Tag: Death Valley National Park

Death Valley National Park, located in eastern California and stretching into Nevada, is a land of extremes. It is the hottest, driest, and lowest national park in the United States, featuring the famously scorching Badwater Basin, which lies 282 feet below sea level. The park’s vast and varied landscape includes towering sand dunes, rugged mountains, and colorful badlands. Despite its harsh conditions, Death Valley is home to a surprising diversity of life, with unique plant and animal species adapted to the extreme environment. The park also boasts stunning geological features such as the salt flats, volcanic craters, and canyons, offering visitors a breathtaking glimpse into the power of nature. Starry night skies and striking sunrises and sunsets add to the park’s otherworldly beauty, making it a unique destination for adventure seekers and nature enthusiasts alike.

McDonald Spring Road

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Death Valley National Park 4x4 and Back Country Roads
Death Valley National Park 4×4 and Back Country Roads

McDonald Spring Road is a roughly 12-mile one-way dirt 4WD route in the Nevada Triangle portion of Death Valley National Park (and adjacent public lands), starting near the Bullfrog turnoff on Rhyolite Road between Nevada Highway 374 and the Rhyolite ghost town. It runs through the western Bullfrog Hills into a large wash, then branches; the north fork leads to McDonald Spring (about 11.9 miles), while a south branch continues toward the Hooligan Mine area and Cave Rock Spring (about 12 miles). Four-wheel-drive is recommended due to sand in the wash.

The road does not connect through to other major routes. Vegetation along the final stretch is relatively sparse and dominated by Great Basin sagebrush and rabbitbrush, with stands of golden cholla. The last ~0.3 mile up a small canyon to the spring itself is closed to vehicles. The spring sits at roughly 5,590 feet elevation (GPS approx. 36°54.272′N 117°01.060′W).

Today the spring is little more than a seep that maintains a couple of shallow pools, often fouled by feral burros. There are no trees. Clear evidence of greater past flow remains in the form of at least three wooden watering troughs and a large metal tank, partially overgrown by dense desert broom.

History of McDonald Spring and Its Connection to Rhyolite

McDonald Spring lies on the east slope of the Grapevine Mountains / Bullfrog Hills area, historically described (early 1900s USGS water-supply data) as having a small supply of water and located roughly 10 miles a little north of west of Bullfrog. Nearby Mexican Camp was a wood-cutting camp serving the mining district.

Rhyolite itself (founded 1904–1905 after Shorty Harris and E.L. Cross’s gold discovery that launched the Bullfrog Mining District) grew explosively into a short-lived boomtown of several thousand people by 1907–1908, complete with banks, a stock exchange, railroads, electricity, and piped water. Water was the critical limiting resource in this arid country. Early on it was hauled by wagon at high cost ($2–5 per barrel); later, multiple competing companies piped water from various local springs (including Indian Springs and others) into town and stored it in tanks.

McDonald Spring was not one of the primary long-distance piped sources that supplied the main Rhyolite townsite, but it formed part of the broader network of small springs and seeps that supported mining, wood camps, travel, and livestock across the Bullfrog Hills and Nevada Triangle during the rush. The surviving troughs and tank show it was developed for watering stock or supporting temporary camps. After the boom collapsed (Montgomery-Shoshone Mine closed 1911; power turned off by 1916; the town essentially abandoned by the early 1920s), such remote springs continued to see intermittent use and later became watering points for wild burros.

The surrounding area contains other minor historic mining sites (Hooligan/Happy Hooligan Mine, Patootse Mine, etc.) and wood-camp remnants tied to the same early-20th-century activity that briefly made Rhyolite one of the largest towns in the region.

Practical notes: This is remote high-desert backcountry. High-clearance 4WD is essential; check current road conditions and any seasonal closures with Death Valley National Park or the BLM. Carry ample water, as the spring itself is not a reliable potable source. Respect historic artifacts and leave them in place. The route offers solitude, views of the Bullfrog Hills and Grapevine Mountains, and a tangible link to the water-scarce realities of the Rhyolite-era mining camps.

Phinney Canyon Road

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Death Valley National Park 4x4 and Back Country Roads
Death Valley National Park 4×4 and Back Country Roads

Phinney Canyon Road is a remote backcountry dirt road in the “Nevada Triangle” portion of Death Valley National Park, in the Grapevine Mountains north of Rhyolite and Beatty, Nevada.

History of Phinney Canyon and Its Connection to Rhyolite

Phinney Canyon lies in the Grapevine Mountains within the broader Bullfrog Mining District, the same district that produced the famous Rhyolite boomtown a few miles to the south.

Rhyolite itself exploded after prospectors Frank “Shorty” Harris and Ernest “Ed” Cross discovered rich gold ore (the “Bullfrog” rock) in August 1904. Within months, competing townsites (Rhyolite, Bullfrog, Beatty, etc.) sprang up, and the district saw thousands of claims, railroads, and a short-lived city of several thousand people before collapsing after the Panic of 1907 and the closure of major mines around 1911.

Phinney Canyon played a much smaller, later role in that mining landscape. The Phinney Mine (also associated with the July 4 and Happy Camp claims) was a modest two-person gold operation active mainly between 1930 and 1938 (well after Rhyolite’s boom-and-bust). The operators drove a tunnel several hundred feet into the mountain, installed track for an ore car, and built a cabin, but total recorded production was only about $850 — a tiny fraction of the district’s earlier output. The mine sits a short hike up a side canyon from the road.

The canyon and road also provided access to scattered prospects, springs, and woodcutting activity in the high country during and after the Rhyolite era. Nearby Strozzi Ranch (reached via the south fork of the same road system) was a small historic ranch with remaining buildings and dugouts. The area saw limited use for timber, water, and minor mining that supported the larger Bullfrog/Rhyolite camps, but it never developed into a significant townsite of its own.

Today the canyon is valued more for its solitude, pinyon woodland, and views than for mining remnants. The road and surrounding lands fall under Death Valley National Park management (with some BLM interface near the highway), and visitors are asked to stay on designated routes, practice Leave No Trace, and check current conditions due to frequent flood damage in the region.

Trail / Road Description

  • Start: Approximately 11.7–11.8 miles north of Beatty on U.S. Highway 95 (look for a gated dirt road on the left/west side; there is often a corresponding road on the opposite side of the highway as a landmark).
  • Length: Roughly 21–23 miles one-way to the high pass / end of vehicle access (sources vary slightly; older descriptions list ~20.8–23 miles).
  • Vehicle requirements (historical/normal conditions): High-clearance recommended for the first ~12–15 miles across Sarcobatus Flat and the lower alluvial fans. Four-wheel-drive (preferably with low-range) is needed beyond that, especially once the road enters the canyon and climbs through pinyon-juniper woodland. The upper section becomes steep, rocky, narrow, and rutted.
  • Route character: The road heads west across open desert flats, then forks after about 12 miles — left/south toward historic Strozzi Ranch, right/north into Phinney Canyon. It climbs into the Grapevine Mountains, transitions from washboard and sandy/rocky sections into denser pinyon pine woodlands, and ends near a high pass (~7,500 ft) with views of the Grapevine high country and distant Sierra Nevada. A short side hike leads to the Phinney Mine. Camping is allowed in designated or dispersed sites along the route (no facilities).
  • Difficulty: Intermediate overall; the upper canyon is more technical.
  • Current status (as of early November 2026): The final ~3 miles are significantly washed out and impassable to all vehicles due to flood damage. Always check the official NPS Death Valley conditions page before attempting the road, as desert conditions change rapidly with storms.

This is one of the least-visited corners of the park — quiet, scenic high-desert country with minimal traffic compared to more popular routes like Titus Canyon.

Tucki Mine

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The hottest place on earth, Death Valley National Park is on the order with California and Nevada
The hottest place on earth, Death Valley National Park is on the order with California and Nevada

The Tucki Mine (also known as the Tucki claim, Tucki No. 1 Mine, and Tucki Nos. 2, 3, and 4 claims) is an abandoned underground gold mine on the southeast slope of Tucki Mountain in the Panamint Range, Inyo County, California. It lies within Death Valley National Park (and the Death Valley Wilderness), approximately 4 miles north-northeast of the ghost town of Skidoo and about 10–10.5 miles by rough 4×4 road from Emigrant Canyon Road via Telephone Canyon. The site occupies roughly three acres along a steep-sided wash that drains eastward toward Death Valley.

Geologically, the deposit consists of thin quartz veins carrying free gold (with minor silver) that occupy fractures in Precambrian metasedimentary rocks, primarily metaquartzite. The host rock strikes roughly northwest and dips southwest. The mine was a small-scale operation that produced ore from shallow stopes and limited underground development.

Early Claims (1909–1920s)

The first formal record appears in the Wild Rose Mining District books: a Notice of Location for the “Tucki No. 1 Mine,” described as “located about 3 miles NE of Skidoo,” dated 12 April 1909 and filed by Henry W. Britt (or Birtt; handwriting is ambiguous). No significant production or development is documented from this period.

The property was relocated in September 1927 by John Millett, Samuel E. Ball, and Charles G. Walker as a group of claims lying about 2½ miles southwest of Tucki Wash and roughly 4 airline miles north-northeast of Skidoo. By October 1927, Edward R. (Ed) Attaway had acquired a one-fourth interest in the Tucki and Tucki Nos. 2, 3, and 4 claims. Activity remained sporadic and inconsequential through the 1920s; no detailed production records survive from this era.

Development and Peak Activity (1930s–1940s)

Serious work began in the mid-to-late 1930s. By 1937 Ed Attaway and Sam Ball were actively mining and trucking ore first to Death Valley Junction for shipment to a smelter and later to the fifty-ton cyanide plant of Keeler Gold Mines, Inc., operated by Roy Troeger in the Owens Valley. Contemporary accounts described ore values ranging from $12 to $60 per ton (with some promotional claims of higher grades).

In August 1938 Attaway and Ball executed a lease/bond agreement on the “Tuck-I Mine” with the Lane Development Company of Hollywood for a total consideration of $25,000. Newspaper reports at the time stated that the lessees had been working the property for about fourteen years and shipping high-grade ore. Roy I. Journigan (operator of Journigan’s Mill, a custom amalgamation-and-cyanide plant in Emigrant Canyon) became a part owner by April 1939 alongside Attaway and Ball. The partners then leased the mine to Felix Castro, Fred Bunting, and Fred Mastagan. A subsequent lease/bond agreement transferred operations to Warnken, Potter, and associates.

Until about 1940, ore was processed at Journigan’s Mill roughly 20 miles away in Emigrant Canyon. In 1940 a small, crude cyanide leaching plant was constructed on-site. Production figures from this period include:

  • Approximately $846 in gold every two weeks in 1940.
  • From August 1940 to April 1941, lessees sold $5,200 worth of ore averaging about $20 per ton (assays $12–$60 per ton).
  • Mine receipts for gold bullion delivered in 1941 totaled nearly $18,000.

Underground development consisted of an inclined shaft (or incline) to the 200-foot level that continued as a winze to about 330 feet, with short drifts on intermediate levels (including 15 feet of drifts at the 50- and 100-foot levels and additional drifts at 130, 170, and 200 feet). Two earlier adits, located 60 and 200 feet northwest of the shaft, represented the initial prospecting work. The operation was essentially underground, producing ore from shallow stopes.

By 1951 the property consisted of four unpatented lode claims owned by Roy I. Journigan and Ed Attaway. Workings remained modest.

Dormancy and Brief Revival (1950s–1970s)

The mine was largely idle through the 1950s and 1960s. In the mid-1970s activity resumed. Early in 1974 Russ Journigan (son or relative of Roy) and his wife held title to the core claims (Tucki, Tucki No. 2, and Tucki No. 3); adjacent claims were allowed to expire. In 1974–1975 Russ Journigan and Paul Barnett reopened the mine. They installed gold-leaching apparatus, including four steel-lined cyanidization tanks, and processed old tailings using the carbon-filtration method (later involving sodium hydroxide and zinc). A more efficient jaw crusher and advanced leaching facility were planned, with a projected capacity of 25 tons of ore per day.

The revival produced only a few dozen additional ounces of gold. The last recorded production occurred in December 1971 (or shortly thereafter in the mid-1970s accounts). Operations ceased by the late 1970s, coinciding with the 1978 Death Valley mining claims moratorium and the site’s incorporation into the national park system. Total documented gold production for the entire life of the mine was modest—little more than $18,000 (period values)—and profits were limited.

Site Description and Later Management

At its peak the cyanide plant included four steel-lined concrete-block tanks, two water reservoirs, crushing equipment, and a pump. Today only the concrete tanks remain; most other processing equipment was removed after shutdown in the early 1980s. The site also includes cabin remains, foundations, an ore chute, waste-rock piles, and residual mine openings (many later sealed by the National Park Service for safety).

The National Park Service has investigated the site under the Comprehensive Environmental Response, Compensation, and Liability Act (CERCLA) because of residual metals (including antimony, arsenic, cadmium, copper, lead, mercury, selenium, silver, and zinc) and potential cyanide-related contamination in soils and tailings. A Preliminary Assessment was completed in 2014, followed by a Site Inspection in 2016 and preparation of an Engineering Evaluation/Cost Analysis to evaluate cleanup alternatives. Visitation is low (NPS estimates fewer than 500 people per year).

Historical Context and Significance

Tucki Mine is a characteristic small-scale, intermittent gold operation of the Death Valley region during the mid-20th century. It never approached the output of major producers such as the nearby Skidoo Mine. Its history is closely tied to the Journigan family and their custom mill in Emigrant Canyon, which supported several local properties during the 1930s–1940s revival of gold mining in the Skidoo–Wildrose district. The mine illustrates the challenges of extracting low-grade, narrow-vein gold deposits in a remote desert environment and the eventual transition of such sites from active claims to protected cultural and environmental resources within Death Valley National Park.

Primary sources for this history include the National Park Service’s Historic Resource Study: A History of Mining in Death Valley National Monument (Linda W. Greene and John A. Latschar, 1981), contemporary mining district records, California Journal of Mines and Geology reports, Mindat locality data, and NPS CERCLA documentation for the Tucki Mine and Mill Site.

Owl Hole Spring Road

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Death Valley National Park 4x4 and Back Country Roads
Death Valley National Park 4×4 and Back Country Roads

Owl Hole Spring Road (also called Owl Springs Road or Owls Hole Springs Road) is one of the most remote backcountry routes in Death Valley National Park. It provides the primary (and essentially only practical) vehicle access into the Owlshead Mountains, a rugged and little-visited range in the extreme southern/southwestern part of the park. The road begins as a junction off Harry Wade Road and climbs westward into increasingly isolated terrain, offering solitude, unusual geology, and historic mining remnants.

Route Overview and Access

The road leaves Harry Wade Road (the main southern through-route across the valley floor) and heads southwest/west toward the Owlshead Mountains. From the junction it runs roughly 10 miles to Owl Hole Spring itself, then continues farther toward abandoned mining areas, a microwave tower/repeater site, and the boundary with military lands (Fort Irwin / Camp Irwin area). Total length is commonly listed around 22–30 miles depending on how far one continues, with a substantial elevation gain of nearly 4,000 feet to the higher ends of the route (reaching approximately 3,996–4,000 feet at the abandoned radio tower).

Access is typically via Harry Wade Road, which itself connects Badwater Road (near Ashford Mill) on the north with California Highway 127 / Saratoga Spring Road on the southeast. The Owl Hole Spring junction lies partway along Harry Wade Road. Because the area is so remote, travelers should be fully self-sufficient—there are no services, no reliable cell coverage, and help can be many hours away.

Road Conditions and Vehicle Requirements

The road is completely unpaved and consists of dirt, gravel, washboard (corrugation), and sandy sections. It is generally passable for high-clearance stock SUVs and trucks in dry conditions, but 4WD is recommended, especially in soft sand stretches, after rain, or beyond the spring. Conditions can change rapidly due to flash flooding. One long sandy wash section and occasional steeper or eroded pitches may require 4WD and careful driving. The road is sometimes used by military convoys and has historically been kept in relatively good shape in places because of access to a former microwave relay tower.

Important safety notes:

  • Avoid entering adjacent military lands (Fort Irwin area). Active bombing ranges and unexploded ordnance make these areas extremely dangerous.
  • Stay on the designated road; off-road travel is prohibited in the park.
  • Carry recovery gear, extra water, a full-size spare (or two), and offline navigation. Summer heat is extreme and potentially life-threatening.

Best seasons are late fall through early spring (November–April). Always check the official NPS Death Valley road conditions page before travel.

Points of Interest

Owl Hole Spring
Located about 10 miles from the Harry Wade Road junction (approximate coordinates 35.638° N, 116.649° W or nearby). This intermittent desert spring historically served as a water stop for 20-mule team borax wagons in the 1880s and later supported mining operations. It is a stagnant pool surrounded by tamarisk, a single fan palm, and reeds, situated along a scarp related to the Garlock Fault. The spring provides water for desert wildlife, including desert tortoise and desert bighorn sheep, though it is not a reliable or safe drinking source for humans. In 2024, a harmful algae bloom at the spring was linked to the deaths of multiple wild burros; the water should be considered unsafe to touch or drink, and carcasses should not be handled.

Historic Mining Area
Near and beyond the spring lie remnants of early- to mid-20th-century manganese mining (New Deal and Black Magic mines). The area produced manganese ore (including ramsdellite, used in lithium batteries) and shows old equipment, stockpiles, structures, and a messy former camp site (occupied as recently as the early 1990s in some accounts). Side roads branch toward these workings. Iron mining evidence (hematite) is also noted in the vicinity. Artifacts should be left in place.

Owlshead Mountains
The road is the main gateway into this remote range, which from the air resembles a giant owl’s head (rounded forms, a central “beak,” and playas as “eyes”). The mountains offer open vistas, unusual geologic formations, dry canyons (including some short slot sections), and opportunities to see wild burros or desert bighorn. Hiking into side canyons requires careful navigation, as routes are unmarked, dry, and extremely remote. Flash-flood risk is real in the canyons.

Higher Elevations and Microwave Tower
Continuing past the spring, the road climbs toward an abandoned military radio tower/repeater at nearly 4,000 feet. Views expand across the southern park and surrounding ranges. The route eventually approaches the military boundary.

Practical Tips and Safety

  • High-clearance vehicle minimum; 4WD strongly preferred for the full route.
  • Travel prepared for self-rescue. Tell someone your plans.
  • Respect wilderness boundaries and sensitive habitats. Do not enter military lands.
  • The spring water is not potable and has had documented toxic algae issues—do not drink or contact it.
  • Dispersed camping is allowed under standard backcountry rules (well away from water sources and developed areas), but the extreme remoteness demands extra caution.
  • Combine with Harry Wade Road or Saratoga Spring for a longer southern Death Valley exploration if conditions allow.

Owl Hole Spring Road delivers true isolation and access to one of Death Valley’s least-visited corners. It rewards prepared, self-reliant travelers interested in remote desert driving, mining history, geology, and wildlife, but it is not a casual side trip. Verify current conditions with the National Park Service and plan thoroughly before setting out.

Badwater Road

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Death Valley National Park 4x4 and Back Country Roads
Death Valley National Park 4×4 and Back Country Roads

Badwater Road is the primary paved route running south through the heart of Death Valley National Park. It begins near Furnace Creek at its junction with California Highway 190 and continues south past many of the park’s most famous valley-floor attractions before reaching its southern terminus near the Ashford Mill ruins. At that point the road meets Harry Wade Road and transitions eastward into Jubilee Pass Road (California Highway 178), which climbs out of the valley over Jubilee and Salsberry Passes to reach California Highway 127 near Shoshone.

The segment most relevant to the user’s request—the southern end of Badwater Road at the Harry Wade Road junction and the continuing paved link toward Highway 127—forms the southern gateway into and out of the main valley floor.

Road Overview and Length

  • From the CA-190 / Badwater Road junction near Furnace Creek to the Harry Wade Road / Jubilee Pass Road junction is approximately 45.6 miles.
  • At the junction (near elevation 22–25 feet), Harry Wade Road continues straight southeast as a dirt road, while the main paved route turns left (east) and becomes Jubilee Pass Road.
  • Jubilee Pass Road then covers roughly 25 miles east over the passes to its junction with CA-127 (about 1.7 miles north of Shoshone).

The entire paved corridor from Furnace Creek south and then east to CA-127 is often referred to collectively in park contexts as the southern Badwater / Jubilee Pass system. South Badwater Road (the portion south of Badwater Basin) has experienced repeated flood damage and closures; it was reopened in late January 2026 after months of debris removal and repairs, though visitors may still encounter missing pavement, loose gravel, soft or eroded shoulders, and short drop-offs.

Road Conditions

Badwater Road is fully paved and suitable for all standard passenger vehicles under normal conditions. It is one of the lowest roads in the park, remaining near or below sea level for long stretches. The southern section can be affected by flash flooding from the Black Mountains, leading to temporary closures or rough patches after storms. High temperatures in summer make travel potentially dangerous; the best seasons are October through May. No services exist along the southern stretch—fuel, water, and supplies must be obtained at Furnace Creek, Shoshone, or Baker.

Key Points of Interest Along the Southern Approach and Junction Area

Ashford Mill Ruins
Located a short distance north of the Harry Wade Road junction (access via a short gravel spur off Badwater Road). These are the remains of a historic borax mill. A small parking area and vault toilet are available. The site offers a quiet stop with views of the southern valley and is a common landmark for those turning onto Harry Wade Road.

Harry Wade Road Junction
Approximately 2 miles south of the Ashford Mill ruins, where Badwater Road bends east toward the passes. Harry Wade Road (dirt, high-clearance recommended) continues southeast across the valley floor toward Saratoga Spring Road and ultimately CA-127. This junction marks the practical southern end of the main Badwater Road alignment and the starting point for the historic Harry Wade Exit Route.

Jubilee Pass Road (Continuation to Highway 127)
From the junction the paved road climbs eastward, crossing Jubilee Pass and Salsberry Pass before descending to CA-127. The drive offers expansive views of the southern Black Mountains, Greenwater Valley, and surrounding desert ranges. It is the main paved connection between the southern valley floor and the communities of Shoshone and Tecopa.

Other Nearby Features on the Broader Badwater Road Corridor
While farther north, the full Badwater Road provides access to:

These northern attractions are the primary reasons most visitors drive Badwater Road; the southern section is quieter and primarily used for through travel or access to Harry Wade Road and the remote southern park.

Practical Information

  • The southern section is remote. Carry ample water, check fuel levels, and verify current road conditions via the official NPS Death Valley alerts page, as flood damage and repairs can change access with little notice.
  • No cell service is reliable in much of this area.
  • Dispersed camping is restricted on the valley floor; follow park backcountry rules.
  • Harry Wade Road itself requires high-clearance (and often 4WD in sandy sections) and is subject to deep sand and possible Amargosa River flooding.

In summary, the southern end of Badwater Road at the Harry Wade Road junction serves as the transition point between the classic paved valley-floor drive and the remote dirt backcountry of the historic Harry Wade Exit Route, while the continuing Jubilee Pass Road provides the paved link eastward to Highway 127. Together they form an important southern access corridor into Death Valley National Park. Always confirm current conditions before travel, especially after storms.