Lippincott Mine Road

The Lippincott Mine Road is a one way trail from Death Valley’s Racetrack Playa to Saline Valley. It is a steep trail which is not for the novice or the feint of heart. Greeting you at the trail head is a sign which reads:

“Lippincott Pass, 4×4 High Clearance, No Tow Service, Caution”

Experienced drivers using 4×4 high clearance vehicles only.  What traveler in their right mind could resist a challenge like this? Provided you are equipped to do so.

Lippincott Mine Road from Racetrack Valley, Death Valley National Park, CA
Lippincott Mine Road from Racetrack Valley, Death Valley National Park, CA
Looking back at some amazing landscapes near the top of the Lippincott Mine.
Looking back at some amazing landscapes near the top of the Lippincott Mine.

The top of Lippincott Mine road starts at the end of the Racetrack Valley road and descends into the west towards Saline Valley.  The road is steep and narrow but is not too technical.  At the top of the route is the Lippencott Mine site which gives the trail it’s name.  The Lippincott Mine offers great views of both Saline and RaceTrack Valley.  

Looking down at Saline Valley in the distance.
Looking down at the road from the mine, with Saline Valley in the distance.

There are several structures, and mines to explore and a lot of time could be spent exploring the site on foot.  The Homestake dry camp offers a great spot of overnight in the area for those of us who are so inclined and look forward to being really away from it all. The best night sky I have seen in the last 35 year was at the Homestake Dry Camp.

The remains of the Lippincott Mine at the southern end of Race Track Valley.
The remains of the Lippincott Mine at the southern end of Race Track Valley.

Lippincott Mine Road Trail Map

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

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 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 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

Silver Cholla (Cylindropuntia echinocarpa)

Silver Cholla (Cylindropuntia echinocarpa) is a common species of cactus which is native to the southwestern United States including Nevada, Arizona and California. The Silver cholla is a larger cactus which is known to grow in excess of 6 feet tall.

Silver Cholla waiting for an incoming storm.
Silver Cholla waiting for an incoming storm.

This species can be found rather easily and quite common in the Mojave Desert, Sonoran Desert and the the Colorado Desert. It is typically found in dry desert washes, Joshua Tree wood lands (as photographed above ) or pinyon-juniper woodland environments.

The body of the cactus is segmented by joints which are typically four to eight inches in length. The joints and body of the cactus are densely covered with spines about 1 inch long with are covered in a papery sheath. The spines are typically yellow in color, which contrast nicely against the green skin of the cactus body. This spiny armor not only protects the cactus, but is also forties the nests of the Cactus Wren and other animals who may seek shelter within this plant.

This cholla typically blooms in spring depending upon conditions. The flowers are green in color however some variants may contain yellow, pink or brown. The lumpy, tan-colored fruit hosts the seeds for germination and is known to have a foul scent.