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.

Main Street shops in Ely, Nevada. Visible are the Bank Club, The Palace, Ely Theatre, State Cafe, Miner's Club, and The Capitol Casino. Ely is the largest city and county seat of White Pine County, Nevada. Ely was founded as a stagecoach station along the Pony Express and Central Overland Route, with the mining boom coming later than the other towns along US 50, with the discovery of copper in 1906. Though the railroads connecting the First Transcontinental Railroad to the mines in Austin and Eureka have long been removed, the railroad to Ely is preserved as a heritage railway by the Nevada Northern Railway and known as the Ghost Train of Old Ely. As of the 2010 census, the population was 4,255.

Cattle grazing in a field, possibly in Lamoille Valley, Nevada. Lamoille is located in Elko County, Nevada. It is located about 17 miles (27 km) east of Elko at the base of the Ruby Mountains at an elevation of 5,889 feet (1,795 m) and is part of the Elko Micropolitan Statistical Area. The early history of the community and surrounding area is summarized in a nearby highway marker. John Walker and Thomas Waterman first settled the area in 1865. Waterman named the valley after his native Vermont. In 1868, Walker erected the Cottonwood Hotel, store and blacksmith shop in the valley, and the settlement became known as "The Crossroads." Here wagons were repaired and food and supplies could be obtained. The original buildings and the more recent 20-bedroom Lamoille hotel, creamery, flour mill and dance hall are gone. Lamoille is nestled off the western flanks of the Ruby Mountains at the end of Nevada State Route 227, and is the principal gateway to this range via the National Forest Scenic Byway up Lamoille Canyon.

Railroad tracks run trough a canyon in Northern Nevada.

A view of the Grand Canyon, taken from the Rim.

Snow on the peaks of Mount Charleston is visible in the background. Several small buildings are visible in the foreground.

Cathedral Gorge near Panaca, Nevada. Cathedral Gorge State Park is a state park of Nevada, USA, featuring a gorge eroded through soft bentonite clay. The park covers 1,608 acres (651 ha). It is located in Central/Eastern Nevada along U.S. Route 93, 1 mile (1.6 km) north of the west end of State Route 319, near Panaca. Cathedral Gorge was established as one of the four original Nevada State Parks in 1935. The park sits at an elevation of 4,800 feet (1,500 m) above sea level, and is typically arid with semi-hot summers, and very cold winters. In the summer, temperatures usually range from 95 °F (35 °C) in midday to roughly 55 °F (13 °C) at night. Rainfall is variable, and thunderstorms are prevalent. At one time, Shakespearean plays were performed with the clay formations in the backdrop. The various naturally formed crevices were used as dressing rooms and as a backstage where actors and actresses would prepare, awaiting their cue.