The Ward Mining District, located in White Pine County, Nevada, near the present-day town of Ely, is a significant chapter in the state’s mining history. Situated at over 8,000 feet elevation in Ward Gulch, the district was a bustling silver mining hub in the 1870s, marked by rapid growth, lawlessness, and eventual decline. Its iconic Ward Charcoal Ovens and remnants of a once-thriving town remain as testaments to its past. Below is a detailed history of the district, from its discovery to its modern legacy.
Discovery and Establishment (1872–1875)
The Ward Mining District was born in 1872 when freighters William Ballinger and John Henry discovered silver-lead ore in Ward Gulch, approximately 11 miles southwest of Ely. Named after B.F. Ward, a claim locator, the district quickly attracted prospectors. The townsite of Ward was established in 1873, and by 1875, the Martin White Company acquired the Paymaster Mine, the district’s most productive operation. One chamber in the Paymaster Mine reportedly yielded $1 million in silver, fueling a rush to the area.
Boom Years (1875–1878)
By 1877, Ward was the largest town in White Pine County, boasting a peak population of around 2,000. The town’s infrastructure grew rapidly, supporting two newspapers (The Ward Reflex and another unnamed paper), a Wells Fargo office, a city hall, and various businesses, including saloons, general stores, and hotels. The district’s social fabric was diverse, with a Chinatown community and a red-light district known as Reform Gulch. Notably, Ward lacked a church, and an abandoned brothel served as the schoolhouse, reflecting the camp’s rough character.
Mining operations relied heavily on six beehive-shaped Ward Charcoal Ovens, constructed in 1876 by Italian masons (carbonari). These ovens, located in Willow Creek Canyon, produced charcoal for smelters, each requiring timber from 5–6 acres per 10-day cycle. The ovens processed up to 35 bushels of charcoal per cord of wood, supporting the smelting of silver-lead ore from mines like the Paymaster, Martin White, and Young America.
The district’s early years were lawless, with claim jumping and disputes common. A vigilante group, the “601” committee, enforced order through extralegal means, including hangings, earning Ward a reputation as a “tough camp.” Racial tensions also surfaced, with a reported murder of a Chinese resident by a mob in 1876, highlighting the era’s social challenges.
Decline and Devastation (1878–1888)
The district’s prosperity was short-lived. By 1878, the quality and quantity of high-grade ore declined, leading to an exodus of residents to the nearby boomtown of Taylor. The population dropped to 250, and businesses struggled. In 1883, a devastating fire destroyed one-third of Ward, including the schoolhouse and city hall. Rather than rebuild, many residents salvaged materials and relocated structures to Taylor. The Ward post office, established in 1876, closed in 1888, marking the town’s effective abandonment. Total production from 1872 to 1890 was valued at approximately $960,000, primarily in silver, with lesser amounts of lead and copper.
Revivals and Modern Exploration (1906–1991)
The Ward Mining District experienced periodic revivals driven by new discoveries and technological advancements. In 1906, renewed exploration uncovered additional silver deposits, prompting small-scale activity. A more significant revival occurred in the 1960s when the Silver King Mining Company acquired the Ward Mine in 1962. By 1967, the mine produced 63,400 metric tons of low-grade ore containing gold, silver, copper, lead, and zinc, valued at nearly $2.5 million through 1967.
In the 1970s and 1980s, joint ventures between Silver King, Phillips Petroleum, and Gulf Minerals explored the district for a porphyry copper deposit. These efforts focused on skarn-hosted sulfide deposits but ultimately failed to identify a major copper system. Sporadic production continued until 1991, with cumulative output exceeding 182 kilotons of ore. The district’s total production included significant quantities of silver, gold, copper, lead, and zinc, reflecting its diverse mineralogy.
Geological Context
The Ward Mining District lies within the Robinson porphyry copper district, part of a mineralized belt in east-central Nevada. The area’s geology features limestone, dolomite, and quartzite intruded by Cretaceous and Tertiary plutons, forming skarn and vein deposits. Major mines, including the Paymaster and Ward, exploited silver-lead-zinc veins and replacement deposits, with gold and copper as byproducts. The Ward Charcoal Ovens, built to support smelting, highlight the district’s reliance on local timber resources, which were heavily depleted during the boom years.
Legacy and Modern Status
Today, Ward is a ghost town, with little remaining due to flash flooding and the relocation of structures in the 1880s. The Ward Charcoal Ovens, preserved as a Nevada State Historical Site since 1998, are the district’s most enduring feature. These 30-foot-tall, beehive-shaped structures, accessible via a graded dirt road, attract visitors and historians. A small cemetery, containing graves of early residents, also survives, though many headstones are weathered or missing.
The Ward Mining District remains an active exploration area, with modern mining companies investigating its potential for undiscovered deposits. The ovens and surrounding landscape, now part of Ward Charcoal Ovens State Historic Park, serve as a reminder of Nevada’s mining heritage and the environmental impact of 19th-century industry. Visitors can explore the site, which includes interpretive signs detailing the district’s history and the ovens’ construction.
Nevada State Historic Marker no. 54
Nevada State Historical Markers identify significant places of interest in Nevada’s history. The Nevada State Legislature started the program in 1967 to bring the state’s heritage to the public’s attention with on-site markers. These roadside markers bring attention to the places, people, and events that make up Nevada’s heritage. They are as diverse as the counties they are located within and range from the typical mining boom and bust town to the largest and most accessible petroglyph sites in Northern Nevada Budget cuts to the program caused the program to become dormant in 2009. Many of the markers are lost or damaged.
Most of the markers across the state are large blue metal markers. However, there are a variety of other marker styles out there. For this guide they have been simplified into a few categories (blue, blue small, concrete, and stone). Sometimes, the markers are on buildings, fences, or metal stands.
Ward Mining District
The ghost town of Ward, in the foothills of the Egan Range, lies some eight miles west of here. Booming from 1876 until 1882, with a peak population of 1,500, Ward was somewhat of a lawless mining camp. Early killings did occur, but justice was meted out by the vigilante committee and the hanging rope.
A million dollars worth of silver was taken from a single chamber of the Ward mine, yet an abandoned house was used for the first school and no movement was ever started to build a church.
The town was abandoned by the late 1880s, but new discoveries and better mining methods prompted a resurgence of activity in 1906 and again in the 1960s.
STATE HISTORICAL MARKER No. 54
STATE HISTORIC PRESERVATION OFFICE
WHITE PINE MUSEUM, INC
Nevada State Historic Marker 54 Map
Summary
| Name | Ward Mining District |
| Location | White Pine County, Nevada |
| Latitude, Longitude | 39.0885, -114.7524 |
| Nevada State Historic Markers No. | 54 |
Sources
- Western Mining History: Ward Mining District
- Mindat.org: Ward Mining District, Nevada
- Nevada Expeditions: Ward, Nevada
- Nevada Appeal: Ward Charcoal Ovens
- Nevada Ghost Towns & Beyond: Ward Ghost Town
- Nevada State Parks: Ward Charcoal Ovens State Historic Park