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Diamond Caverns

Coordinates: 37°06′58″N 86°03′43″W / 37.116°N 86.062°W / 37.116; -86.062
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This is an old revision of this page, as edited by Christine.Humphrey (talk | contribs) at 15:50, 20 January 2020 (→‎External links: Name corrected to Diamond Caverns). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Diamond Caverns in Park City, Kentucky was discovered on July 14, 1859.[1] The Caverns are open for guided tours year-round; Closed on Thanksgiving, Christmas Eve, and Christmas Day.[2]

Geology

The cave is mostly limestone, which was laid in the late Mississippian Period when most of Kentucky was under a shallow warm sea.[3] There are also large deposits of calcite. Fresh water dissolves the limestone, and then deposits the mineral as the water itself loses its acidic nature.[4] Other speleothems (formations) which can be viewed at Diamond Caverns include: Soda Straws, Stalactite, Columns, Flowstone, Drapery/Bacon Strip, and Cave Pearl.

Thin Flowstone Speleothem a.k.a. Cave Bacon
Cave Pearl formation, New Discovery - Diamond Caverns, Park City, Kentucky

[5]

References

  1. ^ Sides, Stanley D. (2007). Diamond Caverns: Jewel of Kentucky's Underground. Dayton, Ohio: Cave Books. p. 5. ISBN 978-0-939748-67-9.
  2. ^ "Diamond Caverns Tours". Historic Diamond Caverns. Retrieved 7 July 2017.
  3. ^ Palmer, Arthur (1981). A Geological Guide to Mammoth Cave National Park. Teaneck, New Jersey: Zephyrus Press, Inc. p. 11.
  4. ^ Schultz, Ron (1993). Looking Inside Caves & Caverns – X - Ray Vision series. John Muir Publications. pp. 4–10, 20–38.
  5. ^ Sides, Stanley D. (2007). Diamond Caverns - Jewel of Kentucky's Underground. Dayton, Ohio: Cave Books. p. 18. ISBN 978-0-939748-67-9.

External links

37°06′58″N 86°03′43″W / 37.116°N 86.062°W / 37.116; -86.062