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

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

Emigrant Campground

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Furnace Creek Campground

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Mahogany Flat Campground

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Mesquite Springs Campground

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Texas Springs Campground

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Thorndike Campground

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

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Photograph of the "Baby Gauge" (aka "Baby Gage") mine train at the mining camp of Ryan, Death Valley, ca.1900-1950. A car with one headlight can be seen at center on tracks pulling a platform with four benches upon it. Someone can be seen driving the car, while four men and women sit on the benches. A small wooden shack with a portion of the roof missing can be seen behind the platform, while a ladder, wooden planks, and more tracks are visible at left. A valley and mountains can be seen in the background. - “University of Southern California. Libraries” and “California Historical Society” as the source. Digitally reproduced by the USC Digital Library.

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

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Greenwater California – Inyo County Ghost Town

In the scorched embrace of the Funeral Mountains, where the Mojave Desert meets the unrelenting heat of Death Valley, lies the spectral outline of Greenwater—a fleeting copper boomtown that flickered to life in the shadow of California’s most infamous wilderness. Perched at approximately 3,500 feet in Greenwater Valley, about 27 miles southeast of Furnace Creek and just over the Nevada border from the Bullfrog Mining District, Greenwater embodied the raw ambition of early 20th-century prospectors. Named for the verdant spring that promised life amid the barren talus slopes and creosote flats, the town rose from two rival camps—Kunze and Ramsey—only to collapse under the weight of unprofitable veins and economic turmoil. Its story is one of explosive speculation, where over $15 million in investments poured into a district yielding little more than oxidized malachite and investor regret. This report traces Greenwater’s turbulent history, its vital ties to neighboring outposts like Rhyolite and Beatty, the lifeline of railroad aspirations, and the mines that lured—and ultimately betrayed—thousands to this unforgiving frontier.

Greenwater Mining District, CA 1906
Greenwater Mining District, CA 1906

Early Discoveries and the Spark of the Boom (1880s–1905)

The Funeral Range, a jagged volcanic spine etched by ancient fault lines, had long guarded its mineral secrets. As early as the 1880s, prospectors whispered of copper outcrops staining the canyon walls with turquoise hues, but the site’s isolation—over 50 miles from the nearest railhead and besieged by summer temperatures exceeding 120°F and winter freezes that cracked water barrels—stifled development. Water, the desert’s cruelest commodity, cost $15 per barrel, hauled by mule teams from distant springs, while the nearest civilization was a grueling three-day trek across the Amargosa Desert.

The tide turned in 1904, when the gold rush in Nevada’s Bullfrog District—ignited by Shorty Harris’s quartz strike near present-day Rhyolite—drew adventurers southward. Prospectors spilling over from Beatty and Rhyolite stumbled upon rich copper oxides near Greenwater Spring, a rare oasis where alkali flats gave way to mineralized breccias. Frank McAllister and Arthur Kunze staked the first claims in late 1904, founding Kunze Camp atop the ridge at 4,000 feet, where a modest cluster of tents sprouted amid the piñon and Joshua trees. By spring 1905, rival Harry Ramsey platted a lower site in the valley floor, dubbing it Copperfield or Ramsey, three miles downhill for easier wagon access. These embryonic outposts, fueled by tales of “picture ore” assaying 20–30% copper, marked the prelude to frenzy, as stages from Beatty rattled in with wide-eyed speculators clutching stock prospectuses.

Greenwater California 1907
Greenwater California 1907

Boomtown Rivalry and Rapid Expansion (1906–1907)

By August 1906, the merger of Kunze and Ramsey birthed Greenwater proper, a canvas metropolis swelling to 2,000 souls in the blink of an eye. Tents blanketed the valley like a vast encampment, housing saloons belching forth raucous laughter and the acrid smoke of hand-rolled cigarettes, alongside assay offices tallying assays that fueled Wall Street dreams. The Death Valley Chuck-Walla, a satirical broadsheet, skewered frauds and boosters alike, its pages alive with cartoons of “copper kings” and exposés of wildcat schemes. A post office opened in October, the Greenwater Banking Corporation erected a two-story frame edifice, and the Tonopah Lumber Company hauled in 150,000 board feet to frame hotels, stores, and a nascent red-light district. Main Street lots fetched $500–$5,000, with over 2,200 platted in 130 blocks, while a justice of the peace and constable imposed a veneer of order amid the chaos of claim-jumpers and saloon brawls.

Seventy-three companies incorporated, backed by titans like Charles Schwab (Greenwater United Copper) and F.M. “Borax” Smith, injecting $15–30 million into shafts piercing the rhyolite and tuff. Nearby Furnace, a tent city three miles west founded by Patsy Clark’s Furnace Creek Copper Company, boomed in parallel, its post office flickering from March 1907 to February 1908. Yet, beneath the bustle, cracks formed: water scarcity forced reliance on hauled barrels, and the first assays revealed shallow oxides giving way to barren ash below 200 feet.

Greenwater California
Greenwater California

Ties to Surrounding Towns: A Web of Supply and Speculation

Greenwater’s isolation bred dependence on its Nevada neighbors, forging a symbiotic yet strained network across the state line. Rhyolite, 35 miles north in the Bullfrog Hills, served as the primary gateway; its gold-fueled boom—peaking at 10,000 residents—drew the initial rush southward, with stages from Rhyolite’s depot ferrying prospectors over Daylight Pass in three bone-jarring days. Beatty, five miles east of Rhyolite and straddling the Amargosa River, emerged as the crucial freight hub, its Montgomery Hotel and saloons provisioning Greenwater’s miners with whiskey, beans, and dynamite via mule trains. Amargosa, a nascent stop three miles west of Rhyolite, briefly thrived as a waystation for Greenwater-bound wagons, its store and blacksmith echoing with the clamor of ore sacks.

This interdependence cut both ways: Greenwater’s copper fever siphoned capital from Bullfrog’s gold fields, irking Rhyolite operators who watched investors pivot south. When Rhyolite’s mines faltered in 1907, its salvaged timbers and machinery migrated to Greenwater, only to be abandoned there in turn. Furnace Creek, 27 miles west in Death Valley proper, supplied scant water and borax lore from “Borax” Smith’s operations, while distant Tonopah and Goldfield funneled speculative stock sales eastward. In essence, Greenwater was a peripheral bloom on the Bullfrog stem, its vitality borrowed from Nevada’s gold rush until both withered.

Train Stops and the Elusive Iron Horse

Railroads were Greenwater’s siren song, promising to conquer the desert’s tyranny. The Tonopah & Tidewater Railroad (T&T), chartered in 1904 by “Borax” Smith to link his Death Valley borax works to Ludlow, California, snaked northward from the Santa Fe mainline, reaching Crucero in 1906 and Death Valley Junction by 1907. Its 160-mile grade skirted Greenwater Valley, with a proposed branch eyeing the copper camps; surveyors plotted routes from Beatty (via the Las Vegas & Tonopah) and Amargosa, but the Panic of 1907 derailed ambitions.

The Tonopah & Greenwater Railroad, incorporated in March 1907, vowed a 50-mile spur from the T&T at Amargosa, complete by July, but it never broke ground. Greenwater’s fate hinged on Ramsey’s lower site for its gentler gradient—saving millions in grading—yet no spike was driven. The T&T’s northern terminus at Gold Center, south of Beatty, became a nominal “stop” for Greenwater freight, but wagons remained king, groaning under 20-ton loads across rutted trails. The railroads’ ghosts linger in graded beds now traced by off-roaders, a testament to promises unfulfilled.

The Mines: Copper Dreams and Barren Realities

Greenwater’s 2,500 claims riddled the Funeral Range’s east face, targeting oxidized copper in brecciated rhyolite—malachite and azurite staining faults amid quartz veins. The Furnace Creek Copper Mine, Greenwater’s crown jewel under Patsy Clark, plunged 200 feet, shipping 20 tons of 20% ore in early 1906 before hitting sterile ash. Schwab’s Greenwater United Copper, capitalized at $5 million, tunneled aggressively, as did the Greenwater Death Valley Copper Company, whose 73 rivals blanketed the valley in a frenzy of drywashers and adits.

Production was a mirage: sporadic shipments in 1916–1918 and 1929 gleaned $10,000 from dumps during copper spikes, but no mine achieved sustained output. The Greenwater Mine yielded one carload in 1916; others, like the Hallelujah and Hidden Valley groups, idled as shafts revealed low-grade sulfides untreatable without a smelter. Fraud tainted the boom—four companies exposed as scams—yet the district’s geology, a cap of shallow oxides over deep barren rock, doomed it utterly. Tailings scar the slopes today, silent witnesses to ambition’s folly.

Decline and Desertion (1907–1920s)

The Panic of 1907 struck like a Mojave dust storm, crashing copper stocks and halting infusions; by summer, saloons shuttered, and the Chuck-Walla fell silent. Guggenheim engineers, inspecting Furnace Creek, pronounced the veins pinched out, triggering a mass exodus—tents folded, wagons creaked northward to Rhyolite’s own ruins. By January 1908, only 50 lingered amid one saloon’s dying echoes; the post office closed in 1908, and Furnace followed suit. Sporadic revivals in World War I’s copper hunger yielded scraps, but by the 1920s, Greenwater devolved into a winter haven for “desert rats”—grizzled prospectors swapping yarns around campfires, their dreams as dry as the valley floor.

Current Status

Today, Greenwater is a true ghost, its tent scars erased by wind and flash floods, leaving scant ruins at the original Kunze site—a few leveled foundations and mine adits—while the valley floor lies barren. Managed within Death Valley National Park, access demands a high-clearance 4WD via the 20-mile Greenwater Valley Road from Highway 190 south of Dante’s View—rutted, washboarded, and prone to seasonal closures from monsoons or snow. No amenities exist; visitors contend with extreme heat (up to 130°F) and hypothermia risks at night, packing water and fuel for the isolation.

Greenwater draws intrepid explorers via the Lonesome Miner Trail—a 40-mile backpacking route linking it to Beveridge and other Inyo relics—championed by the National Park Service for its “outdoor museum” value. Drone footage and geotagged hikes trend on platforms like AllTrails, but the site’s fragility—tailings laced with arsenic—warrants caution; no collecting is permitted. Amid climate whiplash, with 2025’s erratic rains scouring the valley, Greenwater endures as a meditation on hubris, its silence broken only by coyote howls echoing the ghosts of a copper mirage. For current conditions, consult NPS resources.

Greenwater Town Summary

NameGreenwater
Also Known Kunze, Ramsey
LocationInyo County, Death Valley, California
Latitude, Longitude36.179444, -116.616389
Elevation4,280 feet
NewspaperGreenwater Times ( 1906-1908 )

Greenwater Map

References

The Amargosa Opera House

Recently, on a whim, my wife and I loaded up the jeep and opt to just explore the desert West of our home town of Las Vegas and ended up at the Amargosa Opera House. Our original idea was to drive to the winery’s in Pahrump, Nevada. After the winery our plan was to drive up to the townsite of Johnnie, Nevada. The best laid plans were for not. We discovered that the mines of Johnnie, Nevada are located on private property.

The Arargosa Opera House is located in Death Valley Junction, California.
The Arargosa Opera House is located in Death Valley Junction, California.

Honoring the wishes of the Johnnie mine site property owners, we opted to do some exploring. We headed easy through the small town of Crystal, Nevada and drove past the Ash Meadows National Wildlife Refuge. The AMNWR was closed, as the result of, a Government Shutdown.

As our wandering journey continued, we opted to travel South and soon discovered the small desert haven of Death Valley Junction and the world famous Amargosa Opera House.

Death Valley Junction was founded as the town of Amargosa. The town was founded at the intersection of SR 190 and SR 127 just East of Death Valley. Founded in 1907 when the Tonopay and Tidewater railroads ventured into Amargosa Valley.

Origins as a Borax Company Town (Early 20th Century)

The story begins not with ballet slippers but with 20-mule teams and the quest for borax. In the early 1900s, the Pacific Coast Borax Company sought to exploit rich deposits in Death Valley. The Tonopah and Tidewater Railroad reached the area in 1907, establishing a settlement originally called Amargosa (Spanish for “bitter,” referencing the local water). By the 1920s, the company constructed a U-shaped complex of adobe buildings in the Spanish Colonial Revival style, designed by architect Alexander Hamilton McCulloch. Completed between 1923 and 1925, it included offices, employee dormitories, a hotel, store, and a community hall known as Corkhill Hall. This hall hosted everything from church services and town meetings to dances, movies, funerals, and recreational events for the roughly 300 residents.

The town peaked in the 1920s and 1930s, supporting the nearby Lila C. Mine and the Death Valley Railroad, a narrow-gauge line that hauled borax until the early 1940s. World War II damaged the tracks, mining shifted elsewhere, and by 1950, Death Valley Junction had devolved into a near-ghost town—abandoned buildings crumbling under relentless sun, with only dust devils for company.

The Arrival of Marta Becket and Rebirth (1967–1970s)

Fate—or a flat tire—intervened in March 1967. Marta Becket (born Martha Beckett in 1924 in New York City), a classically trained dancer, actress, choreographer, and painter who had performed on Broadway, at Radio City Music Hall, and in touring shows, was camping with her husband Tom Williams when their trailer blew a tire near Death Valley Junction. While it was repaired, Becket explored the derelict town. Peering through a keyhole in the door of Corkhill Hall, she felt the building “speak” to her: a vast, ruined space with a stage, flooded floors, and rodent-infested benches, but brimming with potential.

Enchanted, Becket rented the hall for $45 a month and a dollar down. She and her husband leveled the floor, repaired the roof, and extended the stage. On February 10, 1968, she gave her inaugural performance—a one-woman show of dance, mime, and music—to an audience of just 12 locals on a rainy night. She renamed the venue the Amargosa Opera House, performed weekends without fail, and began restoring the adjacent hotel.

Sparse crowds frustrated her until inspiration struck: she would create her own audience. From 1968 to 1972, working on scaffolding in scorching heat, Becket painted vibrant Renaissance-style murals covering the walls and ceiling—a perpetual crowd of 16th-century nobles, jesters, nuns, kings, queens, and courtesans in opulent attire, gazing eternally at the stage. The ceiling became a trompe-l’œil balcony of revelers. This “painted audience” ensured she was never truly alone.

A 1970 National Geographic article, followed by features in Life magazine, brought fame. Visitors trickled, then poured in from around the world, drawn to this oasis of whimsy in the desert’s void.

The Amargosa Opera House features original hand painted murals by Marta Becket.
The Amargosa Opera House features original hand painted murals by Marta Becket.

Peak Years and Legacy Building (1970s–2017)

In 1974, Becket completed the murals and founded the nonprofit Amargosa Opera House, Inc. With support from friends and the Trust for Public Land, the organization purchased the entire town of Death Valley Junction. On December 10, 1981, it was listed on the National Register of Historic Places. Proper theater seats arrived in 1983, replacing garden chairs.

Becket performed relentlessly—often solo, later with partners like handyman Tom Willett (her comic foil until his 2005 death)—choreographing original ballets and pantomimes. Her shows ran Friday, Saturday, and Monday nights, drawing busloads during peak seasons. She lived simply in a shack behind the opera house, surrounded by cats, burros, peacocks, and the desert’s silence.

The 2000 documentary Amargosa, directed by Todd Robinson, cemented her legend. Becket retired from regular performances after the 2008–2009 season but returned sporadically until her final show on February 12, 2012. She continued painting and overseeing the venue until her death on January 30, 2017, at age 92.

Successors like ballerina Jenna McClintock (inspired as a child visitor and resident performer until 2016) carried the torch briefly, but the focus shifted to preserving Becket’s vision.

Current Status (As of November 20, 2025)

Death Valley Junction remains a near-ghost town—population under 10, no gas stations, no grocery stores, and vast emptiness punctuated by derelict borax-era ruins. Yet the Amargosa Opera House and Hotel endures as a nonprofit-run cultural beacon, owned and operated by Amargosa Opera House, Inc.

The 23-room hotel is open year-round, offering basic, historic accommodations (no TVs, but WiFi and air conditioning) to travelers seeking quirky desert lodging. The adjacent Amargosa Cafe, once a staple, remains closed following prior operational pauses.

The Opera House itself faces challenges from the desert’s extremes. Severe monsoon floods in August 2025 damaged the historic adobe walls, lobby, rooms, and irreplaceable murals, with water inundating the complex. Reserves depleted, the nonprofit launched urgent fundraising campaigns, raising over $18,000 by October 2025 toward a $50,000 goal for floor repairs, roof work, flood mitigation, utilities, insurance, and payroll. As of mid-November 2025, tours—normally daily at 9 AM and often evenings—were suspended, with resumption announced for November 2, 2025 (adults $20, children $10).

Performances are limited or on hiatus during recovery, though the venue occasionally hosts traveling musicians, theater, spoken word, and special events (check amargosaoperahouse.org for schedules). The murals—vibrant depictions of Becket’s imaginary patrons—remain the star attraction, a testament to one woman’s defiance of isolation.

Despite hardships, the Amargosa persists as a symbol of artistic resilience. Visitors describe it as a “miracle in the desert,” where the air still hums with Marta Becket’s spirit—whirling like the dust devils she loved to paint. In an era of fleeting digital spectacles, this hand-built theater reminds us that true creation can bloom anywhere, even in the bitter heart of nowhere. For the latest updates, visit the official site or contribute to preservation efforts.

Ryan California – Inyo County Ghosttown

Perched precariously on the steep eastern flanks of the Amargosa Range at an elevation of 3,045 feet (928 meters), Ryan, California—once a thriving borax mining outpost—clings to the rugged edge of Death Valley National Park like a faded photograph from the early 20th century. This unincorporated community in Inyo County, just 8 miles northeast of Dante’s View and 15 miles southeast of Furnace Creek, embodies the stark contrasts of the American desert frontier: blistering heat by day, bone-chilling nights, and the relentless pursuit of mineral wealth amid isolation. Founded as a company town by the Pacific Coast Borax Company in 1914, Ryan served as the nerve center for extracting the “white gold” of the Mojave, fueling industries from glassmaking to detergents. Today, as a meticulously preserved ghost town under private stewardship, it offers a rare, unvarnished glimpse into the lives of borax miners and the pivot to tourism that briefly extended its lifespan. Though closed to casual visitors, Ryan’s 2025 designation on the National Register of Historic Places underscores its enduring significance as a cultural relic of industrial ambition and human resilience in one of North America’s harshest landscapes.

Postcard showing a panoramic view of Ryan, a mining camp in the Death Valley, California, ca.1920 - Photo Credit “University of Southern California. Libraries” and “California Historical Society” as the source. Digitally reproduced by the USC Digital Library.
Postcard showing a panoramic view of Ryan, a mining camp in the Death Valley, California, ca.1920 – Photo Credit “University of Southern California. Libraries” and “California Historical Society” as the source. Digitally reproduced by the USC Digital Library.

Early Prospecting and Settlement (1880s–1913)

The saga of Ryan unfolds against the backdrop of Death Valley’s borax boom, a chapter in the broader narrative of California’s mineral rushes that followed the silver frenzies of the Comstock Lode. Borax, a sodium borate compound essential for soap, ceramics, and fireproofing, was first discovered in the region in 1872 near Furnace Creek. By 1882, prospector Isadore Daixel had staked claims in the Funeral Mountains, identifying rich deposits of colemanite—a hydrated calcium borate—at what would become the Lila C Mine. Named after Lila C. Coleman, daughter of borax magnate William Tell Coleman, the Lila C site emerged as a modest camp by the early 1900s, drawing hardy laborers to its sun-scorched slopes where temperatures routinely exceeded 120°F (49°C) and water was hauled in by mule teams.

In 1907, the Pacific Coast Borax Company (PCB), under the visionary leadership of figures like Stephen Mather (later the first director of the National Park Service), formalized operations. A post office opened that year at Lila C, marking the camp’s transition from tent city to semblance of permanence. Miners, a mix of American, Mexican, and European immigrants, toiled in hand-dug adits, extracting colemanite via shallow pits and rudimentary ore chutes. The air hummed with the clatter of picks and the lowing of burros, while sagebrush-dotted arroyos carried faint echoes of multilingual banter around campfires fueled by creosote branches. Yet, the site’s remoteness—over 100 miles from the nearest railhead at Ludlow—hampered efficiency, prompting PCB to envision a more ambitious hub.

Boomtown Ascendancy and Industrial Might (1914–1927)

The year 1914 heralded Ryan’s explosive rebirth. To streamline logistics, PCB relocated operations 11 miles northwest of Lila C, constructing a new camp initially dubbed “Devar” (an acronym for Death Valley Railroad, later mangled to “Devair” on maps). Renamed Ryan in tribute to John Ryan (1849–1918), the company’s steadfast general manager who oversaw its expansion from San Francisco’s borax refineries to the Mojave’s veins, the site burgeoned into a model company town. By 1916, it boasted 54 buildings: bunkhouses for 300 workers, a two-story hospital with steam heat, a schoolhouse for the children of miners, a post office-cum-general store stocked with canned goods and patent medicines, assay offices, machine shops, and a recreation hall—originally a church shipped intact from the ghost town of Rhyolite, Nevada, in 1919.

At its core pulsed the mining infrastructure: the Lila C Mine, joined by the Jumbo, Biddy, and Widow complexes, yielded thousands of tons of colemanite annually, processed via a web of aerial tramways that whisked ore 1,000 feet down the canyon to loading platforms. The “Baby Gauge,” a narrow-gauge mine railroad snaking south from Ryan, shuttled loaded skips, while the full Death Valley Railroad—PCB’s 3-foot-gauge marvel—linked Ryan to the borax works at Death Valley Junction 20 miles east, ferrying passengers and freight through tunnel-pocked canyons. Electricity from a hydroelectric plant at Navel Spring illuminated the nights, refrigeration preserved perishables, and a tennis court hinted at leisure amid the grind. Population swelled to around 2,000 at peak, a polyglot mosaic where Cornish pumpmen rubbed shoulders with Mexican muleteers, all sustained by PCB’s paternalistic ethos of fair wages, medical care, and communal suppers under star-pricked skies. Ryan’s streets, graded dirt ribbons flanked by adobe and frame structures, thrummed with the rhythm of shift changes, the whistle of locomotives, and the distant rumble of ore cars—a desert symphony of progress.

Photograph of the "Baby Gauge" (aka "Baby Gage") mine train at the mining camp of Ryan, Death Valley, ca.1900-1950. A car with one headlight can be seen at center on tracks pulling a platform with four benches upon it. Someone can be seen driving the car, while four men and women sit on the benches. A small wooden shack with a portion of the roof missing can be seen behind the platform, while a ladder, wooden planks, and more tracks are visible at left. A valley and mountains can be seen in the background. - “University of Southern California. Libraries” and “California Historical Society” as the source. Digitally reproduced by the USC Digital Library.
Photograph of the “Baby Gauge” (aka “Baby Gage”) mine train at the mining camp of Ryan, Death Valley, ca.1900-1950. A car with one headlight can be seen at center on tracks pulling a platform with four benches upon it. Someone can be seen driving the car, while four men and women sit on the benches. A small wooden shack with a portion of the roof missing can be seen behind the platform, while a ladder, wooden planks, and more tracks are visible at left. A valley and mountains can be seen in the background. – “University of Southern California. Libraries” and “California Historical Society” as the source. Digitally reproduced by the USC Digital Library.

Decline and Reinvention (1928–1950s)

As with many Mojave outposts, Ryan’s fortunes waned with depleting veins and shifting markets. By 1927, high-grade colemanite reserves dwindled, and PCB shuttered the mines in 1928, idling the tramways and silencing the Baby Gauge. Undeterred, the company pivoted to tourism, rebranding Ryan as the Death Valley View Hotel in 1927—a plush resort with 20 guest rooms, a dining hall, and scenic overlooks drawing Hollywood elites and Eastern sightseers via the Tonopah & Tidewater Railroad. The Death Valley Railroad extended its life, offering excursion trains into the ghost mines until its decommissioning in 1930 amid the Great Depression’s grip.

The hotel limped on as overflow lodging for Furnace Creek’s inns through the 1940s, hosting episodes of Death Valley Days radio broadcasts and even serving as a Cold War fallout shelter in the 1950s. Yet, by the mid-1950s, patronage faded, leaving Ryan in caretaker status: a skeletal ensemble of weathered bunkhouses and rusting rail sidings, patrolled by lone watchmen amid encroaching creosote and jackrabbits. The 1933 creation of Death Valley National Monument (upgraded to national park in 1994) encircled but spared the private enclave, preserving its isolation.

Current Status (As of November 2025)

In a twist of serendipitous stewardship, Ryan’s nadir became its salvation. After decades under U.S. Borax (formed by PCB’s 1956 merger) and subsequent owner Rio Tinto (acquired 1967), the site was donated to the newly formed Death Valley Conservancy (DVC) on May 6, 2013—complete with 640 acres, 22 buildings, 16 archaeological sites, and mineral rights, bolstered by endowments for upkeep. This act, championed by Rio Tinto’s Preston Chiaro and spurred by National Park Service overtures since 2005, averted decay and positioned Ryan as a living laboratory for preservation.

Today, Ryan stands as one of the West’s best-preserved mining camps, its adobe walls and timber frames stabilized per the Secretary of the Interior’s standards. The Ryan Rec Hall’s multi-year restoration, ongoing since 2019, exemplifies efforts to blend education with conservation, supporting research in archaeology, industrial history, and desert ecology. The Ryan Historic District—encompassing rail remnants, mine complexes, and trails—was nominated in 2024 and listed on the National Register of Historic Places on January 27, 2025, honoring its multifaceted legacy from borax extraction to mid-century media outpost.

Public access remains tightly controlled for safety—unstable shafts and seismic risks abound—with no roads or services on-site. Visitors must enter a lottery for guided tours via the DVC website, typically limited to small groups exploring the schoolhouse’s chalk-scarred blackboards or the hotel’s faded lobby. Recent 2025 initiatives include enhanced water harvesting at Navel Spring and interpretive signage, while social media whispers of drone-captured sunsets over the bunkhouses fuel #DeathValleyGhostTown fervor. Amid Death Valley’s 2025 tourism surge—bolstered by cooler monsoons—Ryan endures not as a relic, but a resilient echo: where the wind through abandoned tram towers carries the ghosts of gandy dancers and the promise of rediscovery for those who draw the tour ticket. For bookings and updates, consult the Death Valley Conservancy at dvconservancy.org.

Town Summary

NameRyan California
Also Known AsColemanite,
Devair,
New Ryan
LocationDeath Valley National Park, San Bernardino County, California
Latitude, Longitude36.3213, -116.6697
Elevation928 meters / 3045 feet
GNIS1661348

Ryan Town Map

References