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Black Chasm Cave

  • 5 min read
  • 4 chapters

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Through Cave, Metamorphic rock and Marble

Geology

Black Chasm Cavern is a dissolution cave, formed by carbonic acid eroding the subterranean bedrock. This eroded the limestone bedrock to form small to very large chambers. It is formed in what is considered to be part of the Calaveras Complex. The crystal structure of the metamorphic rock has changed over time, and it is now properly referred to as marble. Many lakes make up the lower levels of the cavern. The calcite formations in Black Chasm Cavern are derivative of the marble bedrock, containing primarily calcium or calcium carbonate (CaCO3). There are a variety of formations in Black Chasm Cavern, including stalactites, stalagmites, columns, flowstone, draperies, ribbons, angel's wings, cave bacon, soda straws, helictites, false floors, and others.

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