Lost Burro Mine

The Lost Burro Mine is one of the best-preserved historic gold mining sites in Death Valley National Park, California. Located in a remote draw at the northern end of the mountain range separating Hidden Valley from Racetrack Valley (near Teakettle Junction in the Ubehebe Mining District), the mine sits in rugged terrain accessible only by high-clearance 4WD vehicles via a rough 1-mile dirt track off the Hidden Valley road. Its isolation has helped protect the site from vandalism, making it a fascinating glimpse into early 20th-century prospecting life.

The Lost Burrow Mine is located off Hunter Mountain Road in Death Valley National Park, CA
The Lost Burrow Mine is located off Hunter Mountain Road in Death Valley National Park, CA

Discovery (1907)

The story of the Lost Burro Mine began on April 18, 1907, with a classic tale of serendipity. Prospector Bert Shively, while searching for his stray burros in a remote canyon, picked up a rock intending to throw it at the animals to get their attention. Instead of tossing it, he noticed the rock was laced with visible free gold. Surface assays from the outcroppings reportedly ran from $40 to $1,000 per ton — incredibly rich values for the era.

Shively quickly filed six claims and partnered with others, securing options worth around $45,000. The accidental discovery turned the site into one of the most promising gold properties in the Ubehebe District (an area otherwise known more for lead, silver, and copper).

The Lost Burrow Mine
The Lost Burrow Mine

Early Development and Peak Years (1907–1910s)

Despite the financial panic of 1907, work continued at the Lost Burro, regarded as one of the richest claims in the district. Ore samples averaged high gold values (some reports cite up to $80–$1,450 per ton in early assays), and the mine attracted multiple ownership changes and optimistic plans.

By the 1910s, development included short tunnels along the vein, with ore intersections averaging $25 per ton in later reports. Foundations were laid for a five-stamp mill and cyanide plant, intended to process ore on-site, with water piped in from Burro Spring (about 7.5 miles northeast on Tin Mountain) via a 2-inch pipeline. Remnants of this pipeline — along with rusted oil drums, tin cans, old chairs, and other debris — still litter the site.

The mine’s greatest production likely occurred between 1912 and 1917, though official records are sparse. It stands out as the only exclusively gold-bearing property in the Ubehebe District.

Later Operations and Decline (1920s–1970s)

The mine changed hands several times over the decades and was worked intermittently. In 1942, claims were relocated, and further amendments occurred in 1948 and 1970. A small amount of recorded production (about 255 ounces of gold between 1935 and 1942) exists, but unofficial estimates suggest the total lifetime output may have approached $100,000 in gold value.

Operations wound down by the 1970s, and the site was eventually incorporated into Death Valley National Park, where all mining claims became inactive.

The cabin found at the Lost Burrow Mine is in good shape.
The cabin found at the Lost Burrow Mine is in good shape.

Modern Legacy

Today, the Lost Burro Mine features a remarkably intact wooden cabin (in good condition, with stories of a “curse” leading some visitors to return removed artifacts), an outhouse, multiple adits (some used for storage), a one-chute ore bin, mill foundations stairstepping down the hillside, scattered machinery (including a small retort/smeltor and sluice box remnants), and tailings piles.

The site’s remoteness — requiring a challenging 4WD journey often combined with trips to the nearby Racetrack Playa — has kept it well-preserved and largely free of modern vandalism. Visitors are reminded to leave everything as found, as the area is protected wilderness.

The Lost Burrow Mine cabin interior
The Lost Burrow Mine cabin interior

The Lost Burro Mine remains a testament to the tenacity of Death Valley prospectors — turning a frustrated burro chase into a legendary gold story in one of the harshest environments on Earth. Always check current road conditions and permits with the National Park Service before visiting!

Lost Burro Mine Video

Lost Burro Mine Trail Map

Lippincott Mine

The Lippincott Mine (also known as the Lead King Mine) is a historic lead-silver mine located in the remote southwestern corner of Racetrack Valley within Death Valley National Park, California. Situated in the Ubehebe Mining District on the ridge separating Racetrack Valley from Saline Valley, the site represents one of the area’s more productive small-scale mining operations in the early-to-mid 20th century. Today, it features scattered ruins, adits (horizontal mine entrances), tailings piles, and remnants of mining infrastructure, though much has deteriorated over time. Visitors often access it via rough off-road routes, including the infamous Lippincott Mine Road.

The remains of the Lippencott Mine at the southern end of Race Track Valley.
The remains of the Lippencott Mine at the southern end of Race Track Valley.

Discovery and Early Development (1906–1910s)

The Lippincott Mine was discovered in 1906, with significant development work beginning around 1908. Located in a harsh, water-scarce desert environment, the mine targeted rich lead-silver deposits (primarily galena ore). Early ore samples showed impressive grades, often yielding around 42% lead and 8 ounces of silver per ton, making extraction economically viable despite the remote location.

The mine saw its most productive period during World War I, when demand for lead (used in ammunition and other wartime materials) surged. Miners reportedly used the flat, dry surface of the nearby Racetrack Playa as an improvised landing strip for small aircraft, aiding in supply transport and oversight.

World War II Era and Post-War Operations (1940s–1950s)

Operations ramped up again during World War II, with development of the Lead King Mine (under the Lippincott family) beginning in May 1942. A small crew of about eight miners extracted high-grade silver-lead ore, which was trucked out to Goldfield, Nevada, then railed to smelters in Utah. Only the richest ore was shipped due to challenging logistics — the silver was particularly valuable for wartime storage batteries.

Despite high ore quality (some reports cite up to 63% lead and 35 ounces of silver), federal restrictions shut down operations during the later war years as part of resource conservation efforts. The Lippincott family resumed work from 1946 to 1951, constructing additional infrastructure like a mine camp with wood and tarpaper cabins, an ore tipple, and possibly a tramway system.

Water scarcity remained a major challenge — supplies had to be trucked in over long distances — and this likely contributed to the eventual closure. Limited activity may have continued sporadically into the 1970s under later owners like George Lippincott Jr.’s Polaris Battery Company, which considered further exploration in 1974.

Looking down at the Lippencott Mine Road from the Lippencott Mine, with Saline Valley in the distance.
Looking down at the Lippencott Mine Road from the Lippencott Mine, with Saline Valley in the distance.

Legacy and Modern Significance

The Lippincott Mine is now part of Death Valley National Park, where all mining claims are inactive, and the site is protected as a historic resource. Ruins include adits (some gated for bat protection), scattered timbers, old vehicle parts, and tailings piles — visitors should avoid disturbing soil or inhaling dust due to potential residual lead contamination.

The mine’s access road — the steep, narrow, and extremely challenging Lippincott Mine Road (also called Lippincott Pass) — was originally built in 1906 to reach the site. This 7-mile route from Saline Valley to Racetrack Valley features sheer drop-offs, tight switchbacks, and rough terrain, making it one of Death Valley’s most notorious 4WD trails (high-clearance 4WD with experienced drivers only; uphill traffic has right-of-way).

The Lippincott Mine stands as a testament to the tenacity of early 20th-century prospectors in one of the harshest environments on Earth, contributing to the broader mining history of Death Valley that includes gold, silver, borax, and other metals. While not as famous as sites like Rhyolite or the Keane Wonder Mine, it remains a fascinating, off-the-beaten-path destination for adventurous visitors exploring Racetrack Valley’s moving rocks and remote wilderness. Always check current road conditions with the National Park Service before attempting access!

Ubehebe Lead Mine

The Ubehebe Lead Mine is located just west of theRacetrack Playa Road off of the Bonnie Claire Road.  Discovered in 1906, the mine is located on the west side of the Racetrack valley just south of Teakettle junction.    The site was started as a copper mine and during to coarse of its operation would produce lead, copper, gold and zinc.

Ubehebe Lead Mine Trail sign located just off of the Racetrack, Death Valley, CA
Ubehebe Trail sign located just off of the Racetrack, Death Valley, CA

Early Discovery and Initial Interest (1875–Early 1900s)

The deposit was first discovered by copper prospectors in 1875, with surface samples reportedly assaying as high as 67% copper. However, the extreme remoteness, lack of water, and poor transportation made development unfeasible at the time. The area saw little activity until the early 1900s, when rising copper demand (driven by widespread electrification) sparked renewed interest in Death Valley’s mineral prospects.

Ubehebe Mine with tramway visible at the top of the hill, Death Valley, CA
Ubehebe Mine with tramway visible at the top of the hill, Death Valley, CA

Boom Period and Jack Salsberry’s Involvement (1906–1908)

The modern era began in 1906, when the site gained attention amid the broader mining excitement in the region (including the short-lived Greenwater copper boom). Promoter Jack Salsberry (who later had Salsberry Pass named after him) acquired the property, built access roads from Ubehebe Crater, and promoted ambitious plans — including a proposed Bonnie Claire & Ubehebe Railroad to haul ore to Nevada rail lines. Some hype even linked it to legendary “Lost Spanish Mine” tales.

In February 1908, miners uncovered a thick vein of lead ore (described as up to eight feet wide), shifting focus from copper to lead and prompting the name change to Ubehebe Lead Mine. The first recorded production came that year, with shipments including 491 ounces of silver. Enthusiasm led to stockpiling 26,000 pounds of supplies for an eight-man crew, but assays and processing yielded far lower values than expected.

Exploring the Ubehebe Mine tails pile, Death Valley, CA
Exploring the Ubehebe Mine tails pile, Death Valley, CA

Intermittent Operations (1910s–1950s)

Production remained sporadic due to isolation, high transport costs, and inconsistent ore grades. Key highlights include:

  • 1916: Peak year, with 254 tons of 15% lead ore shipped.
  • 1930s: Successive lessees cleaned out old stopes; in 1937, operator Sol Camp attempted revival amid rising lead prices, contracting hauls to Death Valley Junction for shipment to Utah smelters.
  • 1940s–1950s: Activity continued on a small scale, with shipments in 1951 (averaging 13.8% lead, 4.93% zinc, 3.47 oz silver/ton) and 1952 (12.4% lead, 12.4% zinc, plus silver, copper, and gold). Total historical output from the broader Ubehebe Peak area (1908–1951) included thousands of tons of ore yielding significant lead (over 2.6 million pounds), plus zinc, silver, copper, and minor gold.

The nearby area also saw World War II use for aerial gunnery practice.

Decline and Modern Status

Operations wound down by the mid-20th century, with some reports of activity into the late 1960s. The mine never became a major producer due to logistical challenges. It is now within Death Valley Wilderness on National Park Service land — closed to mining, with no plans for reopening. The site serves as a fascinating (but dangerous) historical remnant of Death Valley’s mining era.

Looking back at the jeep, Death Valley National Park, CA
Looking back at the jeep, Death Valley National Park, CA

The Ubehebe Lead Mine exemplifies the boom-and-bust pattern typical of Death Valley mining: high hopes fueled by rich surface showings, dashed by the desert’s unforgiving realities. Access requires high-clearance (often 4×4) vehicles via the rough Racetrack Road — check current conditions with the National Park Service before visiting!

Ubehebe Mine Trail Map

Death Valley Campgrounds

Death Valley National Park

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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.

Looking into a perfect mirror image on Lake Many in January 2026.  Photo by James L Rathbun
Looking into a perfect mirror image on Lake Many in January 2026. Photo by James L Rathbun

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!

Telescope Peak's reflection in the calm wates of Lake Manly, Death Valley National Park. Photo by James L Rathbun
Telescope Peak’s reflection in the calm wates of Lake Manly, Death Valley National Park. Photo by James L Rathbun

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!

The hills next to Badwater turn green with the rains which cause Lake Manly.  The sea sevel sign is visible high in the rocks on the the right.  Photo by James L Rathbun
The hills next to Badwater turn green with the rains which cause Lake Manly. The sea sevel sign is visible high in the rocks on the the right. Photo by James L Rathbun

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.