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)..

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

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

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 Cabin overlooks Camp Rock Springs
Bert Smith’s Cabin overlooks Camp Rock Springs

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.

Bert Smith's Cabin located in the Mojave National Reserve
Bert Smith’s Cabin located in the Mojave National Reserve

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.

The NPS Sign refers to the site as "Rock House", I prefer Bert Smith's Cabin.
The NPS Sign refers to the site as “Rock House”, I prefer Bert Smith’s Cabin.

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.

Ryan and Rooger welcome you the their porch.
Ryan and Rooger welcome you the their porch.

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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White Tidy Tips (Layia glandulosa)

The White Tidy Tips (Layia glandulosa), also known as whitedaisy tidytips or white layia, is a charming annual wildflower in the sunflower family (Asteraceae) native to the arid and semi-arid regions of western North America, stretching from central Washington south to Baja California and eastward into Utah and Arizona. This low-growing, branched herb, typically reaching 4 to 24 inches in height, features hairy, glandular stems and linear to lobed leaves that give off a subtle fragrance. Its showy daisy-like flower heads bloom from March to June, especially following adequate winter rains, boasting pure white, three-lobed ray florets that encircle a bright yellow disk of central florets—creating a crisp, tidy contrast that evokes its common name—while the rays may occasionally fade to a delicate rose-purple. Thriving in sandy or open soils across desert scrub, grasslands, and coastal habitats, it adds bursts of ethereal beauty to spring landscapes, supports pollinators like butterflies, and provides seeds for birds, embodying the resilient grace of Western wildflowers.

White Tidy Tips (Layia glandulosa), also known as whitedaisy tidytips or white layia.  Photograph by James L Rathbun
White Tidy Tips (Layia glandulosa), also known as whitedaisy tidytips or white layia. Photograph by James L Rathbun

Biological Classification

White Tidy Tips, also known as Whitedaisy Tidytips or White Layia, belongs to the following taxonomic hierarchy:

  • Kingdom: Plantae (Plants)
  • Clade: Tracheophytes (Vascular plants)
  • Clade: Angiosperms (Flowering plants)
  • Clade: Eudicots
  • Clade: Asterids
  • Order: Asterales
  • Family: Asteraceae (Sunflower or Aster family)
  • Genus: Layia
  • Species: Layia glandulosa (Hook.) Hook. & Arn. (described in 1833; the specific epithet glandulosa refers to its glandular hairs)

It is an annual herb in the tarweed tribe (Heliantheae) within the Asteraceae family. The genus Layia is almost entirely restricted to western North America, with 14 species native to the region (12 of which are found in California).

Description of the Plant and Flower

Plant: Layia glandulosa is a low-growing, branched, pubescent annual herb typically reaching 4–24 inches (10–60 cm) tall (occasionally up to about 2 feet). The stems are erect, green to purple-streaked, and covered in soft glandular hairs that can feel sticky and sometimes produce a mild spicy or scented aroma. Leaves are thin, linear to oval-shaped, up to 4 inches (10 cm) long; the lower (basal) leaves are often lobed or pinnatifid, while upper leaves tend to be entire.

Flower: The inflorescences are showy, daisy-like flower heads approximately 1.5 inches (4 cm) across, borne on glandular stalks. Each head features 3–14 (typically 5–8) broad, white ray florets that are often 3-lobed at the tips; these pure white rays surround a central disk of numerous bright yellow disk florets. The involucre (base of the flower head) consists of green, hairy, glandular phyllaries. The rays may fade to rose-purple with age. After flowering, the plant produces hairy achenes (cypselae) with a pappus of stiff white hairs for seed dispersal.

The plant is rapid-growing and blooms primarily in spring, with flowering triggered by adequate winter rainfall; it may not bloom in dry years

Habitat

White Tidy Tips thrives in dry, open environments with well-drained, sandy or gravelly soils. It is commonly found on dry slopes, mesas, grasslands, meadows, desert uplands, and open clearings. It tolerates a range of conditions from lower to upper desert habitats and can occur in chaparral, coastal scrub, valley grasslands, and pinyon-juniper woodlands. Lean, nutrient-poor soils promote compact growth and abundant flowering, while richer soils may cause plants to become leggy.

Range and Distribution

Layia glandulosa is native to western North America. Its range extends from central Washington (and southern British Columbia) south through Oregon, Idaho, California, Nevada, Utah, Arizona, and New Mexico, reaching as far south as Baja California, Mexico. It is particularly common in the southwestern United States, with the largest populations reported in Nevada, Arizona, California, and Oregon. In the U.S., it occurs in the following states: AZ, CA, ID, NM, NV, OR, UT, WA.

Elevation ranges from near sea level up to about 5,000–7,500 feet (1,524–2,286 m), depending on local conditions.

Ecology and Additional Notes

As an annual, Layia glandulosa germinates with winter rains and completes its life cycle quickly in spring. It provides important resources for pollinators, especially native bees, and its seeds are consumed by birds and small mammals. Indigenous groups in the southwestern U.S., such as the Cahuilla and Luiseno peoples, traditionally used the seeds as food (ground into flour or porridge).

The species is drought-tolerant once established and is valued in native plant gardening and restoration for its cheerful blooms and ability to thrive in poor soils. It is not considered invasive and is a native component of western ecosystems.

This report is based on data from botanical authorities including the USDA Plants Database, Lady Bird Johnson Wildflower Center, and regional floras. Population sizes can vary greatly year-to-year depending on rainfall.

Desert Gold Poppy (Eschscholzia glyptosperma)

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. It is a member of the poppy family and a smaller, desert-adapted relative of the more widespread California Poppy (Eschscholzia californica). This species is particularly notable for its vibrant blooms during spring “superbloom” events following adequate winter rainfall, when it can carpet desert washes and flats in golden hues.

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. - Photograph by James L Rathbun
The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. – Photograph by James L Rathbun

Taxonomic Classification

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Order: Ranunculales
  • Family: Papaveraceae (Poppy family)
  • Genus: Eschscholzia
  • Species: Eschscholzia glyptosperma Greene (described by botanist Edward Lee Greene)

The binomial name Eschscholzia glyptosperma reflects the genus honoring Estonian botanist Johann Friedrich von Eschscholtz and the species epithet referring to its sculptured or “engraved” seeds (glyptosperma). It is a strictly annual herb.

Plant and Flower Description

Eschscholzia glyptosperma is a small, scapose (mostly leafless-stemmed) annual herb. It grows from a basal rosette of finely dissected, pointed, grayish-green leaves that are 1–4 times pinnately divided into narrow, pointed segments— an adaptation that reduces water loss in harsh desert conditions. The plant typically reaches 5–25 cm (2–10 inches) in height, with one or more erect, slender stems arising from the base. Each stem bears a single flower atop a long peduncle.

Flower Morphology: The flowers are bright yellow (occasionally with a subtle orange tint), solitary, and actinomorphic (radially symmetrical). They feature four broad, satiny petals, each measuring approximately 1–2.5 cm (⅜–1 inch) long, giving the bloom a cup- or saucer-like appearance when fully open in sunlight. The petals are silky-textured and close at night or in cloudy/cold conditions (nyctinasty). There are typically two (sometimes three) sepals that are glabrous (smooth), often glaucous (waxy blue-green), and shed soon after the flower opens. The center displays numerous yellow stamens surrounding a single superior ovary. Flowers bloom primarily from February to May, peaking in March–April depending on rainfall and elevation.

The fruit is a slender, cylindrical capsule (4–8 cm long) that dehisces (splits) from the base when dry, explosively releasing numerous tiny, rounded, tan-to-brown seeds.

Range and Distribution

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. - Photograph by James L Rathbun
The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. – Photograph by James L Rathbun

The Desert Gold Poppy is endemic to the Mojave and Sonoran Deserts of the southwestern United States. Its distribution includes:

It occurs at elevations from near sea level (30 m / 98 ft) to approximately 1,600 m (5,249 ft). In suitable years, it contributes to spectacular desert wildflower displays.

Habitat and Ecology

This species thrives in desert washes, alluvial fans, dry streambeds, open flats, and gentle slopes within creosote bush scrub and Joshua tree woodland plant communities. It prefers well-drained, sandy or gravelly soils and sheltered microhabitats that protect against wind and extreme desiccation. As an annual, its population fluctuates dramatically with winter precipitation; it is a key component of “superbloom” events. The flowers provide nectar and pollen for native bees, butterflies, and other pollinators, while the foliage supports various caterpillars and the seeds are consumed by birds.

In summary, Eschscholzia glyptosperma exemplifies elegant desert adaptation—compact size, efficient water use, and brilliant, ephemeral blooms that signal the brief bounty of spring in the arid Southwest. Its presence in southern Nevada (including areas near Las Vegas) makes it a locally observable and ecologically important wildflower.