Big Bear, CA
I quiet mountain community full of back country adventure.
Harry Wade Escape Route
The Harry Wade Escape Route (officially Harry Wade Road, California Historical Landmark No. 622) is a historic dirt road that crosses the remote southern end of Death Valley National Park. It commemorates the path taken in 1849 by Harry Wade and his family, who successfully escaped the valley with their ox-drawn wagon after becoming trapped with a larger emigrant caravan seeking a shortcut to the California Gold Rush. The modern road roughly follows that exit route and now serves as a through-route connecting the paved Badwater Road system on the north with California Highway 127 (and Saratoga Spring Road) on the southeast.
Background and the Journey West
Harry Wade was born on March 16, 1800, in Rochester, England. He immigrated to the United States, lived for a time in Pennsylvania, and eventually settled as a farmer near Joliet, Illinois. In early 1849, news of gold discoveries in California prompted him to sell his farm. He packed his wife, Mary Reynolds Leach Wade, and their children (including Harry George Jr., Charles Elliott, Almira, and Richard Angus) into a covered wagon and joined the westward migration.
The family arrived in Salt Lake City too late in the season to risk the northern Sierra Nevada crossings. Like hundreds of other emigrants, they joined a large wagon train—commonly referred to as the Sand Walking Company or San Joaquin Company—that turned south to follow the Old Spanish Trail toward Southern California. Guided in part by Jefferson Hunt, the group of roughly 100 wagons sought a faster route to the gold fields. A poorly planned deviation from the established trail led a significant portion of the travelers, including the Bennett-Arcane (Bennett-Arcan) party and those traveling near them, into the unmapped basin of what is now Death Valley in December 1849.
Entrapment in the Valley
The emigrants found themselves in a deep, arid valley ringed by high mountain ranges. Oxen weakened rapidly, water sources proved unreliable, and progress stalled on the salt flats and harsh terrain. Several people died during the ordeal, helping give the place its grim name. Most parties eventually abandoned or burned their wagons, slaughtered oxen for food, and walked out under extreme hardship.
The Bennett-Arcane contingent became stranded for about a month near the area west of present-day Badwater Basin (later marked as the Bennett-Arcane Long Camp). Two young members of that party, William Lewis Manly and John Rogers, made a heroic roughly 250-mile journey on foot across the Mojave Desert to seek help near Los Angeles. They later returned with supplies and guided the remaining families to safety in early 1850.
Harry Wade’s Independent Decision and Escape
Harry Wade and his family had been traveling slightly behind the main Bennett-Arcane group. They deliberately stayed about a day behind in order to conserve their oxen’s strength and allow the sparse desert springs time to recover between parties. After watching Manly and Rogers depart on their rescue mission, Wade chose not to wait. He doubted that help would return in time (or at all) and decided to seek an independent southern exit.
The family pushed southward through rugged canyons and washes. At a critical moment when water was nearly exhausted, their daughter Almira reportedly noticed birds flying over a ridge and discovered a substantial spring—now known as Saratoga Spring—that provided life-saving water for the family and their animals. From this oasis they continued along an ascending route toward the Amargosa River’s southern bend near Salt Spring. There they regained the Old Spanish Trail. They endured a dry stretch to Bitter Spring, where traders sold them flour, allowing the animals to recover. Following tracks left by earlier parties, they continued through Cajon Pass and reached the Los Angeles area in relative safety.
The Wades were the only known party from the 1849 Death Valley entrapment to exit with both their wagon and oxen intact. This preservation of equipment and draft animals gave them a significant practical advantage over those forced to abandon everything and walk.
Founding and Legacy of the Escape Route
The path Harry Wade pioneered became known as the Harry Wade Exit Route (or Harry Wade Road). It roughly traces a southern exit from the valley floor toward the Amargosa River drainage and the Old Spanish Trail. The modern dirt road within and near Death Valley National Park largely follows this historic corridor, connecting the southern end of Badwater Road with California Highway 127 near the park’s southeast boundary (approximately 30 miles north of Baker).
In 1957 the route was designated California Historical Landmark No. 622. A marker, with a plaque provided by Wade’s descendants, was dedicated near the Highway 127 end of the route (roughly at milepost 29.8, about four miles south of the park boundary). The plaque text summarizes the story: after becoming trapped with the ill-fated 1849 caravan, Harry Wade found an exit route for his ox-drawn wagon, saving his life and those of his wife and children, and at that point the party rejoined the known Spanish Trail to Cajon Pass.
Harry Wade later settled in the Alviso area of Santa Clara County, California, where he died on October 13, 1883. Mary Wade died there in 1889. Their successful escape, achieved through caution, observation, and determination rather than dramatic rescue, remains one of the more practical success stories among the Death Valley ’49ers. The route they opened continues to serve as both a historic landmark and a remote backcountry road, offering modern travelers a tangible connection to the hardships and ingenuity of 1849.
Road Makeup and Route Description
- Northern connection – Badwater Road: Harry Wade Road begins (or ends) about 2 miles south of the Ashford Mill ruins on Badwater Road, near the point where the pavement bends east toward Jubilee and Salsberry Passes. Badwater Road itself is the main paved artery running south from Furnace Creek past Badwater Basin (the lowest point in North America) and other classic valley-floor attractions before reaching this junction.
- Harry Wade Road proper: Approximately 24–32 miles of graded-to-rough dirt road running southeast across the valley floor. It passes between the Owlshead Mountains (southwest) and the Ibex Hills / Saddle Peak Hills (east), crosses the Amargosa River channel, and ends at the junction with Saratoga Spring Road near the park’s southeast corner.
- Southern connection – Saratoga Spring Road / Highway 127: From the junction, Saratoga Spring Road continues a short distance east/northeast to the spring oasis or further to CA-127 (about 30 miles north of Baker). A California Historical Landmark marker stands near the Highway 127 end of the overall escape route.
The full through-drive from Badwater Road to Highway 127 is roughly 30+ miles and can be driven in either direction. It is one of the more remote and least-traveled routes in the park.
Road Conditions
High-clearance is recommended due to washboard, sandy sections, and potential soft spots. As of recent park notices, deep sand is flagged approximately 6 miles south of the Badwater Road junction—this is the most common place vehicles get stuck. The Amargosa River crossing can become impassable when the river is flowing (after storms or in wet winters). Conditions vary widely: the road can be relatively firm after grading or deep and soft at other times. No cell service. Best seasons are late fall through early spring (November–March). Summer heat is extreme and potentially life-threatening. Always check the official NPS Death Valley road conditions page before travel.
Points of Interest Along the Route
Ashford Mill Ruins (near northern junction)
Historic borax mill remnants just north of the Harry Wade / Badwater Road junction. A short stop with interpretive value and views of the southern valley.
Amargosa River Crossing
Usually dry, but a critical potential obstacle. When flowing, it can close the road. The channel marks a key geographic feature of the southern park.
Owlshead Mountains and Owl Hole Spring Road
The range dominates the southwest views. A side road branches toward Owl Hole Spring and the mountains for those seeking additional exploration (higher clearance/4WD often needed).
Ibex Hills, Saddle Peak Hills, and Nearby Dunes
East of the road. White talc waste piles and historic mining areas are visible in the hills. The quiet Ibex Dunes lie nearby and can be reached via connecting routes or short walks.
Saratoga Spring (via short spur from the southern junction)
One of the largest wetland areas in southern Death Valley. Open ponds and marsh grass support waterfowl, the endemic Saratoga Springs pupfish, rare invertebrates, and other wildlife. A short walk from the parking area offers overlooks. The oasis has long served as a watering stop (including for 20-mule teams) and remains a striking green contrast to the arid surroundings. Entry into the sensitive marsh is restricted.
California Historical Landmark Marker (Highway 127 end)
Commemorates Harry Wade’s 1849 escape. Located near the southern entrance, approximately 30 miles north of Baker.
Broader Landscape
Expansive views of the southern valley floor, distant mountain ranges, and occasional wildflower displays in good years. The route feels isolated and true to the “escape” history that gives it its name.
Practical Tips
- High-clearance vehicle strongly preferred; 4WD helpful in deep sand or after rain. Carry recovery gear, extra water, a full-size spare, and offline maps.
- Fuel and supplies are available in Baker, Shoshone, or Furnace Creek—nothing exists along the route itself.
- Dispersed camping is allowed under standard backcountry rules (away from water sources and developed areas).
- Combine with Saratoga Spring for wildlife viewing or continue north on Badwater Road for classic valley-floor sights.
- Respect wilderness boundaries and sensitive habitats; stay on designated roads.
The Harry Wade Escape Route offers a genuine sense of the park’s remote southern reaches and a tangible link to the 1849 emigrant history that helped name Death Valley. It is best suited for prepared travelers seeking solitude, history, and a through-route experience rather than crowded overlooks. Verify current conditions with the National Park Service before setting out.
Harry Wade Exit Route – Some 100 wagons found themselves in Salt Lake City too late to cross the Sierra Nevada. They banded together under the name of Sand Walking Co. and started for the gold fields in California over the Old Spanish Trail. After being in Death Valley with the ill-fated 1849 caravan, Harry Wade found this exit route for his ox-drawn wagon, thereby saving his life and those of his wife and children. At this point the Wade party came upon the known Spanish Trail to Cajon Pass.
Highway Placard on Hgwy 127
Further Reading
Henry Wade Escape Route Trailmap
Aguereberry Point Road
Aguereberry Point Road is a roughly 6–6.5-mile unpaved side road off Emigrant Canyon Road (also called Wildrose Road) in the Panamint Range on the west side of Death Valley. It climbs from the paved road to a high crest viewpoint at 6,433 feet, offering one of the park’s most expansive and least-crowded panoramas of the valley floor. The turnoff is about 10–12 miles south of Highway 190 (near Emigrant/Stovepipe Wells area).
The road is day-use only (no camping along it or within a one-mile buffer). It is rated for high-clearance vehicles due to a rock outcrop in the roadbed around 3.5 miles and a steep, rocky final half-mile. Four-wheel drive is not required under normal conditions, but low-clearance cars are not recommended; some drivers park short of the last stretch and walk. The road can be washboarded, rocky, and subject to snow, mud, or temporary closures after storms—always check current NPS road conditions before going. Cell service is generally absent.
History and Background
The road and viewpoint are named for Jean Pierre “Pete” Aguereberry (1874–1945), a Basque immigrant from France who prospected in the area. In 1905, while traveling with the well-known prospector Shorty Harris, Aguereberry discovered gold. Claims led to the short-lived Harrisburg mining camp (originally intended as “Harrisberry”). Aguereberry worked the Eureka Mine largely alone for decades, living in a simple cabin at the site from 1907 until near his death. In later years he guided visitors to what he called “The Great View” of Death Valley; the point was later officially named for him. He is buried in Lone Pine, California.
Points of Interest Along the Road
- Aguereberry Camp / Harrisburg ruins (early on the road, roughly the first 1–2 miles): Remains of the early-1900s mining settlement. Pete’s original 1907 two-room cabin (with period furnishings such as a stove and refrigerator in accounts), additional later cabins (one built as a guest house around 1941), scattered ruins, and mining relics. The camp was never large or long-lived—most people moved on to better prospects at Skidoo—but it preserves the everyday life of a solitary desert prospector.
- Eureka Mine (about 1.7 miles): The historic gold mine Aguereberry worked for decades. Features include a headframe, shafts/adits (now gated for safety and bat protection—do not enter), ore-cart remnants, and scattered rusty machinery. Nearby is the Cashier Mill (built around 1909), a relatively well-preserved structure that processed ore using gasoline engines and chemical methods of the era. The site offers good photo opportunities of industrial ruins in a stark desert setting. Stay on established paths and treat all mine openings as hazardous.
- The rock outcrop (around 3.5 miles): A notable obstacle that helps define the high-clearance recommendation. The road continues through open flats, then winds through a canyon before reaching the ridgeline.
- Aguereberry Point (road’s end, 6,433 ft): The main destination. A small parking area sits near the crest. Short footpaths lead to the tip of the point and along the ridge for the best vistas. From here you look east across Death Valley toward the Amargosa Range and Black Mountains (Dante’s View is visible on the far side). Highlights include the white salt flats of Badwater Basin (the lowest point in North America at 282 feet below sea level—over a mile of vertical relief), the green oasis of Furnace Creek, Mesquite Flat Sand Dunes to the north, and distant peaks such as Mount Charleston in Nevada (about 80 miles away). On clear days the Sierra Nevada can appear to the northwest. The viewpoint sits on Cambrian quartzite and provides a classic “geologic museum” perspective of tilted fault-block mountains and the valley floor.
Late afternoon into sunset is widely regarded as the best light for photography and viewing, as the western position softens shadows across the valley (complementing the more famous east-side overlooks). Sunrise can also be excellent and quieter. The elevation makes it cooler than the valley floor, though summer heat is still a factor on the approach.
Practical Tips
- High-clearance vehicle strongly preferred; drive slowly and watch for rocks that can puncture tires. Carry a full-size spare, tools, extra water, and sun protection. There is no water or services on the road.
- Emigrant Canyon Road itself has vehicle-length restrictions in places (generally no vehicles over about 25 feet due to narrow, winding sections).
- Combine the drive with nearby sites such as the Wildrose Charcoal Kilns, Skidoo, or higher elevations toward Telescope Peak if road conditions and time allow.
- Always check the official NPS Death Valley alerts and road conditions page before your trip, as flash floods, snow, and maintenance can close sections with little notice.
This is a rewarding, relatively quiet alternative to the busier east-side viewpoints. The combination of mining history, a scenic dirt-road drive through the Panamints, and a sweeping high overlook of Death Valley makes it a classic west-side experience in the park.
Hummingbird Spring Road
Hummingbird Spring Road (access spur off the Wildrose/Mahogany Flat Road) in the Panamint Mountains of Death Valley National Park is a short, relatively straightforward high-clearance dirt spur that leads to a remote, unmarked historic trail to Hummingbird Spring.
Location and Access
The spur sits in the high country of the Panamint Range (western side of Death Valley National Park, Inyo County, California), near Piñon (or Pinon) Mesa, off the main road running from the Wildrose area toward Mahogany Flat / the Telescope Peak trailhead.
It is typically described as the first right turn when driving from the Wildrose area toward Mahogany Flat (consult a detailed map such as the National Geographic Death Valley map, as the turn is easy to miss and not signed as a major park road). The main approach routes are via Emigrant Canyon Road (from CA-190 near Emigrant) or Lower Wildrose / Trona-Wildrose Road (from the Panamint Valley side). Note that Lower Wildrose Road reopened in 2026 as an unpaved route limited to vehicles under 25 feet after major flood damage; conditions on the main Wildrose corridor can change with weather and repairs.
Hummingbird Spring itself is a named spring at roughly 7,300+ feet elevation on the Telescope Peak USGS topo map.
Road Character and Difficulty
- Length and surface: Short dirt/gravel spur. It is described as fairly straight until a sharp left turn, where a green marker post indicates the way toward the spring. Park near the marker and begin the hike from there.
- Vehicle requirements: High-clearance recommended (or required for comfort) to reach a proper trailhead parking spot. Lower-clearance vehicles can park along the main (paved or graded) Wildrose/Mahogany Flat road and walk the extra distance. It is not a long or highly technical 4WD route like some southern Panamint canyons (e.g., Warm Spring, Goler, or Mengel Pass approaches).
- Conditions: Typical high-desert dirt road—expect washboard, loose gravel, possible ruts or minor washouts after storms, and the usual remote-area lack of maintenance. The surrounding upper Wildrose / Mahogany Flat road system is steeper, narrower, and more demanding higher up (high-clearance often needed past the Charcoal Kilns; 4WD helpful when wet, snowy, or rutted). Snow and ice commonly close the higher sections in winter/early spring.
No detailed recent user trip reports specifically rate the spur as extremely rough; accounts treat it as a practical access road rather than a destination 4×4 trail.
The Destination: Trail and Spring
From the parking/marker area, an unmarked/faint trail (sometimes following an old road or wash) leads to the spring. Reported stats from visitors:
- Roughly 1.9–2 miles round-trip.
- ~850 feet elevation gain (one account); another notes a longer/higher approach involving up to ~1,800 feet of climbing through pinyon-juniper from a lower starting point on an old road to a former superintendent’s summer residence site, then continuing past wilderness boundary signs.
The route starts obvious, then enters a dry wash (best to stay in the wash). Historic evidence appears around 0.6 miles: rusted cans, a gypsum pile from past mining, and old water pipes that once carried spring flow down toward Wildrose Valley. The spring itself has been reported as a small, vegetation-covered trickle that soaks into the desert quickly rather than forming a large pool. Views from nearby ridges or high points look out over the surrounding terrain and valley.
The area is remote and quiet. One visitor noted the strong scent of pinyon pine, a hawk overhead, and excellent solitude. It is not shown on standard park service trail maps.
Practical Considerations and Hazards
- Remote and isolated: Cell service is typically nonexistent. If you drive the spur, your vehicle may not be visible from the main road—always leave a trip plan with someone.
- Weather and season: Best in spring, fall, or milder parts of summer/fall at this elevation (significantly cooler than the valley floor). Winter snow/ice can close access higher on the main road. Flash-flood risk exists in washes after storms.
- Water and resources: Carry all water; the spring flow is minimal and not a reliable drinking source without treatment. No facilities.
- Regulations: Standard Death Valley backcountry rules apply (Leave No Trace, wilderness boundary considerations). Check current NPS alerts for Wildrose/Mahogany Flat road status, as flood recovery has affected the corridor in recent years.
- Wildlife and history: Expect typical high-desert species; the spring historically supported people and mining activity in the Wildrose area.
Overall Assessment
Hummingbird Spring Road is a modest, functional high-clearance access spur rather than a challenging or scenic drive in its own right. Its value lies in providing quiet entry to a little-visited historic spring and short hike in the pinyon-juniper zone of the Panamints, with solitude and a sense of discovery that the more popular Telescope Peak or Charcoal Kilns areas lack. Drivers with high-clearance vehicles will find it straightforward in dry conditions; others can still reach the area by walking from the main road. Always verify current conditions via the official Death Valley NPS site before traveling, as desert roads change rapidly with weather.
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.