Category: Historic Monument

Harry Wade Escape Route

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The Harry Wade Escape Route (officially Harry Wade Road, California Historical Landmark No. 622) is a historic dirt road that crosses the remote southern end of Death Valley National Park. It commemorates the path taken in 1849 by Harry Wade and his family, who successfully escaped the valley with their ox-drawn wagon after becoming trapped with a larger emigrant caravan seeking a shortcut to the California Gold Rush. The modern road roughly follows that exit route and now serves as a through-route connecting the paved Badwater Road system on the north with California Highway 127 (and Saratoga Spring Road) on the southeast.

Henry Wade Escape Route Monument located on Highway 127
Henry Wade Escape Route Monument located on Highway 127

Background and the Journey West

Harry Wade was born on March 16, 1800, in Rochester, England. He immigrated to the United States, lived for a time in Pennsylvania, and eventually settled as a farmer near Joliet, Illinois. In early 1849, news of gold discoveries in California prompted him to sell his farm. He packed his wife, Mary Reynolds Leach Wade, and their children (including Harry George Jr., Charles Elliott, Almira, and Richard Angus) into a covered wagon and joined the westward migration.

The family arrived in Salt Lake City too late in the season to risk the northern Sierra Nevada crossings. Like hundreds of other emigrants, they joined a large wagon train—commonly referred to as the Sand Walking Company or San Joaquin Company—that turned south to follow the Old Spanish Trail toward Southern California. Guided in part by Jefferson Hunt, the group of roughly 100 wagons sought a faster route to the gold fields. A poorly planned deviation from the established trail led a significant portion of the travelers, including the Bennett-Arcane (Bennett-Arcan) party and those traveling near them, into the unmapped basin of what is now Death Valley in December 1849.

Entrapment in the Valley

The emigrants found themselves in a deep, arid valley ringed by high mountain ranges. Oxen weakened rapidly, water sources proved unreliable, and progress stalled on the salt flats and harsh terrain. Several people died during the ordeal, helping give the place its grim name. Most parties eventually abandoned or burned their wagons, slaughtered oxen for food, and walked out under extreme hardship.

The Bennett-Arcane contingent became stranded for about a month near the area west of present-day Badwater Basin (later marked as the Bennett-Arcane Long Camp). Two young members of that party, William Lewis Manly and John Rogers, made a heroic roughly 250-mile journey on foot across the Mojave Desert to seek help near Los Angeles. They later returned with supplies and guided the remaining families to safety in early 1850.

Harry Wade’s Independent Decision and Escape

Harry Wade and his family had been traveling slightly behind the main Bennett-Arcane group. They deliberately stayed about a day behind in order to conserve their oxen’s strength and allow the sparse desert springs time to recover between parties. After watching Manly and Rogers depart on their rescue mission, Wade chose not to wait. He doubted that help would return in time (or at all) and decided to seek an independent southern exit.

The family pushed southward through rugged canyons and washes. At a critical moment when water was nearly exhausted, their daughter Almira reportedly noticed birds flying over a ridge and discovered a substantial spring—now known as Saratoga Spring—that provided life-saving water for the family and their animals. From this oasis they continued along an ascending route toward the Amargosa River’s southern bend near Salt Spring. There they regained the Old Spanish Trail. They endured a dry stretch to Bitter Spring, where traders sold them flour, allowing the animals to recover. Following tracks left by earlier parties, they continued through Cajon Pass and reached the Los Angeles area in relative safety.

The Wades were the only known party from the 1849 Death Valley entrapment to exit with both their wagon and oxen intact. This preservation of equipment and draft animals gave them a significant practical advantage over those forced to abandon everything and walk.

Founding and Legacy of the Escape Route

The path Harry Wade pioneered became known as the Harry Wade Exit Route (or Harry Wade Road). It roughly traces a southern exit from the valley floor toward the Amargosa River drainage and the Old Spanish Trail. The modern dirt road within and near Death Valley National Park largely follows this historic corridor, connecting the southern end of Badwater Road with California Highway 127 near the park’s southeast boundary (approximately 30 miles north of Baker).

In 1957 the route was designated California Historical Landmark No. 622. A marker, with a plaque provided by Wade’s descendants, was dedicated near the Highway 127 end of the route (roughly at milepost 29.8, about four miles south of the park boundary). The plaque text summarizes the story: after becoming trapped with the ill-fated 1849 caravan, Harry Wade found an exit route for his ox-drawn wagon, saving his life and those of his wife and children, and at that point the party rejoined the known Spanish Trail to Cajon Pass.

Harry Wade later settled in the Alviso area of Santa Clara County, California, where he died on October 13, 1883. Mary Wade died there in 1889. Their successful escape, achieved through caution, observation, and determination rather than dramatic rescue, remains one of the more practical success stories among the Death Valley ’49ers. The route they opened continues to serve as both a historic landmark and a remote backcountry road, offering modern travelers a tangible connection to the hardships and ingenuity of 1849.

Road Makeup and Route Description

  • Northern connection – Badwater Road: Harry Wade Road begins (or ends) about 2 miles south of the Ashford Mill ruins on Badwater Road, near the point where the pavement bends east toward Jubilee and Salsberry Passes. Badwater Road itself is the main paved artery running south from Furnace Creek past Badwater Basin (the lowest point in North America) and other classic valley-floor attractions before reaching this junction.
  • Harry Wade Road proper: Approximately 24–32 miles of graded-to-rough dirt road running southeast across the valley floor. It passes between the Owlshead Mountains (southwest) and the Ibex Hills / Saddle Peak Hills (east), crosses the Amargosa River channel, and ends at the junction with Saratoga Spring Road near the park’s southeast corner.
  • Southern connection – Saratoga Spring Road / Highway 127: From the junction, Saratoga Spring Road continues a short distance east/northeast to the spring oasis or further to CA-127 (about 30 miles north of Baker). A California Historical Landmark marker stands near the Highway 127 end of the overall escape route.

The full through-drive from Badwater Road to Highway 127 is roughly 30+ miles and can be driven in either direction. It is one of the more remote and least-traveled routes in the park.

Road Conditions

High-clearance is recommended due to washboard, sandy sections, and potential soft spots. As of recent park notices, deep sand is flagged approximately 6 miles south of the Badwater Road junction—this is the most common place vehicles get stuck. The Amargosa River crossing can become impassable when the river is flowing (after storms or in wet winters). Conditions vary widely: the road can be relatively firm after grading or deep and soft at other times. No cell service. Best seasons are late fall through early spring (November–March). Summer heat is extreme and potentially life-threatening. Always check the official NPS Death Valley road conditions page before travel.

Points of Interest Along the Route

Ashford Mill Ruins (near northern junction)
Historic borax mill remnants just north of the Harry Wade / Badwater Road junction. A short stop with interpretive value and views of the southern valley.

Amargosa River Crossing
Usually dry, but a critical potential obstacle. When flowing, it can close the road. The channel marks a key geographic feature of the southern park.

Owlshead Mountains and Owl Hole Spring Road
The range dominates the southwest views. A side road branches toward Owl Hole Spring and the mountains for those seeking additional exploration (higher clearance/4WD often needed).

Ibex Hills, Saddle Peak Hills, and Nearby Dunes
East of the road. White talc waste piles and historic mining areas are visible in the hills. The quiet Ibex Dunes lie nearby and can be reached via connecting routes or short walks.

Saratoga Spring (via short spur from the southern junction)
One of the largest wetland areas in southern Death Valley. Open ponds and marsh grass support waterfowl, the endemic Saratoga Springs pupfish, rare invertebrates, and other wildlife. A short walk from the parking area offers overlooks. The oasis has long served as a watering stop (including for 20-mule teams) and remains a striking green contrast to the arid surroundings. Entry into the sensitive marsh is restricted.

California Historical Landmark Marker (Highway 127 end)
Commemorates Harry Wade’s 1849 escape. Located near the southern entrance, approximately 30 miles north of Baker.

Broader Landscape
Expansive views of the southern valley floor, distant mountain ranges, and occasional wildflower displays in good years. The route feels isolated and true to the “escape” history that gives it its name.

Practical Tips

  • High-clearance vehicle strongly preferred; 4WD helpful in deep sand or after rain. Carry recovery gear, extra water, a full-size spare, and offline maps.
  • Fuel and supplies are available in Baker, Shoshone, or Furnace Creek—nothing exists along the route itself.
  • Dispersed camping is allowed under standard backcountry rules (away from water sources and developed areas).
  • Combine with Saratoga Spring for wildlife viewing or continue north on Badwater Road for classic valley-floor sights.
  • Respect wilderness boundaries and sensitive habitats; stay on designated roads.

The Harry Wade Escape Route offers a genuine sense of the park’s remote southern reaches and a tangible link to the 1849 emigrant history that helped name Death Valley. It is best suited for prepared travelers seeking solitude, history, and a through-route experience rather than crowded overlooks. Verify current conditions with the National Park Service before setting out.

Harry Wade Exit Route – Some 100 wagons found themselves in Salt Lake City too late to cross the Sierra Nevada. They banded together under the name of Sand Walking Co. and started for the gold fields in California over the Old Spanish Trail. After being in Death Valley with the ill-fated 1849 caravan, Harry Wade found this exit route for his ox-drawn wagon, thereby saving his life and those of his wife and children. At this point the Wade party came upon the known Spanish Trail to Cajon Pass.

Highway Placard on Hgwy 127

Further Reading

Henry Wade Escape Route Trailmap

Skidoo Pipeline

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The Skidoo Pipeline was a roughly 21- to 23-mile gravity-fed water line completed in November 1907 that supplied the Skidoo gold mining camp and its mill in the Panamint Mountains of what is now Death Valley National Park, California. It remains one of the notable engineering feats of early 20th-century desert mining.

National Park Sign - Skidoo Pipeline. Photo by James L Rathbun
National Park Sign – Skidoo Pipeline. Photo by James L Rathbun

Discovery and Establishment of Skidoo

In January 1906, prospectors John (or Harry) Ramsey and John “One-Eye” Thompson, traveling toward the gold strike at Harrisburg, were delayed by dense fog near Emigrant Spring. When the fog lifted, they discovered promising gold-bearing ledges and staked claims (part of what became known as the Gold Eagle group). Bob Montgomery soon acquired the claims and organized development, including plans for a quartz mill.

A townsite was laid out by late summer 1906. It was initially called Hoveck (after mine manager Matt Hoveck); the post office opened under that name in 1906, was renamed Skidoo in 1907, and closed in 1917. The name derived from the popular slang phrase “23 skidoo” (meaning to leave or scram). Local explanations often tied the “23” to the approximate length of the planned pipeline, the number of initial claims, the date of discovery, or the number of founders, though the postal service rejected including “23” in the official name.

By March–April 1907 the camp had grown rapidly to an estimated 400–700 residents, with roughly 130 buildings (frame, wood, and iron), stores, saloons, restaurants, a newspaper (Skidoo News), school, bank, doctor, lawyers, telephone/telegraph connection across Death Valley to Rhyolite (Nevada), and stage/auto connections planned or operating toward Beatty, Randsburg, and Keeler. Its elevation of about 5,600–5,700 feet made summer work more practical than in the lower valley.

The Pipeline: Construction, Design, and Operation

Water was the critical limiting factor. Local sources such as Emigrant Spring (hauled by wagon at high cost) were insufficient for a mill and growing town. Montgomery acquired rights to springs near Telescope Peak (notably Birch Spring in Jail Canyon, at roughly 7,200–7,400 feet elevation). Construction of a gravity pipeline began in 1906–1907. About 75 men worked on the line; pipe (primarily spirally riveted steel, with sections of cast iron later, in diameters commonly cited as 6–10 inches or specifically 8 inches) arrived in sections convenient for transport by man and animal.

The line ran approximately 21–23 miles (historical accounts and markers commonly use 23 miles; some contemporary descriptions say 18–22) from Birch Spring/Jail Canyon to the millsite, dropping about 1,800 feet. This provided sufficient head/pressure to power the mill without pumps—a rare achievement in the desert. Estimated early costs were around $150,000; the final cost reached about $250,000. Water first flowed into Skidoo in November 1907. Watering stations along the route also aided prospectors exploring the surrounding country.

The pipeline enabled the only milling plant in the Death Valley region operated almost entirely by water power. The Skidoo Mines Company built a 15-stamp amalgamation and cyanide mill (with later modifications, including rebuilds after damage) using a gravity-feed system for ore processing. This supported large-scale work on relatively narrow high-grade veins.

Years of primary operation: Construction 1906–1907; full service from late 1907. The main mining and milling period ran from 1906/1907 through 1917. The pipeline suffered major damage in January 1913 when it froze and burst in places, forcing a temporary mill shutdown and layoffs. A fire later that year damaged the original mill; a replacement (initially 10-stamp, later expanded) was built. By September 1917 the rich vein had pinched out, the main mine closed, the post office shut down, and much of the pipeline’s iron and steel was dismantled and sold for scrap (some sections remained or proved hard to salvage). Sporadic milling and activity continued intermittently into the 1930s and until about 1942, after which the site was fully abandoned.

Role in Mining and Regional Economy

The Skidoo Mine and district were among the most productive gold operations in the Death Valley region during their peak. Output is commonly estimated at about 75,000 ounces of gold, valued at roughly $1.5–1.6 million at the contemporary price of about $20 per ounce (some accounts place district totals higher). It was the largest mining operation in the area from roughly 1907–1917 and stood out for sustained production compared with many short-lived boom camps. Mining focused on free-gold quartz veins in granitic rocks, with some copper noted later.

The pipeline was essential: without reliable, pressurized water, the water-powered mill and a viable town could not have existed at that remote high-elevation site. It also supported broader prospecting by providing water stations in arid terrain. Development spending exceeded $300,000 in the early years. The Panic of 1907 slowed expansion but did not immediately end the camp; ore depletion and infrastructure failures (especially the 1913 pipeline break) were more decisive in the decline.

Connections to Local Towns and the Broader Area

Skidoo formed part of a network of early-1900s Death Valley and Panamint Range camps:

  • Harrisburg: The nearby gold strike that drew the original prospectors; it largely emptied as people shifted to Skidoo.
  • Rhyolite (Nevada): Linked by telephone/telegraph; a major supply and communication hub across Death Valley. Freight and stage lines connected the camps.
  • Emigrant Spring / Ballarat / Keeler: Water hauling, road proposals, and supply routes. Water rights originated in part from interests near Ballarat.
  • Greenwater and other contemporaneous camps: Shared the regional boom-and-bust cycle; Skidoo outlasted many.

The site later served as a filming location for the 1923 motion picture Greed (one of the early major films shot in Death Valley). Today the Skidoo Historic District (including mill remnants) is listed on the National Register of Historic Places within Death Valley National Park. Visible traces of the pipeline scar remain in places between Telescope Peak/Jail Canyon and the millsite, though much of the pipe was salvaged. The mill ruins (including stamp batteries and cyanide-related features) are among the better-preserved examples of early 20th-century desert milling technology.

In summary, the Skidoo Pipeline (operational primarily 1907–1917, with the broader mining camp active from 1906 into the early 1940s on a reduced scale) transformed a remote gold discovery into one of the more successful and longer-lived mining towns of Death Valley by solving the water problem through ambitious gravity engineering. It powered unique milling operations, sustained a substantial community, and supported regional exploration before ore exhaustion and maintenance challenges ended the boom.

Potosi, Nevada – Clark County Ghost Town

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Potosi (also known as Potosi Camp or Crystal City in the 1870s) is a historic mining ghost town and mining district in Clark County, southern Nevada, located in the Spring Mountains approximately 30–35 miles southwest of Las Vegas. The site, at an elevation of about 5,705 feet, centers on Potosi Mountain (around 8,504 feet) and Potosi Spring. It is significant as the location of Nevada’s first lode mine (the Potosi Mine), with operations dating to the mid-19th century. The Potosi Mining District is listed on the National Register of Historic Places.

Potosi mine, south center of sec. 12, T. 23 S., R. 57 E., the mine workings explore a zone at the base of the Yellowpine limestone. Clark County, Nevada. Circa 1921. Plate 33-B in U.S. Geological Survey. Professional paper 162. 1931.
Potosi mine, south center of sec. 12, T. 23 S., R. 57 E., the mine workings explore a zone at the base of the Yellowpine limestone. Clark County, Nevada. Circa 1921. Plate 33-B in U.S. Geological Survey. Professional paper 162. 1931.

The name “Potosi” derives from the famous silver-mining mountain in Bolivia (Cerro Potosí), passed indirectly through Potosi, Wisconsin, the hometown of an early mine manager. The area’s history spans possible pre-contact Native American use, Spanish exploration theories, Mormon settlement efforts, multiple mining booms and busts, and contributions to national needs during World War I. Today, it is largely abandoned but retains interpretive value and attracts hikers and history enthusiasts.

Early History and Pre-Mormon Activity

Indigenous peoples, including the Chemehuevi, had connections to the area. A giant cave on Potosi Mountain was reportedly used for vision quests by Chemehuevi shamans in the mid-19th century. Paiute guides later directed settlers to mineral deposits.

Speculative accounts suggest Spanish missionaries or Mexican prospectors may have explored or worked silver mines in the region as early as the 1770s or 1830s, possibly linked to the Old Spanish Trail (blazed in 1829–1830). However, these lack strong documentation, and modern recorded history begins in the 1850s. Artifacts like old coins or religious items have been anecdotally reported but are not definitively tied to large-scale operations.

Carol Lombard was killed on a Douglas DC-3, Jan 16, 1942 on Mt Potosi
Carol Lombard was killed on a Douglas DC-3, Jan 16, 1942 on Mt Potosi

Mormon Era and the First Lode Mine (1850s)

The modern history of Potosi is tied to the Mormon (Latter-day Saints) mission at Las Vegas Springs, established in 1855 as part of efforts for economic self-sufficiency in what was then considered part of southern Utah (later New Mexico/Arizona Territory before becoming Nevada). Lead was critically needed for bullets and other uses.

In 1856, a Paiute guide informed Mormon settlers of a lead deposit on the western slope of the Spring Mountains. Nathaniel V. Jones, an experienced miner dispatched from Salt Lake City, inspected and developed the site, naming it Potosi. A small camp with log cabins was built in a ravine below the mine, near a spring. Ore was initially smelted locally with limited success due to fuel and water issues, then hauled to Las Vegas for processing in a smelter inside the stockade (considered the first smelter west of the Missouri River operating in Nevada).

About 9,000 pounds of lead were recovered, but high zinc content complicated smelting. Operations ceased in early 1857 (or late 1856 per some accounts) when Brigham Young recalled the colonists amid tensions with the U.S. government. Potosi became Nevada’s first abandoned mine and ghost town.

Later 19th-Century Revivals (1860s–1870s)

Mining resumed sporadically. In 1861, the Colorado Mining Company (California interests) reopened the mine for silver, building a smelter at Potosi Spring and a camp with rock cabins housing up to 100 miners. Activity lasted until around 1863.

In the 1870s, the Silver State Mining Company worked the mine (sometimes called the Comet) and established Crystal City at Potosi Spring with stone buildings. This phase lasted roughly three years. Prospectors continued small-scale work intermittently for decades.

20th-Century Zinc Boom and Industrial Operations (1900s–1920s)

The arrival of the San Pedro, Los Angeles and Salt Lake Railroad (later Union Pacific) in 1905 enabled economic shipping of complex ores. New assays revealed significant zinc alongside lead and silver, sparking renewed interest.

Operations expanded in the 1910s. The Empire Zinc Company (New Jersey, with Denver offices) took over around 1913, building a modern camp with uniform housing, an electrical plant, a calciner, and an aerial tramway (constructed 1913) to transport ore down the steep hillside. Ore was trucked to railheads like Arden. A Yellow Pine railroad spur aided logistics.

During World War I, Potosi was designated a priority defense project for zinc, lead, and silver production. The mine yielded substantially for the war effort. Population grew temporarily; local newspapers noted births in the camp in 1918. Post-armistice, operations scaled back. The Empire Zinc Company dismantled much of the camp by 1919.

Subsequent lessees, including A.J. and A.R. Robbins and the International Smelting Company (mid-1920s), extracted more zinc (e.g., 31,000 tons in 1925), but high costs led to final abandonment around 1928–1930. Total estimated production reached about $4.5 million in lead, silver, and zinc. Other minerals included gold, copper, and traces of others.

Significance and Legacy

  • Mining Milestone: Nevada’s first lode mine, predating major strikes like the Comstock Lode in importance for early regional development.
  • Mormon Influence: Exemplifies early LDS efforts in the American West for self-sufficiency and settlement.
  • Economic and Military Role: Contributed to national metal supplies, especially in wartime.
  • Cultural/Historic Sites: Nevada State Historical Markers (e.g., No. 115) commemorate the site. The Potosi Mining District is on the National Register of Historic Places. Ruins are minimal today, but the mine itself (multi-level) and tram remnants remain points of interest for explorers.

The site is near the Old Spanish Trail and accessible via dirt roads (high-clearance vehicles recommended). It offers hiking opportunities, including to Potosi Mountain summits and cliffs.

Conclusion

Potosi embodies the boom-and-bust cycle of Nevada mining towns—driven by mineral riches, technological advances (railroads, trams), and national demands, yet challenged by remoteness, ore complexities, and economics. From a short-lived Mormon outpost to a contributor in World War I, its legacy as Nevada’s pioneering lode mine endures in historical markers, archives, and the rugged landscape of the Spring Mountains. While retired and deserted, it remains a tangible link to the state’s frontier past.

Sources: Compiled from Nevada SHPO historical markers, Travel Nevada Magazine archives, and related historical accounts. For on-site visits, consult current land access and safety information, as old mines pose hazards.

Potosi is a designated at Nevada State Historic Marker no. 115.

Town Summary

NamePotosi
LocationClark County, Nevada
GNIS849366
Latitude, Longitude35.9708, -115.5408
Elevation5705
Population100

Potosi Trailmap

References

Unionville, Nevada – Pershing County

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Unionville, Nevada, is a small unincorporated community and census-designated place (CDP) in Pershing County, located in Buena Vista Canyon on the eastern slope of the Humboldt Range. It sits south of Interstate 80, just west of State Route 400. As of the 2020 census, it had a population of 27.

It is often described as a living ghost town or semi-ghost town, with remnants of its mining past including old mill foundations, a historic cemetery, abandoned structures like a one-room schoolhouse and Mark Twain’s former cabin, and a few occupied homes.

Founding and Early History (1861)

Unionville originated during the early Nevada silver mining boom. In spring 1861, Paiute Indians brought silver ore samples from Buena Vista Canyon to Virginia City. Prospectors followed and confirmed rich deposits. The Unionville (or Buena Vista) mining district was organized shortly afterward, and the town was laid out in May 1861 in the upper part of the canyon.

Initially called Buena Vista (after the canyon) and then Dixie by Southern sympathizers, the name changed to Unionville around July 4, 1861 (or late 1861), as Northern and neutral factions gained dominance amid Civil War tensions. The town was divided into sections (e.g., Lower Town/Dixie for Southerners and Upper Town for Northerners), separated by “Centerville” as a sort of Mason-Dixon line.

In November 1861, Unionville became the county seat of the newly created Humboldt County, serving in that role until 1873.

Boom Years (1863–1870)

Unionville experienced its peak mining boom between 1863 and 1870. Exaggerated reports of riches drew prospectors, including Samuel Clemens (Mark Twain), who arrived in late 1861/1862 intending to strike it rich but left disappointed after limited success. He described the early camp as “eleven cabins and a liberty-pole” in Roughing It.

At its height, the population reached 1,000–1,500. The town stretched over two miles along the canyon and featured over 200 houses, ten stores, nine saloons, six hotels, four livery stables, a brewery, and other businesses. Two newspapers served the area: the Humboldt Register and Silver State. An omnibus line ran hourly between sections of town. The Arizona Mine (discovered 1862) was a major producer, along with others like the Henning and Pfluger. Three stamp mills operated in the early 1870s to process lower-grade ores.

Silver was the primary commodity, with some gold. High-grade ore was sometimes shipped to Wales for processing. The town acted as a supply and distribution center.

Social Issues and Challenges

Like many Western mining towns, Unionville had tensions. In January 1869, an Anti-Chinese League forcibly expelled around 35–50 Chinese residents (miners and laborers), transporting them to Mill City on the railroad. This reflected widespread anti-Chinese sentiment in Nevada; federal indictments followed, but few convictions resulted. Some Chinese miners later returned to work claims in the area into the early 20th century.

Decline (1870s Onward)

By 1870, rich surface ores were largely depleted, and deeper mining proved less profitable. A major fire in 1872 caused significant damage. The completion of the Central Pacific Railroad through the Humboldt Valley (bypassing Unionville and favoring Winnemucca as a trade hub) accelerated the decline. In 1873, the Humboldt County seat moved to Winnemucca. By 1880, the population had dropped to around 200. Mining continued on a smaller scale into the 1880s, but Unionville never recovered its former prominence.

Pershing County was created in 1919 from part of Humboldt County (named after General John Pershing); Unionville fell within the new county but was too small to compete for the county seat (Lovelock became the seat). By 1920, only about 70 people remained.

Modern Unionville

Today, Unionville is a quiet hamlet with a small permanent population (around 20–27). It features scattered ruins, preserved sites like Twain’s cabin, a historic cemetery, and some modern structures. There is limited tourism, including a tourist inn, but no formal local government. It serves as a reminder of Nevada’s early mining history.

Unionville highlights the classic boom-and-bust cycle of Nevada mining towns, shaped by mineral wealth, Civil War politics, transportation changes, and shifting economic centers. Its brief but vibrant history contributed to the development of Humboldt and Pershing counties in the American West.

Nevada State Historic Marker 232

Nevada Historical Marker 232
Reunion in Unionville
SR 400 in in County Park
Unionville

Reunion in Unionville

Across the road and down about 300 feet was the original Unionville school. Built in 1862, this adobe building was the first public structure in the county. Used by such organizations as the Union League, Knights of the Golden Circle, the Masons and the Ancient and Honorable Order of E. Clampus Vitus, it served the community until its demolition in 1871.

Exactly 109 years later, members of the E.C.V. gathered here to hold a reunion in commemoration of this propitious event. To the rear of this marker are the remains of Mark Twain’s cabin. Also a member of E.C.V., he built this structure in 1861 and lived here before moving to Virginia City.

Taylor, Nevada – White Pine County Ghost town

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Taylor, Nevada, located in White Pine County approximately 15 miles southeast of Ely, was a quintessential mining boomtown of the late 19th century. Established following the discovery of silver and gold in 1873, Taylor epitomized the rapid rise and fall of mining communities in the American West.

Main Street, Taylor Nevada 1882
Main Street, Taylor Nevada 1882

Founding and Early Development (1872–1880)

Silver and gold were discovered in 1873 by prospectors Taylor and John Platt, guided by a local Native American, Jim Ragsdale, who was paid $500 for leading them to a silver ledge. The Taylor Mine was staked and sold in 1875 to the Martin White Company of Ward for $14,000. Concurrently, the nearby Monitor Mine was discovered, laying the foundation for the town’s growth. However, significant development did not occur until 1880, when the camp of Taylor began to take shape. In 1881, the Monitor Mill and Mining Company constructed a ten-stamp mill seven miles northwest of Taylor on Steptoe Creek, which began operations in September 1881, processing ore from the surrounding mines.

Boom Period (1881–1886)

Taylor’s peak came in 1883, following new ore discoveries and the construction of the Argus Mill. The town’s population reportedly reached 1,500, though some historical markers exaggerate this figure at 15,000, likely an overstatement given the scale of operations. By the end of 1883, Taylor boasted a vibrant community with three general stores, four restaurants, three boarding houses, seven saloons, a brewery, a drugstore, a doctor’s office, a school, an opera house, a Wells Fargo office, and professional services. Two newspapers, the White Pine News and the Taylor Reflex (relocated from Ward), were published, reflecting the town’s cultural and economic vitality. The annual Fourth of July celebration became a social highlight, cementing Taylor’s role as a regional hub by 1886. During this period, the mines shipped over $260,000 worth of ore (approximately $8 million in 2025 dollars), primarily silver, with gold, copper, and lead as secondary outputs.

Decline (1885–1890)

Taylor’s prosperity was short-lived. By 1885, the free-milling silver ore began to deplete, and a tragic accident in 1886 at the Argus Mine—where a drill struck dynamite, killing one miner and blinding another—accelerated the town’s decline. The Monitor Mill closed in 1886, followed by the Argus Mill in 1889. By 1890, only a handful of residents remained, with many businesses and buildings relocated to nearby Ely, which was emerging as a more stable economic center.

Revivals and Final Decline (1918–1991)

Mining in Taylor saw intermittent revivals. In 1918, the Wyoming Mining & Milling Company built a 100-ton cyanide plant at the Argus Mine, processing 60,000 tons of ore in its first year (1919). The mill operated from 1921 to 1923, producing 40–50 tons of ore daily, but closed again due to falling silver prices. World War II temporarily spurred mining activity, with local mines yielding over $3 million in silver, gold, copper, and lead over their lifetime. In 1980, Silver King Mines, Inc., of Salt Lake City initiated a $10 million open-pit operation, which continued until 1991. This final phase destroyed much of what remained of Taylor’s original structures, leaving only a few buildings and mining remnants.

Present Day

Today, Taylor is a ghost town, with only two buildings remaining and much of the site obscured by modern mining operations. Located at coordinates 39°04’47.0″N, 114°41’07.0″W, it is accessible via a well-maintained gravel road off U.S. Highways 6, 50, and 93, near Ely. The Nevada State Historical Marker No. 99, erected by the Nevada State Park System and White Pine Public Museum, marks the site, summarizing its history. The area remains of interest for ongoing mineral exploration, but the town’s historical footprint is minimal, with most structures lost to time or modern mining.

Connection to Nevada Northern Railway

Taylor’s mining operations were closely tied to the Nevada Northern Railway, which connected Ely to national rail networks starting in 1906. While Taylor’s boom preceded the railway’s construction, the railway facilitated ore transport from nearby mines during later revivals, particularly in the early 20th century. The Nevada Northern’s Ore Line, extending to Ruth and McGill, supported the region’s mining economy, indirectly sustaining Taylor’s intermittent operations.

Conclusion

Taylor, Nevada, exemplifies the boom-and-bust cycle of Western mining towns. From its rapid growth in the 1880s to its near-total disappearance by the late 20th century, Taylor’s history reflects the challenges of sustaining resource-dependent communities. Its legacy endures through historical markers, sparse remnants, and its role in White Pine County’s mining heritage, preserved in part by the Nevada Northern Railway Museum’s efforts to document the region’s rail and mining history.

Nevada State Historic Marker

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. These roadside markers bring attention to the places, people, and events that make up Nevada’s heritage. They are as diverse as the counties they are located within and range from the typical mining boom and bust town to the largest and most accessible petroglyph sites in Northern Nevada Budget cuts to the program caused the program to become dormant in 2009. Many of the markers are lost or damaged.

Most of the markers across the state are large blue metal markers. However, there are a variety of other marker styles out there. For this guide they have been simplified into a few categories (blue, blue small, concrete, and stone). Sometimes, the markers are on buildings, fences, or metal stands.

Silver and gold were discovered by Taylor and John Platt in 1873 in what was to become Taylor, a typical mining community supported chiefly by the Argus and Monitor Mines.  In seven years, the town boasted a population of 15,000 people, seven saloons, three general stores, an opera house, a Wells Fargo office, and other businesses.  By 1886, Taylor was the center of county activity, a social highlight being the annual 4th of July celebration.

Mining continued intermittently until 1919.  At that time, a 100 ton cyanide plant at the ArgusMine gave the area new life, but production declined when the price of silver plummeted.  World War II renewed mining activity temporarily.  Local mines yielded more than $3 million in silver, gold, copper, and lead.

STATE HISTORICAL MARKER NO.  99

STATE HISTORIC PRESERVATION OFFICE

WHITE PINE PUBLIC MUSEUM, INCORPORATED

Nevada State Historic Marker Map

Summary

NameTaylor, Nevada
LocationWhite Pine County, Nevada
Latitude, Longitude39.0885, -114.7522
Nevada State Historic Marker99

References