Desert Dandelion ( Malocothryx glabrata )

The Desert Dandelion, also commonly known as Smooth Desertdandelion, is a striking annual wildflower native to the arid regions of western North America. It belongs to the sunflower family and is renowned for forming vibrant carpets of yellow blooms in sandy desert landscapes following wet winters. This report details its scientific taxonomy, plant and flower morphology, habitat, range, distribution, and ecological characteristics, drawing from botanical sources such as regional floras and field guides.

Desert Dandelion ( Malocothryx glabrata ) Photo by James L Rathbun
Desert Dandelion ( Malocothryx glabrata ) Photo by James L Rathbun

Scientific Taxonomy and Categorization

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Clade: Asterids
  • Order: Asterales
  • Family: Asteraceae (Aster or Sunflower Family) – characterized by composite flower heads and milky sap in many genera
  • Genus: Malacothrix (Greek: “soft hair,” referring to the pappus on seeds)
  • Species: Malacothrix glabrata (A. Gray ex D.C. Eaton) A. Gray
  • Binomial Authority: Named by Asa Gray; the epithet “glabrata” refers to the nearly hairless (glabrous) leaves and stems.
  • Synonyms: Malacothrix californica var. glabrata
  • Common Names: Smooth Desertdandelion, Desert Dandelion

This dicotyledonous annual herb is categorized within the tribe Cichorieae (chicory tribe) of Asteraceae, featuring ligulate (strap-shaped ray) florets only, with no disk florets—distinguishing it from true dandelions (Taraxacum spp.).

Detailed Plant Description

Malacothrix glabrata is a low-growing to erect annual forb arising from a taproot. Plants reach 10–40 cm (4–16 inches) tall, with stems that are mostly glabrous (smooth), occasionally sparsely puberulent near the base, and branched proximally and distally. The stems may appear ascending or upright and contain milky latex sap, a hallmark of the Asteraceae family.

Leaves are primarily basal in a rosette, green, linear, and pinnately lobed with narrow, filiform (thread-like) or stringy segments (6.5–12.5 cm long). Cauline (stem) leaves are alternate, reduced upward, and similarly lobed. The foliage is nearly hairless, contributing to its “smooth” common name.

Detailed Flower Description

The inflorescences are solitary or 1–3 per stem, daisy-like composite heads measuring 2.5–6.5 cm (1–2.5 inches) wide (up to 4.5 cm or more). Each head consists of 31–139 ligulate ray florets (strap-shaped, 5-lobed at the tip) that are pale yellow to white, often with purple-tinged undersides. The receptacle is bristly, and the involucre (base) is campanulate to hemispheric, with 20–25+ phyllaries in 2–3 series and 12–20+ lanceolate bractlets with translucent margins at the base.

Immature or young flower heads often display a distinctive orange-to-red “button” or spot in the center (composed of developing structures). The flowers are fragrant and open primarily in the morning, closing by early afternoon. In mass blooms, they create showy yellow displays across the desert floor.

Desert Dandelion ( Malocothryx glabrata ) - Photo by James L Rathbun
Desert Dandelion ( Malocothryx glabrata ) – Photo by James L Rathbun

Fruit and Seeds

The fruit is a single-seeded cypsela (often called an achene), cylindro-fusiform (cylindrical and tapered at both ends), sometimes weakly 5-angled. It bears a pappus of soft hairs for wind dispersal. Seeds mature from March to June.

Habitat

This species thrives in coarse, fast-draining soils (gravel, loam, sand, silt) in open areas, among shrubs, or in vegetation gaps. Preferred habitats include sandy deserts, plains, mesas, rocky hillsides, washes, and flats, often associated with creosote bush (Larrea tridentata) communities. It also occurs in foothill woodlands and desert shrublands. Elevation range: below 2,000 m (6,500 ft). It is highly responsive to winter rainfall, becoming abundant in “good wildflower years.”

Range and Distribution

Malacothrix glabrata is native to the southwestern United States and northwestern Mexico. It occurs across the Mojave, Sonoran, and Great Basin Deserts.

U.S. States: Arizona (AZ), California (CA), Idaho (ID), Nevada (NV), New Mexico (NM), Oregon (OR), Utah (UT). Broader Range: Southwestern Idaho and eastern Oregon south to southern California, much of Arizona, and into Baja California and northwestern Mexico.

It is particularly common in the Mojave Desert (including areas near Las Vegas, Nevada) and intermountain regions. Sporadic records exist in the Colorado Plateau and Chihuahuan Desert fringes.

Ecology and Biology

As an annual, Malacothrix glabrata germinates in response to cool-season precipitation and completes its life cycle rapidly. Blooming occurs February–July (peak March–June), with fruits maturing soon after. It is primarily insect-pollinated (e.g., by solitary bees such as Nomadopsis spp.) but may be self-compatible. Seeds are wind-dispersed.

Ecologically, it serves as an important nectar source for butterflies, moths, bees, and other insects, and provides forage for wildlife including desert tortoises and small mammals. Indigenous groups (e.g., Apache) historically used roots medicinally. It is an indicator species for productive desert bloom seasons and shows no recognized subspecies or varieties. Chromosome number: 2n=14.

In summary, Malacothrix glabrata exemplifies desert adaptation with its ephemeral beauty, glabrous form, and reliance on sporadic rains. Its presence signals healthy desert ecosystems in the American Southwest.

San Bernardino National Forest

San Bernardino National Forest
San Bernardino National Forest

Spanning nearly 823,000 acres in the San Bernardino and San Jacinto mountain ranges, San Bernardino National Forest offers a stunning escape from Southern California’s urban bustle. From desert foothills at 2,000 feet to alpine peaks soaring over 11,000 feet, the forest features dramatic elevation changes, diverse ecosystems, and year-round recreation. It includes eight designated wilderness areas, two national monuments (Sand to Snow and Santa Rosa & San Jacinto Mountains), and some of the tallest mountains in Southern California.

Whether you seek peaceful nature immersion, thrilling outdoor adventures, or family-friendly outings, this forest delivers unforgettable experiences.

Iconic Points of Interest & Sites to See

  • Mount San Gorgonio (Old Grayback) — Southern California’s highest peak at 11,503 feet. Offers panoramic views and challenging hikes.
  • Mount San Jacinto — Towering at 10,834 feet with dramatic rises from the desert floor.
  • Big Bear Lake — A centerpiece for water activities, surrounded by pine forests and resorts.
  • Rim of the World Scenic Byway — A breathtaking 110-mile drive with sweeping vistas of mountains, valleys, and deserts.
  • Deep Creek Hot Springs — Natural thermal pools in a biodiverse canyon (strenuous hike required; follow all regulations).
  • Waterfalls — Big Falls and Bonita Falls, two of the tallest in the region.
  • Santa Rosa & San Jacinto Mountains National Monument — Features palm oases, rugged trails, and cultural significance.
  • Historic & Interpretive Sites — Cahuilla Tewanet, Barton Flats Visitor Center, and remnants of Gold Rush-era history like stamp mills and old cabins.

Activities for Every Season

Hiking & Backpacking Over 300 miles of trails, from easy interpretive paths to strenuous wilderness treks. Popular routes include:

  • Vivian Creek Trail to San Gorgonio Peak
  • Icehouse Canyon to Cucamonga Peak
  • Cougar Crest Trail and Castle Rock Trail (near Big Bear)
  • Pacific Crest Trail (PCT) section

Water Recreation

  • Boating, fishing, swimming, and waterskiing at Big Bear Lake, Silverwood Lake, and Lake Hemet.
  • Kayaking and paddleboarding on mountain lakes.

Winter Sports

  • Downhill skiing and snowboarding at Bear Mountain and Snow Summit.
  • Cross-country skiing, snowshoeing, and snowmobiling on designated trails.
  • Snow play areas.
Big Bear Lake covered in snow. Photo by James L Rathbun
Big Bear Lake covered in snow. Photo by James L Rathbun

Other Adventures

  • Off-Highway Vehicles (OHV): One of Southern California’s premier riding areas.
  • Mountain Biking & Horseback Riding: Extensive trails available.
  • Rock Climbing: World-class granite at Tahquitz and Suicide Rocks.
  • Camping: 42 developed campgrounds plus dispersed and Yellow Post sites.
  • Wildlife Viewing & Birdwatching: Diverse habitats support black bears, deer, mountain lions, and many bird species.
  • Fishing & Hunting: Streams and lakes stocked with trout; seasonal opportunities.

Plan Your Visit

  • Visitor Centers: Big Bear Discovery Center, Mill Creek Visitor Center, and Idyllwild area centers for maps, permits, and programs.
  • Adventure Pass: Required for parking at many recreation sites (purchase online or at vendors).
  • Best Times: Spring for wildflowers, summer for high-country hiking, fall for colors, winter for snow sports.
  • Safety Tips: Check weather and road conditions, stay on trails in wilderness areas, practice Leave No Trace, and be aware of fire restrictions.

San Bernardino National Forest — Where desert meets alpine wonder. Come for a day, stay for a lifetime of memories.

For the latest information, maps, and conditions, visit www.fs.usda.gov/sbnf or contact the Supervisor’s Office in San Bernardino.

Discover Your Wild Side in the San Bernardino Mountains!

San Bernardino National Forest Campgrounds

Applewhite Campground – San Bernardino National Forest

Peaceful Creekside Escape in San Bernardino National Forest San Bernardino National Forest Campgrounds Applewhite Campground is a charming, no-frills forested campground nestled in Lytle Creek…

Hanna Flats Campground

Hanna Flats Campground is located near Big Bear Lake is located in the San Bernardino mountains of California about 90 miles east of Los Angeles in southern…
Holcomb Valley Campground is located in a lush pine forest in Holcomb Valley, San Bernardino Mountains, California

Holcomb Valley Campground

Holcomb Valley Campground features 19 single-family campsites and is located along 3N16 in Holcomb Valley, just outside 0f Big Bear, in San Bernardino County, California.…
Big Bear Lake covered in snow. Photo by James L Rathbun

Serrano Campground

Serrano Campground is a campground with 108 campsites located near Big Bear Lake in San Bernardino, California. the campground is located just across the highway…

Ubehebe Crater

Ubehebe Crater (pronounced “you-bee-HEE-bee”) is one of the most striking and geologically dramatic features in Death Valley National Park, California. Located in the northern part of the park at the base of the Cottonwood Mountains (near the Racetrack Playa area), it is the largest and most prominent of a cluster of volcanic explosion craters known as the Ubehebe Craters or Ubehebe volcanic field. This maar-type crater stands out amid the park’s predominantly sedimentary and tectonic landscape as evidence of relatively recent volcanic activity in an otherwise arid, non-volcanic region.

Ubehebe Crater, Death Valley National Park, California
Ubehebe Crater, Death Valley National Park, California

Geological Description

Ubehebe Crater is a classic maar—a broad, shallow volcanic crater formed primarily by explosive phreatomagmatic eruptions (interactions between rising magma and groundwater). It measures approximately half a mile (about 0.8–1 km) in diameter and reaches depths of 500–777 feet (152–237 m), with steep, unstable inner walls composed of layered ejecta.

  • Formation Mechanism: The crater resulted from basaltic magma rising toward the surface and encountering groundwater in porous sedimentary rocks (primarily Miocene fanglomerates and sandstones). The intense heat caused the water to flash-boil into superheated steam, building enormous pressure. This triggered violent steam-driven explosions that fragmented and ejected large volumes of country rock (pre-existing sedimentary material) along with juvenile basaltic material. The blasts pulverized rock into ash, lapilli, bombs, and blocks, hurling them outward in pyroclastic surges and fallout deposits. Unlike typical lava-flow volcanoes, maar eruptions produce little to no sustained lava flows; instead, they create wide, low-angle rims of mixed ejecta.
  • Composition and Deposits: The ejecta blanket covers roughly 40 km² (15 mi²) around the craters. Deposits consist of approximately one-third basaltic scoria, bombs, and spatter (dark, fresh-looking volcanic material) and two-thirds comminuted fragments of older sedimentary rock (light-colored sandstone, conglomerate clasts). Layers alternate in color—dark basaltic ash and lighter sedimentary breccia—creating vivid banding visible on the crater walls and rim. Pyroclastic surge deposits (dense, ground-hugging flows of hot gas and debris) extend unusually far (up to 9–15 km in some directions, based on recent studies), preserved better here due to the arid environment with minimal erosion.
  • The Cluster: Ubehebe is the northernmost and youngest crater in a group of about 7–12 overlapping maars aligned roughly north-south over 1.5 km, with additional smaller vents east-west and isolated features. Smaller nearby craters include Little Hebe Crater (a nested or satellite maar) and others with tuff rings.
  • Age: Estimates vary due to challenges in dating young maars, but most recent research places the main eruptive sequence (including Ubehebe Crater) at approximately 2,100 years ago (around 100 BCE), based on radiocarbon dating, paleomagnetism, and stratigraphic studies. Earlier estimates ranged from 800–7,000 years old, with some suggesting the entire cluster formed in a brief period (weeks to months) from a single magmatic pulse rather than over centuries.

The eruptions exposed colorful underlying sedimentary layers, revealing Death Valley’s deeper geologic history of ancient lake beds, alluvial fans, and tectonic basin fill.

A Panorama looking from Ubehebe Crater overlooking the cinder fields, Death Valley National Park
A Panorama looking from Ubehebe Crater overlooking the cinder fields, Death Valley National Park

History of Discovery, Naming, and Study

  • Indigenous Context: The area lies within traditional territories of the Timbisha Shoshone people. “Ubehebe” derives from a Shoshone term possibly meaning “big basket” or “big hole in the ground,” reflecting the crater’s appearance. Indigenous knowledge of the landscape predates European-American exploration.
  • Euro-American Discovery: Prospectors and explorers encountered the crater in the late 19th/early 20th century amid Death Valley’s mining booms. It was noted for its dramatic appearance but not initially recognized as volcanic due to the region’s focus on gold, silver, and borax.
  • Scientific Recognition: Early 20th-century geologists identified its volcanic origin. Detailed studies intensified in the late 20th and early 21st centuries. Key research includes:
    • Stratigraphic and paleomagnetic work showing a short eruptive duration.
    • 2016 studies on the cluster’s sequence (phreatomagmatic followed by minor magmatic phases).
    • 2022 research (led by Greg Valentine, University at Buffalo) revealing wider pyroclastic surge runout than typical for maars, implying underestimated hazard zones around similar volcanoes worldwide. Deposits preserved far from the vent highlight risks in arid settings.
  • Modern Status: Ubehebe Crater is a popular, accessible viewpoint in Death Valley National Park. A paved road leads to a parking area and overlook at the rim, with a short trail along the rim offering panoramic views. The interior is extremely hazardous (loose, steep slopes prone to rockfall), and descent is prohibited without permits (rarely granted). It serves as an educational site illustrating explosive volcanism, groundwater-magma interaction, and recent geologic activity in a tectonically active region.

Ubehebe Crater stands as a youthful reminder that Death Valley’s geologic story is ongoing—its formation just a few millennia ago underscores the potential for future volcanic events in this dynamic landscape, even if probabilities remain very low. Visitors experience one of the park’s most otherworldly sights: a stark black-rimmed pit contrasting with multicolored badlands under vast desert skies.

Hiking

The road into Ubehebe serves as the starting points to the Race Track Valley Road, Teakettle Junction and Hunter Mountain Road.

There are a few separate hiking opportunities while exploring the crater.

The crater rim trail, which is about 1.5 miles long, circumnavigates the crater and allows access to Little Hebe crater. The trail has some slight elevation gain, however could be more difficult to hikes with balance issue due to the unstable soil.

There is also a trail down the the bottom of the crater. This is a short trail and very easy going down. The difficulty is hiking back up the 600 feet elevation lost on the way down, in loose volcanic soil.

Ubehebe Crater Trail Map

References

Doble California – San Bernardino Ghost Town

Doble is a near-forgotten ghost town and mining site located near the dry bed of Baldwin Lake, east of Big Bear Lake in the San Bernardino Mountains. It represents a later chapter in the region’s mining story, tied to the “second gold rush” of the 1870s.

In 1873–1874, brothers Barney and Charlie Carter discovered gold-bearing quartz on a hill overlooking Baldwin Lake (then part of Bear Valley). Word reached millionaire investor Elias J. “Lucky” Baldwin, a prominent figure from the Comstock Lode silver boom in Nevada. Baldwin acquired the claims, naming the site the Baldwin Mine (later Gold Mountain Mine). He invested heavily, building a 20-stamp mill in 1875 to process ore and surveying a townsite below the mine.

The town was initially called Bairdstown (possibly after an early partner or prospector) and later briefly Gold Mountain City or Bear Valley. By the mid-1870s, it boomed with saloons, hotels, restaurants, blacksmith shops, and residences—typical of Wild West mining camps. Fistfights, shootings, and a growing cemetery reflected the era’s lawlessness. A shelf road built by Chinese laborers improved access, hauling machinery through Holcomb Valley.

Despite the infrastructure, the ore proved low-grade and unprofitable. The mine and mill shut down after a few years, and the town was largely abandoned by the early 1880s. It sat dormant for about 17 years.

In the late 1890s–early 1900s, Baldwin’s son-in-law, Bud Doble (or possibly a relative/associate), reinvested, leading to a revival. A larger 40-stamp mill was constructed around 1900, and the town was renamed Doble. Operations continued intermittently into the early 20th century, with various owners attempting to extract gold. However, yields remained disappointing, and activity ceased by the mid-20th century (latest records around the 1940s).

Today, Doble is a true ghost town with scattered ruins: dilapidated wooden structures, mill foundations, tailings piles, shafts, and a small cemetery. The site is accessible via off-road trails like Holcomb Valley Road (high-clearance vehicles recommended). It’s part of the San Bernardino National Forest, popular for hiking and historical exploration, though vandalism has removed some markers over the years.

Doble Mine, San Bernardino County, 1930 - Photography by Adelbert Bartlett, UCLA Library Digital Collections
Doble Mine, San Bernardino County, 1930 – Photography by Adelbert Bartlett, UCLA Library Digital Collections

Doble Town Summary

NameDoble California
LocationBig Bear, San Bernarino, California
Also Known AsBairdstown, Gold Mountain
Latitude, Longitude34.2986169,-116.8216958
GNIS270883

History of Mining in the San Bernardino Mountains

The San Bernardino Mountains, part of the Transverse Ranges in Southern California, have a rich mining heritage primarily tied to gold, with significant activity in the 19th and early 20th centuries. Mining in this region was challenging due to rugged terrain, harsh winters with heavy snowfall, and limited water resources, yet it produced notable wealth, especially from placer and lode deposits.

Gold mining began in earnest in the 1860s, spurred by discoveries shortly after the California Gold Rush of 1849. The most prolific area was Holcomb Valley, north of modern Big Bear Lake. In May 1860, prospector William F. “Bill” Holcomb, while tracking a bear, discovered placer gold in a creek that now bears his name. This sparked Southern California’s largest gold rush, drawing thousands of miners. Holcomb Valley became the region’s top gold-producing district, yielding an estimated 350,000 troy ounces historically (valued at over $450 million in modern terms based on early 2010s prices), with potential untapped deposits.

A boomtown called Belleville quickly emerged near the discovery site, named after the first child born there. At its peak around 1861–1862, Belleville had a population of about 1,500–2,000, making it briefly the largest settlement in San Bernardino County. It featured saloons, stores, and even vied (unsuccessfully) to become the county seat. The town was notorious for its rough character—claim jumping, violence, and vigilante justice were common. Placer mining dominated initially, with miners panning streams and using sluices. By the late 1860s, as easy placer gold dwindled, operations shifted to hard-rock quartz mining, requiring stamp mills to crush ore.

Other notable mines in the mountains included the Mammoth, Olio, Pine Tree, Metzger, and Greenlead. Production peaked in the 1860s but declined rapidly due to low yields, difficult access, and environmental hardships. By 1870, most miners had left Holcomb Valley. Intermittent activity continued, including large-scale placer operations in the 1890s and dredging in the 1930s–1940s.

A “second gold rush” occurred in the 1870s around Baldwin Lake (then called Bear Valley), leading to the establishment of the town and mine discussed below. Overall, the San Bernardino Mountains’ gold era transitioned the area from mining to tourism and recreation by the early 20th century, with dams and roads built in the 1880s–1910s facilitating access to Big Bear Lake.

Today, remnants like tailings, shafts, and foundations are preserved in areas like Holcomb Valley (now a historic site with trails), but active gold mining has ceased. Modern extraction in the broader mountains focuses on industrial minerals like high-purity limestone and cement.

Doble Town Map

Referenes

Gold Mountain Mine – Gold Fever Trail

Gold Mountain Mine, also known as the Baldwin Mine or Lucky Baldwin Mine (originally Carters Quartz Hill), stands as one of the most significant gold operations in the Big Bear area of the San Bernardino Mountains. Located east of Big Bear Lake at coordinates approximately 34.3026°N, 116.8291°W, it overlooks Baldwin Lake and the former townsite of Doble. The mine represented the last major gold discovery in the region during the 1870s and highlighted the transition from placer to quartz mining.

The remains of Gold Mountain Mine, "Lucky Baldwin Mine" overlook the townsite of Doble and Baldwin Lake.
The remains of Gold Mountain Mine, “Lucky Baldwin Mine” overlook the townsite of Doble and Baldwin Lake.

Discovery and Early Development (1873-1875)

In 1873, brothers Barney and Charley Carter discovered the site while traveling to the Rose Mine for silver prospecting. Camping along the north shore of Baldwin Lake, Barney investigated a shiny quartz ledge on a hill, revealing rich gold ore. They claimed it as Carters Quartz Hill. This find came amid a broader context where placer gold in nearby streams had been noted since 1855, but harsh conditions limited early efforts. The Carters sold the claim to mining tycoon Elias J. “Lucky” Baldwin for $30,000, who invested an additional $250,000 to develop it. Baldwin, known from the Ophir Mine in Nevada, renamed it and employed up to 180 workers.

Chinese laborers played a key role, constructing roads from the mine to Cactus Flat and a five-mile flume with a 300-foot granite tunnel to supply water for processing. Their expertise in blasting and ditch-building was crucial, reflecting broader involvement of Chinese workers in quartz mining across the mountains. By 1876, a 40-stamp mill was operational, crushing ore for gold extraction via sluicing. The arrival of the Southern Pacific Railroad in Bear Valley boosted local prosperity, including the town of Belleville.

Operations and Challenges (1875-1895)

The mine ran for about eight months initially but faced a major setback in 1875 when Baldwin lost $2,500,000 in the Bank of California collapse, triggering a statewide economic downturn. Operations closed temporarily but reopened intermittently until 1895. Production figures are not precisely documented, but the site contributed to the region’s status as Southern California’s most productive gold district. In 1875, William F. Holcomb, whose 1860 discovery sparked the initial rush, returned to witness the decline of mining camps.

The Gold Mountain Mine
The Gold Mountain Mine

Later Years and Decline (1899-1940s)

In 1899, after resource depletion, J.R. DeLaMar partnered with Baldwin to build a second 40-stamp mill. The original mill operated until 1923, with hard-rock mining continuing until 1919. Various companies managed the site until the 1940s, but yields were disappointing overall. The mine’s concrete foundations and headframe remnants are still visible today.

Current Status and Legacy

Today, the dormant site lies within the San Bernardino National Forest, accessible mainly for hiking and part of the Gold Fever Off-Road Trail. It symbolizes the end of the major gold era in the mountains, with ongoing hobbyist mining in the broader area. The mine’s history underscores the economic volatility of 19th-century mining and the contributions of diverse laborers.

This report highlights how Gold Mountain Mine fits into the larger narrative of San Bernardino Mountains mining, which transformed the region from a frontier outpost to a key resource hub, leaving a lasting cultural and environmental legacy.

Overview of Mining in the San Bernardino Mountains

The San Bernardino Mountains, located in Southern California, have a storied mining history that dates back to the mid-19th century, driven primarily by gold discoveries amid the broader California Gold Rush era. This range, part of the larger Mojave Desert geophysical province, features rugged terrain with fault lines, basins, and arid conditions that influenced mining operations. Mining in the area encompassed a variety of commodities, including gold, silver, copper, lead, zinc, tungsten, borates, and limestone, with gold being the most widespread and economically significant. San Bernardino County, which includes these mountains, hosts over 3,000 documented mines, with approximately 1,585 listing gold as the primary commodity. The history reflects cycles of booms and busts tied to economic events, technological advancements, and global demands, such as those during World Wars I and II.

Early placer mining began in the 1840s and 1850s, with gold strikes in streams and valleys like Bear and Holcomb Valleys as early as 1849-1855, often initiated by prospectors following the California Gold Rush. The shift to hard-rock lode mining occurred as placer deposits depleted, supported by laws like the 1872 General Mining Act. Key districts included Holcomb Valley, Clark, Providence Mountains, and Calico, with operations involving shafts, adits, mills, and infrastructure like railroads and water systems. By 1902, the county had 301 hard-rock quartz mines, producing 45 mineral commodities. The Great Depression revived small-scale gold mining due to higher gold prices, while World War II focused on strategic minerals like tungsten and iron. Post-war activity declined, though sites like the Mountain Pass rare earth mine emerged in the 1950s. Today, remnants such as mine ruins, tailings, and historical landmarks persist, managed by entities like the Bureau of Land Management, facing threats from modern development and recreation.

The mountains are particularly noted for skarn gold deposits and high-purity placer gold, with historical recoveries in Holcomb Valley estimated at around 350,000 troy ounces (valued at $457,660,000 in 2013 prices). Remaining deposits may hold up to 700,000 troy ounces in unmined areas. Limestone mining continues as a major modern resource, with operators like Omya and Mitsubishi Cement extracting from the north slope.

Timeline of Key Mining Events in the San Bernardino Mountains

PeriodKey Events and Developments
1840s-1850sInitial placer gold discoveries in Bear and Holcomb Valleys (1849-1855); Mexican miners extract significant gold from placers in Bear Valley.
1860sMajor gold rush sparked by William F. Holcomb’s discovery in Holcomb Valley (1860); boomtowns like Belleville emerge with populations up to 1,500; largest gold strike in Southern California.
1870s-1880sShift to quartz mining; Gold Mountain Mine discovered (1873); stamp mills built; economic downturns like the 1875 Bank of California collapse affect operations; gold deposits largely exhausted by 1880s.
1890s-1910sIntermittent revivals with new technologies like cyanidation; hard-rock mining at Gold Mountain continues until 1919; borate and tungsten discoveries; steady activity until World War I.
1920s-1940sDecline due to low prices; Depression-era reworking of tailings; WWII focus on iron and tungsten; sporadic operations.
1950s-PresentRare earth mining at Mountain Pass; limestone extraction; hobbyist claims and historical preservation; over 2,000 active claims in Holcomb Valley.

Mine Summary

NameGold Mountain Mine
Also known asLucky Baldwin Mine,
Carters Quartz Hill
LocationSan Bernardino County, California
Latitude, Longitude34.3026, -116.8291
Gold Fever Off Road Trail Marker No.12

Gold Mountain Trail Map