee was a prominent figure in the early LDS Church, serving as an official scribe for the Council of Fifty, a group guiding the church’s westward expansion. After Joseph Smith’s murder in 1844, Lee followed Brigham Young to Utah, where he became a successful farmer and rancher. In 1856, he was appointed a U.S. Indian Agent in Iron County, Utah, tasked with aiding Native Americans in establishing farms. He also served in the Utah Territorial Legislature in 1858. Lee’s involvement with the secretive Mormon militia, the Danites, and his role in defending Mormon interests during conflicts in Missouri further cemented his status within the church.

The Mountain Meadows Massacre

Lee’s legacy is indelibly tied to the Mountain Meadows Massacre of September 1857, a tragic event in southern Utah. As a leader in the Iron County militia and a U.S. Indian Agent, Lee was implicated in the attack on the Baker-Fancher emigrant party, a group of about 120 men, women, and children traveling from Arkansas to California. Tensions between Mormons and non-Mormons were high, fueled by fears of federal intervention and perceived hostility from the emigrants. Lee, along with other Mormon militia members and Paiute allies, orchestrated a siege. On the third day, Lee approached the emigrants under a white flag, convincing them to surrender their weapons for safe passage. Instead, the militia and Paiutes killed approximately 120 emigrants, sparing only 17 small children. Lee later claimed he acted under orders from militia leaders and was a reluctant participant, asserting that Brigham Young had no prior knowledge of the event. However, he initially blamed the Paiutes to deflect responsibility.

Establishment of Lees Ferry

By the late 1860s, federal pressure to investigate the massacre intensified, and in October 1870, Brigham Young excommunicated Lee, making him the sole scapegoat among over 50 participants. In 1871, seeking to evade arrest, Lee was sent by the LDS Church to establish a ferry crossing on the Colorado River in northern Arizona. Accompanied by two of his wives, including Emma Batchelor Lee, he settled at the confluence of the Colorado and Paria Rivers, naming the area “Lonely Dell” due to its isolation. On January 11, 1873, Lee launched the ferry service, which became a vital link for Mormon settlers moving between Utah and Arizona. The ferry, known as Lees Ferry, facilitated thousands of crossings, supported by the nearby Lonely Dell Ranch, where Lee and his family built cabins, cleared fields, and developed irrigation systems. Emma played a crucial role, managing operations and offering hospitality to travelers. The site’s unique geography made it the only accessible crossing point for over 260 miles, cementing its historical significance.

Historic photograph of ferryboat at Lees Ferry. The boat is relatively small. Five people and two horses or mules are on board. The ferry is guided by wires spanning the river. Historic photograph of ferryboat at Lees Ferry. John D. Lee established the first ferry at the confluence of the Colorado and Paria rivers in the 1870s. Ferries operated there until Navajo Bridge opened in 1929.
Historic photograph of ferryboat at Lees Ferry. The boat is relatively small. Five people and two horses or mules are on board. The ferry is guided by wires spanning the river. Historic photograph of ferryboat at Lees Ferry. John D. Lee established the first ferry at the confluence of the Colorado and Paria rivers in the 1870s. Ferries operated there until Navajo Bridge opened in 1929.

Arrest, Trial, and Execution

Despite his efforts to remain hidden, Lee was arrested in November 1874. His first trial in 1875 ended in a hung jury, as the prosecution tried to implicate Brigham Young and the Mormon hierarchy. In a second trial in 1876, the prosecution focused solely on Lee’s role, leading to his conviction for first-degree murder. Lee maintained he was a scapegoat, used by church leaders to deflect blame. On March 23, 1877, he was taken to the Mountain Meadows Massacre site and executed by firing squad. His final words expressed resignation and faith: “I feel as calm as a summer morn, and I have done nothing intentionally wrong. My conscience is clear before God and man.” He also criticized Brigham Young, stating, “I have been sacrificed in a cowardly, dastardly manner.” Lee’s body was buried in Panguitch, Utah.

Legacy and Posthumous Reinstatement

Lees Ferry continued operating after Lee’s death, with Emma running it until 1879, when the LDS Church purchased it for $3,000 and transferred operations to Warren Marshall Johnson. The ferry remained active until 1928, when a bridge replaced it. Today, Lees Ferry is a historic site within the Glen Canyon National Recreation Area, known for fishing and as the starting point for Grand Canyon rafting trips. The Lonely Dell Ranch is listed on the National Register of Historic Places. In April 1961, the LDS Church posthumously reinstated Lee’s membership, reflecting ongoing debates about his role as a scapegoat. His numerous descendants include notable figures like former Solicitor General Rex E. Lee and Senators Mike Lee, Gordon H. Smith, Mark Udall, and Tom Udall.

Conclusion

John Doyle Lee’s life encapsulates the complexities of the American frontier and early Mormon history. A devoted pioneer, farmer, and ferry operator, his contributions to Mormon expansion are overshadowed by his role in the Mountain Meadows Massacre. Lees Ferry stands as a testament to his and Emma’s resilience in a harsh landscape, while his execution highlights the fraught dynamics of justice and blame in a turbulent era. His story remains a compelling chapter in the history of the American West.

Lees Ferry Campground

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Nestled within the Glen Canyon National Recreation Area, Lees Ferry Campground is a scenic, primitive campground located on a bluff overlooking the Colorado River, just 1.5 miles from the historic Lees Ferry boat launch in Marble Canyon, Arizona. Situated about 42 miles from Page, AZ, and 125 miles north of Flagstaff, this first-come, first-served campground offers 54 designated campsites suitable for tents, trailers, and RVs up to 30 feet, with no hookups available. Each site features a picnic table, fire ring with grate, and many include shade structures to provide relief from the desert sun, as there is no natural shade. The campground, open year-round, charges $26 per site per night (as of January 2025), with a discounted rate of $13 for holders of the America the Beautiful Senior or Access Pass.

Amenities include clean flush toilets, potable water spigots (though occasionally turned off during cooler months), and an RV dump station located about 0.75 miles away. There are no showers, but coin-operated showers are available at Marble Canyon Lodge, approximately 5 miles away. Grills are provided, but open ground fires are prohibited outside of grates, and quiet hours are enforced from 10 PM to 6 AM. A gas station, store, and post office are conveniently located in Marble Canyon, just 5 miles from the campground. The sites are slightly unlevel, and tent campers are advised to bring extra stakes or ropes due to frequent windy conditions, especially in the afternoons.

The campground’s prime location offers stunning views of the Colorado River, Vermilion Cliffs, and surrounding red-orange rock formations, making it a haven for stargazing and photography, particularly at night under clear desert skies. Its proximity to the river allows easy access to fly fishing (license required), hiking, and boating activities, with the Lees Ferry boat ramp serving as the starting point for Grand Canyon rafting trips. Nearby trails, such as the River Trail, Paria Riffles, and Cathedral Wash, offer opportunities to explore the area’s geology and spot wildlife like bighorn sheep. The historic Lees Ferry crossing, used from 1872 to 1928, and remnants like the Old Mormon Fort are within walking distance, adding a layer of historical intrigue.

Ideal for adventurers seeking a no-frills camping experience, Lees Ferry Campground is a gateway to the slot canyons, desert ridges, and waters of Lake Powell. Its serene atmosphere and million-dollar views make it a favorite, though arriving early is recommended to secure a spot, especially during peak spring and fall seasons when the weather is most favorable.