Big Bear, CA
I quiet mountain community full of back country adventure.
Ione Nevada – Nye County Ghost Town
Ione is a remote ghost town in Nye County, central Nevada, situated in Ione Valley at an elevation of approximately 6,782 feet (2,067 meters). Located roughly 23 miles (37 km) east of Gabbs, it lies in a high desert basin surrounded by the Shoshone Range. Though often classified as a ghost town, Ione has earned the nickname “the town that refused to die” for its repeated cycles of boom and bust while never fully vanishing.
Prehistoric Inhabitants
The Ione Valley supported a dense and permanent Native American population for at least 5,000 years. Shoshone and Northern Paiute peoples inhabited the area, practicing unusual property arrangements and agricultural methods adapted to the arid environment. Evidence of their long-term presence underscores the valley’s value as a resource-rich location long before European-American settlement.
Founding and Initial Boom (1863–1864)
Ione’s Euro-American history began in November 1863 when prospector P. A. Havens discovered silver ore in the Shoshone Range. The town initially formed in Ione Canyon as a trade and milling center serving the Union Mining District (whose mines were closer to settlements like Union and Grantsville). Within months, it grew rapidly: the original site boasted nearly 50 buildings, and the population swelled as miners, merchants, and entrepreneurs arrived.
In early 1864, residents petitioned the Nevada Territorial government to create a new county. Nye County was officially organized in April 1864 (named after Territorial Governor James Nye), with Ione designated as its first county seat. The territorial government awarded the town an $800 stipend to build the county’s first courthouse—a modest wooden structure. By late 1864, Ione had over 100 buildings, a population nearing 600, two short-lived newspapers (Nye County News and the Advertiser), a post office (opened 1865), stores, saloons, stables, and a stage line to Austin. Mills soon followed, including the Pioneer 5-stamp mill (1865) and the larger Knickerbocker mill three miles south.
The townsite was relocated out of the canyon in 1864 to a more convenient spot nearer the principal mines.
County Seat Era and Rapid Decline (1864–1867)
Ione’s prominence as Nye County’s seat proved short-lived. Richer silver strikes at Belmont, about 50 miles southeast, drew away most of the population by 1865–1866. In February 1867, the county seat officially moved to Belmont. By 1868, Ione’s population had dropped below 200. A brief post-1867 silver resurgence in the 1870s failed to restore its earlier status; by 1880, only about 25 people remained. A major fire in 1887 destroyed many buildings, and the post office was briefly renamed “Midas” in 1882 in a failed attempt to revive fortunes.
Later Revivals (1890s–1930s)
Ione experienced intermittent revivals tied to mining. In 1896, the Ione Gold Mining Company built a 10-stamp mill to process ore from the nearby Berlin mine, briefly boosting the population to around 70. In 1897, prominent businessman A. Phelps Stokes (through the Nevada Company) purchased most mining and milling interests in the Union District, injecting new capital. This resurgence ended abruptly in July 1898 when silver prices collapsed. The post office closed in 1903.
A final small boom occurred around 1912–1914 with the discovery of cinnabar (mercury ore) deposits. The population reached about 100, and a telephone line connected the town to Austin. Mercury mining continued sporadically into the 1920s and 1930s, with operations at nearby Shamrock producing thousands of flasks of mercury. These activities helped Ione survive the Great Depression, though the mill was eventually dismantled in 1950. The post office reopened briefly during this period but closed for the final time on April 30, 1959.
20th Century to Present
Population figures reflect the town’s resilience: it stood at 40 in 1940. In the 1970s, Hugh Marshall acquired most of the townsite and surrounding 24 square miles. A later attempt at large-scale gold mining in the early 1980s by Marshall Earth Resources restored some buildings but ultimately faded.
Ione never became fully abandoned, persisting through mining depressions, milling challenges, and competition from richer strikes elsewhere. Today it remains a living ghost town with a handful of residents (reports from the early 2020s cited around 41; more recent accounts suggest even fewer year-round occupants). A small market once operated, but services are minimal. The remote location—reached via dirt roads off State Route 91—limits tourism, though the site attracts those interested in Nevada’s mining heritage.
Notable Landmarks and Legacy
Surviving structures include historic wooden and stone buildings, an aged corral, stone cabins, and a barn-like structure rumored to be the original (small wooden) Nye County Courthouse. The Ore House Saloon, a turn-of-the-century building, stands as one of the more visible remnants.
Ione Valley’s prehistoric sites and the town’s layered mining history contribute to its significance. It exemplifies the boom-bust pattern of Nevada’s 19th- and early 20th-century mining camps, yet its unbroken (if tenuous) occupation sets it apart.
Sources draw primarily from Nevada historical markers, mining histories, and local records. For further reading, consult Shawn Hall’s Preserving the Glory Days: Ghost Towns and Mining Camps of Nye County, Nevada. Ione stands today as a quiet testament to the enduring, if modest, spirit of Nevada’s frontier mining towns.
Ione Trail Map
Evening Star Mine
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)..
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
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.
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.
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.
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.
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Cathedral Valley
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.
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.
Bert Smith’s Cabin
Bert Smith’s Cabin, commonly known as the Rock House or Rock Spring Cabin, is a historic stone structure located in the Mojave National Preserve in San Bernardino County, California. Situated along the Rock Spring Loop Trail near the ruins of Camp Rock Spring, the cabin overlooks a scenic desert valley and serves as a poignant reminder of one veteran’s resilience in the harsh Mojave Desert environment. Built in 1929, it stands as a testament to homesteading, health-driven migration to arid regions, and the broader history of the Mojave Road corridor. Today, it is preserved by the National Park Service (NPS) as a public hiking destination and interpretive site.
Bert Smith’s Background and Move to the Desert
Bert George Smith (often referred to simply as Bert Smith) was a World War I veteran who served in Europe. During the war, he was exposed to poison gas—likely mustard gas—used in chemical warfare, which severely scarred his lungs. Upon returning to the United States, his health declined dramatically. In the late 1920s, the Department of Veterans Affairs recommended that he relocate to the Mojave Desert, believing the dry climate might extend his life. Doctors gave him only a short time to live, perhaps as little as a year.
Smith arrived in the Mojave in 1929 and chose a site above the historic Camp Rock Spring, a former U.S. Army outpost used from 1866 to 1868 and a vital water source for Native American tribes, explorers, settlers, and military personnel. The area had long been part of desert travel networks, including the Mojave Road.
Construction of the Cabin
Smith initially built a simple wooden shack for shelter. He later upgraded it into a more substantial rock house using local stones, completing the structure around 1929 or in the early 1930s. The single-story cabin featured a functional design suited to the desert: thick stone walls for insulation, basic windows, a chimney, and a modest footprint. It had no electricity or modern amenities like television, emphasizing self-reliance and simplicity.
Smith enhanced the site by constructing wells and dikes in Rock Spring Canyon to improve water availability. He also maintained a small herd of goats, whose milk sustained him and his animals; remnants of the goat pen and corrals are still visible nearby. The cabin’s elevated location provided panoramic views of the surrounding desert, including the New York Mountains to the north.
Life at the Cabin
Despite his grave prognosis, Smith thrived in the isolated desert setting. He lived at the Rock House for approximately 25–27 years, until 1954, far outlasting medical expectations. His existence was one of quiet solitude amid the Mojave’s rugged landscape—tending goats, maintaining the spring improvements, and embracing the peace of a life without modern distractions. A common inscription or description of the site captures this spirit: “Former home of Bert George Smith. No television, no electricity. Just peace and quiet.”
In the 1930s, the area saw brief mining activity nearby when prospectors discovered copper in Watson Wash and built a small mill to process ore. The operation was short-lived and soon abandoned, leaving ruins that the Rock Spring Loop Trail now passes.
Subsequent Residents and Transition
After Smith left the cabin in 1954 (he reportedly moved to a retirement home and passed away in 1967), the structure stood vacant for a time. In 1981, desert artist Carl Faber—already experienced in living rough in the East Mojave—moved in and operated an informal art business there for about five years. He sold his artwork to passing four-wheel-drive travelers along the Mojave Road. Faber later relocated to a nearby property, continuing his art until 2003 before moving to New Mexico. He reflected positively on the lifestyle, noting how many visitors envied his freedom.
Current Status and Preservation
The NPS has restored and maintains the cabin, which remains in good condition with its stone construction intact. It is locked to protect the interior, but visitors can view it closely from the outside. The site is easily accessible via a short walk from a dirt parking area along Rock Spring Road (0.2 miles south of Cedar Canyon Road), with picnic tables and vault toilets nearby. It forms part of the one-mile Rock Spring Loop Trail, which also highlights the miners’ mill ruins and Camp Rock Spring.
An official NPS historical marker at the site details Smith’s story and the area’s layered history. The cabin is a popular stop for hikers, off-road enthusiasts, and history buffs exploring the Mojave National Preserve.
Significance and Legacy
Bert Smith’s Cabin embodies themes of veteran recovery, desert adaptation, and human perseverance. Smith’s defiance of a terminal diagnosis through simple desert living inspired later residents like Carl Faber and continues to captivate visitors. It connects to broader Mojave narratives: military history at Camp Rock Spring, transient mining booms, and the enduring allure of remote homesteading. As part of the protected Mojave National Preserve, the site educates the public about the human stories woven into this arid landscape while preserving its natural and cultural resources for future generations.
In summary, what began as a desperate health refuge became a symbol of endurance. Bert Smith’s Rock House stands today not just as a historic building, but as a monument to the quiet determination of those who sought solace and survival in the Mojave Desert.
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