Category: Destination4x4

Schwab California

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Schwab, also spelled Schwaub, was a short-lived gold mining camp and ghost town in Inyo County, California, situated in the Funeral Mountains on the eastern edge of Death Valley. Located approximately 12 miles north of Ryan at an elevation of 3,389 feet (1,033 m), the townsite lies in Echo Canyon within the Echo-Lee Mining District. Today, it is a largely abandoned site within or near Death Valley National Park, accessible via desert roads best traveled in winter. Little remains beyond scattered ruins, leveled tent sites, piles of rusted tin cans, broken glass, and remnants of the nearby Stray Horse (or Inyo) Mine.

Schwab, California - “In the afternoon the townsite company drinks tea,” Death Valley Chuck-Walla magazine, Vol 2. No. 1, June 1907
Schwab, California – “In the afternoon the townsite company drinks tea,” Death Valley Chuck-Walla magazine, Vol 2. No. 1, June 1907

Founding and Early Development (1905–1906)

The town originated during the intense mining boom that swept the Death Valley region following the 1904 gold strike at Rhyolite, Nevada. Prospectors fanned out in search of extensions of the rich Bullfrog District deposits, including rumored lost mines like the Breyfogle. In January 1905, Mormon prospectors Chet Leavitt and Moroni Hicks discovered a promising quartz ledge known as the Stray Horse in Echo Canyon on the west side of the Funeral Range. Initial assays were disappointing, but a richer vein higher up led them to stake over 20 claims, including the Inyo Mine. They formed the Inyo Gold Mining Company with investors from Provo, Utah.

By late 1905—around Christmas—the townsite began to take shape down Echo Canyon. It was named Schwab in honor of Charles M. Schwab, the prominent American steel magnate (not to be confused with the later financier Charles R. Schwab). Schwab had invested heavily in regional mining ventures, including the nearby Skibo Mining Company (named after his Scottish castle) and claims resembling Rhyolite’s lucrative Montgomery-Shoshone Mine. The townsite was laid out just below the Skibo mine to support workers. Construction accelerated in early 1907, with supplies—including five boxcars of tents and equipment—shipped by rail to the area. A post office opened on March 18, 1907, with Eugene P. Houtz as postmaster (it closed permanently on August 15, 1907).

At its peak, Schwab supported a modest population of around 200 people. It featured basic services: a blacksmith shop, boarding house, general store, bakery, restaurant, and at least one saloon (housed in a tent). Infrastructure included a telephone line connected to Rhyolite via the Lee and Echo camps and a daily stage line. The Echo Miners Union provided some labor organization. The nearby Stray Horse/Inyo Mine served as the economic anchor, though the town primarily functioned as a supply and housing hub for the broader Echo-Lee District.

Unique Governance: The “Women of Schwab” (1907)

One of the most distinctive aspects of Schwab was its ownership and promotion by women—an unusual occurrence in the rough-and-tumble mining camps of the American West. The townsite company was taken over by three women: Gertrude Fesler (a young stockbroker from Chicago who had moved to Rhyolite to broker mining deals), Mrs. F.W. Dunn (of San Bernardino, who received her husband’s interest), and Helen H. Black (who bought out her husband’s share). They marketed the camp with promotional materials proclaiming it “A Mining Camp Built by Ladies: One of the Most Unique Wonders of the New West.” Contemporary newspapers, such as The Bullfrog Miner (March 1907) and Death Valley Chuck-Walla (June 1907), highlighted the novelty of women running a mining town, noting details like the owners drinking afternoon tea in the main tent.

The women reportedly enforced a “respectable” moral code, driving out saloons, gambling, and prostitution. Some contemporary and later accounts (including historian Lingenfelter) suggested this “dry” policy caused most of the male population to leave, accelerating the town’s collapse. However, archaeological evidence—such as beer and wine bottles, champagne bottle caps (agraffes), and dumps near the main tent—indicates that drinking persisted to some degree. Historians now emphasize that economic and logistical factors were the primary drivers of decline, not moral reforms.

Decline and Abandonment (1907 Onward)

Schwab’s boom was brief and fragile, mirroring the fate of many Death Valley mining camps. The Financial Panic of 1907 devastated regional mining investments, including those tied to Charles M. Schwab. Ore quality proved inconsistent, and Schwab’s location was disadvantaged: it depended on the more accessible Lee Camp for shipments, assays, and transport, with no direct route for miners. Most operations in the Echo-Lee District shut down, except for Lee Camp itself (which benefited from rail access). By August 1907, the post office closed, businesses folded, and the town rapidly emptied. Supplies were hauled away, leaving behind tent bases, wooden cellars, and debris.

The Inyo Gold Mining Company continued intermittent operations at the mine into the 1920s–1940s, but the townsite itself was abandoned within a year of its founding. Some later activity occurred after 1928, but Schwab never revived as a community.

Legacy and Current Status

Today, Schwab is a classic California ghost town with minimal visible structures—primarily scattered ruins, mine tailings, and historical debris in Echo Canyon. The Stray Horse/Inyo Mine workings remain, though they are often confused with the townsite itself. Two wooden crosses mark possible graves, one labeled “A Death Valley Victim – 1907.” The site offers a glimpse into the fleeting 1905–1907 mining excitement in Death Valley and stands as a reminder of the boom-and-bust cycle driven by speculation, distant capital (like Schwab’s investments), and harsh desert conditions.

Schwab’s story highlights the role of women in Western mining towns, the broader Death Valley gold rush, and the economic vulnerabilities of early 20th-century prospecting. It remains a point of interest for hikers, historians, and visitors to Death Valley National Park, though it lacks the dramatic intact buildings of better-known sites like Bodie or Rhyolite.

The town of Schwab is situated just below the Inyo and Skibo camps at the junction of the wagon roads leading up the east arm of Echo canyon and to Death Valley on the south. In other words, Schwab is located in the north or upper branch of Echo Canyon, astride the main Echo-Lee wagon road, across a small ridge from the present Inyo ruins, and about 1-1/2 miles from those ruins. At this location, evidence of the old townsite may be found.

The remains consist of seven leveled tent sites, some with ow and crude stone retaining walls remaining. More tent sites were once present, but have been erased by high water in the adjacent wash during Death Valley’s infrequent but violent flash floods. Two of the tent sites have eroded cellars behind them, about ten feet square and five feet deep. Since an immense pile of broken 1900 to 1910-dated beer bottles is located directly behind one of these tent-cellar sites, it is safe to say that this was the tent saloon, where once twenty-nine men were counted drinking at one time. The townsite covers several hundred feet along the-shallow wash which marks the northern branch of Echo Canyon, and remains are mostly restricted to the west side of that wash On the east side, however, is another tent location, and a shallow, unmarked grave, a lonely monument to one prospector who ended his days during the brief life of Schwab. About 300 yards to the west of the townsite is a crude derrick, the remains of Schwab’s well. The well site is dry and completely filled in, but numerous five gallon cans are scattered along the trail from the well to the townsite.

Rhyolite Herald of 22 February 1907.

Town Summary

NameSchwab, California
LocationDeath Valley National Park, California
Latitude, Longitude36.505, -116.7236
Elevation3,340 feet
Population200
Post Office

Schwab Map

References

Sutro Nevada

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Sutro, Nevada, located in Lyon County near the historic town of Dayton in the Carson River Valley, is a quintessential Western ghost town that owes its existence entirely to one of the most ambitious engineering feats of the Comstock Lode era: the Sutro Tunnel. The town, the tunnel, and the man—Adolph Sutro—are inseparable in Nevada mining history. Planned as a model community and operational headquarters for the tunnel project, Sutro briefly flourished as a well-organized settlement supporting the drainage of the flood-prone silver mines beneath Virginia City and Gold Hill. The tunnel itself, a nearly 4-mile-long drainage adit, addressed critical safety and operational challenges in the Comstock Lode, pioneering large-scale mine drainage techniques in the United States.

The town of Sutro Nevada, taken in 1874
The town of Sutro Nevada, taken in 1874

Background: The Comstock Lode and the Need for the Tunnel

The discovery of the Comstock Lode in 1859 transformed the Virginia Range into one of the richest silver and gold districts in American history. As mines deepened—eventually reaching thousands of feet—engineers faced insurmountable problems: sudden floods from underground reservoirs, scalding-hot water inflows, poor ventilation, and skyrocketing costs for surface pumping. Traditional hoisting and pumping systems could not keep pace, endangering lives and limiting production. Disasters like the 1869 Yellow Jacket Mine fire in Gold Hill, which killed dozens partly due to blocked escape routes and flooding, underscored the urgency for a better solution.

Adolph Sutro and the Vision for the Tunnel

Adolph Sutro (1830–1898), a Prussian-born Jewish immigrant and self-taught entrepreneur who had profited from the California Gold Rush as a tobacco merchant and later operated a quartz mill along the Carson River, proposed the tunnel in 1860. His plan was straightforward yet revolutionary: excavate a gently sloping, horizontal adit from the lowlands near Dayton (close to the Carson River) approximately 4 miles southeast, connecting underground to the Comstock mines at a depth of about 1,640–1,750 feet. The tunnel would drain millions of gallons of water daily, provide ventilation, offer an alternative access route for men, supplies, and ore, and serve as a potential emergency escape.

Sutro secured legislative approval from the Nevada state legislature and U.S. Congress by 1865, including a 50-year franchise and land grants. Mining interests initially backed the idea for its safety benefits, but powerful mine owners and banks later opposed it fiercely, fearing it would break their monopoly on underground access and milling.

Adolph Heinrich Joseph Sutro (1830–1898) was the 24th mayor of San Francisco, California, serving in that office from 1894 until 1896 - Photographer Mathew Benjamin Brady
Adolph Heinrich Joseph Sutro (1830–1898) was the 24th mayor of San Francisco, California, serving in that office from 1894 until 1896 – Photographer Mathew Benjamin Brady

Construction and the Birth of the Town (1869–1879)

Construction of the Sutro Tunnel began on October 19, 1869, with ground broken at the Dayton end. The project was initially financed largely by contributions from miners themselves, who recognized its life-saving potential, and later by international bankers through the Sutro Tunnel Company’s stock sales. Crews—often immigrants using hand tools, explosives, and mules—labored for nearly nine years through solid rock. The main tunnel measured 3.88 miles (20,489 feet or about 6.24 km) long, roughly 10–12 feet wide and high (with variations reported up to 17×20 feet in places), and connected precisely to the Savage Mine workings on July 8, 1878 (some accounts note September 1). North and south lateral branches extended the total length to about 4.56 miles and were completed in 1879. The first water was released from the mines on June 30, 1879.

At the tunnel portal, Sutro carefully planned and developed the town of Sutro as the project’s headquarters. What began as a rough construction camp evolved into a well-laid-out community with streets, parks, a church, post office (established March 25, 1872, and operating until October 30, 1920), and its own weekly newspaper, the Sutro Independent. Sutro envisioned it as a miners’ haven where workers could live comfortably and commute underground via the tunnel. The population peaked at 600–800 during construction, including fine residences and Sutro’s own elaborate Victorian mansion (built in 1879 for $60,000, featuring marble fireplaces and a two-story veranda). Tunnel water was even used for irrigation.

The entrance to the Sutro Tunnel in the late 1800s. Suntro, Lyon County, Nevada.
The entrance to the Sutro Tunnel in the late 1800s. Suntro, Lyon County, Nevada.

Operations, Impact, and Decline

Once operational, the tunnel drained up to 3.5 million gallons of water per day in the 1880s, dramatically improving ventilation, reducing pumping costs, and enabling deeper, safer mining. It also facilitated ore and waste removal more efficiently than vertical shafts. The project served as a model for later U.S. drainage tunnels, such as those in Colorado.

Adolph Sutro sold his interest in the company shortly after completion and relocated to San Francisco, where he became a wealthy philanthropist, built the iconic Sutro Baths and Cliff House, and served as mayor (1895–1897). The tunnel company continued under other management, and the town gradually declined as the Comstock Lode’s bonanza faded by the early 1880s. Population dropped to around 375–435 by 1880; most buildings were removed or fell into disrepair. Fires claimed the mansion in 1941 and other structures later. The tunnel operated for about 65 years until the 1940s, when wartime needs, mismanagement, and declining production led to its closure around 1943 (though it continues to drain some water passively).

Legacy and Current Status

The Sutro Tunnel stands as an enduring engineering marvel that protected miners’ lives and sustained Comstock operations long after its richest ores were extracted. The town of Sutro, though now a private ghost town with scattered remnants (wooden shacks, mine tailings, and the iconic portal facade), is undergoing active preservation. The nonprofit Friends of Sutro Tunnel is leading restoration efforts, including site cleanup, structural stabilization, and partial reopening for guided tours. Over 1,000 feet of the tunnel have been explored with modern technology, and the site aims to become a public historical attraction highlighting Nevada’s mining heritage.

Today, Sutro serves as a poignant reminder of the ingenuity, labor, and ambition that defined the Comstock era—a town born of necessity that briefly thrived around humanity’s determination to conquer the depths of the earth.

Town Summary

NameSutro Nevada
LocationLyon County, Nevada
Latitude, Longitude39.28, -119.584167
GNIS856145
Elevation4,478 ft (1,365 m)
Population600 – 800
Post OfficeMarch 1872 – October 1920
NewspaperSutro Independent Sept 25, 1875 – Nov 22, 1880

Sutro Map

References

Evening Star Mine

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The Evening Star Mine (also known as the Evening Star Tin Mine, Maynard Mine, Bernice Mine, or Rex Tin Mine) is located in the Mescal Mining District at the western base of the Ivanpah Mountains, San Bernardino County, California—within what is now Mojave National Preserve. It sits at approximately 4,961 feet elevation, about 1.5 miles south of the Standard No. 1 Mine, near Cima and not far from the California-Nevada border (outside Primm, NV)..

Evening Star Mine, Mojave, California - 2015 Photo by James L Rathbun
Evening Star Mine, Mojave, California – 2015 Photo by James L Rathbun

Discovery and Early Development (1935–1940)

The mine began modestly in 1935 as a copper prospect staked by lifelong desert miner J. Riley Bembry. Bembry, born in Oklahoma in 1899 and a WWI veteran, had prospected extensively in the eastern Mojave since the late 1920s or early 1930s. Within about a year, he sold the claims to Trigg L. Button and Clarence Hammett of Santa Ana, California. They began sinking the No. 1 shaft.

In 1940, Vaughn Maynard of Santa Ana purchased the claims. The site was developed as a combination surface-underground operation on a small deposit.

Peak Operations and Production (1941–1944)

The mine entered its main productive phase during World War II, driven by demand for strategic minerals. In 1941, the Tin Corporation of America leased the property. They continued deepening the shaft and, in June 1942, shipped 25 tons of ore to the Tin Processing Corporation in Texas City, Texas.

In 1943, Carl F. Wendrick, Jr. (owner of Steel Sales and Service Company of Chicago, Illinois) leased the mine. He secured a government loan, employed about eight men, constructed a larger headframe, and built a mill at Valley Wells. Operations ran primarily from 1939 to 1944 (with the most intensive work in the early 1940s).

Production and Significance

The Evening Star Mine was the only producer of tin ore (cassiterite, or tin oxide) in the eastern Mojave Desert—and reportedly the only one in the broader Mojave. It yielded over 400 tons of tin ore during its life. Several tons of tin concentrates (containing 35.96% tin) were sold to the U.S. government stockpile in Jean, Nevada, just across the border. The deposit also carried minor amounts of copper, tungsten, zinc, and possibly gold.

Nearby claims (just west) produced about 1,000 tons of tungsten ore under a separate lease (1939–1940).

Unique Engineering Feature

The mine stands out for its 60-foot headframe, which featured a crusher mounted directly on top—one of the few such setups in the Mojave. Ore fed from the headframe into a sorting structure of three tiered towers (the lowest serving as an ore bin). This design was practical for the remote, small-scale operation.

Closure and Current Status

Production ended around 1944 as wartime demand eased and the deposit proved limited. The site was never a large-scale operation but exemplified the many independent, small-scale ventures that dotted the desert.

Today, the Evening Star Mine is a well-preserved historic site within Mojave National Preserve. The impressive wooden headframe and associated structures (outbuildings, shafts, tunnels, and artifacts) remain visible and have been assessed for stabilization to protect historic timber framing. The main shaft is closed for safety (e.g., with cable netting). It serves as a photogenic reminder of WWII-era mining and the rugged life of desert prospectors.

(Note: A few secondary sources occasionally reference earlier 1900s development or conflicting details, but primary accounts consistently date commercial tin-focused work to the 1935–1944 period.)

The Evening Star Mine, though short-lived, highlights the Mojave’s role in supplying critical minerals during national emergencies and contributes to the rich tapestry of over a century of desert mining history. Many similar sites nearby (e.g., Vulcan for iron) underscore how the region supported both economic booms and wartime needs.

Resources

Kokoweef Mine

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The Kokoweef Mine (more accurately known as the legendary caverns or lost river of gold beneath Kokoweef Peak) is not a conventional operating mine but a persistent folk legend tied to a remote mountain in California’s Mojave Desert. Kokoweef Peak (also called Mt. Kokoweef), rising to about 6,037–6,038 feet in the Ivanpah Mountains of San Bernardino County, lies roughly three miles south of Mountain Pass along Interstate 15, near the Nevada border and within or adjacent to the Mojave National Preserve area.

Kokoweef Mine from below - 2015
Kokoweef Mine from below – 2015

The story blends Native American oral tradition, a prospector’s sworn affidavit, and decades of treasure-hunting fervor. It has inspired mining claims, exploration companies, paleontological digs, and countless seekers—yet no verifiable underground river of gold has ever been confirmed. Real caves exist on the peak (limestone karst formations), and zinc was mined there during World War II, but the core “mine” remains legendary.

My nephew and son searching for the "River of Gold" on Kokoweef peak.
My nephew and son searching for the “River of Gold” on Kokoweef peak.

Origin Story: The Paiute Brothers and Tribal Lore (Late 1800s–Early 1900s)

The legend traces back to three Southern Paiute (or Piute) brothers—Oliver, George, and Buck Peysert—who reportedly worked as ranch hands at the Dorr family ranch near Colorado Springs, Colorado, in the 1890s–early 1900s during the boyhood of prospector Earl Dorr.

According to the tale, tribal elders had long described a vast underground cavern system beneath a peak (later identified as Kokoweef) containing a subterranean river whose black-sand beaches were laden with placer gold. Around 1903–1905, the brothers left the ranch to search for it. They allegedly rediscovered a narrow passageway leading deep into a labyrinth of caverns. After weeks of exploration, they reached an enormous underground river. They extracted gold worth about $57,000 (at the contemporary price of roughly $20 per ounce) over a six-week period. Tragedy struck when George fell to his death into the river. The survivors cashed in their gold at the U.S. Mint and deposited funds in banks in Needles, California, and Las Vegas, Nevada. Tribal custom supposedly forbade them from returning to the site after the death.

The brothers later shared the story with Earl Dorr (some accounts place this encounter in San Francisco around 1906 after the earthquake; others say he heard it as a youth). One version claims they provided him with a map, though Dorr family members later disputed this.

These mine cart rails are a little small to pull the amount of gold claimed to be here.
These mine cart rails are a little small to pull the amount of gold claimed to be here.

Earl Dorr’s Claim and the Birth of the Modern Legend (1920s–1930s)

Earl P. Dorr (born ~1885 near Colorado Springs), a cowboy-turned-prospector and adventurer, became the legend’s central figure. By the early 1920s, he had moved to the Mojave region and reportedly rediscovered an entrance to the cavern system (possibly Crystal Cave or one of the other solution cavities on Kokoweef Peak). In 1927, he enlisted a civil engineer, Mr. Morton from Tempe, Arizona, to help map it. According to Dorr’s later account, the two men spent four days (accounts vary between three and four) exploring over eight miles of passages. They descended thousands of feet into a massive underground canyon hundreds of feet deep, where a 300-foot-wide subterranean river flowed. The river reportedly “breathed,” rising and falling like tides, exposing black-sand beaches and ledges said to be extremely rich in placer gold. Dorr claimed they panned samples that assayed at high values (one report cited $2,144 per cubic yard). They allegedly carried out about 10 pounds each of gold-bearing material.

In 1934, Dorr signed a notarized affidavit detailing these discoveries. He said he dynamited the entrance shut to protect his find while attempting to file a claim. (Some accounts note he could not because earlier claims by a prospector named Pete Ressler—possibly linked to the Hole-in-the-Wall Gang—already covered parts of the area.) Dorr tried to attract investors but never successfully reopened or proved the site. He died in a 1957 mining accident.

The affidavit was later published in the California Mining Journal (1940) and referenced in Desert Magazine and other outlets, turning the story into a classic lost-mine legend. Variations appeared in print as early as the 1930s, sometimes blending it with broader Mojave Desert tales of interconnected cave systems and underground rivers.

Kokoweef Trail Map

Spread, Exploration, and Reality Checks (1940s–1970s)

The legend drew treasure hunters and small-scale miners to Kokoweef Peak, creating a short-lived shantytown at its base. The Wallace family, inspired by Dorr’s story, formed the Crystal Cave Mining Corporation in the mid-1930s. They acquired claims from Pete Ressler in 1939 and mined zinc (not gold) at the Carbonate King during World War II to fund further searches for the river. The claims were patented in later decades.

Successive groups (including the Schnar family in the 1960s–70s and Legendary Kokoweef Cavern Inc.) continued digging and blasting in known caves like Crystal Cave. Real scientific value emerged in the 1970s: paleontologists from the San Bernardino County Museum, led by Bob Reynolds, excavated over five-and-a-half tons of sediment from Kokoweef Cave. They recovered more than 200,000 Pleistocene-era fossils (deposited less than 11,000 years ago), including dire wolves, camels, horses, deer, pronghorn, coyotes, birds, and smaller mammals. These confirmed the caves’ existence and ancient use as animal traps or dens but found no evidence of a flowing river or gold deposits matching Dorr’s description.

Geologically, Kokoweef Peak consists of ancient Mississippian-Pennsylvanian limestone (300–340 million years old) that formed karst caves along faults, primarily during the Ice Age (~1 million years ago). While underground water systems are possible in such formations, experts note the modern Mojave’s extreme aridity makes a large, persistent subterranean river unlikely, and the claimed gold quantities would be unprecedented.

Modern Era and Enduring Search (1980s–Present)

In 1984–1985, Explorations Incorporated of Nevada (later evolving into Kokoweef Inc.) took over, continuing exploration through drilling, geophysical surveys, and tunneling. The company has found additional caverns, crystals, and mineral veins, and some drilling has encountered traces of gold and sulfides. They maintain mining claims and emphasize both the legendary river and potential commercial deposits. Investors (hundreds over the years) have funded the work, with some visions of trillion-dollar riches, but the river itself remains elusive.

Today, the site features old mine entrances, tailings, and ongoing (low-key) activity. Kokoweef Caverns were briefly a curiosity or tourist draw in earlier decades but are no longer promoted that way. The legend still circulates in books, magazines, forums, and videos, sometimes linking to wider desert lore about hidden caves or ancient civilizations. Skeptics view Dorr’s tale as an imaginative hoax or prospector’s yarn designed to attract backers; supporters point to the consistent details, real caves, and ongoing finds as evidence something extraordinary may still lie undiscovered.

In summary, the Kokoweef “mine” endures as one of California’s most captivating lost-treasure legends—rooted in a purported Native American discovery, amplified by Dorr’s dramatic 1934 affidavit, and kept alive by real geology, fossils, and determined explorers. Whether it conceals a river of gold or remains a desert mirage, it continues to draw dreamers to the Mojave’s rugged peaks.

Resources

Cathedral Valley

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Cathedral Valley is a remote, spectacular district in the northern section of Capitol Reef National Park in Wayne County, Utah. It is renowned for its towering sandstone monoliths, spires, and cliffs that evoke Gothic cathedrals and ancient temples, earning it the name. This high-desert landscape, accessible primarily by high-clearance 4×4 roads, features dramatic erosional forms like the Temples of the Sun, Moon, and Stars, colorful Bentonite Hills, and unique geological curiosities such as Glass Mountain and a gypsum sinkhole. It represents one of the least-visited yet most visually striking areas of the park, highlighting the broader story of the Waterpocket Fold monocline.

Temple of the Sun, located on Cathedral Valley Trail in Capital Reef National Park, Utah - Photo by James L Rathbun
Temple of the Sun, located on Cathedral Valley Trail in Capital Reef National Park, Utah – Photo by James L Rathbun

Vehicles with high ground clearance are recommended and should have no issues navigating the sandy roads. Road conditions can vary greatly depending on recent weather conditions with spring and summer rains leaving the route muddy and impassable.  The advantage of this location is the back country travel is light, so for the person seeking seclusion, this is the secluded area in a remote location.

The 60 miles loop trail leaves highway 24 at the River Ford which is about 12 miles easy of the visitor center.  The route follows Hartnet Road to the Cathedral Road ( Caineville Wash Road) and returns to Highway 24 near Caineville.  The river crossing is passable most of the time, however care should be taken during the rainy months.

During my visit in 2004, we just finished Hole in the Rock Road, and headed east out of Escalante, Utah.  We then took the Burr Trail to Notom Road which delivered us to Capital Reef.  That afternoon we chased the light up Cathedral Valley Road and stopped at Temple of the Sun for some photographic opportunities.  We stayed beyond sun down hoping for some amazing light which did not come that evening and drove trail out in the dark.  I was disappointed for the lack of light during the golden hour, but the location is yet another place that I must return just due to the amazing Utah landscapes.

Cathedral Valley Trail Map

Geological Formation: A Detailed Report

Cathedral Valley’s geology is part of the larger Capitol Reef story, exposing nearly 10,000 feet of sedimentary rock layers spanning from the Permian to Cretaceous periods (about 270 to 80 million years ago). The area’s distinctive monoliths and valley formed through three main phases—deposition, uplift, and erosion—over hundreds of millions of years.

Deposition (Middle to Late Jurassic, ~165–160 Million Years Ago)

During the Middle Jurassic, much of what is now Utah was a coastal plain near a shallow inland sea. Extensive tidal flats, barrier islands, sand bars, and sabkhas (evaporative flats) dominated the environment.

  • Carmel Formation (~165 million years ago): Thick layers of gypsum and other evaporites formed as seawater evaporated in restricted basins. This low-density gypsum later played a key role in unusual features.
  • Entrada Sandstone (~160 million years ago): The primary rock of the “cathedrals.” This 400–900-foot-thick formation consists of fine-grained, reddish-orange sandstone and siltstone (colored by hematite/iron oxides). It was deposited as sandy mud on tidal flats. The rock is relatively soft and crumbly, eroding easily into sheer cliffs without prominent talus slopes.
  • Curtis Formation (overlying the Entrada): A thinner (0–175 feet), resistant layer of grayish-green marine sandstone and siltstone (with glauconite). It acts as a protective caprock on many monoliths and buttes.
  • Summerville Formation: Thinly bedded reddish-brown siltstone above the Curtis.
  • Morrison Formation (Brushy Basin Member): Later Jurassic deposits of mud, silt, sand, and volcanic ash in swamps and lakes. Volcanic ash altered into bentonite clay, creating the colorful, banded Bentonite Hills (browns, reds, purples, grays, greens). Bentonite becomes extremely slick and gummy when wet, complicating travel.

These layers were originally buried under thousands of feet of younger sediment.

Uplift: The Waterpocket Fold and Laramide Orogeny (~70–50 Million Years Ago)

About 50–70 million years ago, during the Laramide Orogeny (a major mountain-building event in western North America), tectonic forces reactivated an ancient Precambrian fault. This created the Waterpocket Fold—a 100-mile-long monocline (a step-like fold in the rock layers). In Cathedral Valley, the layers dip gently eastward at only 3–5 degrees, appearing nearly horizontal (unlike the steeper exposures elsewhere in the park).

The west side of the fold was uplifted more than 7,000 feet relative to the east. Later regional uplift of the Colorado Plateau (starting ~15–20 million years ago) further exposed the strata. This set the stage for erosion to carve the modern landscape.

Erosion and Sculpting of the Landscape (~20 Million Years Ago to Present)

Erosion intensified over the last 15–20 million years (and especially 1–6 million years ago), driven primarily by water (flash floods, streams, and groundwater), freeze-thaw cycles, and gravity. Wind plays a minor role. Approximately 7,000 feet of overlying rock has been removed.

  • Monoliths and Cathedrals: Fractures and joints in the Entrada Sandstone (formed during uplift and pressure release) created zones of weakness. Water infiltrated these joints, accelerating chemical and mechanical weathering. Softer, fractured rock eroded away, leaving resistant, unfractured masses as free-standing monoliths or “temples” (e.g., Temples of the Sun and Moon). In Lower Cathedral Valley, the Curtis caprock has largely eroded away, producing steeple-like shapes; elsewhere, it protects taller formations.
  • Glass Mountain: A rare “gypsum plug” of large selenite crystals (clear gypsum, CaSO₄·2H₂O). Groundwater dissolved gypsum from the Carmel Formation and redeposited it within fractures in the Entrada Sandstone, forming a dome-like mass that is now exposed as surrounding rock erodes. It rises about 15 feet above the valley floor.
  • Gypsum Sinkhole: The opposite process—a buried gypsum plug dissolved by groundwater, creating a cavity that collapsed into a ~50-foot-wide, 200-foot-deep sinkhole.
  • Volcanic Features (3–6 million years ago, with some basalt boulders ~20 million years old): Molten lava intruded as dikes (vertical) and sills (horizontal) into sedimentary layers. These dark, resistant igneous rocks now stand out as ridges. Black basalt boulders scattered across the landscape originated from lava flows on nearby Boulder and Thousand Lake Mountains and were transported by glaciers, mudslides, and erosion during the Ice Age.

The result is a landscape of sheer cliffs, isolated monoliths rising hundreds of feet, and badlands-like badlands sculpted from soft Entrada rock—dramatically different from the Waterpocket Fold’s other sections.

Human History

Human presence in Cathedral Valley has been limited by its remoteness and harsh terrain, but it reflects broader patterns in southern Utah.

  • Prehistoric and Native American Use: The broader Capitol Reef region was inhabited by Archaic hunter-gatherers and later the Fremont Culture (related to Ancestral Puebloans, ~A.D. 300–1300), who left petroglyphs, tools, and farming evidence elsewhere in the park. Cathedral Valley itself has fewer documented sites due to its isolation, though occasional artifacts and use for hunting or seasonal travel likely occurred. Later Paiute, Ute, and Navajo peoples traversed the area.
  • Early Exploration and Settlement (19th Century): Spanish explorers, trappers, and the 1853 Fremont expedition passed through southern Utah, but Cathedral Valley remained largely unknown. Mormon pioneers settled nearby valleys in the late 1800s, using the region for grazing.
  • Ranching Era (Early 20th Century): Around 1900, local cattlemen built the Cathedral Valley Corral (one of the oldest ranching structures in the park) using a natural sandstone alcove and cliffs, with wooden fences and a cattle chute. Families like the Jefferys and Morrells used it for branding, vaccinating, and managing livestock on the open range. This period saw heavy grazing that impacted vegetation. An old ranch well (with trough, trees, and abandoned equipment) and the Morrell Cabin (a historic structure on the valley floor) also date to this era. Extensive open-range practices eventually led to overgrazing in parts of the area.
  • Naming and Recognition (1945): In 1945, Frank Beckwith (a local explorer) and Charles Kelly (first superintendent/caretaker of Capitol Reef National Monument) named the area “Cathedral Valley.” The upward-sweeping, fluted monoliths reminded them of ornate Gothic cathedrals, Egyptian temples, and other grand architecture.
  • Park Protection (1937–Present): Capitol Reef was designated a National Monument in 1937 by President Franklin D. Roosevelt to protect its canyons and geology. Cathedral Valley was included as the remote northern district. It became part of Capitol Reef National Park in 1971. The corral was listed on the National Register of Historic Places in 1999 (reference #99001093). Today, the area is preserved for its scenic, scientific, and wilderness values, with ranching largely phased out.

Cathedral Valley remains a backcountry gem—requiring preparation for its rugged 57-mile loop road (often impassable when wet due to bentonite clay). It offers a direct window into deep geologic time and Utah’s ranching past, with features like the Temples of the Sun and Moon still inspiring awe as they did in 1945. For current access details, consult the National Park Service.