Big Bear, CA
I quiet mountain community full of back country adventure.
Lake Manly
Lake Manly is a rare and ephemeral lake that occasionally forms in Badwater Basin, the lowest point in North America at 282 feet (86 meters) below sea level, located in Death Valley National Park, California. This temporary body of water revives an ancient Pleistocene lake that existed during the Ice Age, when it reached depths of up to 700 feet and stretched nearly 100 miles long.
In recent years, including dramatic appearances after Hurricane Hilary in 2023, atmospheric rivers in 2024, and record-breaking fall rains in late 2025 (with more precipitation than an entire typical year), the basin has flooded to create a shallow lake — sometimes just inches deep, other times up to a few feet — allowing rare reflections and even temporary kayaking opportunities.
Badwater Basin itself is a surreal, otherworldly landscape dominated by expansive salt flats covering nearly 200 square miles. The surface is primarily sodium chloride (table salt), along with minerals like calcite, gypsum, and borax. The name “Badwater” comes from a small spring-fed pool near the road that’s extremely salty and undrinkable.
History of the lake
Lake Manly, gets its name from William Lewis Manly, a pioneer and hero of the 1849 California Gold Rush era.
In late 1849, a group of emigrants (known as the “Lost ’49ers”) took a risky shortcut to reach the gold fields and became stranded in the brutal heat and dryness of what would later be called Death Valley. William Lewis Manly, along with John Rogers, volunteered to walk out of the valley on foot to seek help. They trekked hundreds of miles across harsh desert terrain, eventually reaching safety, obtaining supplies, and returning to rescue the remaining group (including families like the Bennetts and Arcans) — saving their lives.
In honor of his bravery and lifesaving efforts, geologists named the prehistoric pluvial lake that once filled much of Death Valley after him. The name “Lake Manly” was formally coined in 1932 (sometimes misspelled as “Manley” in older sources, but Manly is correct). There’s even a proposed alternate name “Lake Rogers” for a potential northern section, after his companion, but “Manly” became the standard term used in scientific literature and by the National Park Service.
The lake itself is a remnant of wetter Ice Age periods (especially around 185,000–128,000 and 35,000–10,000 years ago), when glacial meltwater fed massive inland waters. Today, it only reappears briefly after extreme rainfall events — like the record storms in recent years that turned Badwater Basin into a shallow, reflective lake again.
It’s a fitting tribute: the name connects one of the valley’s most famous human survival stories to its deep geological past of water in a place infamous for being bone-dry!
Conditions That Cause Lake Manly’s Formation
Death Valley is one of the driest and hottest places on Earth, averaging only about 2 inches of rain per year with evaporation rates exceeding 150 inches annually. This extreme aridity normally keeps Badwater Basin as a dry salt pan.
The lake forms only during rare, extreme rainfall events — such as remnants of tropical storms (e.g., Hurricane Hilary in 2023), powerful atmospheric rivers, or record-setting seasonal storms — that deliver several inches of rain in a short time. Runoff from surrounding mountains floods the endorheic (closed) basin, which has no outlet, creating a temporary lake. The water eventually evaporates rapidly under the intense heat and low humidity, returning the area to its characteristic salt flats — often within months.
This fleeting phenomenon highlights how even the harshest deserts can dramatically change with unusual weather patterns!
Winter 2026
Lake Manly is formed following several days of rain, so we opted to drive out to the park for a visit. Our first visit is cut short from a rain storm and flash floods which caused the road to be covered with flood levels. We made the drive from Vegas the next weekend, and were floored by the views of Lake Manly covering the salt flats of Badwater Basin. The walk out to the lake shore is about 1/4 of a mile from the Badwater parking lot.
On our visit, the lake surface is deathly still and the other visitors were silent giving us the feeling of isolation despite their being other travelers. This is my first visit to Lake Manly, and will certainly not be my last, if I am able to arrange the trip.
Billie Mine
The Billie Mine (also known as Billie I and Billie II) is a former underground borate mine located in the Furnace Creek Mining District of Death Valley National Park, Inyo County, California. Situated on the eastern slopes of the Black Mountains overlooking Death Valley, the mine’s surface structures—including the prominent steel headframe, shaft collar, support buildings, and waste rock dumps—are positioned just outside the park boundary along the paved Dante’s View Road, approximately 1.5 miles northwest of the historic ghost town of Ryan and 12 miles southeast of Furnace Creek. However, the rich borate ore body itself extends underground into park lands, with the mine portal offset about 1,500 feet west on Bureau of Land Management property to comply with environmental regulations under the Mining in the Parks Act of 1976.
The site sits in a stark, arid landscape typical of Death Valley: barren alluvial fans sloping down from rugged, basalt-capped ridges, dotted with creosote bush and sparse desert vegetation. The ore body, embedded in the Miocene-Pliocene Furnace Creek Formation, consists primarily of calcium borates such as colemanite, along with probertite and ulexite. Geologically, the deposit is lens-shaped, striking northeast with a southeast dip of 20–40 degrees, averaging 700 feet wide, 3,700 feet long down-dip, and 150 feet thick. Mining involved deep vertical shafts (reaching depths of around 1,200 feet) and long-hole stoping methods with backfilling to maintain stability, leaving tall, narrow pillars critical to the underground structure.
Today, the abandoned mine features a towering headframe silhouetted against the vast valley panorama, evoking the industrial intrusion into this remote wilderness. Visitors driving to Dante’s View often pause for photos, but the site is gated and off-limits—mines in the park are hazardous due to unstable shafts, toxic tailings, and potential collapses.
The Billie Mine’s history is intertwined with Death Valley’s long borax legacy, but it represents a modern chapter amid growing conservation efforts. Borate deposits in the Furnace Creek area were known since the late 19th century, exploited by the Pacific Coast Borax Company at nearby sites like the Lila C. and Widow mines near Ryan. However, after discovering richer sodium borates (kernite) at Boron in 1926–1927, operations in Death Valley largely ceased as companies shifted to more profitable locations.
Interest in the Billie deposit revived in the mid-20th century. In 1958, the Kern County Land Company staked claims and conducted drilling. Development accelerated in the 1970s: after the Mining in the Parks Act of 1976 restricted new claims and imposed strict environmental reviews, valid pre-existing operations like Billie were allowed to proceed with mitigation. Construction began in 1977 under a partnership that became the American Borate Company (initially involving Owens Corning Fiberglass and Texas United, later fully Owens Corning).
The mine reached ore in 1980 and became fully operational shortly after, extracting high-quality colemanite crystals (some large and collectible) alongside probertite and ulexite. Ore was trucked to processing plants in Dunn Siding, California, or Lathrop Wells, Nevada. For over a decade following the 1994 expansion of Death Valley to national park status, the Billie Mine was the only active mine within park boundaries, operating under rigorous National Park Service oversight to minimize surface disturbance.
Production continued into the early 2000s, but economic factors, declining demand, or resource depletion led to closure in 2005—marking the end of all mining in Death Valley National Park. In 2011, American Borate donated related patented claims (including parts of the Billie and nearby Boraxo sites) to the NPS, further securing the area’s protection.
The Billie Mine stands as a poignant reminder of Death Valley’s mining era: born from persistent exploration in a protected landscape, it bridged historic borax booms with modern environmental constraints, ultimately yielding to preservation in one of America’s most extreme and iconic wildernesses.
Belmont Nevada – Nye County Ghost Town
Belmont is a historic ghost town in Nye County, central Nevada, located in the Toquima Range along former State Route 82, about 45 miles northeast of Tonopah. Today, it remains a well-preserved “living ghost town” with a handful of residents, restored buildings, and ruins that attract history enthusiasts. The entire town site was added to the National Register of Historic Places in 1972, and it is Nevada Historical Marker number 138.
Discovery and Boom Years (1865–1880s)
Silver ore was discovered in the area in 1865 by Native American prospectors, leading to a major strike that established the town in the Philadelphia (or Silver Bend) mining district. High-grade surface ores, assaying up to $3,000 per ton, sparked a rush in 1866, drawing miners from camps like Austin and Ione.
By 1867, Belmont had grown rapidly and became the Nye County seat, a role it held until 1905. The town boasted substantial brick and wood-frame buildings—uncommon in arid Nevada—thanks to local access to wood, water, rock, and clay. Amenities included:
- Four stores
- Two saloons
- Five restaurants
- A post office (operating 1867–1911, briefly reopened 1915–1922)
- Assay office
- Bank
- School
- Telegraph office
- Two newspapers (including the Belmont Courier)
- Blacksmith shop
It also featured a Chinatown, red-light district, racetrack, churches, and the famous Cosmopolitan Saloon and Music Hall, which hosted entertainers from across the country.
Population estimates at its peak in the 1870s varied widely, from 2,000 to as high as 15,000 (though the latter is likely exaggerated, as Nye County’s total population remained low).
Mining Operations
Belmont’s economy centered on silver mining, with additional production of copper, lead, and antimony. The district’s ores were high-grade but shallow, primarily silver chloride (cerargyrite) above the water table.
Key operations included:
- Multiple mills, peaking at six
- The Monitor-Belmont Mill (started 1873)
- Combination Mill
- Cameron Mill
A 20-stamp mill was built early on, and by 1868, five sawmills supported construction and mining. Total production from the district is estimated at $15 million (in 19th-century values), with the bulk occurring between 1866 and 1887. The mines dominated Nye County’s silver output during the peak.
The town gained a rowdy reputation, with saloon brawls, shootings, vigilante actions, and feuds common in its early days.
Decline and Later Years (1880s–Present)
A brief lull hit in 1868–1869 as miners chased new rushes (e.g., White Pine district), but production revived in the 1870s. By the late 1880s, falling silver prices, lower-grade ores, and dewatering costs forced most mines to close around 1887–1890.
The county seat moved to Tonopah in 1905 after that town’s boom. Minor revivals occurred:
- 1907–1908 (tailings rework)
- 1914–1917 (Monitor-Belmont Company at Cameron Mill)
- Early 20th-century dump reprocessing
By 1900, only a few businesses remained, and the population dwindled. Unlike many Nevada ghost towns, Belmont was never fully abandoned—a small population prevented vandalism and salvaging.
In the mid-20th century, Rose Walter, a tough local resident known as the “Lady Guardian,” watched over the town; an unconfirmed story claims she once evicted Charles Manson and his followers from the courthouse.
Today, Belmont has a tiny year-round population, seasonal businesses like Dirty Dick’s Belmont Saloon, and ongoing preservation efforts.
Belmont Town Summary
| Name | Belmont Nevada |
| Location | Nye County, Nevada |
| Newspaper | Silver Bend Reporter Mar 30, May 11, 25, 1867;July 29, 1868 Mountain Champion June 3, 1868 – Apr 24, 1869 Belmont Courier Feb 14, 1874 – Mar 2, 1901 |
Several notable Nevadans tied their early careers to Belmont’s mining scene:
- Tasker Oddie → Prospected and worked in the area; later became Nevada’s 12th governor (1911–1915) and a U.S. Senator.
- Jim Butler → Involved in local mining; discovered the Tonopah silver strike in 1900, sparking that boom.
- Jack Longstreet → Gunfighter and prospector who participated in early history.
- Andrew Maute → Early miner with local ties.
The town’s iconic 1876 Nye County Courthouse, a two-story brick structure, stands partially restored (efforts by the Friends of the Belmont Courthouse after Nye County took ownership in 2012). Nearby mill ruins, like the tall Monitor-Belmont chimney (once used for target practice), and preserved buildings like the Philadelphia House evoke its silver rush heyday.
Belmont exemplifies Nevada’s classic boom-and-bust mining story: a brief, prosperous era fueled by silver, followed by quiet preservation amid the desert landscape.
Belmont Nevada State Historic Marker Text
Belmont sits at an elevation of 7,400 feet. A spring flowing year round made this a gathering site of the Shoshone Indians for rabbit drives and celebrations.
In 1865, silver ore discoveries led to the development of an attractive tree-shaded mercantile community. East Belmont became the mining and milling center. A wide range of nationalities worked the mines, operated businesses, and provided services. At its height, Belmont had schools, churches, a post office, and a newspaper, as well as a Chinatown, a red-light district, and a racetrack. The town was the Nye County seat from 1867 to 1905, and a courthouse survives from this period.
Belmont had a reputation as a rowdy town. Incidents of saloon brawls, vigilante actions, shootings, hangings, and feuds made the town notorious. Well known Nevadans such as Jack Longstreet, Tasker Oddie, Jim Butler, and Andrew Maute all participated in local early history.
Silver production totaling four million dollars was from high grade but shallow ore. By 1890, most mines ceased to be profitable and were forced to shut down. Belmont’s population dwindled as most residents left for new discoveries in nearby mining towns.
STATE HISTORIC MARKER No. 138
STATE HISTORIC PRESERVATION OFFICE
Nevada State Historic Marker Summary
| Name | Belmont |
| Location | Nye County, Nevada |
| Nevada State Historic Marker | 138 |
| Latitude, Longitude | 38.5959, -116.8755 |
Belmont Trail Map
Belmont Newspapers
Belmont Courier NewspaperThe Belmont Courier newspaper was a weekly newspaper published in Belmont, Nye County, Nevada, from February 14, 1874, to March 2, 1901. Operating during the… |
Mountain Champion NewspaperThe Mountain Champion Newspaper was a short-lived but significant newspaper published in Belmont, Nevada, during the late 1860s. Operating in a bustling mining region, it… |
Silver Bend Reporter NewspaperThe Silver Bend Reporter newspaper emerged in Belmont, Nevada, a mining town in Nye County that became a hub of activity following the discovery of… |
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 Town Summary
| Name | Doble California |
| Location | Big Bear, San Bernarino, California |
| Also Known As | Bairdstown, Gold Mountain |
| Latitude, Longitude | 34.2986169,-116.8216958 |
| GNIS | 270883 |
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.
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.
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
| Period | Key Events and Developments |
|---|---|
| 1840s-1850s | Initial placer gold discoveries in Bear and Holcomb Valleys (1849-1855); Mexican miners extract significant gold from placers in Bear Valley. |
| 1860s | Major 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-1880s | Shift 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-1910s | Intermittent 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-1940s | Decline due to low prices; Depression-era reworking of tailings; WWII focus on iron and tungsten; sporadic operations. |
| 1950s-Present | Rare earth mining at Mountain Pass; limestone extraction; hobbyist claims and historical preservation; over 2,000 active claims in Holcomb Valley. |
Mine Summary
| Name | Gold Mountain Mine |
| Also known as | Lucky Baldwin Mine, Carters Quartz Hill |
| Location | San Bernardino County, California |
| Latitude, Longitude | 34.3026, -116.8291 |
| Gold Fever Off Road Trail Marker No. | 12 |