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  2. Howe Caverns - Wikipedia

    en.wikipedia.org/wiki/Howe_Caverns

    Inside the caverns. Howe Caverns is a solutional cave formed by the dissolution of limestone rock. The cave, like many on the Helderberg Plateau, such as Secret Caverns, which is also operated as a show cave, and Tory Cave, is composed of thickly bedded Lower Devonian aged Coeymans Limestone and thinly bedded Upper Silurian aged Manlius Limestone, both part of the Helderberg Group.

  3. Secret Caverns - Wikipedia

    en.wikipedia.org/wiki/Secret_Caverns

    The Secret-Benson Cave System, of which Secret Caverns is a part of, is a solutional cave formed by chemical weathering of rock, mainly limestone by rainwater. [5] As part of the Helderberg Plateau , the cave, like others in the region such as Howe Caverns and Tory Cave , is formed in the thickly beded Lower Devonian aged Coeymans Limestone and ...

  4. Luray Caverns - Wikipedia

    en.wikipedia.org/wiki/Luray_Caverns

    Luray Caverns, previously Luray Cave, is a cave just west of Luray, Virginia, United States, which has drawn many visitors since its discovery in 1878. The cavern system is adorned with speleothems such as columns, mud flows, stalactites, stalagmites, flowstone, and mirrored pools. The caverns host the Great Stalacpipe Organ, a lithophone made ...

  5. Cobleskill, New York - Wikipedia

    en.wikipedia.org/wiki/Cobleskill,_New_York

    Two cavern complexes are located just outside Cobleskill and are open to tourists: Howe Caverns and Secret Caverns. Both are north of I-88 and Howes Cave. Secret Caverns is located just outside Cobleskill, and was formed during the last Ice Age. The caverns were discovered in 1928, and include a 100-foot underground waterfall. Howe Caverns is ...

  6. Lake Shasta Caverns - Wikipedia

    en.wikipedia.org/wiki/Lake_Shasta_Caverns

    The caverns are dated to at least 200 million years, and were formed by flowing water. Over the years this water drained leaving the caverns seen today. The caves are made entirely of limestone and feature a wide variety of formations, including stalactites, stalagmites, soda straws, columns, and flowstone. The Discovery Room, one of eight ...

  7. Meramec Caverns - Wikipedia

    en.wikipedia.org/wiki/Meramec_Caverns

    Meramec Caverns is the collective name for a 4.6-mile (7.4 km) cavern system in the Ozarks, near Stanton, Missouri. [1] The caverns were formed from the erosion of large limestone deposits over millions of years. Pre-Columbian Native American artifacts have been found in the caverns. Currently the cavern system is a tourist attraction, with ...

  8. Wookey Hole Caves - Wikipedia

    en.wikipedia.org/wiki/Wookey_Hole_Caves

    Wookey Hole Caves ( / ˈwʊki /) are a series of limestone caverns, a show cave and tourist attraction in the village of Wookey Hole on the southern edge of the Mendip Hills near Wells in Somerset, England. The River Axe flows through the cave. [3] It is a Site of Special Scientific Interest (SSSI) for both biological and geological reasons. [4]

  9. Lookout Mountain Caverns - Wikipedia

    en.wikipedia.org/wiki/Lookout_Mountain_Caverns

    Lookout Mountain Caverns (Lookout Mountain Cave, or Lower Cave) is the second-longest known cave in Hamilton County, Tennessee. [citation needed] Its mapped length of 2.481 miles (3.993 kilometers) places it at 361st on the United States Long Caves List. [citation needed] Unofficially, anecdotal reports of cave expeditions have exceed 12 miles ...