Big Bear, CA
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Skidoo Pipeline
The Skidoo Pipeline was a roughly 21- to 23-mile gravity-fed water line completed in November 1907 that supplied the Skidoo gold mining camp and its mill in the Panamint Mountains of what is now Death Valley National Park, California. It remains one of the notable engineering feats of early 20th-century desert mining.
Discovery and Establishment of Skidoo
In January 1906, prospectors John (or Harry) Ramsey and John “One-Eye” Thompson, traveling toward the gold strike at Harrisburg, were delayed by dense fog near Emigrant Spring. When the fog lifted, they discovered promising gold-bearing ledges and staked claims (part of what became known as the Gold Eagle group). Bob Montgomery soon acquired the claims and organized development, including plans for a quartz mill.
A townsite was laid out by late summer 1906. It was initially called Hoveck (after mine manager Matt Hoveck); the post office opened under that name in 1906, was renamed Skidoo in 1907, and closed in 1917. The name derived from the popular slang phrase “23 skidoo” (meaning to leave or scram). Local explanations often tied the “23” to the approximate length of the planned pipeline, the number of initial claims, the date of discovery, or the number of founders, though the postal service rejected including “23” in the official name.
By March–April 1907 the camp had grown rapidly to an estimated 400–700 residents, with roughly 130 buildings (frame, wood, and iron), stores, saloons, restaurants, a newspaper (Skidoo News), school, bank, doctor, lawyers, telephone/telegraph connection across Death Valley to Rhyolite (Nevada), and stage/auto connections planned or operating toward Beatty, Randsburg, and Keeler. Its elevation of about 5,600–5,700 feet made summer work more practical than in the lower valley.
The Pipeline: Construction, Design, and Operation
Water was the critical limiting factor. Local sources such as Emigrant Spring (hauled by wagon at high cost) were insufficient for a mill and growing town. Montgomery acquired rights to springs near Telescope Peak (notably Birch Spring in Jail Canyon, at roughly 7,200–7,400 feet elevation). Construction of a gravity pipeline began in 1906–1907. About 75 men worked on the line; pipe (primarily spirally riveted steel, with sections of cast iron later, in diameters commonly cited as 6–10 inches or specifically 8 inches) arrived in sections convenient for transport by man and animal.
The line ran approximately 21–23 miles (historical accounts and markers commonly use 23 miles; some contemporary descriptions say 18–22) from Birch Spring/Jail Canyon to the millsite, dropping about 1,800 feet. This provided sufficient head/pressure to power the mill without pumps—a rare achievement in the desert. Estimated early costs were around $150,000; the final cost reached about $250,000. Water first flowed into Skidoo in November 1907. Watering stations along the route also aided prospectors exploring the surrounding country.
The pipeline enabled the only milling plant in the Death Valley region operated almost entirely by water power. The Skidoo Mines Company built a 15-stamp amalgamation and cyanide mill (with later modifications, including rebuilds after damage) using a gravity-feed system for ore processing. This supported large-scale work on relatively narrow high-grade veins.
Years of primary operation: Construction 1906–1907; full service from late 1907. The main mining and milling period ran from 1906/1907 through 1917. The pipeline suffered major damage in January 1913 when it froze and burst in places, forcing a temporary mill shutdown and layoffs. A fire later that year damaged the original mill; a replacement (initially 10-stamp, later expanded) was built. By September 1917 the rich vein had pinched out, the main mine closed, the post office shut down, and much of the pipeline’s iron and steel was dismantled and sold for scrap (some sections remained or proved hard to salvage). Sporadic milling and activity continued intermittently into the 1930s and until about 1942, after which the site was fully abandoned.
Role in Mining and Regional Economy
The Skidoo Mine and district were among the most productive gold operations in the Death Valley region during their peak. Output is commonly estimated at about 75,000 ounces of gold, valued at roughly $1.5–1.6 million at the contemporary price of about $20 per ounce (some accounts place district totals higher). It was the largest mining operation in the area from roughly 1907–1917 and stood out for sustained production compared with many short-lived boom camps. Mining focused on free-gold quartz veins in granitic rocks, with some copper noted later.
The pipeline was essential: without reliable, pressurized water, the water-powered mill and a viable town could not have existed at that remote high-elevation site. It also supported broader prospecting by providing water stations in arid terrain. Development spending exceeded $300,000 in the early years. The Panic of 1907 slowed expansion but did not immediately end the camp; ore depletion and infrastructure failures (especially the 1913 pipeline break) were more decisive in the decline.
Connections to Local Towns and the Broader Area
Skidoo formed part of a network of early-1900s Death Valley and Panamint Range camps:
- Harrisburg: The nearby gold strike that drew the original prospectors; it largely emptied as people shifted to Skidoo.
- Rhyolite (Nevada): Linked by telephone/telegraph; a major supply and communication hub across Death Valley. Freight and stage lines connected the camps.
- Emigrant Spring / Ballarat / Keeler: Water hauling, road proposals, and supply routes. Water rights originated in part from interests near Ballarat.
- Greenwater and other contemporaneous camps: Shared the regional boom-and-bust cycle; Skidoo outlasted many.
The site later served as a filming location for the 1923 motion picture Greed (one of the early major films shot in Death Valley). Today the Skidoo Historic District (including mill remnants) is listed on the National Register of Historic Places within Death Valley National Park. Visible traces of the pipeline scar remain in places between Telescope Peak/Jail Canyon and the millsite, though much of the pipe was salvaged. The mill ruins (including stamp batteries and cyanide-related features) are among the better-preserved examples of early 20th-century desert milling technology.
In summary, the Skidoo Pipeline (operational primarily 1907–1917, with the broader mining camp active from 1906 into the early 1940s on a reduced scale) transformed a remote gold discovery into one of the more successful and longer-lived mining towns of Death Valley by solving the water problem through ambitious gravity engineering. It powered unique milling operations, sustained a substantial community, and supported regional exploration before ore exhaustion and maintenance challenges ended the boom.
Journigan’s Mill
Journigan’s Mill (also known as the Gold Bottom Millsite) was a custom amalgamation-and-cyanide gold mill in Emigrant Canyon, Death Valley National Park (Inyo County, California). It was the largest and longest-operating mill of its type remaining in the park from the 1930s–1950s era and played a key supporting role in the mid-20th-century revival of gold mining in the Skidoo/Harrisburg and Emigrant Spring areas.
Journigan’s Mill (also known as the Gold Bottom Millsite) was a custom amalgamation-and-cyanide gold mill in Emigrant Canyon, Death Valley National Park (Inyo County, California) Photo by James L Rathbun
Location and Physical Setting
The site sits on the west side of Emigrant Canyon Road (also called Wildrose Canyon Road), roughly 1 mile south of Emigrant Springs and about 13.5–14 miles south of Stovepipe Wells, at an elevation of approximately 4,400 feet in the Panamint Range. It covers about 3 acres and is highly visible from the paved road.
Water—the critical limiting resource in Death Valley—came from nearby springs (Green, Burro, Willow, and Burns; earlier accounts also mention additional springs such as Canyon and Malapi). Pipelines delivered water to the mill, enabling continuous operation in an otherwise arid environment.
Today the site consists of scattered concrete foundations (mill platforms on multiple levels, housing footings), remnants of cyanide tanks, two steel water tanks (in earlier descriptions), a wooden floor platform, and tailings piles/stockpiles. Machinery was removed long ago. The ruins are eligible for the National Register of Historic Places for their local significance as the largest surviving amalgamation/cyanide plant of the period and for having the longest contiguous use of any milling site within the former Death Valley National Monument.
Early Use of the Site (Pre-Journigan)
The location had intermittent milling activity for decades before Roy Journigan’s major development, taking advantage of the springs:
- Possible early one-stamp mill processing Skidoo ore around 1909 (unconfirmed in some studies).
- Carl R. Suksdorf and Frank “Shorty” Harris reportedly ran a ball mill here in 1918 for custom work.
- Suksdorf filed for water rights to six nearby springs in the early 1920s for his Gold Dollar Millsite (tied to his nearby Gold Dollar Mine) but lost them for non-development.
- Shorty Borden and Shorty Harris purportedly operated a five-stamp mill in 1924 processing Skidoo and Poppy Mine ore.
- Dr. Archibald and later Walter M. Hoover continued intermittent milling into the early 1930s.
These earlier efforts were smaller and sporadic.
Establishment and Operation under Roy Journigan (mid-1930s–1939)
The decisive impetus came from the Gold Reserve Act of 1934, which raised the official U.S. gold price from $20.67 to $35 per ounce. This made lower-grade ores newly profitable and spurred a revival of mining in the region.
In March 1934, Roy Journigan (with partners E.L. Journigan and L.E. Steinberger) located the five-acre Gold Bottom Mill Site claim. Construction of a new 25-ton-per-day amalgamation and cyanide mill began around 1935; sources commonly date the main plant to 1937. Journigan’s business model was to operate a custom mill: local mine owners would truck ore to the mill rather than ship bulky low-grade material long distances to distant smelters. This reduced transportation costs, allowed higher-grade concentrates to be shipped, and created shared profits.
Key features of the plant (from NPS Historic Resource Study descriptions) included:
- 25-ton ore bin and a finer-ore bin
- 6-inch by 8-inch Blake crusher
- 3 × 4 ft Straub cone-type ball mill
- 4 × 8-foot amalgamation plates
- Seven 14 × 5-ft cyanide tanks
- Four-compartment zinc boxes for precipitation
- Powered by a 15 h.p. Fairbanks-Morse gasoline engine
Four men typically worked the mill. In 1937 Journigan leased the Skidoo mine and also processed ore trucked from the Cashier mine at old Harrisburg. The mill stimulated renewed activity around Emigrant Spring and the reopening of Skidoo/Harrisburg-area mines by lowering production costs.
Journigan sold the mill in 1939 (some contemporary reports say 1938). One account notes that the last ore milled under his direct operation was in 1938; subsequent owners used the water rights for related milling, including at Skidoo.
Later Ownership and Continued Operation (1939–late 1960s)
The mill changed hands multiple times and continued operating under various owners into the late 1960s—making it the longest-running mill in Death Valley. It was rebuilt or renovated in the 1950s. In September 1959 the Argentum Mining Company purchased the machinery, dismantled it, and moved it to Columbia Flats (near Mina/Columbus), Nevada. A final effort in the 1960s used the remaining cyanide tanks to leach the tailings dump; this activity ended by 1967 (some accounts extend minor activity into the early 1970s).
Role in Regional Mining and Output
Journigan’s Mill was never a primary mine producer itself; it was a custom processing facility that enabled profitable extraction of gold from relatively low-grade ores in the surrounding Panamint Range districts. By providing local, efficient amalgamation (mercury-based recovery of free gold) followed by cyanide leaching (dissolving remaining gold into a soluble complex for precipitation), it made remote desert mining more viable during the post-1934 gold-price boom and beyond.
Capacity: 25 tons of ore per day.
Primary feed sources: Skidoo mine (under lease) and Cashier mine (Harrisburg); also custom work for other local properties.
Specific production totals (ounces of gold recovered or total tonnage processed across the mill’s life) are not well documented in available NPS summaries or secondary sources. Contemporary notes indicate ore values in the Skidoo area in the mid-1930s were often in the $15–$30 per ton range (at the new gold price). The mill’s contribution was primarily enabling activity rather than generating independently recorded large-scale output figures comparable to the original early-20th-century Skidoo production (which totaled roughly $1.3–1.5 million before 1917).
An estimated 1,500 cubic yards of mill tailings remain on site, reflecting the volume of material processed over decades.
Significance and Present Status
Journigan’s Mill exemplifies the ingenuity required for desert mining: securing water rights, building pipelines, and running a relatively sophisticated (for its remote setting) cyanide plant that extended the productive life of older districts. It is the largest surviving ruin of a 1930s–1950s amalgamation-and-cyanide operation inside Death Valley National Park and documents the longest continuous milling use of any site in the former monument.
Visitors today see only foundations, tank remnants, and tailings. The National Park Service has conducted environmental assessments because of residual cyanide and elevated metals in soils and tailings; the site is managed with “Stay Out – Stay Alive” warnings due to physical and chemical hazards. An interpretive sign recounts the mill’s history for the public.
In summary, Journigan’s Mill operated primarily from the mid-1930s through the late 1960s (peak development and custom milling under Journigan and successors ~1935/1937–1959, with residual activity into the 1960s), processed ore at a capacity of 25 tons per day drawn mainly from Skidoo and Cashier, and served as a critical local processing hub that helped sustain gold mining in the Emigrant Canyon–Skidoo–Harrisburg corridor long after the original boom towns had faded.
Wildrose Canyon Road
Wildrose Road (also called Wildrose Canyon Road or Upper/Lower Wildrose segments) in the Panamint Mountains of Death Valley National Park is a scenic, historic high-country route that climbs from the desert floor into cooler pinyon-juniper woodlands, providing access to the iconic Wildrose Charcoal Kilns, campgrounds, and trailheads for Wildrose Peak and Telescope Peak.
It is one of the park’s most rewarding drives for those seeking elevation relief, mining history, and solitude away from the valley floor heat and crowds. The road system connects via Emigrant Canyon Road from CA-190 (near Emigrant/Stovepipe Wells) or from the west via Lower Wildrose/Trona-Wildrose Road out of Panamint Valley/Trona. Vehicles longer than 25 feet are prohibited on the narrow, winding sections.
Road Description and Driving Conditions
Access from the east (primary for most visitors): From CA-190 west of Stovepipe Wells, turn south onto Emigrant Canyon Road. This paved, narrow two-lane road with limited or no shoulders climbs steadily through Emigrant Canyon (named for 1849 gold rush pioneers who escaped Death Valley this way), past rock formations, the ruins of Journigan’s Mill (a cyanide mill processing gold ore), the Skidoo side road, and Aguereberry Point turnoff. It crosses Emigrant Pass (~5,300 ft) and Nemo Crest before descending toward Wildrose Junction. The drive features tight curves, blind corners, steep drop-offs in places, and sustained grades—demanding focused driving.
At Wildrose Campground (~4,100 ft), the road continues east/up-canyon as Wildrose Road. Pavement extends most of the way, becoming graded gravel for the final ~2 miles to the Charcoal Kilns (~6,800–6,900 ft). This section is generally suitable for most passenger vehicles with moderate clearance when dry, though it can develop washboards, potholes, or soft spots after storms.
Beyond the kilns, a steeper, rougher gravel road (high-clearance recommended; 4WD often preferred) continues ~3–4 miles past Thorndike Campground (~7,400 ft) to Mahogany Flat (~8,200 ft), the trailhead for Telescope Peak (11,049 ft). This upper section gains significant elevation, has steeper grades, ruts, and is frequently closed by snow/ice in winter into spring.
Western approach (Lower Wildrose/Trona-Wildrose Road): From Panamint Valley (CA-178/Trona area), this route climbs to meet Emigrant Canyon Road near Wildrose. Severely damaged by flash floods from the remnants of Hurricane Hilary in August 2023 (which stripped pavement and cut a ~9-foot channel across the roadbed), it reopened in June 2026 as an unpaved, narrow gravel road restricted to vehicles under 25 feet. Expect soft shoulders, potholes, rough sections, and remnants of old asphalt. It is passable in most standard vehicles when dry but requires caution. Recent storms (e.g., October 2026) have caused additional washouts and debris in places—always check current NPS conditions.
Overall character: The full corridor gains roughly 4,000+ feet from valley approaches to Mahogany Flat. Best months are typically April–June and September–November for milder weather and open access. Summer offers cool relief (15–30°F+ cooler than Furnace Creek) in pinyon-juniper woodland; winters can bring snow closures higher up. No cell service in the canyon. Watch for wild burros (descendants of mining-era animals). Bring all water, fuel, and supplies—facilities are minimal.
Always verify the official NPS Alerts & Conditions page before travel, as flash floods, washouts, and seasonal closures are common in this landscape.
Mining and Other History
Wildrose Canyon and the surrounding Panamint Range have a rich, layered mining history tied to silver, lead, gold, and antimony, interwoven with the broader Death Valley mining booms of the late 19th and early 20th centuries.
Earliest activity: Prospecting reached the area in the 1860s. On Christmas Day 1860, Dr. S.G. George’s party (searching for the legendary Lost Gunsight Lode) discovered antimony near Wildrose Spring (Christmas Gift Mine). Sporadic work followed. The Rose Springs (later Wild Rose) Mining District was active by the early 1870s, formalized in 1888 with boundaries roughly from Townsend Pass north, Panamint Valley west, the Panamint District south, and Death Valley east.
Charcoal Kilns era (peak of early industrial activity): In 1875, rich silver-lead deposits were found on the east slope of the Argus Range (west of Panamint Valley) while prospectors sought the Lost Gunsight. The principal claim became the Modoc (or Modock) Mine. San Francisco investors formed the Modock Consolidated Mining Company (with involvement from George Hearst). Ore averaged 100–300 ounces of silver per ton plus lead. Smelters were built near Lookout/Modoc, but local wood was insufficient for the high heat needed.
In spring 1877, the company built ten large beehive-shaped stone charcoal kilns in upper Wildrose Canyon (~25 miles east), where single-leaf pinyon pine and juniper were more abundant. Constructed of local stone with lime-sand-gravel mortar (overseen by a company man named Morris or under S.B. Morrison), each kiln stood ~25 feet high, held about 4 cords of wood, and produced ~2,000 bushels of charcoal after a week of burning. About 40 woodcutters and workers operated them; a temporary camp (“Wildrose”) housed around 100 people. Charcoal was hauled by pack train (jackasses) and wagons (involving freighters like Remi Nadeau’s company) to the smelters.
The kilns operated primarily 1877–1878/1879. High-grade ore declined, local forests were heavily depleted, and the long haul became uneconomical. The mines closed, and the kilns were abandoned after only a short working life—which is why they survive as the best-preserved 19th-century charcoal kilns in the western U.S. They remain a highlight, with interiors still sometimes carrying a faint charcoal scent. Preservation work continues.
Later mining: Gold activity increased with the 1905 Harrisburg/Skidoo discoveries nearby (Shorty Harris and Pete Aguereberry; Aguereberry worked the Eureka Mine for decades). Antimony mining in Wildrose Canyon (Monarch, Combination, Monopoly, Kennedy claims on Antimony Ridge) saw development from the 1890s, with peak production during World War I (~1,000 tons or more reported in some accounts under Western Metals Company). Workings included open cuts, tunnels, and ore chutes; activity was limited by remoteness and markets. Smaller gold operations (e.g., Burro, Gem, New Discovery) occurred in the 1930s–1940s.
Transportation and settlement history: Wildrose Station (near the spring, about a mile below) served as an oasis and stage stop on the Ballarat–Skidoo route (~1908–1917), with a wooden station, corral, and blacksmith shop. It later offered tourist cabins, a store, and gas into the mid-20th century before NPS closure in 1971 (structures removed; foundations and rockwork remain as a picnic area). The canyon provided a key freight and travel corridor linking Panamint Valley mines to the high country and beyond.
The broader Panamint Range saw earlier silver rushes (Panamint City in the 1870s) and ongoing prospecting. Indigenous Timbisha Shoshone people long used the pinyon woodlands for pine nuts—resources impacted by the charcoal operations.
Highlights Along the Road
- Wildrose Charcoal Kilns: The star attraction—ten aligned beehive structures at ~6,800–6,900 ft amid woodland. Easy to explore; trailhead for the ~8.4-mile round-trip Wildrose Peak hike (excellent views).
- Campgrounds: Wildrose (lower, among mesquite), Thorndike, and Mahogany Flat (higher, cooler, more primitive; winter snow issues).
- Side trips: Aguereberry Point (views into Death Valley; Eureka Mine remnants), Skidoo ghost town road, Journigan’s Mill ruins.
- Scenery: Transition from desert scrub to pinyon-juniper, canyon walls, distant Sierra and Death Valley vistas, wildflowers in season, and cooler air.
Practical notes: No services beyond basic campground amenities (vault toilets; limited or no water). High summer heat is less of an issue higher up, but prepare for desert extremes, sudden weather, and limited recovery options. Respect historic sites—do not enter mine shafts or disturb structures. The road rewards careful drivers with a tangible connection to Death Valley’s mining past and some of its finest high-country scenery. Check nps.gov/deva for real-time road status before any trip.
Emigrant Canyon Road
Emigrant Canyon Road is a scenic, paved mountain road in the western portion of Death Valley National Park, California. It provides the primary paved access from California State Route 190 (near Stovepipe Wells and the Emigrant area) into the higher elevations of the Panamint Mountains, connecting to the Wildrose area. The road is roughly 21 miles long from its junction with CA-190 to Wildrose Campground and is one of the park’s most rewarding drives for its changing landscapes, historical sites, and cooler high-country destinations.
Route and Character
The road begins at Emigrant Junction on CA-190, a short distance west of Stovepipe Wells and just past the historic Emigrant Ranger Station area (notable for its CCC-era stone buildings and trees in an otherwise sparse landscape). From an elevation of around 2,200 feet, it immediately begins climbing as it leaves the main valley floor.
It ascends an alluvial fan and enters Emigrant Canyon proper, a drainage named for the Lost ’49ers (gold-rush emigrants of 1849–1850). Some of those pioneers escaped Death Valley via Emigrant Pass and Wildrose Canyon after becoming stranded in the valley. The lower canyon section features gently winding pavement past steep slopes, low rocky cliffs, and desert vegetation.
The road continues climbing across the more open Harrisburg Flats, offering expansive views of plains and distant mountains to the east and west. It reaches Emigrant Pass (around 5,300–5,500 feet elevation, with nearby Nemo Crest slightly higher). This high point marks a transition to more demanding driving: the road becomes narrower, with tighter curves, hairpin turns, blind corners, steep drop-offs, and limited or no guardrails in places. The pavement “squirms” through the terrain with significant elevation gain (overall climb on the order of 3,000+ feet from the junction).
Beyond the pass, the road descends into the Wildrose Canyon drainage. It remains paved to Wildrose Campground (approximately 4,100 feet elevation). From there, a short graded dirt extension (about 2 miles, generally suitable for passenger cars when conditions allow) continues to the Wildrose Charcoal Kilns. Higher roads beyond require high-clearance vehicles and lead to Thorndike and Mahogany Flat campgrounds (near 8,000 feet) and the trailhead for Telescope Peak (11,049 feet, the park’s highest point).
The full drive from CA-190 to the charcoal kilns is often described as taking about 35–45 minutes under good conditions, though the winding nature and scenery encourage a slower pace. Side roads branch off, including those to Skidoo (ghost town and mill), Aguereberry Point (high overlook), Wood Canyon, and Telephone Canyon.
Road Conditions, Restrictions, and Practical Notes
Emigrant Canyon Road is narrow, two-lane, and lacks shoulders in many sections. Vehicles longer than 25 feet (including trailers and RVs) are prohibited due to the tight curves, steep grades, and drop-offs. It is generally open year-round but can be affected by winter snow/ice at higher elevations or by flash flooding (common in monsoon season).
The road suffered severe damage from flash floods associated with the remnants of Hurricane Hilary in August 2023. Temporary repairs allowed reopening, followed by more permanent work (completed around April 2025) involving buried concrete barriers and rock-filled gabion baskets to improve flood resilience. Always check current conditions on the official NPS Death Valley website or alerts page before traveling, as closures can occur.
No services or potable water are available along the road or at the high-country campgrounds (Wildrose, Thorndike, Mahogany Flat). Visitors must bring all water and supplies. Cell service is typically nonexistent. The higher elevations are substantially cooler than the valley floor—often 15°F cooler at Wildrose Campground and up to 30°F cooler near Mahogany Flat—making the route popular for summer escapes when Furnace Creek temperatures exceed 100°F.
Points of Interest Along or Near the Road
- Journigan’s Mill (also known as Gold Bottom Mill): Ruins of a mid-20th-century cyanide mill (built around 1937) visible on the west side of the road roughly 6–7 miles in. Foundations, tanks, and other relics remain.
- Skidoo Road turnoff: Leads to the Skidoo ghost town site and well-preserved 15-stamp mill (high-clearance recommended for the side road).
- Aguereberry Point Road: High-clearance road to a dramatic overlook of Death Valley and the remains of Aguereberry Camp/Harrisburg mining area.
- Wildrose Campground: Free, first-come, first-served primitive sites at about 4,100 feet; cooler alternative to valley-floor camping. No water.
- Wildrose Charcoal Kilns: Ten well-preserved 1870s beehive-shaped stone kilns used to produce charcoal for silver-lead smelters. Accessible by passenger car via a short dirt stretch beyond the paved road’s end. Nearby is the trailhead for the strenuous Wildrose Peak Trail (roughly 8.4 miles round-trip with significant elevation gain and panoramic views).
- Higher elevations: Thorndike and Mahogany Flat campgrounds and the long Telescope Peak Trail.
Historical Context
The canyon and pass take their name from the Lost ’49ers, groups of California Gold Rush emigrants who became stranded in Death Valley in late 1849 after attempting a shortcut. Some parties escaped westward through Emigrant Pass and Wildrose Canyon after abandoning or burning wagons. The broader area later supported mining activity (including Skidoo and charcoal production for Argus Range smelters) and early tourism. The Civilian Conservation Corps improved access and facilities in the 1930s, including work in the Wildrose area.
Emigrant Canyon Road stands out as one of Death Valley’s premier scenic drives, transitioning from classic desert valley scenery into higher, more mountainous terrain with pinyon-juniper woodlands, mining history, and access to the park’s alpine-like high country. It rewards careful driving with solitude, sweeping views, and a markedly different experience from the famous valley-floor attractions. Always prioritize safety, prepare for remote conditions, and verify current road status with the National Park Service.
Skidoo Road
Skidoo Road (also called Skidoo Trail) is an approximately 7–9 mile one-way (roughly 8 miles by common centerline measurements) high-clearance dirt road in Death Valley National Park that climbs northwest off Emigrant Canyon Road (Wildrose Road) in the Panamint Mountains to the site of the early-1900s gold mining town of Skidoo and its well-preserved stamp mill.
It is a classic Death Valley backcountry spur: remote, scenic, historically rich, and generally manageable for prepared drivers, though conditions can change with weather.
Road Access, Character, and Driving Conditions
Turn off Emigrant Canyon Road about 9.4 miles south of the junction with CA-190 (near Emigrant, between Stovepipe Wells and Panamint Springs). The road is unpaved dirt/gravel with washboard sections, loose material, embedded rocks, and occasional washouts. It is an out-and-back dead-end route.
- Difficulty: Moderate / high-clearance recommended. The National Park Service and recent road guides rate it high-clearance primarily because of a single steep grade with protruding rock through the roadbed at about 3.5 miles. Sedans risk undercarriage damage there; the downhill return can be the more problematic direction. Four-wheel drive is not required in normal dry conditions.
- Surface and length: Starts relatively good across flatter terrain and through low hills, then climbs a ravine and traverses hillsides. First ~4 miles are often the smoother portion; it roughens higher up. Total distance to the townsite/mill area is commonly listed around 7–9 miles one way.
- Elevation: Climbs to roughly 5,700 ft (about 1,734 m) at the townsite.
- Vehicle needs: High-clearance recommended. Good off-road or all-terrain tires, at least one (preferably two) full-size spare(s), air compressor, shovel, and recovery gear are wise. Street-legal vehicles only—no OHVs or green-sticker off-highway vehicles. Bicycles are allowed on the road.
- Best seasons: March–May and October–November. Summer heat is extreme even at elevation (dehydration risk on the approach and while exploring). Winter can bring snow or mud that closes or complicates the road. Always check the NPS Death Valley road conditions/alerts page before going, as flash floods and storms alter surfaces.
- Other notes: Day-use only—no camping on or within one mile of the road. No cell service. No water, fuel, or services on the road or at the site. Nearest fuel is typically Stovepipe Wells. Flat tires are common on park dirt roads. Stay on the designated road; off-road driving is prohibited.
Side tracks branch off (keep left at forks for the main route to the mill in many descriptions). Early points of interest include a single-room cabin and a mine headframe around 2.8 miles. Higher up, views open toward Death Valley basins, with distant sightlines toward Telescope Peak and surrounding ranges. The landscape is barren, rocky, sagebrush-dotted desert hills.
Mining History and the Town of Skidoo
Skidoo was one of Death Valley’s most successful and longest-lived gold camps of the early 20th century boom era, thriving roughly 1906–1917 (with some later intermittent activity). Unlike many short-lived desert camps, it produced substantial gold—commonly cited around $1.3–1.6 million (at the then ~$20/oz price), or on the order of tens of thousands of ounces—making it among the top producers in the region (second only to operations like the Montgomery-Shoshone or Keane Wonder in some rankings).
Discovery and founding: In January 1906, prospectors John (or Harry) Ramsey and John “One-Eye” Thompson, heading toward the nearby Harrisburg strike, were forced by a rare fog to camp near Emigrant Spring. When it cleared they found promising gold-bearing ledges (the Gold Eagle Group claims, free-milling quartz veins running north–south for about 1.5 miles, 2–12 feet wide, assaying high). They staked claims; news spread and a rush followed. Nevada mining interests quickly dominated. Ernest A. “Bob” Montgomery (of Montgomery-Shoshone fame) bought the key claims and formed the Skidoo Mines Company. Other investors included Charles M. Schwab and figures from the Tonopah/Rhyolite scene.
The townsite was platted in 1906 (initially called Montgomery or Hoveck after the mine manager Matt Hoveck). It was renamed Skidoo in 1907, drawing from the popular slang “23 Skidoo” (meaning “get lost,” “beat it,” or “go away”). Theories for the “23” include the number of initial claims, distance of the water line, blocks in the survey, or other local lore; the postal service rejected “23” in the official name. At its peak (around 1907–1909) the population reached several hundred (estimates 400–700), with stores, saloons, restaurants, a bakery, laundry, meat market, lodging, newspaper (Skidoo News), school, physician, bank (Southern California Bank of Skidoo / related entities), telephone service (linked toward Rhyolite), clubs, and assayers. Stages and early autos connected it to Rhyolite, Ballarat, and other points.
The water pipeline and mill: Water was the limiting factor. Domestic supply came from Emigrant Springs, but milling needed more power and volume. The company built a gravity pipeline (commonly described as ~20–23 miles long, though some sources cite ~15–22) from Birch Spring (or related springs near Telescope Peak at higher elevation). It dropped roughly 1,800 feet and supplied hydraulic power—making the Skidoo Mill the only water-powered stamp mill in the Death Valley region. The 15-stamp (or similar capacity) mill, built on a steep hillside bench below the townsite, processed ore via a cyanide system suited to the free-milling quartz. Ore was trammed or hauled by burros/mine cars. Production was strong for years; the main ore bodies pinched out or became uneconomic by September 1917, ending the primary boom. Sporadic work continued later (including 1930s activity after the gold price rise), but the town faded. Buildings were scavenged; little of the town itself remains beyond foundations, rubble, scattered debris, and an NPS interpretive board.
The mill is the standout remnant—timber framing, corrugated iron, machinery, and platforms still largely standing on the steep slope overlooking Emigrant/Telephone Canyon country. It is regarded as one of the largest and best-preserved mills in the park. Surrounding hills hold numerous shafts, adits, headframes, cabins, machinery, old vehicles, can dumps, and other workings (over a thousand openings in the broader district by some counts). Stay out of all mine structures, shafts, and tunnels—they are extremely hazardous (unstable timber, falls, bad air, etc.). Hantavirus risk exists in rodent-contaminated enclosed spaces; rattlesnakes are possible around ruins.
Other History and Context
Skidoo fit into the broader early-1900s Nevada–California gold rush that followed Tonopah, Goldfield, and Rhyolite discoveries. It was one of the last major gold camps in the Death Valley/Panamint area and benefited from systematic development rather than pure boom-and-bust chaos. The pipeline was a notable engineering effort for the remote setting. In 1923 the site served as a location for the film Greed. By the mid-20th century it was fully abandoned as a community; the Park Service now manages it as a historic non-interpreted site within the national park.
Today the “trail” (road) rewards visitors with isolation, big Panamint views, tangible mining archaeology, and a tangible sense of how briefly and intensely these desert camps flourished. The mill and scattered ruins are the main draws; the townsite itself is subtle. Explore carefully on foot from the road end, respect closures and leave-no-trace rules (historic objects are protected), and treat the area as remote desert: carry ample water, tell someone your plans, and be self-sufficient.
Practical tips: Walk the rock section at ~3.5 miles before driving if unsure of clearance. Check current NPS conditions. Combine with nearby Aguereberry Point Road or Wildrose area stops if time allows. Best experienced in cooler months with a high-clearance vehicle and time to walk the mill overlook and surrounding workings.
This is one of the more approachable historic mining roads in the Panamints—rewarding without being extreme—provided you respect the clearance limit, weather, and the fragile historic fabric.