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

Lost Burro Mine

Founded in 1907 when Bert Shively picked up a rock to throw at some stray burros and discovered gold, the Lost burro Mine is a great destination in Death Valley. The mine was operated from 1907 to the 1970s, with its greatest production of gold being from 1912 – 1917. The road into the mine is just 1.1 mile from Hunter Mountain road located in Death Valley National Park.  The trail is very easy to pass and suitable for most stock SUVs, although it does get narrow in two places.

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

As you approach the site, there is evidence of human occupation and the large amount of tin cans and artifacts gradually increase the closer you get to the mine site.  There is a long history of haunting and curses place upon people who remove artifacts from the location.  There are at least four structures still standing at the site.  The main cabin, a storage cabin, outhouse and the mine located high above on a cliff.  You can enter the cabin and storage cabin but posted warnings of Hantavirus warn of the potential danger.

The Lost Burrow Mine
The Lost Burrow Mine

The Upper Mill

The upper mill site is accessible using a steep short trail and well worth the effort.  The structure appears to be reinforced with guy wires to help maintain its state.  Much of the pulley system remains intact and the terrain and remote location reminds us of what these men endured to survive in this location.

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

There is evidence of many people returning removed items in the hopes of removing the curse. There are two buildings at the site with the Mill located just to the North.  Two short hikes to the hills above offer amazing views of the Racetrack Valley and Hunter Mountain.

The Lost Burrow Mine cabin interior
The Lost Burrow Mine cabin interior

Lost Burro Mine Video

Lost Burro Mine 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

Chloride City California – Inyo County Ghost Town

Chloride City California is located within Death Valley National Park and Inyo County, California. The town arose out of silver discoveries in nearby Chloride Cliff in 1873 and is one of the earliest of the Death Valley mines.

The first road through Death Valley was constructed from Chloride City, California to San Bernardino, California which was the nearest town 180 miles away. In the 1870’s ore was shipped out using trains of pack mules which would return carrying food and supplies to the camp. The mines of this small community struggled on for a few years, but by 1880 no mines were producing and everybody had moved on.

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

The nearby Bullfrog, Nevada, gold discovery excitement of 1904 brought in new capital. The Chloride Cliff Mine was bought by investors in nearby Rhyolite and re-opened in 1908. Sufficient ore was produced in subsequent years to warrant the construction of a cyanide mill in 1916. By 1918 the camp was deserted again.

The ghost town contains numerous adits, dumps and the grave of James McKay, of whom nothing is known. The town also holds the remains of three stamp mills.

Chloride City Trail Map

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