William Morris Stewart

William Morris Stewart (August 9, 1827 – April 23, 1909), often called the “Silver Senator,” was a prominent American lawyer, politician, and mining investor whose career intertwined deeply with the mining booms of California and Nevada. Known for his aggressive legal tactics, advocacy for free silver and mining rights, and involvement in high-profile (and sometimes controversial) ventures, Stewart amassed significant wealth through prospecting, litigation, and speculation before and during his long political tenure.

William M. Stewart. Photo by Matthew Brady
William M. Stewart. Photo by Matthew Brady

Early Life and Arrival in the West

Born in Galen, near Lyons, Wayne County, New York, Stewart was the oldest son of Frederick A. and Miranda Morris Stewart. His family moved to a farm in Trumbull County, Ohio, during his childhood, but he returned to Lyons for high school. In 1848, he entered Yale University but left after three semesters to join the California Gold Rush. Traveling via the Isthmus of Panama, he arrived in San Francisco in spring 1850 and headed to the gold fields near Nevada City, California. There, he prospected successfully, discovering the famed Eureka diggings and profiting enough to sell his interests at a substantial gain. This early success funded his shift from mining to law.

Legal Career and California Mining Ties (1850s)

Stewart studied law under John R. McConnell in Nevada City and was admitted to the bar in 1852. He served as district attorney of Nevada County in 1853 and briefly as acting attorney general of California in 1854. In 1855, he married Annie Elizabeth Foote (daughter of former Mississippi Senator Henry S. Foote) and moved to Downieville, California, in 1856, continuing his legal practice amid the region’s placer and quartz mining operations. His expertise in mining law—gained through litigation over claims, water rights, and ore disputes—laid the foundation for his later prominence.

Move to Nevada and the Comstock Lode (1859–1875)

The 1859 discovery of the Comstock Lode—one of the richest silver deposits in history—in what was then Utah Territory (soon Nevada) drew Stewart to Virginia City in 1860. He became the most prominent lawyer on the Comstock, specializing in mining litigation. He championed the “single ledge” theory (arguing the Comstock was one continuous vein), which influenced massive stakes in control of the lode. Stewart estimated earning $500,000 from four years of such cases, amid litigation costing up to $10 million overall. His aggressive style—sometimes described as not always strictly ethical—earned him a fearsome reputation.

Politically, Stewart helped shape Nevada: he served on the territorial council (1861), attended the 1863 constitutional convention, and became one of Nevada’s first U.S. Senators upon statehood in 1864 (serving until 1875). He drafted key national mining laws (1866 and 1872) formalizing Western practices like claim location and free access to public lands. He also contributed to the Fifteenth Amendment and supported railroad interests.

Investments and Controversies in Mining

Beyond law and politics, Stewart invested directly in mining:

  • Comstock Lode: He participated as a capitalist after his legal work, profiting from the silver boom.
  • Emma Mine (Utah, 1870s): Stewart promoted this silver mine in Little Cottonwood Canyon to British investors, raising millions. Accusations of fraud arose when the mine proved depleted or overvalued; he and partners sold shares profitably, tarnishing his reputation.
  • Panamint City (California, 1873–1877): In late 1872/early 1873, prospectors (including outlaws) discovered rich silver in Surprise Canyon, Panamint Range (near Death Valley), while searching for the legendary Lost Gunsight Mine. Stewart partnered with fellow Nevada Senator John P. Jones (both dubbed “Silver Senators” for their mining ties) to form the Panamint Mining Company (capitalized at $2 million). They invested heavily—over $250,000–$350,000—buying claims (e.g., Wyoming, Wonder, Challenge), arranging amnesty for bandit discoverers (with restitution to Wells Fargo), and promoting the boom. Panamint City swelled to 1,500–2,000 residents with mills and infrastructure, but ore depleted quickly, and a 1876 flash flood devastated the town. The venture collapsed by 1877, adding to Stewart’s controversial legacy.

Stewart’s mining pursuits often blended speculation, promotion, and politics, drawing criticism for prioritizing profit and development over restraint.

Later Career and Legacy

After leaving the Senate in 1875 (due to financial pressures against rival William Sharon), Stewart practiced law in San Francisco and pursued unsuccessful mining schemes. He represented clients in scandals (e.g., William Sharon’s divorce) and briefly joined the Silver Party (1892–1899) to advocate remonetizing silver, editing the Silver Knight newspaper. Rejoining Republicans in 1900, he returned to the Senate (1887–1905), championing Western irrigation, mining safety, and opposing figures like John Wesley Powell on land policy.

In 1905, at nearly 80, Stewart moved to the Bullfrog mining district in southern Nevada, opening a law firm and dabbling in ventures. He died in Washington, D.C., in 1909, leaving a fortune from mining and law (estimated at millions earlier). Inducted into the Hall of Great Westerners (1964), Stewart embodied the rugged, opportunistic spirit of the mining West—shaping laws that enabled its development while embodying its excesses and controversies. His investments in California (early gold fields, Panamint) and Nevada (Comstock, later camps) helped fuel booms that transformed the region, for better and worse.

Keane Wonder Mine

The Keane Wonder Mine (also known as Keane Wonder Mine and Mill) stands as one of the most significant and best-preserved historic gold mining sites in Death Valley National Park, California. Located in the Funeral Mountains on the eastern side of Death Valley, it represents a rare success story amid the region’s typically short-lived and unprofitable mining ventures during the early 20th-century gold rushes.

Jack Keane discovered an immense ledge of free milling gold ore in 1904 in the northern Funeral Range in Death Valley. The Keane Wonder Mine was one of the most productive gold mine in the area. www.nps.gov/parkhistory/online_books/deva/section4b3.htm
Jack Keane discovered an immense ledge of free milling gold ore in 1904 in the northern Funeral Range in Death Valley. The Keane Wonder Mine was one of the most productive gold mine in the area. www.nps.gov/parkhistory/online_books/deva/section4b3.htm

Discovery and Early Development (1903–1906)

Prospecting in the Funeral Mountains dated back to the 1860s, but no major strikes occurred until the early 1900s. In December 1903, two prospectors from the nearby supply camp of Ballarat—Jack Keane, an Irish immigrant who had been struggling in the desert for years, and Domingo Etcharren, a one-eyed Basque butcher—explored an area known as Chloride Cliffs, initially targeting silver deposits.

After months of unsuccessful work on a ledge, Etcharren grew discouraged and left. Keane persisted and, by chance (some accounts credit Etcharren noticing a quartz outcropping as he departed), discovered a rich vein of free-milling gold ore—high-quality ore that could be processed relatively easily. This was Keane’s first major find after nearly a decade of hardship, leading him to name it the “Keane Wonder” (or “Keane’s Wonder”) in astonishment and optimism.

The pair quickly staked and patented eighteen claims to secure the site. They sold options on the property to investors, including a New Yorker named Joseph DeLamar, but initial deals fell through—partly due to competing discoveries elsewhere in the region (like the Bullfrog boom to the north). It wasn’t until 1906 that serious development began when investors, including John F. Campbell and later Homer Wilson (an experienced miner from California’s Mother Lode), purchased the claims for sums reportedly ranging from $150,000 to $250,000 before significant extraction.

As part of the agreements, Keane and Etcharren retained stakes: Keane became president of the Keane Wonder Mining Company, and Etcharren served as secretary.

Jack Keane discovered an immense ledge of free milling gold ore in 1904 in the northern Funeral Range in Death Valley. The Keane Wonder Mine was one of the most productive gold mine in the area. www.nps.gov/parkhistory/online_books/deva/section4b3.htm
Jack Keane discovered an immense ledge of free milling gold ore in 1904 in the northern Funeral Range in Death Valley. The Keane Wonder Mine was one of the most productive gold mine in the area. www.nps.gov/parkhistory/online_books/deva/section4b3.htm

Peak Operations and Infrastructure (1907–1912)

Under new ownership, the mine rapidly expanded into a full-scale operation. By 1907, it featured:

  • A 20-stamp mill at the lower site to crush and process ore.
  • An ice plant to combat the extreme desert heat.
  • Support facilities for a mining camp, including worker housing.

The site’s steep, rugged location high on the mountainside posed major logistical challenges for transporting ore downhill to the mill. To address this, the company constructed a remarkable mile-long aerial tramway (approximately 1 to 1.5 miles, with about 1,000–1,500 feet of vertical drop) in 1907. This gravity-powered system used wooden towers, cables, and metal ore buckets to move material efficiently from the upper mine workings to the lower mill.

At peak production (roughly 1908–1911), the tramway transported up to 70 tons of ore per day (some sources note higher daily figures in short bursts). The ingenious design reduced costs dramatically compared to pack mules or manual labor on the treacherous slopes, making the operation profitable despite Death Valley’s harsh conditions (extreme heat, water scarcity, and isolation). The Keane Wonder became known as the “King of the Desert” in local papers like the Rhyolite Herald, and it was the most productive and longest-operating mine in the Funeral Mountains region—outlasting many flash-in-the-pan camps.

The mine yielded substantial gold (with some silver), with total output estimates ranging from $750,000 to over $1.1 million (equivalent to tens of millions in modern dollars) between 1904 and 1917, with the bulk from 1907–1912. It was one of the few truly profitable gold mines in Death Valley during this era.

Jack Keane discovered an immense ledge of free milling gold ore in 1904 in the northern Funeral Range in Death Valley. The Keane Wonder Mine was one of the most productive gold mine in the area. www.nps.gov/parkhistory/online_books/deva/section4b3.htm
Jack Keane discovered an immense ledge of free milling gold ore in 1904 in the northern Funeral Range in Death Valley. The Keane Wonder Mine was one of the most productive gold mine in the area. www.nps.gov/parkhistory/online_books/deva/section4b3.htm

Decline and Closure (1912–1942)

By 1912, easily accessible high-grade ore was largely depleted, leading to financial struggles and reduced activity. The mine was sold amid speculation that it was “played out.” Intermittent small-scale operations continued, but major production ended around 1916–1917. A final revival attempt ceased by 1942.

Keane Wonder Mine - 1916 - Quartz mill. Mine said to have produced $1,000,000. Closed May 1916 as the developed ore bodies were worked out.
Keane Wonder Mine – 1916 – Quartz mill. Mine said to have produced $1,000,000. Closed May 1916 as the developed ore bodies were worked out.

Post-Mining History and Preservation in Death Valley National Park

The National Park Service acquired the claims in the 1970s as part of Death Valley’s expansion and protection (Death Valley became a national monument in 1933 and a national park in 1994). The site preserves over 18,000 mining features park-wide, with Keane Wonder exemplifying early 20th-century engineering and hardship.

The area closed from 2008 to 2017 for safety reasons, including structural stabilization of unstable mine workings, hazard mitigation (e.g., after a fatal fall into a shaft in 1984), and soil sampling for contamination. Restoration focused on the aerial tramway towers, upper and lower terminals, and other structures. It reopened in November 2017 and is now a popular hiking destination via the Keane Wonder Mine Trail (a strenuous 3+ mile round-trip with significant elevation gain).

Keane Wonder Mine Trail Map

Today, visitors can view remnants including:

  • Foundations of the stamp mill.
  • Mine adits and shafts (do not enter—unsafe and illegal).
  • The iconic line of wooden tramway towers and terminals stretching up the mountainside, with some ore buckets still in place.

The aerial tramway remains a highlight: a testament to innovative engineering that overcame the site’s extreme topography and enabled the mine’s success. It symbolizes how infrastructure could turn marginal deposits profitable in one of Earth’s harshest environments.

The Keane Wonder Mine offers a tangible link to Death Valley’s mining heritage—boom-and-bust cycles, perseverance, and the fleeting allure of gold in the desert.

Marta Becket

Marta Becket, 87, performed her final show at the Amargosa Opera House at Death Valley Junction on February 12th, 2012. She happened upon the abandoned headquarters for the Pacific Coast Borax Works in 1967 and, as a professional dancer, adopted the community hall and has been residing on the property and giving performances since. A real Death Valley original.  Rick Cooper, CC BY 2.0 <https://creativecommons.org/licenses/by/2.0>, via Wikimedia Commons
Marta Becket, 87, performed her final show at the Amargosa Opera House at Death Valley Junction on February 12th, 2012. She happened upon the abandoned headquarters for the Pacific Coast Borax Works in 1967 and, as a professional dancer, adopted the community hall and has been residing on the property and giving performances since. A real Death Valley original. Rick Cooper, CC BY 2.0 , via Wikimedia Commons

Marta Becket (August 9, 1924 – January 30, 2017) was an extraordinary American dancer, choreographer, painter, and performer whose life took a legendary turn in the remote desert of California. Best known for transforming an abandoned building in Death Valley Junction into the iconic Amargosa Opera House, she created a unique artistic oasis in one of the most isolated places in the United States, performing there for over four decades.

Here are some glimpses of the stunning Amargosa Opera House interior, where Becket hand-painted elaborate murals of a colorful, eternal audience—including Renaissance figures, clowns, monks, and even a nod to theater critics—watching her performances forever:

Early Life and Artistic Beginnings

Born Martha Becket in New York City’s Greenwich Village on August 9, 1924, she showed creative talent from a young age. She began studying ballet at 14—a relatively late start—encouraged by her supportive yet demanding mother. Despite the delay, her natural ability shone through. By her early twenties, she was dancing professionally with the corps de ballet at Radio City Music Hall and later appeared on Broadway in productions such as Showboat. Beyond dance, she excelled in painting, drawing, and piano, laying the foundation for her multifaceted career.

She later changed her name to Marta Becket and, in the early 1960s, began performing her own one-woman shows on regional tours. In 1962, she married her manager, Tom Williams, and the couple continued traveling across the western U.S., where she first fell in love with the vast desert landscapes.

The Fateful Flat Tire: Birth of the Amargosa Opera House

The Arargosa Opera House is located in Death Valley Junction, California.
The Arargosa Opera House is located in Death Valley Junction, California.

In March 1967, while on tour and heading to an engagement, Becket and her husband experienced a flat tire in the tiny, nearly abandoned town of Death Valley Junction (originally called Amargosa), near the eastern edge of Death Valley National Park. While the tire was repaired at the local gas station, Becket wandered across the street and peered through a hole in the door of Corkhill Hall, a dilapidated former community social hall built in the 1920s by the Pacific Coast Borax Company.

She later described the moment as mystical—the empty, rundown building seemed to speak to her: “Take me. Do something with me. I offer you life!” Enchanted by the potential, she rented the space for $45 a month (with a dollar down) and took full responsibility for repairs. The couple returned in August 1967 to begin renovations. She renamed it the Amargosa Opera House in homage to the town’s original name.

Here’s the iconic exterior of the Amargosa Opera House and Hotel complex in the remote desert landscape:

A Life of Dedication in the Desert

Becket staged her first performance on February 10, 1968, to an audience of just 12 people. Early years were challenging—she often performed for empty seats—but she persisted, creating her own choreography blending ballet, mime, and vaudeville. Over seven years, she painstakingly painted the theater’s walls and ceiling with vibrant murals depicting a permanent, whimsical audience.

In 1970, a National Geographic article brought national attention, and audiences began arriving from around the world. By 1974, she established the nonprofit Amargosa Opera House, Inc. to preserve the property. She continued performing weekly (later on Saturdays) until her final show in February 2012, at age 87.

Becket also expanded to own and restore the adjacent hotel, infusing it with her artistic vision.

Legacy and Final Years

Marta Becket passed away on January 30, 2017, at her home in Death Valley Junction at the age of 92, from natural causes. Her story of following her heart—leaving the bright lights of New York for a solitary desert stage—has inspired countless artists and dreamers.

The Amargosa Opera House remains a living tribute to her vision, hosting performances, tours, and events to this day. Her legacy endures as a testament to the power of art, determination, and the magic that can bloom even in the most unexpected places.

Here are a few beautiful portraits and moments of Marta Becket herself, capturing her grace and enduring spirit:

Lost Burro Mine

The Lost Burro Mine is one of the best-preserved historic gold mining sites in Death Valley National Park, California. Located in a remote draw at the northern end of the mountain range separating Hidden Valley from Racetrack Valley (near Teakettle Junction in the Ubehebe Mining District), the mine sits in rugged terrain accessible only by high-clearance 4WD vehicles via a rough 1-mile dirt track off the Hidden Valley road. Its isolation has helped protect the site from vandalism, making it a fascinating glimpse into early 20th-century prospecting life.

The Lost Burrow Mine is located off Hunter Mountain Road in Death Valley National Park, CA
The Lost Burrow Mine is located off Hunter Mountain Road in Death Valley National Park, CA

Discovery (1907)

The story of the Lost Burro Mine began on April 18, 1907, with a classic tale of serendipity. Prospector Bert Shively, while searching for his stray burros in a remote canyon, picked up a rock intending to throw it at the animals to get their attention. Instead of tossing it, he noticed the rock was laced with visible free gold. Surface assays from the outcroppings reportedly ran from $40 to $1,000 per ton — incredibly rich values for the era.

Shively quickly filed six claims and partnered with others, securing options worth around $45,000. The accidental discovery turned the site into one of the most promising gold properties in the Ubehebe District (an area otherwise known more for lead, silver, and copper).

The Lost Burrow Mine
The Lost Burrow Mine

Early Development and Peak Years (1907–1910s)

Despite the financial panic of 1907, work continued at the Lost Burro, regarded as one of the richest claims in the district. Ore samples averaged high gold values (some reports cite up to $80–$1,450 per ton in early assays), and the mine attracted multiple ownership changes and optimistic plans.

By the 1910s, development included short tunnels along the vein, with ore intersections averaging $25 per ton in later reports. Foundations were laid for a five-stamp mill and cyanide plant, intended to process ore on-site, with water piped in from Burro Spring (about 7.5 miles northeast on Tin Mountain) via a 2-inch pipeline. Remnants of this pipeline — along with rusted oil drums, tin cans, old chairs, and other debris — still litter the site.

The mine’s greatest production likely occurred between 1912 and 1917, though official records are sparse. It stands out as the only exclusively gold-bearing property in the Ubehebe District.

Later Operations and Decline (1920s–1970s)

The mine changed hands several times over the decades and was worked intermittently. In 1942, claims were relocated, and further amendments occurred in 1948 and 1970. A small amount of recorded production (about 255 ounces of gold between 1935 and 1942) exists, but unofficial estimates suggest the total lifetime output may have approached $100,000 in gold value.

Operations wound down by the 1970s, and the site was eventually incorporated into Death Valley National Park, where all mining claims became inactive.

The cabin found at the Lost Burrow Mine is in good shape.
The cabin found at the Lost Burrow Mine is in good shape.

Modern Legacy

Today, the Lost Burro Mine features a remarkably intact wooden cabin (in good condition, with stories of a “curse” leading some visitors to return removed artifacts), an outhouse, multiple adits (some used for storage), a one-chute ore bin, mill foundations stairstepping down the hillside, scattered machinery (including a small retort/smeltor and sluice box remnants), and tailings piles.

The site’s remoteness — requiring a challenging 4WD journey often combined with trips to the nearby Racetrack Playa — has kept it well-preserved and largely free of modern vandalism. Visitors are reminded to leave everything as found, as the area is protected wilderness.

The Lost Burrow Mine cabin interior
The Lost Burrow Mine cabin interior

The Lost Burro Mine remains a testament to the tenacity of Death Valley prospectors — turning a frustrated burro chase into a legendary gold story in one of the harshest environments on Earth. Always check current road conditions and permits with the National Park Service before visiting!

Lost Burro Mine Video

Lost Burro Mine Trail Map

Lippincott Mine

The Lippincott Mine (also known as the Lead King Mine) is a historic lead-silver mine located in the remote southwestern corner of Racetrack Valley within Death Valley National Park, California. Situated in the Ubehebe Mining District on the ridge separating Racetrack Valley from Saline Valley, the site represents one of the area’s more productive small-scale mining operations in the early-to-mid 20th century. Today, it features scattered ruins, adits (horizontal mine entrances), tailings piles, and remnants of mining infrastructure, though much has deteriorated over time. Visitors often access it via rough off-road routes, including the infamous Lippincott Mine Road.

The remains of the Lippencott Mine at the southern end of Race Track Valley.
The remains of the Lippencott Mine at the southern end of Race Track Valley.

Discovery and Early Development (1906–1910s)

The Lippincott Mine was discovered in 1906, with significant development work beginning around 1908. Located in a harsh, water-scarce desert environment, the mine targeted rich lead-silver deposits (primarily galena ore). Early ore samples showed impressive grades, often yielding around 42% lead and 8 ounces of silver per ton, making extraction economically viable despite the remote location.

The mine saw its most productive period during World War I, when demand for lead (used in ammunition and other wartime materials) surged. Miners reportedly used the flat, dry surface of the nearby Racetrack Playa as an improvised landing strip for small aircraft, aiding in supply transport and oversight.

World War II Era and Post-War Operations (1940s–1950s)

Operations ramped up again during World War II, with development of the Lead King Mine (under the Lippincott family) beginning in May 1942. A small crew of about eight miners extracted high-grade silver-lead ore, which was trucked out to Goldfield, Nevada, then railed to smelters in Utah. Only the richest ore was shipped due to challenging logistics — the silver was particularly valuable for wartime storage batteries.

Despite high ore quality (some reports cite up to 63% lead and 35 ounces of silver), federal restrictions shut down operations during the later war years as part of resource conservation efforts. The Lippincott family resumed work from 1946 to 1951, constructing additional infrastructure like a mine camp with wood and tarpaper cabins, an ore tipple, and possibly a tramway system.

Water scarcity remained a major challenge — supplies had to be trucked in over long distances — and this likely contributed to the eventual closure. Limited activity may have continued sporadically into the 1970s under later owners like George Lippincott Jr.’s Polaris Battery Company, which considered further exploration in 1974.

Looking down at the Lippencott Mine Road from the Lippencott Mine, with Saline Valley in the distance.
Looking down at the Lippencott Mine Road from the Lippencott Mine, with Saline Valley in the distance.

Legacy and Modern Significance

The Lippincott Mine is now part of Death Valley National Park, where all mining claims are inactive, and the site is protected as a historic resource. Ruins include adits (some gated for bat protection), scattered timbers, old vehicle parts, and tailings piles — visitors should avoid disturbing soil or inhaling dust due to potential residual lead contamination.

The mine’s access road — the steep, narrow, and extremely challenging Lippincott Mine Road (also called Lippincott Pass) — was originally built in 1906 to reach the site. This 7-mile route from Saline Valley to Racetrack Valley features sheer drop-offs, tight switchbacks, and rough terrain, making it one of Death Valley’s most notorious 4WD trails (high-clearance 4WD with experienced drivers only; uphill traffic has right-of-way).

The Lippincott Mine stands as a testament to the tenacity of early 20th-century prospectors in one of the harshest environments on Earth, contributing to the broader mining history of Death Valley that includes gold, silver, borax, and other metals. While not as famous as sites like Rhyolite or the Keane Wonder Mine, it remains a fascinating, off-the-beaten-path destination for adventurous visitors exploring Racetrack Valley’s moving rocks and remote wilderness. Always check current road conditions with the National Park Service before attempting access!