The caves in carbonate rock are located in the valley of central and southeastern New York. The middle of the state is divided from north to south by the Appalachian Plateau. In this central region, gently folded Silurian and Devonian limestone (about 375 Ma) allowed Tertiary karst development. Later, during the ice ages, this area was the path of enormous glaciers from the north, which crushed larger caves with their weight. So only narrow and therefore stable caves survived until today.
Ace of Diamonds Mine
Brotherhood Winery
Cave of the Winds
Clarksville Cave
Cooper’s Cave
Dover Stone Church
Ellenville Fault Ice Caves
Federal Reserve Bank of New York Gold Vault
Herkimer Diamond Mines
Howe Caverns
Ice Age Glacial Exhibit
Kaaterskill Falls
Lockport Cave Raceway Tour
LowLine
Natural Stone Bridge and Caves
Old City Hall Station
Oyster Bar
Panama Rocks Scenic Park
Ramble Cave
Secret Cavern
Speakeasy 518
New York Transit Museum
Watkins Glen State Park
Widow Jane Mine