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.
The Karst Waters Institute is a 501(c)3 nonprofit institution whose mission is to improve the fundamental understanding of karst water systems for professionals and the public.
The institute works to engage professionals in small conferences and workshops to advance karst science; increase recognition and publication of karst science; foster development of karst professionals; and to communicate and disseminate information to the public.
The ghost town of Belmont Mill was established following a silver strike in 1865. Other minerals, such as copper lead and antimony were also mined here. The boom brought in settlers and Belmont grew. The town boasted four stores, two saloons, five restaurants, livery stable, post office, assay office, bank, school, telegraph office, two newspapers, and a blacksmith shop.
As the price of metals fluctuated, so did the fortunes of the town. By 1887, several of the mines closed. Like many towns which are now ghost towns, this one lasted for only a short time.
Some of the buildings are still standing, including the courthouse, the Cosmopolitan Saloon, the Monitor-Belmont Mill, and the combination mill.