Goodsprings, Nevada

Goodsprings is an unincorporated community and census-designated place (CDP) in Clark County, southern Nevada, located in Goodsprings Valley at the southeastern foothills of the Spring Mountains. Situated along Nevada State Route 161, about five miles northeast of Jean and Interstate 15 (roughly 30-45 minutes southwest of Las Vegas), it sits at an elevation of 3,717 feet in an arid desert environment. Once the heart of one of Clark County’s most productive mining districts, Goodsprings thrived as a boomtown in the early 20th century before declining into a small, semi-preserved settlement often described as a “living ghost town.” As of the 2020 census, its population was 162.

Goodsprings, Nevada - 1924
Goodsprings, Nevada – 1924

Pre-History and Early Settlement (Pre-1900)

The area around Goodsprings has long been a rare water source in the Mojave Desert. Indigenous peoples, including the Ancient Puebloans and later the Paiute, used the natural springs seasonally. White settlers first documented the springs in 1830 along the Old Spanish Trail.

Mining in the broader region began in 1856 when Mormon miners established a lead operation at nearby Potosi Mountain—possibly Nevada’s oldest underground lode mine. Gold was discovered in the area in 1893. In the 1860s, cattleman Joseph Good discovered silver near the springs (sometimes dated to 1861 or 1868) and established a small store while using the water for his herd. The settlement was initially called “Good’s Springs” or “Goods Springs” in his honor. By 1868, additional silver and lead deposits attracted more prospectors, forming a rudimentary mining camp. The Yellow Pine Mining District (also known as the Goodsprings Mining District) was formally organized around 1882 following further gold discoveries.

Before 1900, the area consisted mainly of tent cabins and a small mill. A post office opened in 1899 (initially at the nearby Keystone Mine, later relocated), and Lincoln County established Goodsprings Township. In 1904, Salt Lake City mining interests platted the township. Early structures were limited until transportation improved.

An old water tower located inside Goodspings, Nevada
An old water tower located inside Goodspings, Nevada

The Mining Boom and Peak Prosperity (1900s–1920s)

The arrival of railroads transformed Goodsprings. The San Pedro, Los Angeles & Salt Lake Railroad (later Union Pacific) reached nearby Jean in 1905. In 1911, the narrow-gauge Yellow Pine Railroad connected the mines to Jean, drastically reducing ore transport costs and spurring construction of permanent buildings. The Yellow Pine Mining Company consolidated claims in 1909, operating a mill and focusing on oxidized zinc, lead, silver, copper, and gold.

World War I dramatically boosted the economy, as demand for lead (for ammunition) and zinc surged. By 1916–1918, the population peaked at around 800 (some accounts cite up to 1,000), supporting a developed downtown with a hospital, luxury hotel, post office, weekly newspaper (Goodsprings Gazette, 1918–1921), stores, churches, and multiple saloons. The district became Clark County’s most productive, yielding a total of approximately $25 million in minerals—primarily lead and zinc, with lesser amounts of gold, silver, copper, and rarer elements like molybdenum, vanadium, nickel, cobalt, platinum, palladium, and uranium. It represented the greatest variety of minerals in Nevada.

Key Infrastructure and Landmarks Built During the Boom

1916: The 20-room Fayle Hotel (considered one of Nevada’s finest at the time, with modern amenities; destroyed by fire in 1966).

1913: The Pioneer Saloon (built by Clark County Commissioner George Fayle using prefabricated stamped-tin construction), General Store, and Community Church. The saloon, Nevada’s oldest continuously operating bar in southern Nevada, featured an original cherry-wood bar and quickly became the social hub.

1913: Goodsprings Schoolhouse (the oldest school in Clark County built specifically as a school; still in use today and listed on the National Register of Historic Places).

The Pioneer Saloon located in Goodsprings, Nevada is still open and quite busy
The Pioneer Saloon located in Goodsprings, Nevada is still open and quite busy

Notable events include a 1915 saloon shooting during a card game (miner Paul Coski killed by Joe Armstrong; ruled self-defense, with bullet holes still visible) and the 1942 plane crash of actress Carole Lombard on nearby Mount Potosi. Her husband, Clark Gable, waited at the Fayle Hotel and Pioneer Saloon for news of the tragedy; a memorial to the victims remains in the saloon today.

Decline and Transition (1920s–1950s)

Post-World War I, falling metal prices led to mine closures and population decline (down to about 400 by 1920). The Yellow Pine Railroad ceased operations around 1930 (tracks removed by the mid-1930s). A brief resurgence occurred during World War II due to renewed demand, but mining largely ended by the 1950s. The town contracted but never fully vanished, unlike many desert boomtowns. Fires destroyed several structures, and atomic testing occurred in the region during the 1950s. By the late 20th century, fewer than 100–200 residents remained, living among preserved and restored buildings, mobile homes, and newer structures.

Modern Era and Preservation (1960s–Present)

Goodsprings endures as a quiet desert community with a focus on historic preservation. The Goodsprings Historical Society (established in the 1990s) works to educate the public, restore buildings (e.g., roof repairs), and maintain sites like the 1886 Campbell Stone Cabin (one of the oldest structures), the cemetery, and mill ruins. The Pioneer Saloon continues operating as a tourist draw, hosting events, filming locations (The Misfits, Fear and Loathing in Las Vegas), and even inspiring a recreation in the 2010 video game Fallout: New Vegas (which has boosted visitation through annual festivals since 2022).

In 2010, the Goodsprings Waste Heat Recovery Station (a 7.5 MW geothermal-style plant using pipeline waste heat) opened as Nevada’s first renewable energy facility of its kind. The town remains accessible for day trips from Las Vegas, with the saloon, schoolhouse, and surrounding desert landscape attracting history enthusiasts and off-roaders.

Conclusion

Goodsprings exemplifies the classic Nevada mining town arc: from obscure springs and prospector camps to wartime prosperity and eventual contraction, while retaining its historic character. Its $25+ million in mineral wealth, pioneering infrastructure, and resilient landmarks like the Pioneer Saloon underscore its significance in Clark County’s development. Today, it stands not as a fully abandoned ghost town but as a preserved chapter of the American West—tied to Indigenous heritage, railroad expansion, world wars, Hollywood tragedy, and modern tourism—offering a tangible link to Nevada’s rugged past amid the Mojave Desert.

Goodsprings Mines

  • Alice Mine
  • Argentina Mine
  • Belle Mine
  • Columbia Mine
  • Cosmopolitan Mine
  • Fredrickson Mine
  • Green Copper Mine
  • Hermosa Mine
  • Hoosier Mine
  • Iron gold Mine
  • Lookout Mine
  • Keystone Mine
  • Lavina Mine
  • Middlesex Mine
  • Surprise Mine
  • Table Top Mine
  • Yellow Pine
The mill site located just outside of Goodsprings, Nevada
The mill site located just outside of Goodsprings, Nevada

Goodsprings Nevada Trailmap

Titus Canyon

Titus Canyon has it all, rugged mountains, colorful rock formations, a small ghost town, mines, petroglyphs, wildlife, rare plants and spectacular canyon narrows as a grand finale! Titus Canyon is the most popular back-country road in Death Valley National Park and just plain fun to run.  The canyon is easily accessible from Stovepipe wells and Furnace Creek.

Titus Canyon, a narrow canyon drive in Death Valley National Park, CA
Titus Canyon, a narrow canyon drive in Death Valley National Park, CA

Although the Grapevine Mountains were uplifted relatively recently, most of the rocks that make up the range are over half a billion years old. The gray rocks lining the walls of the western end of the Canyon are Cambrian limestone. These ancient Paleozoic rocks formed at a time when the Death Valley area was submerged beneath tropical seas. By the end of the Precambrian, the continental edge of North America had been planed off by erosion to a gently rounded surface of low relief. The rise and fall of the Cambrian seas periodically shifted the shoreline eastward, flooding the continent, then regressed westward, exposing the limestone layers to erosion. The sediments have since been upturned, up folded (forming anticlines), down folded (forming synclines) and folded back onto themselves (forming recumbent folds).

Leadfield Gost Town, Death Valley, California
Leadfield Gost Town, Death Valley, California

Although some of the limestone exposed in the walls of the canyon originated from thick mats of algae (stromatolites) that thrived in the warm, shallow Death Valley seas, most of the gray limestone shows little structure. Thousands of feet (hundreds of meters) of this limey goo were deposited in the Death Valley region. Similar limestone layers may be seen at Lake Mead National Recreation Area and at the bottom of the Grand Canyon.
At one of the bends in the canyon, megabreccia can be seen.

Leadfield was an unincorporated community, and historic mining town found in Titus Canyon in Death Valley National Park.

Titus Canyon Trail Map

Old Mojave Road

The Old Mojave Road (Government Road) is an east-west route that enters the Mojave National Preserve off the highway 95 in Nevada, and Afton Canyon on the west side.  Some sections are rough and sandy; 4 x 4 recommended. Roads can become slick, muddy and impassable after rains. Be sure to inquire about road conditions, especially if you plan to cross Soda Dry Lake.

The railroad monument along the Old Mojave Road in the Mojave National Preserve.
The railroad monument along the Old Mojave Road in the Mojave National Preserve.

The Mojave Road is party of the Old Spanish Trail, which is a 700 mile long historical trade route that connected the northern New Mexico settlements near Santa Fe, New Mexico with those of Los Angeles, California. The Old Spanish trail’s rugged terrain discouraged the use of wagons. It was always a pack route, mainly used by men and mules. Used by Indians to transport goods from the southwest to trade with the Chumash and other coastal tribes, this route later served the cause of westward expansion. Military forts were established along the route to protect key water sources and provide assistance for travelers.

The route at one time was for all intents and purposes lost until Dennis Casebier and Friends researched the route and reestablished the trail as if it know today and is a popular four-wheel drive road.

The eastern section of the Old Mojave Road leaves US 95 in Nevada near Laughlin moving westward.  The eastern section climbs up to Fort Piute and continues past an old corral one a rocky climb.  Once up on the plateau, the road continues to travel west to Nipton Road.

Bert Smith's Cabin located in the Mojave National Reserve
Bert Smith’s Cabin located in the Mojave National Reserve

The central section starts at Nipton Road and continues west to Kelbaker road near Baker, CA.  The road starts rather narrow with high brush offering the opportunity for some new desert pin-striping.

Government Holes in the central section of the Old Mojave Road.
Government Holes in the central section of the Old Mojave Road.

A short declination which offers the only real obstacle near Rock Spring.  Burt Smiths cabin and the Government Holes water offer short hikes and distractions from the trail.  Once you cross the Kelso Cima Road, about 5 miles of  “whoop de doos” will rock you to sleep.  The center section offers the most to see, and if you choose one section, this would be it in our opinion.

The western section leaves Kelbaker road and continues west into the dry soda lake south of Baker.  The western section of the route can best be described as dry and sandy.  A larger mine complex and Afton Canyon are the major sights.

Afton Canyon in the Mojave National Preserve.
Afton Canyon in the Mojave National Preserve.

In addition to over 100 miles of 4×4 trail, the Old Mojave road offers access to mines, old homesteads, and other 4×4 routes.  The Old Mojave can be run either way and in a single long day, or in thirds with access being provided from Kelbaker road out of Baker or the Nipton Road in the the East.  However, for the best experience, take your time and run the trail in Multiple days and overnight in one of many primitive or established Campgrounds.

Old Mojave Road Trail Map

Skidoo California – Inyo County Ghost Town

Skidoo, California, once a bustling gold mining town in the early 20th century, now stands as a ghost town within Death Valley National Park. Located in Inyo County at an elevation of 5,689 feet, Skidoo epitomized the boom-and-bust cycle of mining communities in the American West. Its history, marked by rapid growth, innovative engineering, and eventual decline, offers a glimpse into the challenges and ambitions of desert mining during the gold rush era. This report explores Skidoo’s origins, development, key events, and legacy, drawing on historical records and contemporary accounts.

Skidoo, CA 1907
Skidoo California, 1907

Origins and Establishment

Skidoo’s story began in January 1906, when prospectors John Ramsey and John “One-Eye” Thompson, en route to the gold strike at Harrisburg, were halted by a rare fog near Emigrant Spring. When the fog lifted, they discovered promising gold-bearing ledges, leading them to file claims for what became the Gold Eagle Group. News of their find spread, and Bob Montgomery, a prominent mining figure from Rhyolite, purchased these claims for $100,000, fueling the rapid development of the area. Initially named Hoveck after Matt Hoveck, the Skidoo Mine’s manager, the town was renamed Skidoo in 1907, inspired by the popular slang phrase “23 skidoo,” meaning to leave quickly or take advantage of an opportunity. Local lore suggests the name also referenced the 23 miles of pipeline bringing water to the town, though this remains speculative.

Right here on the border line between California and Nevada, just a few miles from arid within speaking distance of Nevada’s big, bonanza gold camps of Goldfield, Rhyolite, Tonopah, California promises to give birth to the most wonderful gold mines America has yet produced . . . . Here the golden goddess is again singing her siren song of enchantment and California is again beckoning to the world with a finger of gold: and the world is listening, and looking, and coming–TO SKIDOO!

Rhyolite Herald, 4 January 1907

Boom Years (1906–1917)

Skidoo quickly grew into a thriving community, peaking at around 700 residents by mid-1907. The town boasted advanced amenities for its time, including a post office (established as Hoveck in 1906 and renamed Skidoo in 1907), a telephone exchange, the Skidoo News newspaper, a school with 29 students, four saloons, three restaurants, and the Southern California Bank of Skidoo. Stagecoach connections to Rhyolite and Ballarat, along with private automobiles, linked Skidoo to nearby settlements, while a telephone line to Rhyolite facilitated communication.

The Skidoo Mine, operated by the Skidoo Mines Company, was the town’s economic backbone, producing approximately 75,000 ounces of gold—valued at over $1.5 million at the time—between 1906 and 1917. The mine’s success was bolstered by two remarkable engineering feats. First, Skidoo hosted the only milling plant in the Death Valley region powered almost entirely by water, using a gravity-feed system to separate gold from ore. Second, a 23-mile pipeline, constructed by Bob Montgomery, transported water from springs near Telescope Peak to the mill, an extraordinary achievement given the desert’s harsh terrain. The pipeline’s scar remains visible today, and watering stations along its route supported prospectors exploring the region.

By 1907, over 100 men were employed at the Skidoo mines, and development costs exceeded $300,000. The town’s prosperity attracted attention, with the Rhyolite Herald proclaiming in January 1907, “California promises to give birth to the most wonderful gold mines America has yet produced… TO SKIDOO!” However, the national financial panic of 1907 strained the town, particularly impacting the Southern California Bank of Skidoo, which faced creditors and operated out of cramped quarters in a grocery store.

	Cook's horse-drawn wagon at Death Valley's gold mining camp, Skiddo.
Cook’s horse-drawn wagon at Death Valley’s gold mining camp, Skiddo.

Notable Events

Skidoo was relatively peaceful compared to other mining camps, but it was not without incident. In April 1908, Joe Simpson, a gambler with a notorious reputation, attempted to kill the Southern California Bank’s cashier, Dobbs, and murdered James Arnold, a popular local butcher. With no jail in Skidoo, Simpson was held in a cast-iron building under guard. An armed mob demanded his release and lynched him from a telephone pole, an event that underscored the town’s rough justice.

Another challenge came in 1913, when the pipeline froze and burst, followed by a fire that destroyed much of the original stamp mill. The Skidoo Mines Company swiftly rebuilt a ten-stamp mill, adding five more stamps by 1915, but these setbacks foreshadowed the town’s decline.

The Skidoo Mine is located 65 miles north of Trona, California, at 6500 ft. elevation. The property was established in 1906; the mill erected in 190?. The mill burned and was reconstructed in 1913. Owner: Skidoo Mines Co., Skidoo, CA. C. W. Cross, president, and Crynski , superintendent .

Two systems of quartz veins occur in a pegmatite granite. The main vein system strikes M-SE and the other E~W. The veins average from 18″ to 2 ‘ in width, with a maximum of 4’.

The ore is free milling and values average about $15.00 per ton. Ore is hauled to the mill through tunnels. The mill equipment consists of: ten 850-lb. stamps, five 1150-lb. stamps and amalgamation tables. Table tailings run to the cyanide plant and precipitated in zinc boxes. The mill is operated by water conveyed in an 8″ pipeline 21 miles
from Telescope Peak. The pipe was installed at a cost of over $200,000, 35 men were employed at the mine mill. Total production to date over $1,500,000,

California State Mining Bureau’s “Report of State Mineralogist,” 1915-16, Report XV:
Rare Air Photograph of Skidoo California Taken from the air in 1923
Rare Air Photograph of Skidoo California Taken from the air in 1923

Decline and Abandonment

Skidoo’s fortunes waned as its gold veins diminished. By early 1909, the town’s population began to decline, and the school district closed in September 1909. In July 1909, the Los Angeles Mining Review reported that the Skidoo Mine was California’s second-most productive, clearing all debts and paying a $50,000 dividend. However, the town itself was depleting, and by 1917, the rich vein had “pinched out,” leading to the mine’s permanent closure. The post office shut down the same year, and the mill and pipeline’s iron and steel components were dismantled and sold.

Sporadic mining resumed in the 1920s and 1930s under new ownership, and a tungsten boom in the early 1950s brought renewed activity, though the ore was low-grade. These efforts left behind shafts, cuts, and tailings, but the townsite itself was abandoned, with the last buildings gone by the 1980s. Today, Skidoo is listed on the National Register of Historic Places, with the Skidoo Stamp Mill—stabilized by cables and maintained by the National Park Service—standing as the most prominent remnant.

Legacy and Modern Significance

Skidoo’s brief existence encapsulates the transient nature of mining boomtowns, driven by the allure of gold and undone by the exhaustion of resources. Its innovative water-powered mill and pipeline highlight the ingenuity required to sustain life and industry in the unforgiving Mojave Desert. The ghost town, accessible via an 8-mile unpaved road off Wildrose Road, attracts visitors who explore its mining relics, including the stamp mill, adits, and scattered debris like rusty cans and glass fragments. The surrounding hills, with over 1,000 mine entrances, evoke the frenetic activity of Skidoo’s heyday.

Tripadvisor reviews reflect mixed visitor experiences. Some find the site underwhelming, noting the absence of town structures and the challenge of the rugged road, recommending high-clearance vehicles. Others praise the stamp mill and the sense of history, emphasizing the need to continue past the townsite to reach the mill. The site’s remoteness and stark landscape amplify its haunting appeal, inviting reflection on the ambition and impermanence of Skidoo’s past.

Conclusion

Skidoo, California, rose and fell within a decade, leaving behind a legacy of resilience and adaptation in one of America’s harshest environments. From its accidental discovery in 1906 to its abandonment by 1917, Skidoo embodied the hope and hardship of the gold rush era. Its engineering achievements, preserved ruins, and place on the National Register of Historic Places ensure its story endures, offering a window into the fleeting dreams of a desert boomtown.

Town Summary

NameSkidoo
LocationInyo County, California
Latitude, Longitude36.4355016, -117.1475604
GNIS1656631
Elevation5689 ft / 1734 m
NewspaperSkidoo News
National Register of Places74000349

Skidoo Trail Map

Resouces

Hole in the Rock

Recognized on the National Register of Historic Places, the Hole in the Rock trail is an old Mormon trail in Utah that was used to establish colonies on the east side of the Colorado River in 1879. The Hole in the Rock from which the trail is named, is a narrow canyon from the rim of the canyon down into the Colorado River Valley. This canyon provided access to the Colorado River and the much needed water require to survive in these remote locations. Months were spent widening the narrow canyon to allow “safe” passage of all the wagons and cattle.

Hole in the wall trail in Escalante, Utah
Hole in the wall trail in Escalante, Utah

The original trail was bisected when the Glen Canyon damn bottled the Colorado River and started to fill up Lake Powell in 1966. However, thE road continues to exist and allows access to the Escalante Canyon system, along with access to the Devils Garden, numerous slot canyons and lots of back country hiking and camping opportunities.

Devils Garden off the Hole in the Rock Trail, Lake Powell, Utah
Devils Garden off the Hole in the Rock Trail, Lake Powell, Utah

The road passes between the Kaiparowits Plateau and the Escalante River. This area is a labyrinth of roads and trails.  The trail leaves the small town of Escalante and travels 44 miles south along a sandy road.

Camping at Dance Hall Rock, Hole in the Rock trail
Camping at Dance Hall Rock, Hole in the Rock trail

Do not underestimate how cool this area is to visit. The rock formations, remote locations and sunsets are beyond comprehension. One can get the feeling of isolation on just a short visit.

Escalante Canyon, Utah
Escalante Canyon, Utah

Hole in the Rock Trail Map