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.

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.

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.

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.

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.

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.