Bonnie Claire Nevada – A Nye County Ghost Town

Bonnie Claire (sometimes spelled Bonnie Clare) is a historic ghost town in Nye County, Nevada, situated on the edge of Sarcobatus Flat along Nevada State Route 267, approximately 40 miles north of Beatty and near the California border. At an elevation of about 3,980–3,950 feet, the site lies in a remote desert landscape characterized by dry lake beds, sparse vegetation, and proximity to Gold Mountain (roughly six miles northwest). Once a small mining and railroad hub supporting gold and silver operations, Bonnie Claire experienced a brief boom in the early 20th century before fading into abandonment. Today, it consists primarily of decaying mill ruins, scattered building foundations, railroad beds, and a small cemetery, offering a glimpse into Nevada’s mining past.

Long Team in front of the Bonnie Claire Mine, Nevada
Long Team in front of the Bonnie Claire Mine, Nevada

Early Settlement and Mining Origins (1880s–1905)

Gold mining began in the region in the 1880s on the south side of Gold Mountain. Ore from mines such as the Rattlesnake was hauled by mule teams to a five-stamp mill constructed by Guy Thorpe at a site known as Thorp’s Wells (or Thorp’s Well; also briefly called Montana Station). This mill processed ore for about two decades and supported a modest camp. A small stage station developed at Thorp, serving overland traffic between emerging mining districts like Goldfield and Bullfrog.

In 1904, the Bonnie Clare Bullfrog Mining & Milling Company acquired the original mill and constructed a new facility—the Bonnie Clare Mill—near the stage station to handle ore from across the district. A small camp formed around the mill, and a post office opened on June 15, 1905, under the name Thorp. These developments laid the foundation for growth, though activity remained limited until railroads arrived.

Boom Period and Railroad Era (1906–1910s)

The town’s peak began in September 1906 when the Bullfrog-Goldfield Railroad reached Thorp, establishing a station initially called Montana Station. Residents disliked the name and platted a new townsite in October 1906, officially renaming it Bonnie Clare. The Las Vegas & Tonopah Railroad arrived in spring 1907, constructing an impressive two-story depot. These rail connections transformed Bonnie Clare into a supply and milling center.

At its height, the town featured a railroad depot, mercantile stores, saloons, and a population estimated at around 100–250 residents. It served as a junction and siding for ore shipments and supplies. The post office name officially changed to Bonnie Clare on July 13, 1909. A brief 1910 renovation of the mill by the New Bonnie Clare Mining Company and further milling efforts (such as the 1913 Jumbo Extraction Company mill at Thorp’s Well, later operated by the Quigley Reduction Company) provided temporary support, but ore supplies from nearby mines dwindled.

Decline and Transition (1910s–1930s)

Mining activity declined sharply by 1909–1914 as local gold and silver deposits played out. Railroad consolidation in 1914 (merging operations of the Bullfrog-Goldfield and Las Vegas & Tonopah lines) reduced service, with only limited freight continuing. The railroads ultimately ceased operations around 1928, and tracks were later salvaged. The post office closed on December 31, 1931, when only two residents remained.

In the 1920s, Bonnie Claire experienced a modest revival as a supply point for the construction of Scotty’s Castle (Death Valley Ranch) in Death Valley, about 20 miles to the southwest. Building materials were unloaded here and transported onward.

Later Revivals and Final Operations (1940s–1950s)

Sporadic activity occurred between 1940 and 1954, including minor mining and a short-lived cyanide mill in 1940. In December 1951, George Lippincott of the Sun Battery and Nic-Silver Battery Companies (later associated with the Lippincott Lead Company) constructed a lead mill and smelter at the site of the old Bonnie Clare Mill. It processed lead-silver ore trucked from Death Valley mines (such as the Lead King Mine in the Panamint Range), operating at up to 100 tons per day starting in February 1952. The facility included a diesel power plant, worker quarters, and related infrastructure but lasted only a few years until the ore was depleted. A brief reopening was reported in 1955, after which the site was fully abandoned.

Additional infrastructure from this era included temporary use by highway reconstruction crews in 1951 and a Civil Aeronautics Authority airport (Scotty’s Intermediate Field/Bonnie Claire Airport) built circa 1943 nearby, which was later abandoned.

Current Status and Legacy

Bonnie Claire has remained a ghost town since the mid-1950s, with visible ruins including stone and concrete mill foundations, a leaning steel-frame structure, tailing piles, metal tanks, crucibles, and scattered residential remnants (such as the Huson House and stone buildings). A small cemetery contains graves from the early 20th century. The site is easily accessible via a short unpaved spur off NV-267 and attracts occasional visitors, historians, and off-road enthusiasts. In 2005, Tonogold Resources announced plans for the “Bonnie Claire Gold Tailings Project” to rework historic mill tailings, though large-scale revival did not materialize.

The town’s story exemplifies the boom-and-bust cycle of Nevada’s desert mining camps: rapid growth fueled by railroads and mineral strikes, followed by swift decline once resources and transportation waned. Its ruins stand as a testament to the Gold Mountain mining district and the interconnected rail networks that once linked remote Nevada outposts. Coordinates for the site are approximately 37°13’37.7″N 117°07’15.6″W.

Bonnie Claire Trail Map

Salt Wells, Nevada – Churchill County Ghost Town

Salt Wells, Nevada, is a historic site and former locale in Churchill County, located on the northern edge of the Salt Wells Marsh (also known as part of the Carson Sink region) approximately 15 miles east/southeast of Fallon along U.S. Highway 50. Situated near Sand Mountain at an elevation of about 3,888 feet, it lies in a remote, arid Great Basin environment characterized by alkali flats, playas, and geothermal features.

The area derives its name from natural salt wells and saline deposits, which have been noted since the mid-19th century. While not a major Pony Express station like nearby Cold Springs or Sand Springs, some historical lists associate a “Stillwater / Salt Well” or similar designation with the broader Stillwater dogleg route variant of the Pony Express (1860–1861) in Churchill County. However, Salt Wells itself gained prominence later for mineral extraction and as a transportation waypoint rather than as a primary relay during the mail service’s brief operation.

Early Mineral Development: Salt and Borax (1860s–1870s)

In the 1860s, rich saline deposits and salt wells were recognized in the area, with early accounts describing thick, high-purity salt formations suitable for table use and mining. Captains Mead, Dickson, and Judge Byran reportedly held interests and planned commercial production once regional Indian conflicts subsided. Salt from the marsh was harvested and shipped, contributing to local resources amid the Comstock Lode boom and other Nevada mining districts.

Borax (borate of soda) became the site’s most notable early industry. In 1870, William Throop discovered surface deposits of borax at the western edge of what was then called Alkali Valley. That same year, the American Borax Company erected borax works. A smaller additional plant followed in 1871. Operations focused on surface crusts in a low-lying flat about 1–1.5 miles southeast of the main wells, where borax content ranged from 10% to as high as 30% across roughly 400 acres. Workers harvested the material, which naturally reformed after extraction, and processed it using basic boiling and crystallizing methods before shipping crude product to San Francisco for refining.

Production reached 20 tons per month at one point, and by 1872–1873 multiple companies were active, yielding 70–80 tons annually valued at $400–$450 per ton. Contemporary reports described the transformation of a once “sterile” alkali flat into a bustling site with chimneys, steam whistles, and expanded milling capacity. Despite initial promise, the operations proved short-lived due to the relatively low grade of the deposit, market conditions, and competition from richer California borax fields. The works shut down within a few years. Remnants today include scattered corroded metal, glass, wood, a possible unloading ramp, and fragments of processing pans—modest traces of this early industrial effort.

20th Century: Water Stop, Roadside Services, and Later Uses

Salt Wells saw renewed activity in the early 1900s following the 1905 silver discovery at Fairview (to the southeast in Churchill/Nye counties). It functioned as a practical water stop for freight wagons and stagecoaches traveling between Fairview and Fallon, supporting mining supply lines in the arid terrain.

As automobile travel grew along the evolving Lincoln Highway and modern U.S. 50, roadside amenities appeared. In the 1920s–1930s, a bar and gas station operated here; the site even made news for Prohibition-era raids and a 1932 hold-up. By the 1960s, a restaurant known as the Big Top (or similar) served travelers. John Peterson ran an earlier service station, bar, and restaurant.

In 1974–1975, the old restaurant building was repurposed as the Salt Wells Villa, a legal brothel that operated until around 2003–2004 (closed partly due to water quality and code issues). The site gained notoriety in 1977 when it was firebombed by Mildred Banovich, wife of the Churchill County Sheriff. The structure was fully destroyed by another suspicious fire (possibly arson) on July 29, 2007. Today, little remains of these businesses beyond an RV dump station at the approximate site.

Modern Context and Geothermal Resources

The Salt Wells basin features geothermal activity, including hot springs documented as early as 1885 (such as the intermittent Borax Spring). In 2009, the Salt Wells Geothermal Plant (approximately 23–24 MW capacity) began operations south of the historic site, harnessing the area’s basin-and-range tectonics for renewable energy production. The region has also been explored for lithium brines in the deep sedimentary basin.

In recent decades, transportation planners have occasionally discussed the Salt Wells corridor as a potential alignment for future Interstate 11 extensions, though no firm developments have occurred as of the latest available information.

Preservation and Legacy

Unlike well-preserved Pony Express ruins at sites like Cold Springs or Sand Springs, Salt Wells lacks dramatic standing structures. Visitors encounter a desolate landscape with scattered mining artifacts from the borax era, interpretive potential tied to U.S. 50’s “Loneliest Road” heritage, and proximity to Sand Mountain (a prominent landmark in the Salt Wells Basin with its own Paiute cultural significance and historic associations). The site exemplifies the boom-and-bust cycles of Nevada’s resource economy: from 19th-century salt and borax extraction, to early 20th-century mining support, mid-century roadside commerce, late 20th-century vice industry, and 21st-century geothermal energy.

Salt Wells highlights how even minor waypoints in Churchill County adapted to changing transportation, mining, and economic needs across more than 150 years, leaving subtle traces on the high desert floor.

White Tidy Tips (Layia glandulosa)

The White Tidy Tips (Layia glandulosa), also known as whitedaisy tidytips or white layia, is a charming annual wildflower in the sunflower family (Asteraceae) native to the arid and semi-arid regions of western North America, stretching from central Washington south to Baja California and eastward into Utah and Arizona. This low-growing, branched herb, typically reaching 4 to 24 inches in height, features hairy, glandular stems and linear to lobed leaves that give off a subtle fragrance. Its showy daisy-like flower heads bloom from March to June, especially following adequate winter rains, boasting pure white, three-lobed ray florets that encircle a bright yellow disk of central florets—creating a crisp, tidy contrast that evokes its common name—while the rays may occasionally fade to a delicate rose-purple. Thriving in sandy or open soils across desert scrub, grasslands, and coastal habitats, it adds bursts of ethereal beauty to spring landscapes, supports pollinators like butterflies, and provides seeds for birds, embodying the resilient grace of Western wildflowers.

White Tidy Tips (Layia glandulosa), also known as whitedaisy tidytips or white layia.  Photograph by James L Rathbun
White Tidy Tips (Layia glandulosa), also known as whitedaisy tidytips or white layia. Photograph by James L Rathbun

Biological Classification

White Tidy Tips, also known as Whitedaisy Tidytips or White Layia, belongs to the following taxonomic hierarchy:

  • Kingdom: Plantae (Plants)
  • Clade: Tracheophytes (Vascular plants)
  • Clade: Angiosperms (Flowering plants)
  • Clade: Eudicots
  • Clade: Asterids
  • Order: Asterales
  • Family: Asteraceae (Sunflower or Aster family)
  • Genus: Layia
  • Species: Layia glandulosa (Hook.) Hook. & Arn. (described in 1833; the specific epithet glandulosa refers to its glandular hairs)

It is an annual herb in the tarweed tribe (Heliantheae) within the Asteraceae family. The genus Layia is almost entirely restricted to western North America, with 14 species native to the region (12 of which are found in California).

Description of the Plant and Flower

Plant: Layia glandulosa is a low-growing, branched, pubescent annual herb typically reaching 4–24 inches (10–60 cm) tall (occasionally up to about 2 feet). The stems are erect, green to purple-streaked, and covered in soft glandular hairs that can feel sticky and sometimes produce a mild spicy or scented aroma. Leaves are thin, linear to oval-shaped, up to 4 inches (10 cm) long; the lower (basal) leaves are often lobed or pinnatifid, while upper leaves tend to be entire.

Flower: The inflorescences are showy, daisy-like flower heads approximately 1.5 inches (4 cm) across, borne on glandular stalks. Each head features 3–14 (typically 5–8) broad, white ray florets that are often 3-lobed at the tips; these pure white rays surround a central disk of numerous bright yellow disk florets. The involucre (base of the flower head) consists of green, hairy, glandular phyllaries. The rays may fade to rose-purple with age. After flowering, the plant produces hairy achenes (cypselae) with a pappus of stiff white hairs for seed dispersal.

The plant is rapid-growing and blooms primarily in spring, with flowering triggered by adequate winter rainfall; it may not bloom in dry years

Habitat

White Tidy Tips thrives in dry, open environments with well-drained, sandy or gravelly soils. It is commonly found on dry slopes, mesas, grasslands, meadows, desert uplands, and open clearings. It tolerates a range of conditions from lower to upper desert habitats and can occur in chaparral, coastal scrub, valley grasslands, and pinyon-juniper woodlands. Lean, nutrient-poor soils promote compact growth and abundant flowering, while richer soils may cause plants to become leggy.

Range and Distribution

Layia glandulosa is native to western North America. Its range extends from central Washington (and southern British Columbia) south through Oregon, Idaho, California, Nevada, Utah, Arizona, and New Mexico, reaching as far south as Baja California, Mexico. It is particularly common in the southwestern United States, with the largest populations reported in Nevada, Arizona, California, and Oregon. In the U.S., it occurs in the following states: AZ, CA, ID, NM, NV, OR, UT, WA.

Elevation ranges from near sea level up to about 5,000–7,500 feet (1,524–2,286 m), depending on local conditions.

Ecology and Additional Notes

As an annual, Layia glandulosa germinates with winter rains and completes its life cycle quickly in spring. It provides important resources for pollinators, especially native bees, and its seeds are consumed by birds and small mammals. Indigenous groups in the southwestern U.S., such as the Cahuilla and Luiseno peoples, traditionally used the seeds as food (ground into flour or porridge).

The species is drought-tolerant once established and is valued in native plant gardening and restoration for its cheerful blooms and ability to thrive in poor soils. It is not considered invasive and is a native component of western ecosystems.

This report is based on data from botanical authorities including the USDA Plants Database, Lady Bird Johnson Wildflower Center, and regional floras. Population sizes can vary greatly year-to-year depending on rainfall.

Desert Gold Poppy (Eschscholzia glyptosperma)

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. It is a member of the poppy family and a smaller, desert-adapted relative of the more widespread California Poppy (Eschscholzia californica). This species is particularly notable for its vibrant blooms during spring “superbloom” events following adequate winter rainfall, when it can carpet desert washes and flats in golden hues.

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. - Photograph by James L Rathbun
The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. – Photograph by James L Rathbun

Taxonomic Classification

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Order: Ranunculales
  • Family: Papaveraceae (Poppy family)
  • Genus: Eschscholzia
  • Species: Eschscholzia glyptosperma Greene (described by botanist Edward Lee Greene)

The binomial name Eschscholzia glyptosperma reflects the genus honoring Estonian botanist Johann Friedrich von Eschscholtz and the species epithet referring to its sculptured or “engraved” seeds (glyptosperma). It is a strictly annual herb.

Plant and Flower Description

Eschscholzia glyptosperma is a small, scapose (mostly leafless-stemmed) annual herb. It grows from a basal rosette of finely dissected, pointed, grayish-green leaves that are 1–4 times pinnately divided into narrow, pointed segments— an adaptation that reduces water loss in harsh desert conditions. The plant typically reaches 5–25 cm (2–10 inches) in height, with one or more erect, slender stems arising from the base. Each stem bears a single flower atop a long peduncle.

Flower Morphology: The flowers are bright yellow (occasionally with a subtle orange tint), solitary, and actinomorphic (radially symmetrical). They feature four broad, satiny petals, each measuring approximately 1–2.5 cm (⅜–1 inch) long, giving the bloom a cup- or saucer-like appearance when fully open in sunlight. The petals are silky-textured and close at night or in cloudy/cold conditions (nyctinasty). There are typically two (sometimes three) sepals that are glabrous (smooth), often glaucous (waxy blue-green), and shed soon after the flower opens. The center displays numerous yellow stamens surrounding a single superior ovary. Flowers bloom primarily from February to May, peaking in March–April depending on rainfall and elevation.

The fruit is a slender, cylindrical capsule (4–8 cm long) that dehisces (splits) from the base when dry, explosively releasing numerous tiny, rounded, tan-to-brown seeds.

Range and Distribution

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. - Photograph by James L Rathbun
The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. – Photograph by James L Rathbun

The Desert Gold Poppy is endemic to the Mojave and Sonoran Deserts of the southwestern United States. Its distribution includes:

It occurs at elevations from near sea level (30 m / 98 ft) to approximately 1,600 m (5,249 ft). In suitable years, it contributes to spectacular desert wildflower displays.

Habitat and Ecology

This species thrives in desert washes, alluvial fans, dry streambeds, open flats, and gentle slopes within creosote bush scrub and Joshua tree woodland plant communities. It prefers well-drained, sandy or gravelly soils and sheltered microhabitats that protect against wind and extreme desiccation. As an annual, its population fluctuates dramatically with winter precipitation; it is a key component of “superbloom” events. The flowers provide nectar and pollen for native bees, butterflies, and other pollinators, while the foliage supports various caterpillars and the seeds are consumed by birds.

In summary, Eschscholzia glyptosperma exemplifies elegant desert adaptation—compact size, efficient water use, and brilliant, ephemeral blooms that signal the brief bounty of spring in the arid Southwest. Its presence in southern Nevada (including areas near Las Vegas) makes it a locally observable and ecologically important wildflower.

Joseco, Nevada – Lincoln County Ghost Town

Ghost Towns of Lincoln County, Nevada
Ghost Towns of Lincoln County, Nevada

Joseco is an extinct ghost town and former Mormon agricultural settlement in Clover Valley, Lincoln County, Nevada (coordinates approximately 37°30′07″N 114°13′45″W, elevation 5,430 ft).

Early Settlement and Naming

Joseco formed as part of broader 19th-century Mormon colonization efforts in southern Nevada and the surrounding region. Mormon pioneers from Utah, often called from settlements like St. George, established farming communities in valleys such as Meadow Valley (Panaca) and nearby areas starting in the 1860s. These settlements aimed to support agricultural self-sufficiency, supply mining camps (notably Pioche), and expand the Mormon “Kingdom” under Brigham Young’s direction.

Clover Valley saw early settlement in the 1860s. It was initially known as Clover Valley (with a post office under that name opening in 1871, then associated with nearby Barclay). The name changed due to duplication with another Clover Valley in northern Nevada. The post office for the area became Joseco, derived from “Joseph” and named after a leader of the Mormon Church (likely referring to a figure such as Joseph Smith or a local leader).

Joseco itself emerged as a distinct or renamed settlement within or near this valley. Like neighboring Barclay (which had a church and school built in 1898), it represented the enduring presence of Latter-day Saint families focused on ranching and farming in the high desert.

Development and Peak Period

The community remained small and rural, centered on agriculture rather than mining (unlike prominent Lincoln County boomtowns such as Pioche). A post office operated at Joseco from 1916 to 1943, indicating official recognition and some stability in the early 20th century.

Residents raised crops and livestock in the valley’s meadows, contributing to the regional economy that supported larger mining operations elsewhere in Lincoln County. The area’s history ties into the broader pattern of Mormon “calls” for settlement, temporary abandonments (e.g., due to conflicts like the Black Hawk War in the 1860s), and re-settlement in the late 1860s–1870s.

Decline and Abandonment

As with many small rural Nevada settlements, Joseco declined in the mid-20th century due to economic shifts, improved transportation, and the pull of larger towns. The post office closed in 1943. The community became fully extinct, transitioning into a ghost town.

Stone ruins mark the site today. The last standing structure was reportedly destroyed relatively recently (as of reports from around 2025), leaving primarily foundations and rubble.

Current Status and Context

Joseco is listed among Lincoln County’s ghost towns and historical sites. It is one of several forgotten corners of the county, alongside places like Barclay, Newland, and Ursine. The broader Lincoln County area features a rich tapestry of Native American presence (thousands of years), Mormon agricultural colonies from the 1860s onward, and intense mining activity in the late 19th and early 20th centuries.

The site offers a quiet reminder of pioneer resilience in arid lands. Visitors to Lincoln County can explore it as part of ghost town tours, alongside better-preserved spots like Panaca (oldest continuous settlement in southern Nevada, with structures from the 1860s–1870s).

Sources: Information draws primarily from GNIS and Federal Writers’ Project references, Lincoln County tourism/historical pages, and firsthand ghost town documentation. Limited detailed primary records exist due to the town’s small size and remote nature. For deeper research, consult Lincoln County historical museums (e.g., in Pioche) or Mormon settlement archives.