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The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast California. It is also known as the Kaibab Formation in Arizona, Nevada, and Utah. The Kaibab Limestone forms the rim of the Grand Canyon. In the Big Maria Mountains, California, the Kaibab Limestone is highly metamorphosed and known as the Kaibab Marble.

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  • Kaibab Limestone
  • Kaibab Limestone
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  • The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast California. It is also known as the Kaibab Formation in Arizona, Nevada, and Utah. The Kaibab Limestone forms the rim of the Grand Canyon. In the Big Maria Mountains, California, the Kaibab Limestone is highly metamorphosed and known as the Kaibab Marble.
  • De Kaibab Limestone, Kaibab Marble of Kaibab Formation is een geologische formatie in het zuidwesten van de Verenigde Staten, die voornamelijk uit kalksteen bestaat en gevormd werd tijdens het vroegste deel van het Perm (ongeveer 270 miljoen jaar geleden). De formatie dagzoomt in Nevada, het zuiden van Utah, noorden van Arizona en het zuidoosten van Californië en is onderdeel van de Park City Group.
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