Tucki Mine Road is a roughly 10-mile (one-way) unmaintained 4×4 backcountry road in Death Valley National Park. It leads from Emigrant Canyon/Wildrose Road into Telephone Canyon and ends at the historic Tucki Mine ruins on the southeast slope of Tucki Mountain in the Panamint Range.
Access & Route
- Start: About 1.5–1.7 miles up Emigrant Canyon Road (Wildrose Road) from Emigrant Junction (near the junction with Highway 190). The road is visible climbing the bank across from the canyon mouth.
- The route follows the base of the mountains, then enters Telephone Canyon. At about 2.5 miles from the canyon mouth the canyon forks: the right (closed to vehicles) leads a short walk to a natural arch and an old mill site; the left fork continues to the mine.
- Total distance to the mine: approximately 10 miles. Elevation gain is significant as the road climbs into the higher elevations of Tucki Mountain (mine area roughly 5,000–6,000+ ft).
Vehicle Requirements & Difficulty
- High-clearance 4WD is required. Obstacles commonly include large rocks, deep gravel, washouts, and several dry falls (drops of 3–4 feet).
- Rated roughly “2” (moderate) on some local 4×4 scales, but conditions vary greatly with weather. High-clearance 2WD vehicles have occasionally reached intermediate points (e.g., Martin’s Crossing) in good conditions, but full access to the mine typically needs 4WD and careful driving.
- Not recommended for low-clearance vehicles, street tires, or long vehicles.
Camping & Regulations
- No camping in the first 2 miles.
- Dispersed camping is allowed farther along after the restricted zone (standard Death Valley backcountry rules apply: pack out all waste, no open fires in many areas, etc.).
- Stay on designated roads; off-road driving is prohibited.
What You’ll See
- Scenic Telephone Canyon with rocky walls and desert vegetation.
- Optional short hike up the right fork to a natural arch and old mill remains.
- At the end: ruins of Tucki Mine (cabins, concrete cyanide tanks, ore chutes, waste rock, sealed or open workings depending on NPS management), plus views toward Death Valley and surrounding peaks. Martin’s Crossing cabin (farther along related routes) is sometimes visited by hikers continuing toward Tucki Mountain summit.
- Wildlife possible (bighorn sheep reported by some visitors).
Current Conditions Note (as of early November 2026)
Death Valley experiences frequent flash flooding that damages dirt roads. Recent storms (including October 2026) closed or heavily damaged several major and backcountry routes (e.g., Titus Canyon, Cottonwood, Darwin Falls, Lower Wildrose caution). Tucki Mine Road itself is not specifically listed as closed in the latest NPS alerts, but conditions change rapidly. Always check the official NPS Alerts & Conditions page (nps.gov/deva/planyourvisit/conditions.htm) and the Backcountry Roads map immediately before travel. Carry extra water, tools, recovery gear, and be prepared to self-rescue.
Best Time
Fall through spring (cooler temperatures). Summer is extremely hot and not advised.
Trail Report Summary
This is a classic moderate Death Valley 4×4 route that rewards careful drivers with solitude, mining history, and canyon scenery. Expect a rough, rocky drive rather than a smooth dual-track. Plan for 1–2+ hours each way depending on vehicle and conditions.
History Report: Tucki Mine, Death Valley National Park
Location & Geology
Tucki Mine (also associated with the Tucki claims / Tucki Nos. 1–4) sits on the southeast slope of Tucki Mountain in the Panamint Range, roughly 4 miles north-northeast of the ghost town of Skidoo and about 10–10.5 miles by rough road from Emigrant Canyon via Telephone Canyon. It is an underground gold mine that worked thin quartz veins containing minor gold in fractures within Precambrian metasedimentary rocks (primarily metaquartzite).
Early Claims (1909–1920s)
The first recorded claim (Tucki No. 1) was located in April 1909 by Henry W. Britt (or Birtt), described as about 3 miles northeast of Skidoo. The property was relocated several times in the late 1920s (including by John Millett, Samuel E. Ball, and Charles G. Walker in 1927). There is little evidence of significant production in these early decades.
Active Period (1930s–1940s)
Serious work began in the late 1930s. By 1937 Ed Attaway and Sam Ball were trucking ore to Death Valley Junction and later to a cyanide mill in Keeler (Owens Valley). Ore values were reported in the $12–$60 per ton range (some higher claims of $100–$700/ton appear in contemporary accounts). Roy Journigan (associated with Journigan’s Mill in Emigrant Canyon) became involved.
In 1938 the property was leased/bonded. A crude cyanide leaching mill was built on-site around 1940. Production that year was reported at about $846 in gold every two weeks. Ore mined before 1940 was largely treated at Journigan’s custom mill; after that, on-site cyanide processing was used. Recorded bullion receipts in 1941 totaled nearly $18,000. Workings included an incline to the 200-foot level continuing as a winze to about 330 feet, with short drifts on several levels and two adits.
Later Activity & Closure
The mine was largely dormant through the 1950s and 1960s. In the mid-1970s operators (including Russ Journigan and Paul Barnett) reopened remaining claims, constructed improved crushing and carbon-filtration/leaching facilities, and processed old tailings. Only a few dozen additional ounces of gold were recovered. Final recorded production was in December 1971. Operations ceased around the late 1970s/early 1980s, coinciding with the Death Valley mining claims moratorium and the site’s incorporation into the national park (and later wilderness). Total known production was modest—little more than $18,000 in gold overall—and profits were limited.
Site Today
The nearly 3-acre site contains cabin remains, concrete cyanide tanks (steel-lined rectangular tanks that still hold some crushed rock), foundations, an ore chute, waste rock, and sealed or residual mine openings. The NPS has investigated the site under CERCLA for residual metals (antimony, arsenic, cadmium, copper, lead, mercury, selenium, silver, zinc) and cyanide-related contamination. An Engineering Evaluation/Cost Analysis has been prepared to evaluate cleanup options. Visitation is low (NPS estimates fewer than 500 people per year).
Significance
Tucki Mine is a typical small-scale Death Valley gold operation of the early-to-mid 20th century—intermittent, low-profit, and dependent on cyanide milling. It forms part of the broader Skidoo–Wildrose mining district history and is now preserved as an abandoned mineral lands (AML) site within the national park.
Sources primarily draw from NPS documents, historic mining records summarized by the National Park Service, Mindat, and contemporary backcountry guides. Always verify current access and safety conditions with the National Park Service before visiting.