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

Purple Sand Verbena (Abronia angustifolia Greene)

Purple Sand Verbena (Abronia angustifolia Greene) is a member of the four o’clock family (Nyctaginaceae) and a distinctive annual (occasionally perennial) wildflower adapted to arid sandy environments in the southwestern United States and northern Mexico.

Purple Sand Verbena (Abronia angustifolia Greene) Photo by James L Rathbun
Purple Sand Verbena (Abronia angustifolia Greene) Photo by James L Rathbun

Scientific Taxonomy

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Order: Caryophyllales
  • Family: Nyctaginaceae (four o’clock family)
  • Genus: Abronia (sand-verbenas)
  • Species: Abronia angustifolia Greene (binomial name)

Synonyms: Abronia angustifolia var. arizonica, Abronia torreyi.

Description

Purple sand verbena is a low-growing herbaceous plant with decumbent to ascending, much-branched, elongate stems that are often reddish, glandular-pubescent, and viscid (sticky). Stems reach up to about 1 foot (30 cm) long. Leaves are opposite, with petioles 1–7 cm long and blades ovate-oblong to elliptic, measuring 1–5.5 × 0.7–3 cm; margins are entire to sinuate, often undulate, and infrequently shallowly lobed; both surfaces are viscid-pubescent. The plant forms sprawling mats or clumps suited to loose, sandy substrates. Fruits are broadly obdeltoid, scarious (dry and membranous), 5–10 × 4–8 mm, with 5 wings extending to or beyond a prominent beak and conspicuous dilations.

Blooms

Flowers appear in dense, rounded heads (inflorescences) 2 inches (≈5 cm) across, typically containing 10–30 individual flowers on peduncles longer than the subtending petioles. Each flower has a tubular perianth with a pink tube 10–20 mm long and a limb 6–8 mm in diameter ranging from bright magenta to pale pink (or infrequently pale rose). Bracts are lanceolate to oblong-lanceolate, papery, and glandular-pubescent. Blooms are conspicuous and ornamental, often described with shades that give the species its “purple” common name despite the primary pink-to-magenta palette. Flowering occurs from spring through fall (March–August or longer in favorable conditions). Like many Nyctaginaceae, the flowers are adapted for pollination by nocturnal insects such as moths and may open or become more fragrant in the evening.

Range and Habitat

Purple sand verbena is native to the southwestern United States (Arizona, New Mexico, Texas) and northern Mexico (Chihuahua, Coahuila). It grows at elevations of 300–1,300 m (1,000–4,300 ft) in sandy soils, desert scrub, prairies, plains, meadows, pastures, savannas, and woodland edges or openings. It prefers well-drained, dry sandy substrates and can tolerate full sun to part shade with low water requirements. Plants on gypsum flats (e.g., White Sands, New Mexico) may behave as perennials but often flower in their first season. It is not documented in Nevada or California.

This species is valued for its drought tolerance, showy flower heads, and ability to stabilize sandy soils. It is primarily propagated by seed and is suitable for ornamental use in rock gardens or native plantings in arid landscapes.

Ashford Mill Site

Ashford Mill Site is a historic mining ruin located in Death Valley National Park, California. It represents one of the many short-lived gold mining operations that dotted the region during the early 20th century, embodying the boom-and-bust cycles typical of desert prospecting in one of the harshest environments in North America.

Ashford Mill Ruins Sign.  Photo by James L Rathbun
Ashford Mill Ruins Sign. Photo by James L Rathbun

Location and Setting

The site lies on the valley floor along Badwater Road (California State Route 178), approximately 28 miles (45 km) west of the Shoshone entrance to the park. The associated Ashford Mine (also known as the Golden Treasure Mine) is located about 5 miles (8 km) east in the Black Mountains, roughly 3,500 feet (1,067 m) higher in elevation within Ashford Canyon. The mill was strategically placed on the valley floor to process ore trucked down from the mine. Today, visitors find concrete foundations, scattered debris from machinery, and the crumbling walls of a former office building. The site includes parking, picnic tables, scenic viewpoints, and vault toilets. Nearby Shoreline Butte displays ancient wave-cut terraces from the prehistoric Lake Manly.

Discovery and Claim Acquisition (1907–1910)

In January 1907, prospector Harold J. Ashford arrived in the Death Valley region, drawn by recent gold strikes at the nearby Desert Hound Mine. He noticed that the Keys Gold Mining Company had failed to perform required assessment work on several claims in the Black Mountains. Ashford relocated (re-staked) the claims under mining law and began working them. The Keys company did not discover the issue for nearly two years. In January 1910, they sued to reclaim the property, but a judge ruled in Ashford’s favor, securing title for him and his brothers, Henry and Lewis. The Ashfords worked the mine intermittently from 1910 to 1914 but achieved only modest results.

Ashford Mill, Death Valley National Park. Photo by James L Rathbun
Ashford Mill, Death Valley National Park. Photo by James L Rathbun

Development and Mill Construction (1914–1915)

In November 1914, the Ashford brothers leased the mine to wealthy Los Angeles residents B.W. McCausland and his son Ross. Under their leadership, the operation expanded dramatically. They drove a 180-foot tunnel, developed approximately 2,000 feet of underground workings, and employed up to 28 men at peak. The lessees invested over $125,000 in infrastructure, including construction of a 40-ton-capacity mill on the valley floor in 1915. The mill featured a jaw crusher, a 10-foot Lane mill, a Wilfley concentrating table, and a Diester slime table. Ore was trucked five miles down the mountain for processing before shipment to a smelter. The mill became operational by late August 1915. A popular (but unverified) local legend claims that a double shipment of cement arrived during construction; rather than return the excess, the McCauslands used it to build the durable concrete foundations and office that still stand today.

Operations, Decline, and Initial Closure (1915)

Despite extracting an estimated $100,000 worth of gold ore, the operation proved unprofitable. The ore grade was too low to cover the enormous costs of extraction, processing, and transportation across the remote desert terrain. Operations ceased in September 1915, only weeks after the mill opened. The McCauslands withheld lease payments, leading the Ashfords to file a lawsuit that yielded no compensation. The mill and mine then lay idle for more than a decade.

Intermittent Later Activity (1926–1941)

Brief revivals occurred over the following years. In 1926, four men worked the mine briefly before abandoning it again. In 1935, the Ashfords leased the property to Golden Treasure Mines, Inc., which reopened the mine and shipped high-grade ore to Shoshone via the Tonopah & Tidewater Railroad. High trucking costs limited profitability; total production through 1938 was valued at no more than $18,000. The Ashfords briefly operated the mine themselves in 1938, shipping 38 tons of ore. Later that year they leased it to Bernard Granville and Associates of Los Angeles, who installed a short aerial tramway to consolidate ore from scattered workings. The operation employed about 10 men but produced no recorded shipments and ceased by 1941. The Ashfords retained ownership but performed no further significant work. Over its entire history (1910–1941), the mine yielded just enough gold to sustain the brothers in basic supplies and legal fees.

Legends, Myths, and Cultural Significance

Early tourists were drawn by colorful legends surrounding the mine, including a story that the Ashford brothers sold it for $50,000 to a Hungarian count, who then resold it to B.W. McCausland for $105,000. An old wooden interpretive sign at the site perpetuated this tale for decades. However, National Park Service records describe these stories as more intriguing than factual. The site nonetheless symbolizes the persistent yet often futile quest for riches in Death Valley’s extreme environment.

Abandonment and Preservation

The mill was never reopened after 1915; its wooden walls, windows, and most machinery were removed or decayed over time, leaving only the concrete foundation and debris. The nearby office building survives as crumbling concrete ruins. The Ashford Mill Site was incorporated into Death Valley National Monument (later National Park) and is preserved today as a historic resource. The mine site higher in the canyon contains collapsed shacks, bunkhouses, headframes, and tramway remnants from the 1930s–1940s era, accessible via a strenuous hike up Ashford Canyon (the old road is washed out).

Visiting the Site Today

The Ashford Mill Site remains a popular roadside stop along Badwater Road. A short walk reveals the ruins and interpretive signage (the older legend-bearing sign may still be present). It offers a poignant reminder of the human ambition and environmental challenges that defined early 20th-century mining in the American Southwest. The site is open year-round, though summer heat and flash-flood risks in the canyon require caution. No artifacts should be disturbed, as the area is protected within the national park.

Desert Five-Spot (Eremalche rotundifolia)


The Desert Five-Spot (Eremalche rotundifolia) is a striking annual wildflower commonly observed in Death Valley National Park, particularly during favorable bloom years following sufficient winter rainfall.

Desert Five-Spot (Eremalche rotundifolia) - Photo by James L Rathbun
Desert Five-Spot (Eremalche rotundifolia) – Photo by James L Rathbun

Scientific Taxonomy

  • Kingdom: Plantae
  • Phylum: Tracheophyta (vascular plants)
  • Class: Magnoliopsida (dicotyledons)
  • Order: Malvales
  • Family: Malvaceae (mallow family, which includes hibiscus and cotton)
  • Genus: Eremalche
  • Species: Eremalche rotundifolia (A. Gray) Greene

This species is a dicotyledonous annual herb native to desert regions.

Description

The desert five-spot is a low-growing annual herb typically reaching 8–60 cm (3–24 inches) in height. It has an erect, sparsely branched stem (often simple or branched only at the base) covered in bristly hairs; stems are frequently reddish-brown. The leaves are distinctive: rounded to kidney-shaped (reniform), 1.5–6 cm broad, with toothed or crenate margins, and borne on long petioles. Leaves are green (sometimes with reddish phases) and covered in short bristly hairs.

The most striking feature is the flower: bisexual, cup- to globe-shaped, with five overlapping petals 15–30 mm long. Petals are rose-pink to lilac or purplish-pink, each featuring a prominent dark red-to-purple spot at the base that serves as a nectar guide for pollinators. When fully open, the petals curve slightly inward, forming a nearly spherical “lantern” shape (hence the occasional nickname “Chinese lantern flower”). The center reveals a ring of light pink stigmas surrounding smaller stamens. The calyx has 5 lobes, and three small bractlets subtend it. After flowering, the plant produces a schizocarp fruit that splits into 25–35 wafer-like segments.

Note on identification: Do not confuse it with the unrelated “five-spot” (Nemophila maculata), a white-flowered plant of the Sierra Nevada and foothills with purple spots at the petal tips.

Blooming Period and Behavior

The beautiful and delicate flower of the Desert Five Spot Flower.  - Photo by James L Rathbun
The beautiful and delicate flower of the Desert Five Spot Flower. – Photo by James L Rathbun

Flowering occurs primarily from March to May, with peak displays in the lower desert elevations from mid-February through mid-April, depending on winter rainfall. In Death Valley National Park, it is a signature wildflower during “superbloom” years (such as the notable events following heavy rains).

The flowers exhibit daily nyctinastic movement: they open in the morning (or midday) to reveal the vivid red spots and close at night or late afternoon. Leaves also show diurnal movement to optimize sunlight exposure. The red basal spots on each petal function as “runways” directing bees and other insects to the nectar at the flower base, aiding pollination. The plant thrives in years with adequate winter precipitation and is one of the more sought-after desert wildflowers for its vivid color contrast against the arid landscape.

Range and Distribution

Eremalche rotundifolia is native to the Mojave Desert and Colorado Desert (part of the Sonoran Desert region) in the southwestern United States and northwestern Mexico. It occurs in southeastern California (including Death Valley National Park and Anza-Borrego Desert State Park), southern Nevada, western Arizona, and extends slightly into Utah. In California it is found primarily in the Desert bioregion (excluding the high Desert Mountains). Elevation range is approximately -50 to 1,500 m (-164 to 4,921 ft), though it is most common between 50 and 1,200 m.

The closed flower of the Desert Five Spot Flower.  Photo by James L Rathbun
The closed flower of the Desert Five Spot Flower. Photo by James L Rathbun

Habitat and Ecology

This species prefers open, sunny sites in dry desert scrub, desert flats, sandy or rocky washes, alluvial fans, and open stony areas. It grows best in fast-draining, gravelly alkaline soils and is frequently associated with creosote bush scrub communities. In Death Valley National Park it appears on lower-elevation alluvial fans, foothills, and along roadsides (e.g., Badwater Road areas) following sufficient winter rains.

As an annual, it completes its life cycle quickly after winter rains, producing abundant seeds that remain dormant in the soil until the next favorable season. It provides nectar for native bees and supports larvae of certain butterflies and skippers (including confirmed hosts for Northern White-Skipper and Common Checkered-Skipper).

The desert five-spot is a beautiful and iconic Mojave Desert wildflower, particularly celebrated in Death Valley for its glowing pink blooms and striking red-spotted “lantern” flowers during spring displays. Its presence is highly dependent on winter precipitation, making it a highlight of rare superbloom events.

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.