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How long has Rhyolite been around?

How long has Rhyolite been around?

Rhyolite, Nevada began when Frank “Shorty” Harris and Ernest L. Cross discovered gold on August 4, 1904. Calling their claim Bullfrog, it was located few miles south of where Rhyolite would soon sprout up. When they took their samples to nearby Goldfield it was assessed at $665/ton.

When was Rhyolite founded?

1904
Founded in 1904 and dead by 1916, Rhyolite was one of several short lived boom-towns from the late Gold Rush era.

What is there to do in Rhyolite Nevada?

Ruins include the railroad depot, the Cook Bank Building and the Kelly bottle house, made completely out of medical, beer and whiskey bottles. It makes for a fascinating day trip. Heading north on US 95 from Las Vegas, travel 116 miles to Beatty, Nevada’s gateway to Death Valley National Park.

How tall is Rhyolite Nevada above sea level?

Rhyolite is about 25 miles (40 km) west of Yucca Mountain and the proposed Yucca Mountain nuclear waste repository, which is adjacent to the Nevada Test Site. Bordered on three sides by ridges but open to the south, the ghost town is at 3,800 feet (1,200 m) above sea level.

How old are the rocks in the rhyolite series?

Extensionally faulted volcanic rocks, ranging in age from about 13.3 million years to about 7.6 million years, overlie the region’s Paleozoic sedimentary rocks. The prevailing rocks, which contain the ore deposits, are a series of rhyolitic lava flows that built to a combined thickness of about 8,000 feet (2,400 m) above the more ancient rock.

Is there a gold mine in Rhyolite Nevada?

Only a few hundred yards up the road from the Goldwell sculptures stands what is left of the abandoned gold mining town of Rhyolite. The government-owned area contains hundreds of old mines, and a scattering of buildings — some still standing and others little more than broken walls.

Where did the name rhyolite come from in New Zealand?

Rhyolite, Nevada was named after a rhyolite deposit that characterised the area. The Taupo Volcanic Zone in New Zealand has a large concentration of young rhyolite volcanoes. The Gondwana Rainforests of Australia World Heritage Area contains rhyolite-restricted flora along the Great Dividing Range.