Stine, Nevada – Lincoln County Ghost Town

Official seal of Lincoln County, Nevada
Official seal of Lincoln County, Nevada

Stine is a classic Nevada ghost town and extinct settlement in Lincoln County, located in Rainbow Canyon along the Union Pacific Railroad line. Situated at an elevation of approximately 4,085 feet (1,245 m), it lies between the communities of Boyd and Etna, roughly two miles south of modern Caliente. Unlike many mining boomtowns, Stine originated as a ranching homestead before transforming into a specialized industrial site—a power plant, pump station, and railroad siding—built to support the operations of the distant Delamar gold mines. Its life was brief, and today little remains beyond its historical footprint in one of Nevada’s scenic canyon corridors.

Early Settlement: Kershaw Ranch (1873–1904)

The story of Stine begins with the arrival of Samuel and Hannah Kershaw in 1873. They established a ranch in the canyon, known as the Meadow Valley Wash Ranch, taking advantage of natural springs and fertile land in an otherwise arid region. The ranch featured orchards and served as a modest settlement in the Rainbow Canyon area.

A post office named Kershaw opened on October 29, 1892, reflecting the family’s prominence. By the turn of the 20th century, the site gained new importance as a water source. Engineers constructed a pump station to supply water from Meadow Valley Wash to the booming gold mining town of Delamar (about 12–13 miles away), which sat at a higher elevation and required significant pumping infrastructure, including booster stations.

In 1904, the Kershaws sold their holdings to James and Patrick Ryan. The post office name changed from Kershaw to Stine at the end of that year.

Industrial Development and Boom (1903–1909)

Between 1903 and 1905, the Union Pacific Railroad built its line through Rainbow Canyon, establishing a siding at the site. A coal-fired power plant was constructed around 1903–1905 to generate electricity for the Bamberger De Lamar Gold Mines (Delamar), transmitting power over the distance. The facility and siding were named Stine after Marcus Stine, vice-president of the International Pump Corporation and a major investor in the Delamar operations.

At its peak, Stine functioned as a small but critical support hub: railroad siding, power generation, and water pumping operations sustained the larger mining enterprise. Variant names included “Cana” and “Stine Station.” However, like many satellite facilities tied to mining, its fortunes were directly linked to Delamar’s productivity.

Decline and Abandonment (1909–1949)

Delamar’s gold production waned in the early 20th century. By the end of 1909, the power plant and pump station at Stine were dismantled (the equipment was possibly relocated). The post office closed on October 30, 1909. The site saw minimal activity afterward and was largely abandoned by 1949.

The Ryan family retained ties to the land; James Ryan donated portions of the former Kershaw Ranch for public use. In 1935, the area became Kershaw-Ryan State Park, one of Nevada’s original four state parks. The Civilian Conservation Corps (CCC) developed visitor facilities in the 1930s. Today, the park is a popular oasis with camping, hiking, rock climbing, and scenic views—preserving the natural beauty of the original homestead while the industrial remnants of Stine have faded into history.

Legacy and Significance

Stine exemplifies the interconnected infrastructure that supported Nevada’s early 20th-century mining booms. It highlights how railroads, power generation, and water engineering enabled remote mining operations in harsh desert environments. While Delamar earned a notorious reputation (known as the “Widow Maker” due to silica dust), Stine quietly powered it from the canyon below.

Little physical evidence of the town remains today, but its location in Rainbow Canyon ties it to broader regional history, including prehistoric rock art sites and the development of Lincoln County’s transportation network. The adjacent Kershaw-Ryan State Park serves as a living memorial to the area’s ranching and recreational heritage.

Stine stands as a reminder of Nevada’s boom-and-bust cycles—fleeting industrial outposts that rose quickly to meet mining demands and vanished once those demands faded.

The Comstock Lode – Nevada State Historic Monument

The Comstock Lode stands as one of the most significant mining discoveries in American history: the first major silver deposit found in the United States. Located beneath the eastern slope of Mount Davidson in the Virginia Range, near what became Virginia City, Nevada (then part of western Utah Territory), it transformed the region from a sparsely populated frontier into a booming industrial center. The lode’s riches fueled the development of Nevada as a state, bankrolled much of San Francisco’s growth, influenced national monetary policy debates, and advanced deep-level mining technology.

"Mining on the Comstock", depicting the headframes and mills of the various mines, and mining technology used at Comstock, most prominently the method of square-set timbering developed there to work the veins. -T.L. Dawes (drawing); Le Count Bros., San Fransisco (lithographers)
“Mining on the Comstock”, depicting the headframes and mills of the various mines, and mining technology used at Comstock, most prominently the method of square-set timbering developed there to work the veins. -T.L. Dawes (drawing); Le Count Bros., San Fransisco (lithographers)

Early Discoveries and the Path to 1859

Placer gold mining began in the area as early as 1850, when Mormon emigrants led by Abner Blackburn found gold in Gold Canyon (near present-day Dayton, Nevada). Small-scale placer operations continued through the 1850s, with miners washing gold from streams flowing down from the Virginia Range. These efforts were modest and overshadowed by the California Gold Rush.

In 1857, brothers Ethan Allen Grosh and Hosea Ballou Grosh (experienced prospectors from Pennsylvania) reportedly discovered rich silver-gold veins while searching the area. They documented promising samples but tragically died before recording formal claims—Ethan from a mining accident and Hosea from frostbite after a winter trek. Their knowledge passed to others indirectly.

By early 1859, prospectors including Peter O’Riley and Patrick McLaughlin were working claims in Six-Mile Canyon and Gold Canyon. On June 12, 1859 (the generally accepted date of the major “rediscovery”), they uncovered a rich vein of gold mixed with heavy blue-gray clay while digging for water to process placer gold. The clay proved frustrating until assayed and revealed as rich silver sulfide ore—marking the true start of the Comstock Lode.

Henry Tompkins Paige Comstock (“Old Pancake”), a talkative Canadian prospector and sheepherder, quickly inserted himself into the discovery. He claimed the ground for “grazing” and pressured the finders into giving him and partner Emanuel “Manny” Penrod shares. Though Comstock contributed little technically and sold his interests cheaply soon after (dying poor later), the lode bore his name.

News of the strike spread rapidly, sparking the “Rush to Washoe” (named for the Washoe Valley region). Thousands poured in from California, creating instant camps.

Boom Period and Development (1859–1870s)

The Comstock Lode stretched about 2.5–3 miles along the base of Mount Davidson, with ore bodies in narrow, steeply dipping veins that required deep underground mining. Initial placer and shallow diggings gave way to hardrock operations.

  • Towns and Infrastructure: Virginia City (founded 1859) and Gold Hill exploded in population, reaching peaks of 20,000–25,000 by the mid-1870s. Virginia City became the most important city between San Francisco and Denver, with saloons, theaters, newspapers (including the Territorial Enterprise), churches, schools, and an opera house. Other settlements included Silver City and Dayton.
  • Mining Challenges and Innovations: Early miners faced flooding, cave-ins, and unstable ground. German engineer Philipp Deidesheimer invented the square-set timbering system in 1860, allowing safe excavation of large ore bodies. Deep shafts reached over 3,000 feet by the 1880s. Adolph Sutro engineered the Sutro Tunnel (completed 1878), a 4-mile drainage and transport tunnel that relieved flooding and cut costs dramatically.
  • Economic Control: The Bank Crowd (led by William Sharon of the Bank of California and William Ralston in San Francisco) dominated early financing, mills, and stock manipulation on the San Francisco Mining Exchange. They controlled much of the early production but faced competition.
  • Key Bonanzas:
    • Ophir (early producer until ~1864).
    • Crown Point (major strike in 1871).
    • The Big Bonanza (1873) in the Consolidated Virginia and California mines—discovered by the Bonanza Firm (or “Bonanza Kings”/”Silver Kings”): Irish immigrants John William Mackay, James Graham Fair, James Clair Flood, and William S. O’Brien. This massive ore body (54 feet wide at points) produced over $100 million (hundreds of millions today) and made them among the richest men in the world.

Mark Twain (Samuel Clemens) worked briefly as a miner before becoming a reporter for the Territorial Enterprise, drawing on Comstock experiences for Roughing It.

Peak Production and Decline (1870s–1880s)

Peak output came in 1877–1878, with annual production exceeding $35 million ($14–21 million gold and silver combined, equivalent to over $1 billion today). From 1859 to the early 1880s, the district yielded roughly $400–500 million in metals (at then-current prices), including estimates of ~192–200 million ounces of silver and ~8–8.3 million ounces of gold. About 7 million tons of ore were extracted by 1880, with 57% silver value and 43% gold.

The lode’s riches helped finance the Union during the Civil War (prompting Nevada’s rushed statehood in 1864 for electoral votes and senators like William Morris Stewart and John P. Jones). Wealth flowed to San Francisco, building infrastructure and mansions.

By the late 1870s, rich bonanzas depleted, flooding worsened, and costs soared. Production declined sharply after 1880, though small-scale mining continued into the 20th century (sporadic until the 1940s, with minor revivals).

Nevada State History Marker #13

Nevada State Historical Markers identify significant places of interest in Nevada’s history. The Nevada State Legislature started the program in 1967 to bring the state’s heritage to the public’s attention with on-site markers. Budget cuts to the program caused the program to become dormant in 2009. Many of the markers are lost of damaged.

Near this spot was the heart of the Comstock Lode, the fabulous 2 ½ mile deposit of high-grade ore that produced nearly $400,000.00 in silver and gold.  After the discovery in 1859, Virginia City boomed for 20 years, helped bring Nevada into the union in 1864 and to build San Francisco.

Several major mines operated during the boom.  Their sites are today marked by large yellow dumps, several of which are visible from here – the Sierra Nevada a mile to your left, the Union, Ophir, Con Virginia and, on the high hill to the southeast, the combination.  The Lode was worked from both ends, north up Gold Canyon and south from the Sierra Nevada Utah mines.

NEVADA CENTENNIAL MARKER NO. 13
STATE HISTORIC PRESERVATION OFFICE

The Comstock Lode – Nevada State History Marker Summary

Nevada State History Marker13
NameThe Comstock Load
LocationVirginia City, Storey County, Nevada
Latitude, Longitude39.31668, -119.64736

References

Rochester Nevada – Pershing County Ghost Town

Rochester, Nevada, is a historic ghost town and former mining camp located in Rochester Canyon within the southern Humboldt Range in Pershing County, Nevada. Situated roughly 10-15 miles southeast of Interstate 80 (near the Oreana exit) and about 110 miles east of Reno, it lies in a narrow, steep canyon that once supported a booming silver and gold mining community.

Upper Rochester, Nevada 1918
Upper Rochester, Nevada 1918

Early Discovery and Initial Development (1860s–Early 1900s)

The Rochester district was first discovered in the early 1860s by prospectors from Rochester, New York, who found gold and silver deposits in the canyon. They named the area after their hometown. Small-scale mining occurred during this period, including work at sites like the Relief Mine in the southern part of the range. However, these early efforts yielded limited success, and the district remained relatively insignificant for decades, with only sporadic activity through the 1870s and into the early 20th century.

In 1905, Charles E. Stevens located claims on Nenzel Hill at the head of Rochester Canyon. These claims later passed to Joseph F. Nenzel.

Lower Rochester, Nevada 1913
Lower Rochester, Nevada 1913

The Boom Period (1912–1920s)

The true transformation came in 1912, when Joseph Nenzel shipped a small lot of float ore that assayed surprisingly high values. This led to the discovery of rich silver-bearing veins, sparking a major boom. Word spread quickly, and by 1913, the canyon’s population swelled to around 2,000 people.

The town developed in sections due to the steep terrain:

  • Upper Rochester (also called Old Town or Rochester Heights) sat higher up the canyon.
  • Lower Rochester was laid out on November 20, 1912, lower in the canyon and became the main hub, hosting the original post office.

Additional settlements included East Rochester and areas like Packard.

Two major companies drove operations:

  • The Rochester Mines Co. built an all-slime cyanidation mill starting at 100 tons per day (later expanded to 160 tons).
  • The Nevada-Packard Mines Co. constructed a 120-ton mill. In 1917, the Rochester Combined Mines Co. erected a $300,000 mill at Packard, though it operated briefly before shutting down (equipment later moved to Candelaria in 1922).

The district produced valuable silver, gold, copper, and lead, with estimates of total output ranging from $6 million to $10 million (primarily silver) during the main boom years from 1912 to 1928. Peak activity occurred in the mid-1910s, with the Rochester Mines Co. as a principal producer (facing but avoiding major apex litigation through compromise and consolidation into the Rochester Silver Corporation in 1920).

Moving a tent of Rochester, Nevada 1913
Moving a tent of Rochester, Nevada 1913

Decline and Ghost Town Status

Operations declined sharply in the late 1920s. The Rochester Silver Corporation ceased major work by 1929, and equipment was sold. Limited activity continued into the 1930s (e.g., the Buck and Charley Mine under the Rochester Plymouth Mines Co. in 1936), but the town faded as ore values dropped and the boom ended.

By the mid-20th century, Rochester had become a ghost town, with scattered ruins, mill foundations, and remnants stretching over two miles through the canyon.

Role in Pershing County History

Rochester played a significant role in the mining heritage of Pershing County, one of Nevada’s key mining regions. Pershing County—formed on March 18, 1919 (the newest county in Nevada, carved from Humboldt County and named after General John J. Pershing of World War I fame)—has long relied on mining and ranching. The area was part of early westward expansion routes like the Humboldt Trail.

Rochester’s 1912–1920s boom stood out as one of north-central Nevada’s most successful mining camps during a period when many districts struggled. Its production contributed to the region’s economy and highlighted Pershing County’s silver and gold potential in the Humboldt Range.

While the historic Rochester town is abandoned, modern mining revived in the district. The Coeur Rochester Mine (an open-pit heap-leach silver-gold operation) began in 1986, paused from 2007–2010, and resumed in 2011. It remains the largest employer in Pershing County today, building on the legacy of the early 20th-century discoveries.

Rochester exemplifies Nevada’s classic boom-and-bust mining cycle: modest beginnings, a dramatic silver rush, rapid growth, and eventual decline—leaving behind a poignant ghost town that attracts historians, explorers, and off-road enthusiasts.

Rochester Nevada Trail Map

Futher Reading

Cave Valley Nevada

Official seal of Lincoln County, Nevada
Official seal of Lincoln County, Nevada

Cave Valley is a remote, largely abandoned settlement (often classified as a ghost town or extinct town) in northern Lincoln County, Nevada. It sits in a valley of the same name within the Basin and Range Province, at an elevation of approximately 6,457 feet (1,968 m). Coordinates are roughly 38°38′36″N 114°48′15″W.

Early History and Naming

The valley derives its name from prominent limestone cave systems, particularly Cave Valley Cave (also known as Cave Valley Cave), one of the most notable caves in Nevada after Lehman Caves.

  • Prehistoric and Indigenous Use: Like much of Lincoln County, the area has evidence of long-term Native American presence, including Southern Paiute and possibly earlier groups. Caves in the region served as shelters, storage sites, or ceremonial locations, though specific archaeological details for Cave Valley Cave are less publicized than sites like Hidden Cave or Etna Cave.
  • European Exploration: The cave gained early attention during U.S. Army surveys. In 1869, First Lieutenant George M. Wheeler (of the Wheeler Survey, also associated with Wheeler Peak) explored and mapped the cave as part of broader reconnaissance efforts. His party, guided in part by local knowledge, surveyed around 2,400–3,000 feet of passages, documenting chambers, a deep shaft, and muddy sections. This ranks among the earliest systematic cave surveys in the American West.
  • An 1881 county history described the cave vividly: an opening on the east side of the valley (then seen as a continuation of Steptoe/Perry Valley), with expanding chambers up to 10–12 feet high, a 90-foot dry shaft, a small spring, and explorations extending over two miles. It was called the “most remarkable cave” in the county.

19th and Early 20th Century Development

Lincoln County’s broader history involves Native American habitation, Mormon settlement attempts in nearby valleys (e.g., Meadow Valley/Panaca in the 1860s), and mining booms in the 1860s–1870s around Pioche and other districts.

Cave Valley itself saw limited settlement but featured mining activity. The Cave Valley Mine (Patterson Mining District) produced silver, with associated lead, copper, and minor uranium. It operated as an underground past producer at around 6,500 feet elevation. Ore deposits drew interest in the early 20th century, though it was never a major district.

A small community existed, supported by ranching potential in the grassy valley and mining prospects. A post office operated from 1926 to 1933, marking the peak of formal recognition for the settlement.

Later History and Current Status

By the mid-20th century, Cave Valley declined into an extinct town, typical of many remote Nevada mining/ranching outposts as economic activities shifted. The area remains sparsely populated, with ongoing ranching in surrounding watersheds. It has been noted in conservation contexts (e.g., water rights cases) and as a site of historical interest.

The cave has been highlighted among Nevada’s endangered historic places due to its significance and vulnerability. Red clay from the cave was historically mined for cosmetics. Access is via Cave Valley Road (gravel), about 45 miles northwest of Pioche off U.S. Route 93.

Summary

Cave Valley exemplifies Nevada’s remote high-desert history: shaped by geology (caves formed in limestone), early exploration and surveying, modest mining and ranching, and the boom-and-bust cycles of the American West. It lacks the dramatic scale of Pioche’s mining heyday but holds unique value for its cave system and place in regional surveys. Today, it appeals mainly to historians, cavers, off-road enthusiasts, and those seeking quiet Nevada backcountry.

Sources: Primarily drawn from 1881 Lincoln County histories, Western Mining History, Nevada Bureau of Mines reports, and county tourism resources. For visits, check road conditions, respect private property, and note that old mines and caves can be hazardous.

Parran, Nevada – Churchill County Ghost Town

Parran, Nevada, is a short-lived ghost town and former railroad station in Churchill County, located in the remote desert landscape near the margins of the Carson Sink (part of the historic Humboldt and Carson Sinks region). Today, it consists of scattered ruins including remnants of an old salt plant, a water tank, and pump station, set against salt-encrusted playas, greasewood, and sand dunes typical of the Great Basin.

Location and Setting

Parran sits approximately 22–32 miles north of Fallon, Nevada, along or near U.S. Highway 95 (with access via a rural section between I-80 west of Lovelock and Highway 50 at Fallon). Its coordinates are roughly 39°48′05″N 118°46′24″W (or 39.8020751° N, 118.773551° W). The area is part of the broader White Plains Flat / Parran Flat region in northwestern Churchill County, characterized by arid conditions, lack of local water sources, and proximity to saline deposits. Nearby historic railroad points included Huxley (to the north) and Ocala (to the northeast), with Parran positioned between Desert and Huxley on the line.

The surrounding environment features playa margins with standing water in the sink at times, distant cottonwoods along the lower Carson River channel, barren dunes of clay and sand, and gravel pits from ancient Lake Lahontan beach deposits. Water for the station had to be imported by tank cars into an underground cistern and pumped to a tank, highlighting the harsh desert challenges.

Establishment and Railroad Context (1902)

Parran originated in 1902 during a major realignment and rebuilding of the railroad line by the Southern Pacific Railroad (SP). The original Central Pacific Railroad (completed across Nevada in the late 1860s as part of the first transcontinental railroad) had been sold to the Southern Pacific in 1899 amid financial difficulties. To improve efficiency, SP rerouted over 200 miles of track between 1902–1903 (and later phases in 1907–1908), shifting from the older Truckee River route across the Forty-Mile Desert to a flatter path following the Carson River south and southwest of the Humboldt Dike. This avoided steep grades like the “White Plains hill,” though it slightly increased distance; the change reduced travel time and operational costs.

New stations and sidings were established along this rerouted line, including at Huxley, Parran, and a section house at Ocala. Parran functioned primarily as a telegraph station and “jerkwater” stop—a minor siding where steam locomotives could quickly refill water tanks from overhead hoses without the crew leaving the cab. It included sidings for passing trains during congestion and supported track maintenance in the dry desert stretch. It was one of several such stops between Lovelock and Wadsworth.

In anticipation of the new rail access, the Kinney Saline Deposits Association constructed a salt works near Parran in 1902 to exploit nearby saline deposits through solar evaporation of brines.

Salt Production and Economic Activity

The primary (and short-lived) industry tied to Parran was salt production. The Kinney works shipped small quantities of salt, mainly to local farmers and ranchers in the region, as well as some to silver mines in earlier decades from broader Churchill County deposits. Production at Parran continued on a limited scale under the International Salt Company, which operated under a lease from the Desert Crystal Salt Company in 1911 and 1912. Annual output was modest—on the order of a few hundred tons at peak for the broader area—and the plant’s valuation remained low (around $1,000 in 1915).

Salt extraction in the vicinity (including sites like White Plains, Sand Springs, and Leete) had roots going back to the 1870s with companies like the Desert Crystal Salt Co., but operations at Parran specifically lasted only about seven to eight years before declining sharply. By 1915–1916, the works were largely idle or abandoned, with minimal tax contributions and no sustained market to support larger-scale shipping despite rail access. No significant mining (metallic) or other industries developed, and the area lacked a newspaper or substantial permanent population.

Post Office and Peak Period (1910–1913)

A post office opened at Parran on January 29, 1910, reflecting modest activity and a small service population (a 1909 request noted it would serve about 30 people in the surrounding area). It operated as a telegraph station as well. The post office closed on July 31, 1913, marking the effective end of Parran’s brief formalized community phase.

Decline and Abandonment

Parran’s decline stemmed from the short lifespan of the salt works, limited economic diversification, and the railroad’s emphasis on larger hubs like Wadsworth. The broader Carson Sink region saw some impetus from nearby projects (such as the Newlands Reclamation Project and Fallon’s agricultural development), but Parran remained a minor stop with no reliable local water and harsh conditions. By the mid-1910s, salt production had largely ceased, and the site transitioned into abandonment. It never grew beyond a functional railroad and industrial outpost.

Today

Parran is classified as a ghost town. Visible remnants include ruins of the old salt plant, the water tank, and pump station infrastructure. The site is remote and accessible via dirt roads or tracks off US 95 north of Fallon, though visitors should exercise caution in the desert terrain. It offers a glimpse into early 20th-century railroad engineering, resource extraction in the Great Basin, and the challenges of sustaining settlements in water-scarce environments. Nearby, other Churchill County ghost towns and historic sites (such as those tied to the Pony Express era farther east or the original Central Pacific alignments) provide broader context for Nevada’s transportation and mining history.

Parran exemplifies the boom-and-bust pattern of many small Nevada railroad-dependent outposts—born from infrastructure improvements and resource hopes in the early 1900s, but quickly fading when those hopes did not materialize into lasting development. Its story is intertwined with the evolution of the Southern Pacific line and the modest salt industry of the Carson Sink region.