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Howe Caverns is a limestone solutional cave, operated as a show cave, in the hamlet of Howes Cave, Schoharie County, New York. Howe Caverns is a popular tourist attraction , providing visitors with a sense of caving or spelunking, without needing the advanced equipment and training usually associated with such adventures.
Secret Caverns is a limestone solutional cave, located in Howes Cave, New York. As a show cave , Secret Caverns is open to the public as a tourist attraction, with guides taking visitors through the cave, which features karst and glacial geological features, culminating in a 100 ft (30 m) waterfall.
Tory Cave (Albany, New York) This page was last edited on 11 November 2018, at 21:28 (UTC). Text is available under the Creative Commons Attribution ...
Natural Stone Bridge and Caves is park with a system of eleven marble caves and karst formations, operated as a show cave located in Pottersville, New York. [1] Visitors to the park can walk a trail which features the eponymous Stone Bridge Cave, advertised as the "largest marble cave entrance in the eastern United States", small caves, potholes, and various other karst features along Trout Brook.
Ausable Chasm is a sandstone gorge and tourist attraction located near the hamlet of Keeseville, New York, United States, [1] due west of Port Kent.The gorge is about two miles (3.2 km) long and is about 150 feet (46 m) deep.
Howes Cave is a hamlet in Schoharie County, New York, United States. The community is 5.3 miles (8.5 km) east of Cobleskill . Howes Cave has a post office with ZIP code 12092, which opened on November 18, 1867.
The Dutchess Quarry Cave Site is located along NY 17A in the Town of Goshen in Orange County, New York.It is midway between the village of Goshen and Florida, at the junction of Quarry Road (Orange County Route 68), built into the side of a 580-foot (177 m) hill known as Mount Lookout.
Clark Reservation State Park is a state park in Onondaga County, New York.The park is in Jamesville, NY, in the Town of DeWitt, south of Syracuse.It was the site of a large waterfall formed by melting glacial ice at the end of the last Ice Age; the plunge basin at the base of the old falls is now a small lake.