The geology of Nevada began to form in the Proterozoic at the western margin of North America. Terranes accreted to the continent as a marine environment dominated the area through the Paleozoic and Mesozoic periods. Intense volcanism, the horst and graben landscape of the Basin and Range Province originating from the Farallon Plate, and both glaciers and valley lakes have played important roles in the region throughout the past 66 million years.
The official event schedule for the 2025 NCKMS has now been updated. Please check our schedule page or download a PDF to your mobile device.
In July of 1986, Life magazine dubbed Nevada's Highway 50 the "Loneliest Road in America." The article claimed there were "no points of interest" along the route and "warned" readers not to risk traveling it unless they were confident of their survival skills. However, Nevada adventurers knew better then - and still do. Sure, a road doesn't get much more wide-open than Highway 50. But that's exactly why we dig it!
Nevada's Lovelock Cave is one of the most important classic sites of the Great Basin archaeological record because conditions of the cave are conducive to the preservation of organic and inorganic material.
In 1911 two miners, David Pugh and James Hart, were hired to mine for bat guano from the cave. They removed a layer of guano estimated to be three to six feet deep and weighing about 250 tons. The miners were aware of the artifacts they were disturbing but, unfortunately, only the most interesting specimens were saved. Archaeologists were quickly alerted to the existence of the cave where they found 11 pre-historic duck decoys stored inside two woven baskets.
The cave was placed on the National Register of Historic Places on May 24, 1984. It was the first major cave in the Great Basin to be excavated.