Tag: Trails

4×4 trails offer enthusiasts an exhilarating blend of rugged adventure and natural beauty. These trails wind through diverse terrain, from dense forests and rocky mountainsides to muddy river crossings and sandy dunes, presenting a challenging playground for off-road vehicles. Each trail brings its own unique obstacles and breathtaking vistas, inviting drivers to test their skill and their vehicle’s capabilities. Whether navigating steep inclines, conquering deep mud pits, or maneuvering around fallen logs, 4×4 trails provide an immersive experience in the heart of untamed landscapes, where every turn promises both adrenaline-pumping excitement and moments of serene wilderness immersion.

Carrara Nevada – Nye County Ghost Town

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Carrara in Nye County Nevada

Carrara Ghost town is a small ghost town and marble mine located about ten miles south of Beatty in Nye County, Nevada on the east side of US 95.

In 1904 first attempts to quarry the high quality marble at the Carrara site. These initial efforts failed with the inability to produce larger slabs from the highly fractured and unstable marble.  More suitable deposits of marble are found in 1911. The American Carrara Marble Company laid out the Carrara town. The town was named for Carrara, Italy, which produced world class marble. 

A Metropolis in waiting

The marble is hauled by a standard cable railway down three miles from the quarry to town. This designed utilized town cars on a single track. At the midway point, siding in the tracked allowed the two trains to pass each other in opposing directions. The car at the top of the track loaded with marble would supply all the pull the empty car at the bottom of the track up the mountain on a free return.

Rail lines were already available in the Vegas and Tonopah Railroad. Water is pumped from Gold Center, NV using a nine mile long pipe line. The supply was generous enough to allow the town to boast a town fountain, which would shoot water six feet into the air. The fountain was built by the Marble Company to promote the appearance of longevity for the fledgling town.

The rail road line to town is completed in 1914. Soon thereafter, large marble blocks, which could weight up to 15 tons, are shipped to Los Angeles. In Los Angeles, the large marble blocks are cut to size, finished and polished.

Eventually, the company with founded the town lost profits. The towns people saw hardship and soon moved away. With the exception of a few hangers on, the town is gone in 1924.

The town boasted a newspaper appropriately named the Carrara Obelisk ( 5/8/1913 – 09/1916 ), a post office, hotel, store, saloon and restaurant to serve the 150 people who called the place home. The site contained  about 40 buildings. The post office was open from May 5, 1913 to September 15, 2914.

Carrara Town Summary

NameCarrara Nevada
LocationNye County, Nevada
Population 150
Post OfficeMay 5, 1913 – September 15, 2914
NewspapersCarrara Obelisk Feb 7, 1914 – Sept 9, 1916
Carrara Miner July 21, 1929

Carrara Trail Map

Resources

Skidoo California – Inyo County Ghost Town

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Skidoo California was famous in the first decade of the 20th century when gold had been found in Inyo County and the town established in 1905. The towns existence was support by the output and economy driven by the gold mines. Within a decade the town was left deserted abandoned. At this time few structures remain and access to the mines are closed to prevent accidents.

Skidoo, CA 1907
Skidoo California, 1907

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

Skidoo, originally known as Hoveck, is typical of mining towns, which flourished so long as the mines continued to produce. The small town of Hoveck was named for Matt Hoveck, who managed the Skidoo mine. The town was named Skidoo in 1907. The name Skidoo was derived from the slang phrase “23 Skidoo” which was quite popular at this time.

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.

The Skidoo Mine operated from 1906 and 1917. During operation the mine produced about 75,000 ounces of gold, which would have been worth about 1.6 million dollars. The mill in Skidoo was the only desert mill which operated complete using water. The water to power the mill was piped in from Telescope Peak was a feat of engineering and work of this still scars the landscape.

The Skidoo News is founded by James G. Sterrett and Edwin S. Drury when they arrive from Encapement, Wyoming with a four horse load and printing material.

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

The remains of the town of Skidoo are located within Death Valley National Monument and Inyo County.

The fifteen-stamp mill built by the Skidoo Mines Company is a rare surviving example of an early 20th-century gravity-feed system for separating gold from its ore.

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

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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

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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

Cathedral Valley

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Located in Capital Reef National Park, the Cathedral Valley District of Capitol Reef National Park is open all year and the perfect spot for the back county explorer seeking to get away from it all.

Temple of the Sun, located on Cathedral Valley Trail in Capital Reef National Park, Utah - Photo by James L Rathbun
Temple of the Sun, located on Cathedral Valley Trail in Capital Reef National Park, Utah – Photo by James L Rathbun

Vehicles with high ground clearance are recommended and should have no issues navigating the sandy roads. Road conditions can vary greatly depending on recent weather conditions with spring and summer rains leaving the route muddy and impassable.  The advantage of this location is the back country travel is light, so for the person seeking seclusion, this is the secluded area in a remote location.

The 60 miles loop trail leaves highway 24 at the River Ford which is about 12 miles easy of the visitor center.  The route follows Hartnet Road to the Cathedral Road ( Caineville Wash Road) and returns to Highway 24 near Caineville.  The river crossing is passable most of the time, however care should be taken during the rainy months.

During my visit in 2004, we just finished Hole in the Rock Road, and headed east out of Escalante, Utah.  We then took the Burr Trail to Notom Road which delivered us to Capital Reef.  That afternoon we chased the light up Cathedral Valley Road and stopped at Temple of the Sun for some photographic opportunities.  We stayed beyond sun down hoping for some amazing light which did not come that evening and drove trail out in the dark.  I was disappointed for the lack of light during the golden hour, but the location is yet another place that I must return just due to the amazing Utah landscapes.

Cathedral Valley Trail Map