Etna, Nevada – Lincoln County Ghost Town

Etna, Nevada (Lincoln County) is a former railroad siding and small settlement in southeastern Nevada, now considered a ghost town or abandoned site. It lies in Rainbow Canyon (also associated with Meadow Valley Wash), north of the Narconon Rainbow Canyon Retreat along Nevada State Route 317, near coordinates 37°11′20″N 115°44′07″W and at an elevation of about 4,229 feet (1,289 m).
Prehistoric and Early Human Context
The area around Etna has evidence of long-term human occupation. Etna Cave (also historically known as Wheeler Cave), located nearby in a tributary canyon south of Caliente, is a significant archaeological site. It was excavated in the 1930s (primarily 1935–1937) by S.M. Wheeler under the Nevada State Park Commission.
The cave yielded stratified deposits showing multiple periods of use, including artifacts linked to earlier Great Basin cultures (sometimes classified under older terms like Gypsum Cave, Basketmaker, and Pueblo occupations in early reports). Recent studies have also documented rock art, including pictographs and petroglyphs at the site. This makes Etna Cave one of the first systematically studied archaeological locations in Lincoln County and an important reference for understanding prehistoric life in the region.
19th Century and Railroad Development
European-American activity in Lincoln County intensified in the mid-19th century with Mormon missionary and settler efforts (e.g., in nearby Meadow Valley/Panaca areas in the 1850s–1860s) and mining booms, such as at Pioche. However, Etna itself emerged later as part of railroad infrastructure.
Etna developed as a siding on the San Pedro, Los Angeles and Salt Lake Railroad (later part of the Union Pacific Railroad). The line was constructed through Rainbow Canyon between 1903 and 1905. Like many other small stops in the canyon (e.g., Carp, Stine, or Leith), it served operational needs such as passing sidings, section houses for track maintenance, and support for local ranches.
A 1912 newspaper reference mentions a section house at Etna being robbed, indicating some infrastructure and personnel were present in the early 20th century.
20th Century Settlement and Decline
In 1941, according to the Federal Writers’ Project, Etna had a population of 14, consisting of owners of the nearby Tennille (or Tenille) ranch. It functioned more as a small ranching-related community tied to the railroad rather than a mining boomtown.
The last occupants left in the late 1970s. The remaining residence was demolished in the early 1990s, leaving little visible above-ground structures today.
Significance and Current Status
Etna exemplifies the many minor railroad sidings that dotted Lincoln County’s rail lines, supporting transportation, ranching, and maintenance in a remote high-desert environment. Unlike prominent mining ghost towns, its history is modest and tied to infrastructure and agriculture. The proximity to Etna Cave adds archaeological value to the broader locale.
Today, the site is largely abandoned and fits the description of a ghost town. It is located in a scenic but arid canyon area, part of the broader historical landscape of Lincoln County, which includes Mormon settlement roots, mining districts, and the Union Pacific route. Visitors interested in history may find more to see at nearby sites like Caliente or through guided explorations of Rainbow Canyon rock art and railroad remnants.
Sand Springs Station, Nevada – Churchill County Ghost Town
Sand Springs Station, located in Churchill County, Nevada, is a historic site best known as a relay station on the Pony Express route. Its stone ruins represent a layered history of 19th-century western expansion, mail service, overland travel, and frontier life in the remote Great Basin desert. The site is one of the best-preserved Pony Express stations in Nevada, thanks to natural burial by sand and later archaeological efforts.
Location and Setting
The station lies approximately 20–26 miles east of Fallon along U.S. Route 50, at the entrance to the Sand Mountain Recreation Area (managed by the Bureau of Land Management). It sits near the base of Sand Mountain, a large dune complex formed from ancient Lake Lahontan sediments. The area is arid and windswept, with shifting sands that both challenged and preserved the site. The ruins occupy less than one acre and are accessible via a short interpretive trail from a parking area.
The name “Sand Springs” derives from a sand-filled summit with an emanating spring, though travelers often described the water as poor quality—thick, stale, and laden with sulphury salts that could blister the skin.
Early Exploration and Construction (1859–1860)
Army Lieutenant James H. Simpson surveyed the area in 1859 while exploring potential emigrant and mail routes across the Central Overland Trail. In early 1860, Bolivar Roberts, J.G. Kelly (sometimes spelled Kelley), and a small crew constructed the station using local stone. It served as Nevada Pony Express Station No. 26 (also associated with Mountain Well in some records). James McNaughton was the first station keeper before transitioning to a rider role.
The original Pony Express structure was relatively modest—roughly half the size of the final ruins. Built in phases, it included living quarters with a fireplace. The station provided a critical stop where riders could change horses, rest briefly, and continue the high-speed mail relay across the approximately 1,900-mile route from St. Joseph, Missouri, to Sacramento, California.
Pony Express Era (1860–1861)
The Pony Express operated from April 1860 to October 1861. Riders covered the full distance in about 10–12 days (longer in winter), relying on a network of roughly 30 stations in Nevada alone. Sand Springs served as a relay point for fresh mounts and minimal rest amid harsh desert conditions.
The service embodied frontier daring but proved short-lived and unprofitable. It ended when the transcontinental telegraph line was completed in October 1861, rendering the expensive pony relay obsolete.
British explorer and writer Sir Richard Burton visited on October 17, 1860 (while traveling by stagecoach). His vivid, unflattering description captured the station’s grim reality:
“Sand Springs deserved its name… the land is cumbered here and there with drifted ridges of the finest sand, sometimes 200 feet high and shifting before every gale… The water near this vile hole was thick and stale with sulphury salts: it blistered even the hands. The station-house was no unfit object in such a scene, roofless and chairless, filthy and squalid, with a smoky fire in one corner, and a table in the centre of an impure floor, the walls open to every wind, and the interior full of dust.”
Burton also noted the employees lounging about and a crippled rider injured by a horse fall. Despite the hardships, the station provided essential support along the route.
Later Uses (1860s–Late 1800s)
After the Pony Express folded, the site continued in service:
- As an overland stage station for passenger and freight lines.
- As a telegraph station (archaeological evidence includes insulators and resistor wire).
- In 1866, as a stop on the Fort Churchill and Sand Springs Toll Road, linking Dayton to the Reese River mining district near Austin.
The structure expanded over time with additional rooms (including a later addition that doubled the size). It eventually served as a home and corral for two prospectors. Artifacts from these periods include ox shoes, wagon parts, and even a ceramic item dated to 1896. Liquor bottle fragments were notably common, despite official bans on alcohol at stations.
The multi-phase construction and extended use explain why the ruins are larger than a typical short-lived Pony Express relay station.
Abandonment, Burial, and Rediscovery (Late 1800s–1970s)
After abandonment in the late 19th century, drifting sands from Sand Mountain buried the station, preserving the stone walls remarkably well for over a century. The site faded from view and memory.
In 1976–1977, Bureau of Land Management personnel and archaeologists from the University of Nevada, Reno rediscovered and excavated it. They uncovered artifacts, mapped the layout (including evidence of phased additions), and stabilized the dark stone walls. The excavation clarified the site’s history and resolved discrepancies with historical descriptions.
Preservation and Current Status
The ruins were listed on the National Register of Historic Places on November 21, 1980 (reference #80002465). They form part of the Pony Express National Historic Trail and are designated a National Park Service “Vanishing Treasure” site. Interpretive signs describe station life, the Pony Express, and the challenges of desert travel.
Today, visitors can walk a short loop trail (about 0.5 miles) to view the stabilized stone foundations and walls, including the smoky fireplace corner noted by Burton. The site offers scenic views of Sand Mountain. Rules prohibit climbing on or disturbing the ruins to prevent further deterioration. It remains a popular roadside stop for those traveling U.S. 50 (“The Loneliest Road in America”).
The Sand Springs Station encapsulates broader themes of American westward expansion: the ambition of rapid communication, the harsh realities of desert life, and the rapid technological shifts that made the Pony Express a brief but legendary chapter in U.S. history. Its survival through natural burial and careful excavation makes it a tangible link to Nevada’s frontier past.
For visitors in the Fallon area, the site pairs well with Sand Mountain Recreation Area (known for its booming sand dunes) and other nearby Pony Express or Overland Trail remnants. Always practice Leave No Trace principles to help preserve this historic resource.
The documentary record of Sand Springs gives evidence that the building was used as a telegraph station as well as a stage and pony express station, probably from the end of July 1861 until the line was discontinued. An 1868 survey o f Township 17N Range 32E, Section 31, on Fourmile Flat just west of the site, shows a telegraph line running on a course that would intercept Sand Springs station. The remnants o f the line can still be seen today, although it was removed from the sand dunes in the immediate vicinity of the building during the early part of this century (1979).
Archaeological evidence from Sand Springs also suggests that it was used for telegraphing. Two vulcanite fragments from Room 3 are part of a flange on a Goodyear’s “peg type” telegraph insulator popular during the 1850s. A third hard rubber artifact from Room 1 is probably also part of peg type insulator. In addition, several pieces of braided copper wire from Room 3 are from some kind of electrical equipment and most probably are from the resistor of a telegraph key.
-The Pony Express in Central Nevada, Donald L. Hardesty, BLM Nevada, 1979
References
Desert Dandelion ( Malocothryx glabrata )
The Desert Dandelion, also commonly known as Smooth Desertdandelion, is a striking annual wildflower native to the arid regions of western North America. It belongs to the sunflower family and is renowned for forming vibrant carpets of yellow blooms in sandy desert landscapes following wet winters. This report details its scientific taxonomy, plant and flower morphology, habitat, range, distribution, and ecological characteristics, drawing from botanical sources such as regional floras and field guides.

Scientific Taxonomy and Categorization
- Kingdom: Plantae
- Clade: Tracheophytes (vascular plants)
- Clade: Angiosperms (flowering plants)
- Clade: Eudicots
- Clade: Asterids
- Order: Asterales
- Family: Asteraceae (Aster or Sunflower Family) – characterized by composite flower heads and milky sap in many genera
- Genus: Malacothrix (Greek: “soft hair,” referring to the pappus on seeds)
- Species: Malacothrix glabrata (A. Gray ex D.C. Eaton) A. Gray
- Binomial Authority: Named by Asa Gray; the epithet “glabrata” refers to the nearly hairless (glabrous) leaves and stems.
- Synonyms: Malacothrix californica var. glabrata
- Common Names: Smooth Desertdandelion, Desert Dandelion
This dicotyledonous annual herb is categorized within the tribe Cichorieae (chicory tribe) of Asteraceae, featuring ligulate (strap-shaped ray) florets only, with no disk florets—distinguishing it from true dandelions (Taraxacum spp.).
Detailed Plant Description
Malacothrix glabrata is a low-growing to erect annual forb arising from a taproot. Plants reach 10–40 cm (4–16 inches) tall, with stems that are mostly glabrous (smooth), occasionally sparsely puberulent near the base, and branched proximally and distally. The stems may appear ascending or upright and contain milky latex sap, a hallmark of the Asteraceae family.
Leaves are primarily basal in a rosette, green, linear, and pinnately lobed with narrow, filiform (thread-like) or stringy segments (6.5–12.5 cm long). Cauline (stem) leaves are alternate, reduced upward, and similarly lobed. The foliage is nearly hairless, contributing to its “smooth” common name.
Detailed Flower Description
The inflorescences are solitary or 1–3 per stem, daisy-like composite heads measuring 2.5–6.5 cm (1–2.5 inches) wide (up to 4.5 cm or more). Each head consists of 31–139 ligulate ray florets (strap-shaped, 5-lobed at the tip) that are pale yellow to white, often with purple-tinged undersides. The receptacle is bristly, and the involucre (base) is campanulate to hemispheric, with 20–25+ phyllaries in 2–3 series and 12–20+ lanceolate bractlets with translucent margins at the base.
Immature or young flower heads often display a distinctive orange-to-red “button” or spot in the center (composed of developing structures). The flowers are fragrant and open primarily in the morning, closing by early afternoon. In mass blooms, they create showy yellow displays across the desert floor.

Fruit and Seeds
The fruit is a single-seeded cypsela (often called an achene), cylindro-fusiform (cylindrical and tapered at both ends), sometimes weakly 5-angled. It bears a pappus of soft hairs for wind dispersal. Seeds mature from March to June.
Habitat
This species thrives in coarse, fast-draining soils (gravel, loam, sand, silt) in open areas, among shrubs, or in vegetation gaps. Preferred habitats include sandy deserts, plains, mesas, rocky hillsides, washes, and flats, often associated with creosote bush (Larrea tridentata) communities. It also occurs in foothill woodlands and desert shrublands. Elevation range: below 2,000 m (6,500 ft). It is highly responsive to winter rainfall, becoming abundant in “good wildflower years.”
Range and Distribution
Malacothrix glabrata is native to the southwestern United States and northwestern Mexico. It occurs across the Mojave, Sonoran, and Great Basin Deserts.
U.S. States: Arizona (AZ), California (CA), Idaho (ID), Nevada (NV), New Mexico (NM), Oregon (OR), Utah (UT). Broader Range: Southwestern Idaho and eastern Oregon south to southern California, much of Arizona, and into Baja California and northwestern Mexico.
It is particularly common in the Mojave Desert (including areas near Las Vegas, Nevada) and intermountain regions. Sporadic records exist in the Colorado Plateau and Chihuahuan Desert fringes.
Ecology and Biology
As an annual, Malacothrix glabrata germinates in response to cool-season precipitation and completes its life cycle rapidly. Blooming occurs February–July (peak March–June), with fruits maturing soon after. It is primarily insect-pollinated (e.g., by solitary bees such as Nomadopsis spp.) but may be self-compatible. Seeds are wind-dispersed.
Ecologically, it serves as an important nectar source for butterflies, moths, bees, and other insects, and provides forage for wildlife including desert tortoises and small mammals. Indigenous groups (e.g., Apache) historically used roots medicinally. It is an indicator species for productive desert bloom seasons and shows no recognized subspecies or varieties. Chromosome number: 2n=14.
In summary, Malacothrix glabrata exemplifies desert adaptation with its ephemeral beauty, glabrous form, and reliance on sporadic rains. Its presence signals healthy desert ecosystems in the American Southwest.
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.

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.

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.

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.

