Chloride City California – Inyo County Ghost Town

Chloride City is a remote ghost town and historic mining site located in the Funeral Mountains on the eastern side of Death Valley National Park, Inyo County, California. Situated at an elevation of approximately 4,770 feet (1,454 m) in a saddle high above the valley floor, it offers dramatic panoramic views across Death Valley to the Panamint Mountains—over 5,000 feet below—making it one of the more scenic yet challenging historic locations in the park. Access requires a high-clearance vehicle (often 4WD) via rough dirt roads, such as Chloride City Road off Daylight Pass Road or near Hell’s Gate, and the site remains largely untouched, with scattered remnants rather than intact structures.

Crowells Mill under construction in Chloride City, CA about 1915
Crowells Mill under construction in Chloride City, CA about 1915

Early Discovery and Initial Mining (1870s)

The area’s mining history dates back to one of the earliest documented strikes in the Death Valley region. In August 1871, prospector August J. Franklin (a civil engineer involved in U.S. government surveying work on the Nevada-California border) made the initial discovery. According to local legend, Franklin killed a rattlesnake with a rock, noticed rich-looking float (loose ore fragments) beneath it, and traced the material uphill to its source—a vein of silver chloride (a form of silver ore) at what became known as Chloride Cliff.

Franklin staked claims and formed the Chloride Cliff Mining Company, sinking a shaft to about 70 feet by mid-1873 and employing several miners. Ore samples reportedly assayed at high values—between $200 and $1,000 per ton in silver—indicating significant potential. However, the remote location, harsh desert conditions, lack of water, and transportation difficulties limited development. Activity was intermittent; Franklin and later his son George worked claims sporadically to maintain ownership, but the site saw little sustained production through the 1870s and remained largely deserted from around 1873 until the early 1900s.

Boom Period and Establishment of Chloride City (1905–1906)

Interest revived in the early 20th century amid the broader Death Valley mining boom, particularly following the major gold discovery at Bullfrog, Nevada (near Rhyolite) in 1904 and the development of the nearby Keane Wonder Mine (discovered in late 1903). Prospectors from Bullfrog crossed into the Funeral Mountains, reworking older claims and exploring new ones.

By 1905, enough activity centered on the Chloride Cliff area (including renewed work on silver-lead and emerging gold veins) that a small support camp was laid out: Chloride City. It served as a hub for nearby operations, featuring basic facilities such as an assay office, bunkhouse, and possibly other rudimentary structures. The town was positioned in a picturesque but wind-swept saddle, supporting miners extracting ore from adits (horizontal tunnels) and shafts in the vicinity.

Despite initial promise, the boom was short-lived. Most operations proved uneconomical due to low-grade ore, high processing costs, and isolation. Chloride City became a ghost town by late 1906, abandoned as miners moved to more promising strikes elsewhere.

Later Activity and Nearby Mines (1910s–1940s)

Sporadic mining returned in the 1910s and especially the 1930s, when higher gold prices during the Great Depression spurred renewed prospecting. Nearby sites like the Big Bell Mine (and Big Bell Extension) saw more substantial work, including construction of an aerial tramway, ore bins, ball mills, cyanide tanks, and other equipment—much of which remains remarkably preserved due to the site’s inaccessibility. These operations focused on gold and silver, with some claims reportedly changing hands through dramatic means (e.g., gambling, disputes, or even a reported duel). Activity largely ceased by the early 1940s, with the last major shutdown around 1941.

Chloride City itself did not revive as a town; it remained a loose collection of mining features rather than a populated settlement.

Current Status and Remnants

Today, Chloride City is within Death Valley National Park and protected as part of its historic resources. Little of the actual “town” survives—mostly scattered foundations, mine dumps, numerous adits (some explorable with caution), ore remnants, and the remains of three stamp mills. A single grave marks the site: that of James McKay, about whom virtually nothing is known.

The area includes dramatic overlooks at Chloride Cliff, where visitors can stand on old dumps and gaze down into Death Valley. Nearby hikes lead to well-preserved ruins like those of the Big Bell Mine complex, featuring rusting machinery, collapsed shacks, and tramway elements frozen in time.

The site exemplifies the fleeting nature of desert mining booms: early promise, rapid influx, quick bust, and long-term abandonment. Its isolation has helped preserve artifacts, offering a glimpse into the grit of 19th- and early 20th-century prospectors in one of Earth’s harshest environments. Visitors should prepare for rough roads, extreme conditions, and practice Leave No Trace principles, as the area has no facilities or signage in many spots.

Chloride City Trail Map

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

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Death Valley Points of Interest

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Crowells Mill under construction in Chloride City, CA about 1915

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

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White Rim Trail

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Mesa Light taken from the White Rim Trail and Lathrop Canyon Road. Photograph by James L Rathbun
Mesa Light taken from the White Rim Trail and Lathrop Canyon Road. Photograph by James L Rathbun

The trailhead is reached by leaving the Islands in the Sky Mesa, using the steep and twisty Shafer Trail.  The Shafer Trail is a back county route that takes you back to Moab, UT and a fun way out at the end of your trip.  The Shafer trail drops quickly and about 700 feet using 6 switch backs.  The Shafer Trail and White Rim Trail are well maintained and not very narrow, but the elevation and views give the feeling the route is dangerous.

Sunset along the White Rim Trail in Canyonlands NP, Utah Photograph by James L Rathbun
Sunset along the White Rim Trail in Canyonlands NP, Utah Photograph by James L Rathbun

Once down on the bottom, the well marked Shafer Trail continues on, while the White Rim Trail branches right and to the south.  All along the backcountry dirt road there are numerous spur trails, vistas, and points of interest give you much to explore including Lathrop Canyon, Musselman Arch, Washer Woman Arch and the Monster Tower.  The entire route is easy to follow, well maintained, well traveled and pure joy to run.

The trail winds along a layer of erroded light colored sandstone called the White Rim which undulates around several smaller side canyons which lead down the the Colorado River.  

Available Campsites

There are several small primitive campsites throughout the route.

  • Shafer – Mile 7 – 1 site
  • Airport – Mile 19 – 4 sites
  • Gooseberry – Mile 30 – 2 sites
  • White Crack – Mile 39 – 1 site
  • Murphy Hogback – Mile 45 – 3 sites
  • Candlestick – Mile 55 – 1 sites
  • Potato Bottom – Mile 66 – 3 sites
  • Hardscrabble Bottom – Mile 70 – 2 sites
  • Labyrinth – Mile 72 – 2 sites
  • Taylor – Mile 77 – 1 site

White Rim Trail

The White Rim Trail is a renowned 100-mile loop through Canyonlands National Park’s Island in the Sky district, offering a bucket-list adventure for overlanders, mountain bikers, and 4×4 enthusiasts. This rugged, high-clearance 4×4 route circumnavigates the Island in the Sky mesa, winding along the “white rim” ledge between the mesa top and the Green and Colorado Rivers below. The trail showcases breathtaking vistas of red rock canyons, towering buttes (like Airport Tower, Monster Tower, and Junction Butte), and the rivers’ confluence, rivaling views from the Grand Canyon’s South Rim. Key highlights include Gooseneck Overlook, Musselman Arch, White Crack (with views of the Maze and Needles districts), and Murphy Hogback, which offers 360-degree panoramas.

The trail features a mix of wide dirt roads, sandy patches, and technical jeep trails with some cliff exposure, particularly at Shafer Trail, Lathrop Canyon Road, Murphy Hogback, Hardscrabble Hill, and Mineral Bottom switchbacks. It’s moderately difficult for vehicles and challenging for mountain bikes, with an elevation gain of approximately 9,160 feet. The route can be driven clockwise (starting at Shafer Trail) or counterclockwise (starting at Mineral Bottom Road), typically taking 2-3 days to complete, though hardcore cyclists may attempt it in one day. Permits are required for both day-use and overnight trips, with 20 designated campsites across 10 camping areas, including Airport Campground. No potable water is available, and high water on the Green River (May-June) can flood western sections, making a full loop impossible. The best seasons are spring (March-May) and fall (September-November) due to milder temperatures and more predictable weather, as summer is extremely hot and winter may bring closures.

Trail Map

White Rim Trail Campsites

Canyonlands National Park is located in the south eastern corner of the state of Utah

Airport Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Located in the heart of Canyonlands National Park’s Island in…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Gooseberry Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Gooseberry Campground is a remote backcountry camping area located along…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Hardscrabble Bottom Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Hardscrabble Bottom Campground is a remote backcountry camping area along…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Murphy Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Murphy Campground is a remote backcountry camping area along the…
Canyonlands National Park is located in the south eastern corner of the state of Utah

Potato Bottom Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah Potato Bottom Campground is a remote backcountry camping area along…
Canyonlands National Park is located in the south eastern corner of the state of Utah

White Crack Campground

Canyonlands National Park is located in the south eastern corner of the state of Utah White Crack Campground is a remote backcountry camping area in…

Carrara Nevada – Nye County Ghost Town

Carrara is a historic ghost town located in southern Nye County, Nevada, within the Amargosa Desert. Situated approximately 8.5 to 10 miles southeast of Beatty and adjacent to U.S. Route 95, the townsite lies on the valley floor at an elevation of about 2,881 feet. It is named after the renowned marble-producing city of Carrara in Italy, reflecting ambitious hopes that its local deposits would rival the famous Italian quarries. To the northeast, a former railroad grade (now a dirt road) ascends about 3 miles up Carrara Canyon on the southeast flank of the Bare Mountains to the old marble quarry, which sits roughly 1,400 feet higher in elevation. The site was once served by spurs from the Las Vegas & Tonopah Railroad and later the Tonopah & Tidewater Railroad.

Unlike the gold and silver boomtowns that dotted early 20th-century Nevada, Carrara was uniquely founded on marble quarrying — a rare commodity in the region’s mining history. Its story exemplifies the classic boom-and-bust cycle of the American West, driven by optimism, geological challenges, and economic realities in a harsh desert environment.

Carrara in Nye County Nevada

Discovery and Founding (1904–1913)

Marble deposits in the area were first identified as early as 1904, but initial attempts to quarry them yielded poor results due to highly fractured stone that produced only small, unusable pieces. Prospectors persisted, and in 1911, a more promising vein was located, leading to the formation of the American Carrara Marble Company under president P.V. Perkins, with Eastern investors providing capital.

The company platted a townsite on the flat desert floor below the quarry, strategically positioned along the Las Vegas & Tonopah Railroad for shipping. Infrastructure developed rapidly: a 9-mile pipeline brought water from Gold Center across the valley (a rarity in the arid region), electricity was supplied, and a 3-mile inclined cable railway (using a Lidgerwood counterbalance system) transported marble blocks downhill from the quarry to the finishing mill and rail spur.

On May 8, 1913, Carrara was officially dedicated with great fanfare — a grand celebration featuring a ball, live music from a Goldfield band, a baseball game, and swimming in the new town pool. That same day, the town’s newspaper, the Carrara Obelisk, published its first issue, and a post office opened shortly after (operating until 1924). Amenities included a hotel, store, restaurant, saloon, dance hall, telephones, electric lights, and even a public park with a flowing fountain fed by the pipeline — luxurious features that made Carrara stand out in the desolate Nevada landscape.

Boom Period and Operations (1913–1917)

At its peak around 1915–1916, Carrara boasted about 150 residents and roughly 40 buildings. The quarry produced a variety of marble types, including pure white, blue, black, yellow, and striped varieties, which promoters claimed were chemically superior to Italian Carrara or Colorado Yule marble. Blocks were partially finished at the townsite mill before shipment via railroad, primarily southward on the Tonopah & Tidewater line after a spur was added.

The American Carrara Marble Company invested heavily, completing the cable railway in 1914 and shipping the first slabs that year. The town fostered a sense of community, with the Obelisk chronicling local events and aspirations. For a brief moment, Carrara represented a diversified industrial future beyond precious metals, capitalizing on proximity to West Coast markets.

Decline and Abandonment (1917–1920s)

Despite the hype, geological issues doomed the venture. Much of the marble was too fractured and impure for large-scale commercial blocks, competing poorly with higher-quality sources from Vermont and abroad. Production costs soared, and by late 1916, the Nevada-California Power Company deemed the operation unprofitable and cut electricity to the quarry.

Operations halted in 1917, the Obelisk ceased publication that year, and the railroad discontinued service to Carrara in 1918. Residents departed quickly, leaving the town abandoned by the early 1920s. A brief gold rush in 1929 sparked minor excitement, including the short-lived Carrara Miner newspaper promoting the Gold Ace Mining Company, but it failed to revive the site.

Later attempts, such as a 1940s proposal for a white cement plant using crushed marble (and nearby unrelated Elizalde cement ruins from the 1930s), also collapsed without success.

Current Status

Carrara remains a classic Nevada ghost town — uninhabited, with no active population or commercial activity. The desert has largely reclaimed the site, leaving minimal physical remnants visible from U.S. 95. Key surviving features include:

  • Concrete foundations of buildings (e.g., the hotel, with scattered marble tile fragments).
  • The iconic concrete basin of the town fountain, one of the most intact structures.
  • Cellars, scattered debris, and railroad grades (including the old cableway route up to the quarry).
  • At the quarry itself in Carrara Canyon: abandoned equipment, openings in the mountainside, and accessible veins of white marble (collectible in small amounts by visitors, though the area is remote and requires off-road travel).

The townsite is easily accessible via a short, bumpy dirt road east from Highway 95 (near mile marker 51), making it a popular stop for ghost town enthusiasts, historians, and off-road explorers. The quarry road is rougher and leads to the Bare Mountains base. No modern development has occurred, and the area falls under public land management, preserving its desolate, historic character. Nearby ruins (e.g., the 1930s cement plant) are sometimes confused with Carrara but are distinct.

Carrara’s legacy endures as a poignant reminder of Nevada’s transient mining era: grand dreams dashed by nature’s unforgiving realities, yet offering quiet ruins that whisper of a fleeting marble empire in the desert.

Carrara Town Summary

NameCarrara Nevada
LocationNye County, Nevada
Population 150
Post OfficeMay 5, 1913 – September 15, 2914
NewspapersCarrara Obelisk Feb 7, 1914 – Sept 9, 1916
Carrara Miner July 21, 1929

Carrara Trail Map

Carrara Nevada Newspapers

Carrara Miner Newspaper

The Carrara Miner was a brief newspaper published in Carrara, Nevada, a small ghost town in Nye County located approximately nine miles south of Beatty.…

Carrara Obelisk

The Carrara Obelisk was a short-lived but significant weekly newspaper published in the early 20th century in Carrara, Nevada, a small marble quarrying town located…

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