Courtland, Arizona

Courtland is a classic example of an Arizona ghost town, born from the rapid boom-and-bust cycle typical of early 20th-century mining communities in the American Southwest. Located in Cochise County at the foot of the Dragoon Mountains, approximately 15 miles northeast of the famous town of Tombstone, Courtland played a brief but significant role in the region’s copper mining industry.

A panorama of Courtland in 1909, facing east.  West Coast Art Co. - Original publication: June 12, 1909, Los Angeles, California
A panorama of Courtland in 1909, facing east. West Coast Art Co. – Original publication: June 12, 1909, Los Angeles, California

Early Mineral History and Pre-Town Activity

The area’s mineral wealth dates back further than the town itself. Mining claims in the broader district (now known as the Turquoise Mining District or Courtland-Gleeson Mining District) were first discovered and located in the early 1890s. The region had even earlier significance, with Native American groups like the Navajo and Apache mining turquoise in the Dragoon Mountains for centuries, trading it for jewelry and other items. In the late 19th and early 20th centuries, turquoise mining gained prominence, particularly after a fad boosted by retailers like Tiffany & Co. in the 1890s. Nearby Gleeson (originally called Turquoise) was tied to this activity, but turquoise production declined when the fashion waned.

The shift to copper transformed the area. In 1908, rich copper ore veins were discovered in the hills, with assays showing exceptionally high grades—around 7.5% copper in some deposits, far above the typical 2-3% that made large-scale operations viable elsewhere.

Founding and Boom Period (1909–1910s)

The Crescent Cafe in Courtland in July 1909.  Original publication: 1909 Courtland, Arizona
The Crescent Cafe in Courtland in July 1909. Original publication: 1909 Courtland, Arizona

Courtland was officially founded in 1909 amid a copper mining boom. It was named after Courtland Young, one of the owners of the Great Western Mining Company (his brother W.J. Young was more actively involved in establishing the town). The Young brothers, lumber magnates from Clinton, Iowa, capitalized on the rich ore discoveries by acquiring significant land holdings.

Four major mining companies quickly entered the scene:

  • Great Western Mining Company
  • Calumet & Arizona
  • Copper Queen (associated with Bisbee operations)
  • Leadville Mining Company

These operations drew hundreds of settlers almost overnight, turning the site into a bustling tent city that rapidly grew into a proper town. At its peak, Courtland had a population of over 2,000 residents.

To support the influx, two railroads extended lines to the town:

  • The Mexico & Colorado Railroad (owned by the El Paso & Southwestern Railroad)
  • The Arizona & Colorado Railroad (owned by Southern Pacific)

These rail connections linked Courtland northward to Cochise and helped transport ore and supplies, making it a key hub in the local mining network.

The post office opened on March 13, 1909, reflecting the town’s rapid establishment and official recognition.

Historic Events and Daily Life

Courtland’s heyday was marked by typical boomtown activity: mining operations, general stores, hotels, cafes (such as the Crescent Cafe documented in 1909 photos), a jail, and community infrastructure. It formed part of the “Ghost Town Trail” alongside nearby Gleeson and Pearce, a string of mining settlements in the Sulphur Springs Valley.

While no major violent events like those in Tombstone are prominently recorded, the town experienced the standard challenges of mining camps, including labor demands and economic fluctuations tied to copper prices. Some later remnants include concrete structures from copper precipitation (cementation) processes near the Mame Mine, though these post-date the initial boom.

Major activity in the district peaked around 1919, after which production declined.

Decline and Ghost Town Status

The copper boom was short-lived. As ore quality diminished and market conditions changed, mining operations wound down. The population dwindled rapidly, and the post office closed on September 30, 1942, marking the end of Courtland as an active community. By 1938 or the early 1940s, it had largely been abandoned, with the bust completing the classic boom-to-bust cycle seen in many Arizona mining towns.

Today, Courtland is a true ghost town with no permanent residents (though some ranches occupy the broader area). Scattered ruins remain, including remnants of buildings, a jail, sidewalks, old mine sites, and a cemetery. It attracts off-road enthusiasts, history buffs, and those exploring the Ghost Town Trail. Some turquoise mines in the vicinity are still privately operated for collecting and sales by appointment.

Role in the Region

Courtland served as an important satellite in southeastern Arizona’s copper mining economy during the early 20th century, complementing larger operations in nearby Bisbee (Copper Queen) and contributing to the region’s output of copper, along with some base metals, manganese, and turquoise. Its railroads made it a transportation node connecting remote mines to broader rail networks. Part of Cochise County’s mining heritage—tied to the post-Apache Wars settlement boom—Courtland exemplified how mineral discoveries could spawn instant communities in the desert, supporting the growth of southern Arizona as a key U.S. copper-producing area.

Though short-lived, Courtland’s story highlights the transient nature of resource-based towns in the American West, leaving behind a legacy of ruins that preserve Arizona’s mining history for modern visitors.

Baldwin Lake-Bear Valley Mining District

The Baldwin Lake-Bear Valley Mining District (also referred to as the Baldwin Lake District or encompassing parts of the broader Bear Valley area) is located in the northern San Bernardino Mountains of San Bernardino County, California, east of Baldwin Lake and in the vicinity of Big Bear Valley and Holcomb Valley. This high-elevation region (around 6,700–7,000 feet) saw episodic gold mining activity, primarily from the mid-19th century through the early 20th century, with some intermittent prospecting later.

The remains of Gold Mountain Mine, "Lucky Baldwin Mine" overlook the townsite of Doble and Baldwin Lake.
The remains of Gold Mountain Mine, “Lucky Baldwin Mine” overlook the townsite of Doble and Baldwin Lake.

Geology

The district features a complex geologic setting typical of the San Bernardino Mountains, including metamorphic rocks such as mica schist, quartzite, and limestone, intruded by granite. Ore deposits primarily consist of irregular quartz-calcite veins hosting free gold, along with scheelite (tungsten mineral) and various sulfides (e.g., pyrite and others). Gold occurs in lode (vein) systems, with some associated placer deposits in alluvium from erosion of these veins. The area lacks a major “mother lode” but has numerous small to medium quartz veins and stringers, often fault-controlled. The region’s rugged terrain, with colluvial and alluvial processes, has influenced deposit exposure and mining challenges.

History and Significant Developments

Gold mining in the broader San Bernardino Mountains dates to reports of placer activity by Mexican miners possibly as early as the 1800s (or 1850s in some accounts), but the district’s main activity began around 1860. The nearby Holcomb Valley gold rush (triggered by William F. “Grizzly Bill” Holcomb’s 1860 discovery) drew prospectors to the region, leading to boom towns, violence, and short-lived placer operations. The Baldwin Lake area saw lode quartz mining emerge later.

The Rose Mine was active by 1860, marking early lode efforts. Activity increased in the 1870s with quartz vein discoveries. In 1873, Elias Jackson “Lucky” Baldwin—a wealthy investor known for prior mining successes elsewhere—purchased claims (including what became the Gold Mountain Mine, originally Carters Quartz Hill) for around $30,000. He formed the Gold Mountain Mining Company, shifting toward larger-scale quartz operations.

The area transitioned from individual placer prospecting to company-driven lode mining. Towns like Doble (also called Bairdstown) boomed briefly in the 1870s–1890s near the mines, supporting miners with stores, saloons, and mills. Belleville (in nearby Holcomb Valley) rivaled San Bernardino in population during peak rushes but declined quickly.

Mining peaked in the 1890s–early 1900s, with renewed interest in the 1930s (e.g., at some properties during the Great Depression). The district never produced at the scale of major California districts, lacking rich bonanzas, and activity waned by the 1920s–1940s as high-grade ore depleted and economics shifted.

No large towns or extensive mills were permanent fixtures solely in the Baldwin Lake sub-district; support came from nearby Holcomb Valley/Big Bear settlements. Small stamp mills or arrastres processed ore locally, but details on major mills are limited.

Significant Mines

  • Gold Mountain Mine (also Baldwin Mine or Lucky Baldwin Mine): The district’s most prominent, overlooking Doble and Baldwin Lake. Operated intermittently into the 1920s (last major activity ~1923). Focused on quartz veins with free gold.
  • Rose Mine: Active 1860; one of the earliest lode operations.
  • Erwin Gold Mine: Near Big Bear City/Baldwin Lake area; historical producer.
  • Doble-area claims (e.g., Gold Mountain group): Multiple unpatented claims in the 1870s onward.
  • Others: Numerous small prospects (e.g., Gold Hill Mine, various Gold Mountain extensions); some with scheelite or polymetallic potential.

Mine Owners/Operators

  • Early prospectors: Individual miners (including Mexican placer workers pre-1860) and discoverers like the Carter brothers (filed claims in 1873).
  • Elias J. “Lucky” Baldwin: Dominant figure from 1873; purchased and developed Gold Mountain claims into a company operation.
  • Later operators: Various small companies and lessees in the 1890s–1930s; no single long-term corporate dominance.

Production, Money Earned, and Tonnage

Specific district-wide totals are sparse in records, as much activity was small-scale and unreported. The broader San Bernardino Mountains gold region (including Holcomb/Bear Valleys) yielded modest placer and lode output compared to Sierra Nevada districts—likely in the low hundreds of thousands of dollars total (at historical gold prices of ~$20–$35/oz).

  • No comprehensive tonnage or value figures exist for the Baldwin Lake-Bear Valley District alone; it was not a major producer.
  • Individual mines like Gold Mountain/Baldwin had limited documented output, with operations described as modest.
  • Nearby Holcomb Valley placers were richer per square mile in Southern California but short-lived (~1860s boom).
  • Overall, the district contributed to Southern California’s minor gold output, with values far below millions; activity was intermittent and often unprofitable long-term.

Today, remnants (e.g., Gold Mountain Mine ruins) are visible along trails like the Gold Fever Trail, and the area is part of recreational and ecological reserves near Baldwin Lake. Mining claims persist (some active), but commercial production ceased decades ago.

Desert Chicory (Rafinesquia neomexicana)

Desert Chicory (Rafinesquia neomexicana), also known as New Mexico plumeseed or plumeseed, is a delicate annual wildflower native to the arid deserts of the southwestern United States and northwestern Mexico. This grayish-green plant features sparse foliage, weak zigzag stems that often climb through or lean on nearby shrubs for support, and exudes a milky sap when broken. Its basal leaves are pinnately lobed with narrow segments, while upper leaves are smaller and reduced. The most striking feature is its large, showy white flower heads—resembling dandelion-like blooms with strap-shaped ray florets often tinged with faint purplish streaks on the undersides—blooming in spring (typically March to May or June) after sufficient winter rains, brightening sandy or gravelly desert landscapes in habitats like creosote bush scrub and Joshua tree woodlands.

Desert Chicory (Rafinesquia neomexicana)
Desert Chicory (Rafinesquia neomexicana)

Scientific Taxonomy and Categorization

Scientific Name: Rafinesquia neomexicana A. Gray Common Names: Desert Chicory, New Mexico Plumeseed, California Chicory, Desert Chickory

Taxonomic Hierarchy (based on standard botanical classification):

  • Kingdom: Plantae (Plants)
  • Clade: Tracheophytes (Vascular plants)
  • Clade: Angiosperms (Flowering plants)
  • Clade: Eudicots
  • Clade: Asterids
  • Order: Asterales
  • Family: Asteraceae (Aster or Sunflower family; also known as the daisy family)
  • Genus:Rafinesquia
  • Species:Rafinesquia neomexicana

This species belongs to the tribe Cichorieae within Asteraceae (the chicory tribe), characterized by flower heads composed entirely of ligulate (strap-shaped) ray florets with milky sap — traits shared with common chicory (Cichorium intybus) and dandelions. It is a native annual herbaceous forb (herb), completing its life cycle in one season from a taproot. It is not a true chicory but earns the common name from its superficial resemblance to chicory flowers. Synonyms include Nemoseris neomexicana.

Detailed Plant Description

Desert Chicory is a delicate, grayish-green annual forb growing 6–24 inches (15–61 cm) tall, typically reaching up to 2 feet. The stems are weak, purplish at the base, zigzag-shaped, glabrous (completely hairless), and often climb or lean on neighboring shrubs for support. All parts exude a milky sap when broken. Leaves are sparse and alternate along the stems: lower (basal) leaves are larger (2–8 inches or 5–20 cm long), pinnately lobed with narrow, teeth-like lobes; upper leaves are reduced to small, bract-like appendages. The entire plant has a sparse, upright appearance adapted for arid conditions.

Detailed Flower Description

The showy, bright white flower heads measure about 1½ inches (3.8 cm) across and appear solitary or in small clusters at the tips of branches. Each head consists exclusively of ligulate ray florets (no central disk florets), giving it a dandelion- or chicory-like appearance. The rays are strap-shaped, with 5 small teeth at the tips and often purplish streaks or veins on the undersides or midribs. The phyllaries (bracts enclosing the head) are ½–1 inch (1.5–2.5 cm) long and feature purple-streaked midribs. Flowers open in response to adequate winter rainfall and close at night or in cloudy weather. The overall effect is a starburst of pure white against the desert backdrop.

Fruit: A cypsela (achene) with a pappus of dark gray bristles (hence “plumeseed”).

Habitat

Desert Chicory thrives in arid, dry-climate environments with sandy, gravelly, or rocky well-drained soils. It is commonly found in creosote bush scrub, Joshua tree woodland, arid plains, mesas, bajadas, moderate slopes, washes, and lower desert flats. It often grows nestled among or supported by other desert shrubs. Elevation range: 200–4,500 feet (61–1,067 m), primarily in lower to upper desert zones.

Range and Distribution

Native Range: Southwestern United States and northwestern Mexico.

  • U.S. States: Arizona (AZ), California (CA), Nevada (NV), New Mexico (NM), Texas (TX), Utah (UT).
  • Mexico: Northern and central Baja California, Sonora.

It occurs across the Mojave Desert and Sonoran Desert (including the Colorado Desert subregion). In California, it is native and found in creosote bush scrub and Joshua tree woodland communities. Distribution is concentrated in southeastern California, southern Nevada, and central/western/northeastern Arizona. It is absent from the eastern United States (where “Carolina desert-chicory” refers to the unrelated Pyrrhopappus carolinianus).

Phenology and Ecology

Bloom Period: February–June (primarily March–May), peaking as a conspicuous spring bloomer following adequate winter rainfall.

Ecologically, it provides nectar and pollen for butterflies, moths, native bees, and other insects. Seeds and plants may attract hummingbirds, rodents, granivorous birds, and even red-eared blister beetles (which feed on petals). It is an important early-season wildflower in desert ecosystems. Similar species include Rafinesquia californica (smaller heads, more restricted in Arizona) and Calycoseris wrightii (tackstem, with glandular herbage).

This native desert annual plays a key role in post-rainfall displays across the Southwest, including areas around Las Vegas, Nevada, where it brightens sandy washes and slopes each spring.

Coppereid, Nevada – Churchill County Ghost Town

Coppereid, also known as White Cloud City, is a historic ghost town and mining camp in Churchill County, Nevada, located in White Cloud Canyon on the western slope of the Stillwater Range. The site lies approximately 35 miles southeast of Oreana (or roughly 20–25 miles south/southeast of Fallon, depending on the route), accessible via dirt roads off Stillwater Road into the canyon. Coordinates are approximately 39.849°N, 118.189°W. It is a remote, scenic location with a seasonal stream, wildlife, and remnants of stone and adobe structures, including building foundations and smelter ruins.

Early Discovery and Development (1860s–1890s)

Copper ore was first discovered in White Cloud Canyon in 1868 by Frederick Smith and Major B.B. Bee. Initial small-scale work occurred in the early 1870s (around 1871–1873), with a copper smelter erected near the mouth of the canyon at what was then called White Cloud City or the White Cloud mining area. Operations were limited due to transportation challenges, low-grade ore, and the remote desert setting. Further intermittent activity took place in 1889–1896, particularly in 1893–1896, focusing on copper with some associated iron, lead, and other minerals.

In the early 1890s, the area saw renewed interest under the name Clemens (with a post office established October 29, 1892, and discontinued June 26, 1895). Mining remained modest, reflecting the boom-and-bust cycle typical of small Nevada mining districts in the Great Basin.

Peak Activity as Coppereid (1900s–1910s)

A more substantial camp emerged around 1907 when the site was redeveloped as Coppereid. A new townsite formed adjacent to the Coppereid Mine, featuring a steam hoisting plant, air compressor, and several buildings to support underground mining. By 1908, the camp included infrastructure for processing ore. A 3,790-foot aerial tramway was constructed to transport ore from mines higher in the canyon down to a smelter near the mouth.

The Coppereid post office opened on April 8, 1907, and operated until June 15, 1914, serving a small population that peaked at around 40 residents. The settlement supported miners, their families, and support workers in a typical early-20th-century mining camp layout. Ore production remained relatively small overall, with copper as the primary commodity alongside iron. The mine is classified in the Copper Kettle Mining District (or associated with the White Cloud/White Cloud Canyon area).

Decline and Later Attempts

Like many small Nevada mining operations, Coppereid struggled with economic viability. High transportation costs, fluctuating metal prices, and the challenges of water and isolation contributed to its decline after the post office closed in 1914. The site was largely abandoned by the 1910s–1920s, transitioning into a ghost town.

A final attempt to revive the mine occurred from 1948 to 1952. Workers recovered nearly $10,000 in ore, but operations ended abruptly when a flash flood—caused by water issuing from the main adit—damaged equipment and infrastructure. No significant production has occurred since, and the mine is now closed with no known plans for reopening.

Today and Preservation

Coppereid/White Cloud City remains a popular destination for ghost town enthusiasts, historians, and off-road explorers. Visible ruins include stone building foundations, smelter remnants, mine workings, and scattered debris from the mining era. The canyon setting provides a picturesque contrast of desert landscape, riparian vegetation along the stream, and rugged mountain terrain.

The site is on public land (likely Bureau of Land Management) and is accessible but requires high-clearance or 4WD vehicles for the final approach. Visitors are encouraged to practice “leave no trace” principles, avoid disturbing structures or artifacts, and be prepared for remote conditions with no services. It is sometimes visited alongside other nearby Churchill County sites like those in the Stillwater Range.

Coppereid exemplifies the small-scale, speculative copper mining that occurred across rural Nevada in the late 19th and early 20th centuries. Unlike larger silver or gold rushes (such as those in Austin or Tonopah), it never developed into a major boomtown but left tangible ruins that illustrate the optimism, hardship, and transience of frontier mining life in the Great Basin. Its history ties into broader patterns of mineral exploration in Churchill County, which has seen varied but generally modest production compared to neighboring counties.

Etna, Nevada – Lincoln County Ghost Town

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

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.