Lechuguilla Cave in the context of "Speleothem"

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⭐ Core Definition: Lechuguilla Cave

Lechuguilla Cave is a cave in Carlsbad Caverns National Park, New Mexico, United States, known for its unusual geology, rare formations, and pristine condition. At 150.4 miles (242.0 km), it is the eighth-longest explored cave in the world. Its measured depth of 1,604 feet (489 m) makes it the second-deepest in the United States.

The cave is named for the canyon through which it is entered, which is named for Agave lechuguilla, a species of plant found there. Access to the cave is limited to approved scientific researchers, survey and exploration teams, and National Park Service management-related trips.

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Lechuguilla Cave in the context of Cave

Caves or caverns are natural voids under the surface of the Earth and have been observed in other rocky worlds also (viz. on Mars). Caves often form by the weathering of rock and can extend deep underground. Exogene caves are smaller openings that extend a relatively short distance underground (such as rock shelters). Caves which extend farther underground than the opening is wide are called endogene caves.

Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called caving, potholing, or spelunking.

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Lechuguilla Cave in the context of Solutional cave

A solutional cave, solution cave, or karst cave is a cave usually formed in a soluble rock like limestone (Calcium carbonate, with chemical formula CaCO3). It is the most frequently occurring type of cave. It can also form in other rocks, including chalk, dolomite, marble, salt beds, and gypsum.

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