Saint Joseph, Nevada – Clark County Ghost Town

Ghost towns of Clark County, Nevada
Ghost towns of Clark County, Nevada

Saint Joseph, Nevada, is a historic ghost town located in Clark County in the Moapa Valley along the east bank of the Muddy River. It played a brief but notable role in the mid-19th-century Mormon colonization efforts in southern Nevada. Today, little physical evidence remains of the original settlement, though its legacy connects to the modern community of Logandale.

Founding and Early Settlement (1865)

Mormon settlers, directed by Brigham Young as part of the broader Muddy Mission (or Moapa Mission), established Saint Joseph in May 1865. A group led by Thomas Smith initially founded the nearby community of St. Thomas at the confluence of the Muddy and Virgin Rivers earlier that year. In June 1865, a second group moved about nine miles north and built a fort on a bluff overlooking the east side of the Muddy River, roughly five miles north of present-day Overton.

The settlement was named Saint Joseph, reportedly after Joseph Young, a colonizer and son of Brigham Young. Like other Muddy Mission outposts, its purpose was agricultural: to grow crops such as cotton, wheat, and corn in the fertile river valley, while also securing the area against non-Mormon (“Gentile”) travelers and supporting the broader Latter-day Saints expansion in the American West.

Settlers constructed adobe buildings, a wooden gristmill (sometimes associated with the nearby Simonsville or Mill Point area), and other infrastructure. The mill processed salt, corn, and wheat. By 1867, the community had grown enough to receive its own post office (established August 26, 1867). It briefly served as the county seat when the Utah Territory created Rio Virgen County, even as the Arizona Territory claimed parts of the valley under Pah-Ute County.

The 1868 Fire and Relocation

In 1868, a fire—reportedly started by young boys attempting to roast potatoes—swept through the town and destroyed most of the structures, sparing at least one adobe building. Residents attempted to rebuild, but many relocated a few miles northwest to a new site along the Muddy River (sometimes described as on the west side or a short distance upstream). This new location also took the name Saint Joseph and grew to several hundred residents. The original post office transferred there.

Abandonment Due to Boundary Issues (1870–1871)

A major turning point came with the 1870 boundary survey, which determined that the Moapa Valley, including Saint Joseph, lay within Nevada rather than the Utah or Arizona territories as previously assumed. Nevada authorities demanded that the Mormon settlers pay substantial back taxes in gold coin—a burden the community found unsustainable. With permission from Brigham Young, most residents abandoned the settlement in 1871. Only one family reportedly remained initially.

This abandonment mirrored the fate of other Muddy Mission towns like St. Thomas. Non-Mormon settlers (“Gentiles”) soon moved in to claim the farmlands and remaining structures.

Later History and Connection to Logandale

Mormon pioneers began returning to the Moapa Valley around 1880, repurchasing land and re-establishing communities such as Overton and parts of the former Saint Joseph area. The relocated Saint Joseph site was renamed Logan (after an early pioneer or to avoid confusion) and later Logandale in 1917. Logandale incorporated the post office and became a lasting agricultural community in Clark County.

A Saint Joseph Cemetery in the area dates back to the 1860s, with initial use around 1864–1869 and additional burials in the 1890s. Some remnants, such as foundations or the occasional adobe structure, have been noted by historians and local explorers, though the original townsite is largely gone. Nearby historic buildings in the Logandale area, like the Gubler House (built 1909), reflect the continued settlement history.

Geographic and Modern Context

Saint Joseph (historical) is situated in Clark County, Nevada, with coordinates approximately 36°34′22″N 114°26′59″W. It lies in the Moapa Valley, part of the broader region that includes Overton and Logandale, north of Las Vegas. Clark County itself was not organized until 1909 (carved from Lincoln County), long after the town’s abandonment.

Today, Saint Joseph is classified as a ghost town, with minimal visible ruins compared to better-preserved sites like St. Thomas (partially submerged and later exposed due to Lake Mead fluctuations). The area’s history is preserved through local historical societies, the Clark County Museum, and accounts of the Muddy Mission.

Significance in Nevada History

Saint Joseph exemplifies the challenges faced by early Mormon settlements in the arid West: ambitious agricultural missions, conflicts over territorial boundaries, and tensions with state taxation. The Muddy Mission towns, including Saint Joseph, St. Thomas, and others, represented Brigham Young’s vision of a self-sustaining “Zion” corridor stretching from Utah southward. Their short-lived nature highlights how federal boundary decisions and economic pressures shaped settlement patterns in southern Nevada during the post-Civil War era.

The story of Saint Joseph underscores the resilience of the Moapa Valley’s communities, which transitioned from short-term missionary outposts to enduring agricultural towns like Logandale and Overton that still thrive today on farming and ties to Las Vegas.

Sources for further reading include local histories such as Pearson Starr Corbett’s work on the Muddy Mission, Nevada historical society publications, and sites documenting Clark County ghost towns. Remnants and related sites can sometimes be viewed in the Moapa Valley area, though visitors should respect private property and protected lands.

Garnet, Nevada – Clark County Ghost Town

Ghost towns of Clark County, Nevada
Ghost towns of Clark County, Nevada

Garnet is an extinct town, commonly classified as a ghost town, located in Clark County, Nevada, in the United States. Unlike many well-documented Nevada ghost towns tied to major mining booms, Garnet has left behind almost no physical remnants or detailed historical records. Its significance today stems primarily from its geographic position in a region that has been repurposed for large-scale modern infrastructure, most notably the Apex Regional Landfill. The town’s name likely derives from the garnet minerals abundant in the surrounding desert hills and valleys, a common naming practice in mineral-rich areas of the American West.

Location and Geography

Garnet is situated in the arid desert landscape north of Las Vegas, at coordinates 36°23′19″N 114°52′16″W (approximately 36.38861°N, 114.87111°W) and an elevation of 2,467 feet (752 m). It lies near the junction where Interstate 15 (I-15) meets U.S. Route 93 (US 93). The Garnet Interchange (I-15 exit 64) marks the point where US 93 branches northward toward more remote areas such as Ely.

The broader area, sometimes associated with Garnet Valley, is part of the Apex region. Nearby features include Garnet Hill (a distinct but related site east of Las Vegas, popular for collecting pyrope and almandine garnets in volcanic outcrops). The region’s geology—featuring ancient rock formations and mineral deposits—reflects southern Nevada’s desert environment, with sparse vegetation and rugged terrain shaped by erosion and the Great Unconformity (a significant geologic feature).

Historical Background

Clark County itself has a rich history dating back thousands of years, with evidence of Southern Paiute and other Native American presence, followed by Spanish explorers, Mormon settlers in the mid-19th century, and rapid growth after the San Pedro, Los Angeles and Salt Lake Railroad arrived in the early 1900s. The county was formally created in 1909 from the southern portion of Lincoln County and named after Senator William A. Clark, whose railroad investments spurred development.

Specific details about Garnet’s origins, founding date, or early settlement are virtually nonexistent in public historical sources. It appears in geographic information systems (GNIS feature ID: 845843) as an extinct town but is not featured in major Nevada ghost town guides, mining histories, or local historical society records. There are no accounts of a population boom, notable mines, businesses, or events tied directly to the site. It was likely a very small, short-lived settlement—possibly a minor mining camp, railroad-related stop, or supply point—that never developed beyond a handful of structures. “Not much remains of the former community,” as noted in available descriptions.

The name “Garnet” aligns with the area’s mineral resources, similar to Garnet Hill to the south. It coexisted with other nearby extinct towns like Apex (after which the modern landfill is named). These small outposts reflect the pattern of transient communities in early 20th-century southern Nevada, many of which faded as larger towns like Las Vegas grew and transportation routes shifted. No significant mining production, census data, or newspaper mentions specific to Garnet have been widely preserved.

Modern Significance and Development

In the late 20th and 21st centuries, the Garnet area’s location along major highways made it ideal for industrial use. Its most prominent feature is the Apex Regional Landfill (operated by Republic Services), one of the largest landfills in the world by area and volume. Opened in 1993, the landfill is situated in the Garnet/Apex vicinity and serves as the primary municipal solid waste facility for the Las Vegas metropolitan area. It can accept up to 13,600 tons of waste per day and has capacity for over 250–300 years at current rates. The facility spans thousands of acres, with engineered liners, methane capture systems, and ongoing expansion that involves quarrying surrounding rock.

Although officially named after the nearby extinct town of Apex, the landfill is frequently associated with Garnet in geographic references. The site also supports the broader Apex Industrial Park, one of the largest in southern Nevada, which includes limited additional development such as power infrastructure and other facilities. The Garnet Interchange continues to serve as a critical transportation node.

Conclusion

Garnet, Nevada, stands as a quiet footnote in Clark County’s history—a place that never achieved the fame or longevity of Nevada’s iconic mining towns yet endures in official records and modern geography. Its story mirrors the broader narrative of the American West: fleeting settlements born of opportunity in a harsh desert environment, later overshadowed by urbanization and infrastructure. While the original community has vanished, the area now plays a vital, if unseen, role in sustaining the Las Vegas Valley’s growth by managing its waste for generations to come. Further primary-source research (such as old county maps, railroad records, or unpublished local archives) might uncover additional details, but publicly available information remains limited, underscoring Garnet’s status as one of Clark County’s most obscure ghost towns.

Hobson, Nevada – White Pine County Ghost Town

Ghost Towns of White Pine County, Nevada
Ghost Towns of White Pine County, Nevada

Hobson is a small ghost town in White Pine County, eastern Nevada, located in or near Ruby Valley on the western side of Ruby Lake. Its coordinates are approximately 40.07444° N, 115.53278° W, at an elevation of about 6,020 feet (1,835 m).

Unlike many White Pine County settlements tied to mining booms, Hobson is best known as the site of Fort Ruby (also called Camp Ruby), a U.S. Army post and National Historic Landmark. The area served as a key stop along the Overland Trail and Pony Express route.

Founding and Military History (1862)

Fort Ruby was established in September 1862 during the American Civil War by the United States Army. Its primary purpose was to protect emigrants, stagecoaches, and telegraph lines along the Overland Trail from potential Native American attacks and to secure the vital transportation and communication link between California and the Union states.

The fort was strategically placed at the east entrance to the Overland Pass into Ruby Valley, near the Ruby Mountains. It housed between 100 and 300 soldiers at its peak and included barracks, officer quarters, storehouses, and other military structures.

The post played a defensive role in the remote high-desert environment, where harsh winters and isolation made service challenging. It was never a large permanent installation but served as an important temporary emergency outpost.

Post-Civil War Period and Civilian Settlement

After the Civil War ended, the military presence at Fort Ruby diminished. The fort was eventually abandoned by the Army in the late 1860s or early 1870s.

A small civilian settlement known as Hobson developed near the former fort site. It remained a modest community supporting local ranching, stage travel, and overland activities. A post office operated intermittently in the area, and the site retained some importance due to its location along historic travel corridors.

By 1940, the population of Hobson was recorded as just 25 residents, reflecting its decline into a tiny ranching outpost.

Decline and Abandonment

Hobson never experienced the dramatic mining booms seen in nearby areas like Hamilton, Treasure City, or Shermantown. Its economy was tied more to transportation, military presence, and limited agriculture/ranching in Ruby Valley rather than mineral extraction.

As railroads and improved roads bypassed the remote valley, and with the end of stagecoach and Pony Express eras, the settlement faded. By the mid-20th century, it had become a true ghost town, with only ruins remaining from both the fort and later civilian structures.

Legacy and Current Remains

Hobson and Fort Ruby hold historical significance for their role in protecting the Overland Trail during a critical period in American history. Fort Ruby was designated a National Historic Landmark and added to the National Register of Historic Places in 1966.

Today, visitors can find:

  • Foundations and ruins of the original fort buildings
  • Interpretive trails and markers (a historical trail was opened in recent years)
  • Remnants of the small settlement in the scenic Ruby Valley setting near Ruby Lake

The site offers insight into Civil War-era frontier military life in the Great Basin and the challenges of maintaining supply lines across the vast Nevada landscape. It attracts historians, military history enthusiasts, and those exploring Nevada’s Pony Express and Overland Trail heritage.

Historical Context

While White Pine County is famous for its intense 1860s–1870s silver mining rushes, Hobson represents a different facet of the county’s history — transportation, communication, and military protection during national crisis. It complements other sites like Fort Schellbourne in the same county.

Sources

This report is based on National Park Service records, Nevada historical resources, and accounts of Fort Ruby’s military role. Shawn Hall’s books on White Pine County ghost towns also provide valuable context for the region.

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!