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Film transparency of Mr. L. J. (Lewis J.) Murphy and the famous Tom Kelly Bottle House in Rhyolite, Nevada, November 25, 1948

Date

1948-11-25

Description

Mr. L. J. (Lewis J.) Murphy and the famous Tom Kelly Bottle House in Rhyolite, Nevada, which he operated as a free museum in the old ghost town. L. J. Murphy took care of the Bottle House from 1929 until his death in 1953. Two wagon wheels are visible in the front yard. Rhyolite is a ghost town in Nye County, Nevada. It is in the Bullfrog Hills, about 120 miles (190 km) northwest of Las Vegas, near the eastern edge of Death Valley. The town began in early 1905 as one of several mining camps that sprang up after a prospecting discovery in the surrounding hills. During an ensuing gold rush, thousands of gold-seekers, developers, miners and service providers flocked to the Bullfrog Mining District. Many settled in Rhyolite, which lay in a sheltered desert basin near the region's biggest producer, the Montgomery Shoshone Mine. Rhyolite declined almost as rapidly as it rose. After the richest ore was exhausted, production fell. The 1906 San Francisco earthquake and the financial panic of 1907 made it more difficult to raise development capital. In 1908, investors in the Montgomery Shoshone Mine, concerned that it was overvalued, ordered an independent study. When the study's findings proved unfavorable, the company's stock value crashed, further restricting funding. By the end of 1910, the mine was operating at a loss, and it closed in 1911. By this time, many out-of-work miners had moved elsewhere, and Rhyolite's population dropped well below 1,000. By 1920, it was close to zero. After 1920, Rhyolite and its ruins became a tourist attraction and a setting for motion pictures. Most of its buildings crumbled, were salvaged for building materials, or were moved to nearby Beatty or other towns, although the railway depot and a house made chiefly of empty bottles were repaired and preserved. The town is named for rhyolite, an igneous rock composed of light-colored silicates, usually buff to pink and occasionally light gray. It belongs to the same rock class, felsic, as granite but is much less common.

Image

Film transparency of a boy looking at an abandonded building, Rhyolite, Nevada, November 25, 1948

Date

1948-11-25

Description

A young boy looks at the ruins of the H. D. and L. D. Porter Brothers Store in Rhyolite, Nevada. Several other buildings are visible in the background. Rhyolite is a ghost town in Nye County, Nevada. It is in the Bullfrog Hills, about 120 miles (190 km) northwest of Las Vegas, near the eastern edge of Death Valley. The town began in early 1905 as one of several mining camps that sprang up after a prospecting discovery in the surrounding hills. During an ensuing gold rush, thousands of gold-seekers, developers, miners and service providers flocked to the Bullfrog Mining District. Many settled in Rhyolite, which lay in a sheltered desert basin near the region's biggest producer, the Montgomery Shoshone Mine. Rhyolite declined almost as rapidly as it rose. After the richest ore was exhausted, production fell. The 1906 San Francisco earthquake and the financial panic of 1907 made it more difficult to raise development capital. In 1908, investors in the Montgomery Shoshone Mine, concerned that it was overvalued, ordered an independent study. When the study's findings proved unfavorable, the company's stock value crashed, further restricting funding. By the end of 1910, the mine was operating at a loss, and it closed in 1911. By this time, many out-of-work miners had moved elsewhere, and Rhyolite's population dropped well below 1,000. By 1920, it was close to zero. After 1920, Rhyolite and its ruins became a tourist attraction and a setting for motion pictures. Most of its buildings crumbled, were salvaged for building materials, or were moved to nearby Beatty or other towns, although the railway depot and a house made chiefly of empty bottles were repaired and preserved. The town is named for rhyolite, an igneous rock composed of light-colored silicates, usually buff to pink and occasionally light gray. It belongs to the same rock class, felsic, as granite but is much less common.

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Film transparency of buildings located on Golden Street, Rhyolite, Nevada, November 25, 1948

Date

1948-11-25

Description

Two buildings that were located on Golden Street in Rhyolite, Nevada. The building on the left was possibly the John T. Overbury building. The building on the right was the John S. Cook & Co. Bank building. Rhyolite is a ghost town in Nye County, Nevada. It is in the Bullfrog Hills, about 120 miles (190 km) northwest of Las Vegas, near the eastern edge of Death Valley. The town began in early 1905 as one of several mining camps that sprang up after a prospecting discovery in the surrounding hills. During an ensuing gold rush, thousands of gold-seekers, developers, miners and service providers flocked to the Bullfrog Mining District. Many settled in Rhyolite, which lay in a sheltered desert basin near the region's biggest producer, the Montgomery Shoshone Mine. Rhyolite declined almost as rapidly as it rose. After the richest ore was exhausted, production fell. The 1906 San Francisco earthquake and the financial panic of 1907 made it more difficult to raise development capital. In 1908, investors in the Montgomery Shoshone Mine, concerned that it was overvalued, ordered an independent study. When the study's findings proved unfavorable, the company's stock value crashed, further restricting funding. By the end of 1910, the mine was operating at a loss, and it closed in 1911. By this time, many out-of-work miners had moved elsewhere, and Rhyolite's population dropped well below 1,000. By 1920, it was close to zero. After 1920, Rhyolite and its ruins became a tourist attraction and a setting for motion pictures. Most of its buildings crumbled, were salvaged for building materials, or were moved to nearby Beatty or other towns, although the railway depot and a house made chiefly of empty bottles were repaired and preserved. The town is named for rhyolite, an igneous rock composed of light-colored silicates, usually buff to pink and occasionally light gray. It belongs to the same rock class, felsic, as granite but is much less common.

Image

Film transparency of the ruins of possibly the John T. Overbury building, Rhyolite, Nevada, November 25, 1948

Date

1948-11-25

Description

Film transparency of the ruins of possibly the John T. Overbury building, Rhyolite, Nevada. Rhyolite is a ghost town in Nye County, Nevada. It is in the Bullfrog Hills, about 120 miles (190 km) northwest of Las Vegas, near the eastern edge of Death Valley. The town began in early 1905 as one of several mining camps that sprang up after a prospecting discovery in the surrounding hills. During an ensuing gold rush, thousands of gold-seekers, developers, miners and service providers flocked to the Bullfrog Mining District. Many settled in Rhyolite, which lay in a sheltered desert basin near the region's biggest producer, the Montgomery Shoshone Mine. Rhyolite declined almost as rapidly as it rose. After the richest ore was exhausted, production fell. The 1906 San Francisco earthquake and the financial panic of 1907 made it more difficult to raise development capital. In 1908, investors in the Montgomery Shoshone Mine, concerned that it was overvalued, ordered an independent study. When the study's findings proved unfavorable, the company's stock value crashed, further restricting funding. By the end of 1910, the mine was operating at a loss, and it closed in 1911. By this time, many out-of-work miners had moved elsewhere, and Rhyolite's population dropped well below 1,000. By 1920, it was close to zero. After 1920, Rhyolite and its ruins became a tourist attraction and a setting for motion pictures. Most of its buildings crumbled, were salvaged for building materials, or were moved to nearby Beatty or other towns, although the railway depot and a house made chiefly of empty bottles were repaired and preserved. The town is named for rhyolite, an igneous rock composed of light-colored silicates, usually buff to pink and occasionally light gray. It belongs to the same rock class, felsic, as granite but is much less common.

Image

Film transparency of the famous Tom Kelly Bottle House in Rhyolite, Nevada, November 25, 1948

Date

1948-11-25

Description

The famous Tom Kelly Bottle House in Rhyolite, Nevada, which L. J. (Lewis J. Murphy operated as a free museum in the old ghost town from 1929 until his death in 1953. Two wagon wheels are visible in the front yard. Rhyolite is a ghost town in Nye County, Nevada. It is in the Bullfrog Hills, about 120 miles (190 km) northwest of Las Vegas, near the eastern edge of Death Valley. The town began in early 1905 as one of several mining camps that sprang up after a prospecting discovery in the surrounding hills. During an ensuing gold rush, thousands of gold-seekers, developers, miners and service providers flocked to the Bullfrog Mining District. Many settled in Rhyolite, which lay in a sheltered desert basin near the region's biggest producer, the Montgomery Shoshone Mine. Rhyolite declined almost as rapidly as it rose. After the richest ore was exhausted, production fell. The 1906 San Francisco earthquake and the financial panic of 1907 made it more difficult to raise development capital. In 1908, investors in the Montgomery Shoshone Mine, concerned that it was overvalued, ordered an independent study. When the study's findings proved unfavorable, the company's stock value crashed, further restricting funding. By the end of 1910, the mine was operating at a loss, and it closed in 1911. By this time, many out-of-work miners had moved elsewhere, and Rhyolite's population dropped well below 1,000. By 1920, it was close to zero. After 1920, Rhyolite and its ruins became a tourist attraction and a setting for motion pictures. Most of its buildings crumbled, were salvaged for building materials, or were moved to nearby Beatty or other towns, although the railway depot and a house made chiefly of empty bottles were repaired and preserved. The town is named for rhyolite, an igneous rock composed of light-colored silicates, usually buff to pink and occasionally light gray. It belongs to the same rock class, felsic, as granite but is much less common.

Image

Film transparency of the famous Tom Kelly Bottle House in Rhyolite, Nevada, November 25, 1948

Date

1948-11-25

Description

The famous Tom Kelly Bottle House in Rhyolite, Nevada, which L. J. (Lewis J. Murphy operated as a free museum in the old ghost town from 1929 until his death in 1953. Two wagon wheels are visible in the front yard. Rhyolite is a ghost town in Nye County, Nevada. It is in the Bullfrog Hills, about 120 miles (190 km) northwest of Las Vegas, near the eastern edge of Death Valley. The town began in early 1905 as one of several mining camps that sprang up after a prospecting discovery in the surrounding hills. During an ensuing gold rush, thousands of gold-seekers, developers, miners and service providers flocked to the Bullfrog Mining District. Many settled in Rhyolite, which lay in a sheltered desert basin near the region's biggest producer, the Montgomery Shoshone Mine. Rhyolite declined almost as rapidly as it rose. After the richest ore was exhausted, production fell. The 1906 San Francisco earthquake and the financial panic of 1907 made it more difficult to raise development capital. In 1908, investors in the Montgomery Shoshone Mine, concerned that it was overvalued, ordered an independent study. When the study's findings proved unfavorable, the company's stock value crashed, further restricting funding. By the end of 1910, the mine was operating at a loss, and it closed in 1911. By this time, many out-of-work miners had moved elsewhere, and Rhyolite's population dropped well below 1,000. By 1920, it was close to zero. After 1920, Rhyolite and its ruins became a tourist attraction and a setting for motion pictures. Most of its buildings crumbled, were salvaged for building materials, or were moved to nearby Beatty or other towns, although the railway depot and a house made chiefly of empty bottles were repaired and preserved. The town is named for rhyolite, an igneous rock composed of light-colored silicates, usually buff to pink and occasionally light gray. It belongs to the same rock class, felsic, as granite but is much less common.

Image

Film transparency of a ghost town, Delamar, Nevada, 1956

Date

1956

Description

A view of some of the abandonded buildings on a hillside in Delamar, Nevada. One of the structures has a covered porch Delamar, Nevada, nicknamed The Widowmaker, is a ghost town in central eastern Nevada, USA along the east side of the Delamar Valley. During its heyday, primarily between 1895 and 1900, it produced $13.5 million in gold. In 1889, prospectors John Ferguson and Joseph Sharp discovered gold around Monkeywrench Wash. A mining camp was then born west of the Monkeywrench Mine. It was called Ferguson. In April 1894, Captain Joseph Raphael De Lamar bought most of the important mines in the area and renamed the Ferguson camp as Delamar. In the same year, a newspaper called the Delamar Lode began publication and a post office was opened. Soon, the new settlement boasted more than 1,500 residents, a hospital, an opera house, churches, a school, several businesses and saloons. Most buildings were made of native rock. By 1896, the Delamar mill was handling up to 260 tons of ore daily. Water for the camp was pumped from a well in Meadow Valley Wash, some twelve miles away. Supplies and materials traveled even further, by mule team over mountainous terrain from the railroad head at Milford, Utah, which was 150 miles from Delamar. Silicosis The gold in the Delamar mines was embedded in quartzite which when crushed created a fine dust. Miners breathing the dust often developed silicosis and the town became known as a "widow-maker." Many ruins now stand semi-intact in the Delamar ghost town region. Foundations can easily be seen from adjacent hills. There are two graveyards, which have been vandalized. The area is honeycombed with mines and mineshafts, but in recent years the main shaft has been blasted closed. Wild horses roam the area. The nearby dry lake is known to pilots as Texas Lake because its outline resembles the state of Texas.

Image

Film transparency of a ghost town, Delamar, Nevada, 1956

Date

1956

Description

A view of some of the abandonded buildings in Delamar, Nevada, taken from a nearby hill. Delamar, Nevada, nicknamed The Widowmaker, is a ghost town in central eastern Nevada, USA along the east side of the Delamar Valley. During its heyday, primarily between 1895 and 1900, it produced $13.5 million in gold. In 1889, prospectors John Ferguson and Joseph Sharp discovered gold around Monkeywrench Wash. A mining camp was then born west of the Monkeywrench Mine. It was called Ferguson. In April 1894, Captain Joseph Raphael De Lamar bought most of the important mines in the area and renamed the Ferguson camp as Delamar. In the same year, a newspaper called the Delamar Lode began publication and a post office was opened. Soon, the new settlement boasted more than 1,500 residents, a hospital, an opera house, churches, a school, several businesses and saloons. Most buildings were made of native rock. By 1896, the Delamar mill was handling up to 260 tons of ore daily. Water for the camp was pumped from a well in Meadow Valley Wash, some twelve miles away. Supplies and materials traveled even further, by mule team over mountainous terrain from the railroad head at Milford, Utah, which was 150 miles from Delamar. Silicosis The gold in the Delamar mines was embedded in quartzite which when crushed created a fine dust. Miners breathing the dust often developed silicosis and the town became known as a "widow-maker." Many ruins now stand semi-intact in the Delamar ghost town region. Foundations can easily be seen from adjacent hills. There are two graveyards, which have been vandalized. The area is honeycombed with mines and mineshafts, but in recent years the main shaft has been blasted closed. Wild horses roam the area. The nearby dry lake is known to pilots as Texas Lake because its outline resembles the state of Texas.

Image

Film transparency of a ghost town, Delamar, Nevada, 1956

Date

1956

Description

Some of the abandonded buildings in Delamar, Nevada. A tailing pile from one of the mines is visible in the center of the photograph. A stone structure is visible on the right side of the photograph. Delamar, Nevada, nicknamed The Widowmaker, is a ghost town in central eastern Nevada, USA along the east side of the Delamar Valley. During its heyday, primarily between 1895 and 1900, it produced $13.5 million in gold. In 1889, prospectors John Ferguson and Joseph Sharp discovered gold around Monkeywrench Wash. A mining camp was then born west of the Monkeywrench Mine. It was called Ferguson. In April 1894, Captain Joseph Raphael De Lamar bought most of the important mines in the area and renamed the Ferguson camp as Delamar. In the same year, a newspaper called the Delamar Lode began publication and a post office was opened. Soon, the new settlement boasted more than 1,500 residents, a hospital, an opera house, churches, a school, several businesses and saloons. Most buildings were made of native rock. By 1896, the Delamar mill was handling up to 260 tons of ore daily. Water for the camp was pumped from a well in Meadow Valley Wash, some twelve miles away. Supplies and materials traveled even further, by mule team over mountainous terrain from the railroad head at Milford, Utah, which was 150 miles from Delamar. Silicosis The gold in the Delamar mines was embedded in quartzite which when crushed created a fine dust. Miners breathing the dust often developed silicosis and the town became known as a "widow-maker." Many ruins now stand semi-intact in the Delamar ghost town region. Foundations can easily be seen from adjacent hills. There are two graveyards, which have been vandalized. The area is honeycombed with mines and mineshafts, but in recent years the main shaft has been blasted closed. Wild horses roam the area. The nearby dry lake is known to pilots as Texas Lake because its outline resembles the state of Texas.

Image

Photograph of Judy Bayley at a public event at the Hacienda Hotel and Casino, Las Vegas, Nevada, 1971

Date

1971

Description

Judy Bayley at a public event relating to the Trailrides at the Palomino Room at the Hacienda Hotel and Casino. The unidentified man standing behind Judy Bayley is wearing a badge that says "Judy Bayley's 4th Annual Las Vegas Hacienda Trail Ride Thru Paradise Valley 1971." "Participant" is stamped on the attached ribbon. Judith “Judy” Bayley, namesake of the Judy Bayley Theatre at the University of Nevada, Las Vegas, was once known as “The First Lady of Gambling.” Judy and her husband Warren “Doc” Bayley opened the Hacienda Hotel and Casino on October 17, 1956. After Warren’s unexpected death from a heart attack on December, 26, 1964, Judy Bayley took over the ownership and operations of the Hacienda. By doing so, she became the first woman in Nevada history to be the sole owner and operator of a hotel-casino. An avid horsewoman, as a publicity campaign, Judy started “The Hacienda Trailrides.” Which some considered the social event of the year. The first trailride was held in December, 1968 to commemorate Pearl Harbor. The ride began at the Valley of Fire State Park and Ended in Overton, Nevada. Judy donated all proceeds from the trailride to benefit the local Veterans of Foreign Wars. Four Trailrides were held over the next four years, leaving from Tule Springs (now Floyd Lamb State Park), and from the Hacienda itself before they were discontinued after her death. After Judy’s death from cancer on December 31, 1971, the Hacienda was sold in 1972. The Hacienda’s doors closed to the public on December 10, 1996. The hotel was imploded on December 31, 1996 on the 25th anniversary of Judy Bayley’s death, and was broadcast on the Fox news network as part of their New Year’s Eve 1996 telecast. In March 1999, it was replaced with the Mandalay Bay Hotel and Casino.

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