Zabriskie Point

Zabriskie Point is a renowned scenic overlook and erosional landscape in Death Valley National Park, California, part of the Amargosa Range on the eastern side of the valley. It sits roughly 4–5 miles (about 6–8 km) southeast of Furnace Creek along California Highway 190, at coordinates approximately 36°25′12″N 116°48′40″W and an elevation of around 710–713 feet (216–217 m) above sea level.


The site is famous for its dramatic badlands: intricately eroded yellow, gold, brown, and rust-colored hills and ridges with almost no vegetation. The most prominent feature visible from the overlook is Manly Beacon, a high outcrop rising to about 823 feet (251 m), named for William L. Manly (one of the “Forty-niners” who helped guide stranded emigrants out of Death Valley during the 1849–1850 California Gold Rush). Distant views often include the valley’s salt flats and the Panamint Mountains to the west. A short paved walk (about ¼ mile / 400 m) leads from the parking area to the viewpoint; trails such as the Badlands Loop also begin nearby.

Zabriskie Point bathed in warm afternoon light in Death Valley National Park - Photo by James L Rathbun
Zabriskie Point bathed in warm afternoon light in Death Valley National Park – Photo by James L Rathbun

Geology

The landscape is older than modern Death Valley itself. Millions of years before the current valley formed and Lake Manly existed, a prehistoric lake known as Furnace Creek Lake occupied the area (beginning roughly 9 million years ago). Over several million years, sediments—saline muds, gravels from nearby mountains, and ashfalls from the then-active Black Mountain volcanic field—accumulated on the lake bottom, forming what is now called the Furnace Creek Formation (mudstones, siltstones, and related deposits).

Around 5 million years ago the lake dried up. Later tectonic activity—widening and sinking of Death Valley plus uplift of the Black Mountains—tilted the sediments. Rare but intense rains then carved the soft rocks into the intricate badlands seen today. Darker lava caps from eruptions 3–5 million years ago resist erosion in places and help explain why Manly Beacon stands higher than surrounding ridges. The primary source of borate minerals historically mined in the area is also the Furnace Creek Formation.

History and Namesake

The point is named for Christian Brevoort Zabriskie (1864–1936). Born October 16, 1864, at Fort Bridger, Wyoming Territory (where his father was stationed), he worked early as a telegrapher for the Virginia & Truckee Railroad in Carson City, Nevada, and held various jobs in Nevada mining towns (including banking and even a partnership in a mortuary).

In 1885 he was hired by Francis “Borax” Smith to supervise Chinese laborers for the Pacific Coast Borax Company near Candelaria, Nevada. He rose to become vice president and general manager, serving about 36 years until retiring in 1933. Under his tenure the company expanded operations into Death Valley (famous for its 20-mule-team borax transport) and later other sites. The overlook itself was developed by the Pacific Coast Borax Company in the late 1920s as a roadside stop for automobile visitors to view Manly Beacon and the badlands, well before the area became Death Valley National Monument in 1933 (later a national park). Zabriskie died on February 8, 1936.

Zabriskie Point - Photo by James L Rathbun
Zabriskie Point – Photo by James L Rathbun

Role in Popular Culture

Zabriskie Point has long attracted artists, filmmakers, and photographers for its otherworldly appearance.

Michelangelo Antonioni’s 1970 film Zabriskie Point takes its title from the location. Key scenes, including a lengthy desert sequence with the protagonists and a surreal, choreographed group of bodies in the dunes (sometimes called the “orgy” scene), were shot there. The film was a commercial and critical failure on release but later gained cult status for its cinematography, countercultural themes, and soundtrack (featuring Pink Floyd and others).

The cover of The Joshua Tree by U2 was taken in Death Valley - photograph by Anton Corbijn
The cover of The Joshua Tree by U2 was taken in Death Valley – photograph by Anton Corbijn

U2’s 1987 album The Joshua Tree is closely linked to the site. In December 1986, photographer Anton Corbijn and the band (along with designer Steve Averill) drove through the California desert seeking images that captured themes of America, the desert, and a sense of displacement. The iconic black-and-white cover photograph of the four band members was taken at Zabriskie Point. The landscape’s stark, cinematic quality suited the album’s widescreen aesthetic; the actual lone Joshua tree that appears in other photos (and inspired the title) was found nearby along Highway 190, not in Joshua Tree National Park (which is more than 200 miles away). Working titles had included “The Two Americas” and “The Desert Songs”; the final name came after Corbijn recounted the Mormon settlers’ association of the tree’s form with the biblical Joshua. The shoot was brief and cold; the band’s serious expressions partly reflected the freezing conditions.

The location continues to draw visitors, photographers, and fans of the album, and it has appeared in other media (including later television productions). Its combination of geological drama, mining-era history, and cultural associations makes it one of Death Valley’s most iconic and photographed viewpoints, especially at sunrise and sunset when the colors of the badlands are most vivid.

Zabriskie Point Map

References

Back County Camping in Death Valley National Park

Primitive backcountry camping in Death Valley National Park offers profound solitude amid vast desert landscapes, with few other people, excellent wildlife viewing, and some of the darkest night skies in the United States.

Homestake, Death Valley
Homestake, Death Valley

Death Valley encompasses more than 3 million acres of designated wilderness (over 93% of the park). Away from developed areas and popular roads, campers often experience true isolation—nights without the sounds or lights of other visitors, under an immense canopy of stars. The park is an International Dark Sky Park (Gold Tier level), with exceptionally clear, dry air and minimal light pollution. On moonless nights the Milky Way can stretch horizon to horizon, and celestial objects invisible from most urban or suburban locations become visible. Backcountry locations far from Furnace Creek or Stovepipe Wells provide the darkest viewing.

Wildlife viewing opportunities arise from the park’s surprising diversity of habitats—colorful badlands, canyons, alluvial fans, springs, and higher-elevation woodlands. Desert bighorn sheep, coyotes, kit foxes, lizards, snakes, birds, and smaller mammals inhabit the area. Springs and water sources are critical for wildlife; camping near them is restricted to protect these fragile habitats. Visitors should never feed or approach animals.

NPS Directives on Campsite Locations, Campfires, Water, and Related Rules

Campsite locations

  • Dispersed (backcountry) camping is generally allowed at least one mile from any paved road, developed area, or “day-use only” dirt road.
  • Roadside (vehicle-accessible) camping along many dirt roads is permitted only in previously disturbed areas immediately adjacent to the roadway (vehicles must stay on designated roads; off-road driving is prohibited). The wilderness boundary typically begins 50 feet from the centerline of most dirt roads.
  • Certain popular corridors (Echo Canyon, Hole in the Wall, Cottonwood Canyon/Marble Canyon, and Greenwater Valley/Furnace Creek Wash) require mandatory paid permits ($10/night) for designated or limited dispersed roadside sites; these are reserved online via Recreation.gov up to six months in advance. Overnight backpacking in those corridors is allowed farther than one mile from the road centerline.
  • All other roadside camping, backpacking, or canyoneering is free and permits are recommended (not mandatory); obtain them at Furnace Creek Visitor Center, Stovepipe Wells Ranger Station, the self-service drop box, or online.
  • Prohibited areas include: the valley floor from Ashford Mill north to the Mesquite Flat Sand Dunes; Eureka and Mesquite Flat Sand Dunes; within one mile of Greenwater Canyon or Darwin Falls Trail; many “day-use only” roads (Titus Canyon, Mosaic Canyon, West Side Road, Wildrose Road, Skidoo Road, Aguereberry Point Road, first 8 miles of Cottonwood Canyon Road, etc.); and near certain historic mining sites.
  • Camp at least 100 feet from any flowing stream, spring, or natural body of water (some older guidance references 100–200 yards; follow the stricter current rule).
  • Group size is limited to 12 people and no more than 4 vehicles; larger groups must split up and camp/travel at least ½ mile apart.
  • Maximum stay is generally 30 days per calendar year (some developed sites have shorter limits). Camp only in previously disturbed spots where possible and practice Leave No Trace.

Campfires

  • Traditional campfires (wood or charcoal that contact the ground) are not allowed in the backcountry.
  • Portable gas stoves are permitted.
  • Fire pans or other fireproof barriers that keep the fire completely off the natural surface are allowed in many areas (below 3,000 feet year-round; above 3,000 feet only from approximately September 16 to June 14). Wood gathering is prohibited; all ash and unburned material must be packed out. Check current fire restrictions, as they can change.
  • In designated primitive campgrounds (e.g., Wildrose area), fires may be restricted or limited to provided grates during high-fire-danger periods.

Water and other essentials

  • There is no potable water in the backcountry. Natural springs are unreliable, often dry, and can be contaminated (e.g., by wildlife or other sources). Carry all the water you will need—commonly one gallon or more per person per day in hot weather—or carefully cache it in advance. Purify any backcountry water before drinking.
  • Pack out all trash, leftover food, and (in many situations) human waste. Bury human waste at least 6 inches deep and 200 feet from water sources; pack out toilet paper.
  • Pets are restricted: they are not allowed on trails or in wilderness areas and must stay within 50 feet of roads or developed areas.
  • Cell service is nonexistent in most of the park. Self-reliance is essential—carry extra food, water, spare tires/repair kits, maps, and a communication plan. High-clearance (and often 4WD) vehicles are required for most backcountry roads.

Primitive backcountry camping here rewards careful preparation with solitude, wildlife encounters, and unparalleled night skies. Always check current conditions, road status, and regulations on the official NPS Death Valley website (nps.gov/deva) before your trip, as rules and access can change with weather, fire danger, or management needs.

Schwab California

Schwab, also spelled Schwaub, was a short-lived gold mining camp and ghost town in Inyo County, California, situated in the Funeral Mountains on the eastern edge of Death Valley. Located approximately 12 miles north of Ryan at an elevation of 3,389 feet (1,033 m), the townsite lies in Echo Canyon within the Echo-Lee Mining District. Today, it is a largely abandoned site within or near Death Valley National Park, accessible via desert roads best traveled in winter. Little remains beyond scattered ruins, leveled tent sites, piles of rusted tin cans, broken glass, and remnants of the nearby Stray Horse (or Inyo) Mine.

Schwab, California - “In the afternoon the townsite company drinks tea,” Death Valley Chuck-Walla magazine, Vol 2. No. 1, June 1907
Schwab, California – “In the afternoon the townsite company drinks tea,” Death Valley Chuck-Walla magazine, Vol 2. No. 1, June 1907

Founding and Early Development (1905–1906)

The town originated during the intense mining boom that swept the Death Valley region following the 1904 gold strike at Rhyolite, Nevada. Prospectors fanned out in search of extensions of the rich Bullfrog District deposits, including rumored lost mines like the Breyfogle. In January 1905, Mormon prospectors Chet Leavitt and Moroni Hicks discovered a promising quartz ledge known as the Stray Horse in Echo Canyon on the west side of the Funeral Range. Initial assays were disappointing, but a richer vein higher up led them to stake over 20 claims, including the Inyo Mine. They formed the Inyo Gold Mining Company with investors from Provo, Utah.

By late 1905—around Christmas—the townsite began to take shape down Echo Canyon. It was named Schwab in honor of Charles M. Schwab, the prominent American steel magnate (not to be confused with the later financier Charles R. Schwab). Schwab had invested heavily in regional mining ventures, including the nearby Skibo Mining Company (named after his Scottish castle) and claims resembling Rhyolite’s lucrative Montgomery-Shoshone Mine. The townsite was laid out just below the Skibo mine to support workers. Construction accelerated in early 1907, with supplies—including five boxcars of tents and equipment—shipped by rail to the area. A post office opened on March 18, 1907, with Eugene P. Houtz as postmaster (it closed permanently on August 15, 1907).

At its peak, Schwab supported a modest population of around 200 people. It featured basic services: a blacksmith shop, boarding house, general store, bakery, restaurant, and at least one saloon (housed in a tent). Infrastructure included a telephone line connected to Rhyolite via the Lee and Echo camps and a daily stage line. The Echo Miners Union provided some labor organization. The nearby Stray Horse/Inyo Mine served as the economic anchor, though the town primarily functioned as a supply and housing hub for the broader Echo-Lee District.

Unique Governance: The “Women of Schwab” (1907)

One of the most distinctive aspects of Schwab was its ownership and promotion by women—an unusual occurrence in the rough-and-tumble mining camps of the American West. The townsite company was taken over by three women: Gertrude Fesler (a young stockbroker from Chicago who had moved to Rhyolite to broker mining deals), Mrs. F.W. Dunn (of San Bernardino, who received her husband’s interest), and Helen H. Black (who bought out her husband’s share). They marketed the camp with promotional materials proclaiming it “A Mining Camp Built by Ladies: One of the Most Unique Wonders of the New West.” Contemporary newspapers, such as The Bullfrog Miner (March 1907) and Death Valley Chuck-Walla (June 1907), highlighted the novelty of women running a mining town, noting details like the owners drinking afternoon tea in the main tent.

The women reportedly enforced a “respectable” moral code, driving out saloons, gambling, and prostitution. Some contemporary and later accounts (including historian Lingenfelter) suggested this “dry” policy caused most of the male population to leave, accelerating the town’s collapse. However, archaeological evidence—such as beer and wine bottles, champagne bottle caps (agraffes), and dumps near the main tent—indicates that drinking persisted to some degree. Historians now emphasize that economic and logistical factors were the primary drivers of decline, not moral reforms.

Decline and Abandonment (1907 Onward)

Schwab’s boom was brief and fragile, mirroring the fate of many Death Valley mining camps. The Financial Panic of 1907 devastated regional mining investments, including those tied to Charles M. Schwab. Ore quality proved inconsistent, and Schwab’s location was disadvantaged: it depended on the more accessible Lee Camp for shipments, assays, and transport, with no direct route for miners. Most operations in the Echo-Lee District shut down, except for Lee Camp itself (which benefited from rail access). By August 1907, the post office closed, businesses folded, and the town rapidly emptied. Supplies were hauled away, leaving behind tent bases, wooden cellars, and debris.

The Inyo Gold Mining Company continued intermittent operations at the mine into the 1920s–1940s, but the townsite itself was abandoned within a year of its founding. Some later activity occurred after 1928, but Schwab never revived as a community.

Legacy and Current Status

Today, Schwab is a classic California ghost town with minimal visible structures—primarily scattered ruins, mine tailings, and historical debris in Echo Canyon. The Stray Horse/Inyo Mine workings remain, though they are often confused with the townsite itself. Two wooden crosses mark possible graves, one labeled “A Death Valley Victim – 1907.” The site offers a glimpse into the fleeting 1905–1907 mining excitement in Death Valley and stands as a reminder of the boom-and-bust cycle driven by speculation, distant capital (like Schwab’s investments), and harsh desert conditions.

Schwab’s story highlights the role of women in Western mining towns, the broader Death Valley gold rush, and the economic vulnerabilities of early 20th-century prospecting. It remains a point of interest for hikers, historians, and visitors to Death Valley National Park, though it lacks the dramatic intact buildings of better-known sites like Bodie or Rhyolite.

The town of Schwab is situated just below the Inyo and Skibo camps at the junction of the wagon roads leading up the east arm of Echo canyon and to Death Valley on the south. In other words, Schwab is located in the north or upper branch of Echo Canyon, astride the main Echo-Lee wagon road, across a small ridge from the present Inyo ruins, and about 1-1/2 miles from those ruins. At this location, evidence of the old townsite may be found.

The remains consist of seven leveled tent sites, some with ow and crude stone retaining walls remaining. More tent sites were once present, but have been erased by high water in the adjacent wash during Death Valley’s infrequent but violent flash floods. Two of the tent sites have eroded cellars behind them, about ten feet square and five feet deep. Since an immense pile of broken 1900 to 1910-dated beer bottles is located directly behind one of these tent-cellar sites, it is safe to say that this was the tent saloon, where once twenty-nine men were counted drinking at one time. The townsite covers several hundred feet along the-shallow wash which marks the northern branch of Echo Canyon, and remains are mostly restricted to the west side of that wash On the east side, however, is another tent location, and a shallow, unmarked grave, a lonely monument to one prospector who ended his days during the brief life of Schwab. About 300 yards to the west of the townsite is a crude derrick, the remains of Schwab’s well. The well site is dry and completely filled in, but numerous five gallon cans are scattered along the trail from the well to the townsite.

Rhyolite Herald of 22 February 1907.

Town Summary

NameSchwab, California
LocationDeath Valley National Park, California
Latitude, Longitude36.505, -116.7236
Elevation3,340 feet
Population200
Post Office

Schwab Map

References

Pebble Pincusion (Chaenactis carphoclinia)

Scientific Name: Chaenactis carphoclinia A. Gray (primarily var. carphoclinia in Death Valley and most of its range)

Pebble Pincusion (Chaenactis carphoclinia) Found near Ashford Mill, Death Valley National Park.  Photo Heather Rathbun
Pebble Pincusion (Chaenactis carphoclinia) Found near Ashford Mill, Death Valley National Park. Photo Heather Rathbun

Scientific Taxonomy

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Clade: Asterids
  • Order: Asterales
  • Family: Asteraceae (Sunflower or Daisy family)
  • Genus:Chaenactis (pincushions or dustymaidens)
  • Species:Chaenactis carphoclinia A. Gray

Common names include Pebble Pincushion, Pincushion Flower, and Straw-bed Pincushion. Two varieties exist: the widespread var. carphoclinia (smaller plant, common in Death Valley) and the rarer var. peirsonii (larger, limited to southern California’s Santa Rosa Mountains).

Description

Pebble Pincushion is a native annual forb/herb that grows from an erect, branching stem (usually one main stem) reaching 4–16 inches (10–40 cm) tall, occasionally up to 2 feet (60 cm) in favorable conditions. The stems are whitish-pubescent (hairy).

Leaves are green, mostly linear, and pinnately dissected or lobed (basal leaves highly divided and wither early; cauline leaves smaller with slender petioles), up to 4–10 cm long.

The inflorescence consists of 1–several small discoid flower heads (no ray flowers) per stem, each 0.25–1 cm wide. Heads feature white to pinkish-tinted disk florets with enlarged outer corollas and prominently exserted (protruding) anthers. Flat, sharp-pointed phyllaries (bracts) line the heads and often appear reddish. The fruit is a small achene tipped with a scaly pappus.

The plant resembles other desert Chaenactis species (e.g., Esteve’s Pincushion), but is generally smaller with multiple cream-to-white heads per stem.

Blooms

As a desert annual, Pebble Pincushion germinates after winter rains and blooms primarily in spring (January/February/March through May or June, depending on elevation and rainfall). In Death Valley, it is a signature species during “superbloom” years, often peaking in March–April alongside other desert annuals. The flowers are visited by bees, butterflies, and other small insects for nectar and pollen.

Range and Habitat

Pebble Pincushion is native to the southwestern United States and northwestern Mexico. Its range spans Arizona, California, Nevada, New Mexico, Utah, Baja California, and Sonora—primarily in the Mojave Desert, with extensions into the Sonoran Desert, southern Great Basin, and northwestern Chihuahuan Desert. Elevations range from 300–6,200 feet (90–1,900 m).

It thrives in rocky, gravelly, or sandy soils, including washes, open plains, mesas, slopes, and flats within desert shrublands. In Death Valley National Park, it is commonly found in gravelly washes and rocky areas (e.g., near Emigrant Pass, Badwater, and Mosaic Canyon), where it can form dense displays after sufficient winter precipitation. Seeds may be consumed by birds, small mammals, and desert tortoises.

Pebble Pincushion growing in typical Death Valley habitat—gravelly washes with mixed desert annuals under clear desert skies.

This hardy annual plays a key role in desert ecosystems as a quick-response bloomer that stabilizes soil and supports pollinators and wildlife following rainy periods.

Panamint City California – Inyo County Ghost Town

Panamint City is one of the most legendary ghost towns in the Panamint Range of Death Valley National Park, California. Perched high in Surprise Canyon at an elevation of around 6,000–6,500 feet (about 1,800–2,000 m), it was once a notorious silver boomtown known for its lawlessness, rapid rise, and swift decline. Today, the site lies in a remote, rugged wilderness area within the park (though some remnants are on private inholdings or patented claims).

Panamint City California - 1875
Panamint City California – 1875

Historical Background and Founding (1872–1873)

The story of Panamint City begins in late 1872 amid the chaotic aftermath of earlier California gold and silver rushes. Prospectors William L. Kennedy, Robert Polk Stewart, and Richard C. Jacobs (some accounts name them as William Ledlie Kennedy et al.) were searching for the fabled Lost Gunsight Mine (a legendary lost gold deposit tied to early Death Valley lore) when they stumbled upon rich silver outcrops in Surprise Canyon. The canyon’s isolation had long made it a favorite hideout for outlaws evading law enforcement after stagecoach robberies and other crimes.

When the prospectors returned to stake formal claims, a gang of six bandits (who had followed them) forced a partnership to share in the profits—despite the outlaws being wanted for crimes like robbing a Wells Fargo stage of $12,000. This unlikely alliance marked the birth of the Panamint Mining District, officially formed in February 1873. Ore samples sent to Los Angeles attracted attention, and word spread quickly.

Senator John Percival Jones
Senator John Percival Jones

Boom Period (1873–1875)

The real boom ignited when Nevada’s “Silver Senators”—John P. Jones and William M. Stewart (prominent Comstock Lode investors)—learned of the discoveries. They organized the Panamint Mining Company with $2 million in capital stock and bought up major claims, injecting serious investment. By late 1874, Panamint City exploded into a full-fledged town:

  • Population peaked at around 1,500–2,000 residents, including miners, merchants, saloonkeepers, prostitutes, gamblers, and outlaws.
  • The main street stretched nearly one mile up the narrow canyon, lined with wooden buildings: hotels, restaurants, stores, assay offices, two banks, a post office, and the Panamint News newspaper.
  • Saloons and a red-light district thrived, contributing to the town’s reputation as one of the “toughest, rawest, most hard-boiled little hellholes” in the West.
  • Lawlessness was rampant—reports claim over 50 murders in the first few years, with shootouts, claim-jumping, and vigilante justice common. Wells Fargo refused to operate a stage line due to the banditry; instead, bullion was cast into heavy 400-pound cubes to deter theft during transport.
  • Key mines included the Wyoming Mine, Wonder Mine, and others producing high-grade silver ore (some assays showed values in the thousands of dollars per ton), along with copper and lesser gold.

The town even inspired ambitious infrastructure plans, such as Senator Jones’ short-lived railroad project from Santa Monica (which never fully materialized beyond initial segments).

William M. Stewart. Photo by Matthew Brady
William M. Stewart. Photo by Matthew Brady

Decline and Abandonment (1875–1877)

The bust came as quickly as the boom. By late 1875, the richest surface and near-surface ore bodies in the major mines began depleting rapidly. Veins pinched out or became too low-grade to process profitably with 1870s technology. Investors pulled out, and production plummeted.

A catastrophic flash flood in 1876 roared down Surprise Canyon, washing away much of the lower town, destroying buildings, roads, and equipment. This disaster accelerated the exodus. By 1877, major operations shut down entirely, and Panamint City was largely abandoned. Scavengers and a few holdouts lingered briefly, but the population evaporated within months.

Later History and Remnants

The site is protected; visitors must hike and plan trips carefully (flash flood risk remains high). Sporadic small-scale prospecting occurred in the early 20th century, but nothing revived the town. The area saw renewed minor activity during later Panamint Range booms (e.g., gold at nearby Skidoo in 1905–1917), but Panamint City itself remained a ghost town.

In the mid-20th century, some structures were salvaged or burned; flash floods continued to erode the site.

Today, within Death Valley National Park (established 1994, expanded to include the Panamint Range), remnants include:

  • Foundation stones and walls of former buildings.
  • Mine adits, shafts, and tailings piles.
  • The old smelter stack base and scattered artifacts.
Panamint City Stamp Mill
Panamint City Stamp Mill

Panamint City exemplifies the classic Western mining boom-bust cycle: fueled by rich silver discoveries, hyped by big investors, plagued by lawlessness and isolation, and doomed by ore depletion and natural disaster. Its brief, violent heyday left an enduring legend in Death Valley lore—one of outlaws turning prospectors, senators chasing silver, and a canyon that swallowed a town almost as fast as it rose.

Panamint Town Summary

NamePanamint
LocationInyo County
Latitude, Longitude36.1182827, -117.0953327
GNIS1661185
Elevation6,300 Feet
NewspaperPanamint News ( 1874-1875 )

Panamint Map

References