Lechuguilla cave: Jewel of the Underground. Nigel Ball in the Chandelier Ballroom in Lechuguilla Cave Carlsbad Boneyard
Discovered in the late 80's, Lechuguilla Cave is the ultimate destination for any caver.
Lechuguilla Cave is the deepest in the continental United States (1,604 feet or 489 meters), But it is most famous for its unusual geology, rare formations, and pristine condition.
The cave is named for Agave lechuguilla, a species of plant found near its entrance. Lechuguilla is in Carlsbad Caverns National Park, New Mexico. Access to the cave is limited to approved scientific researchers, survey and exploration teams, and National Park Service management-related trips.
|NPS Photo/Gavin Newman
Scientific exploration has been conducted. For the first time, a Guadalupe Mountains cave extends deep enough that scientists may study five separate geologic formations from the inside. The profusion of gypsum and sulfur lends support to speleogenesis by sulfuric acid dissolution. The sulfuric acid is believed to be derived from hydrogen sulfide that migrated from nearby oil deposits. Therefore this cavern formed from the bottom up, in contrast to the normal top-down carbonic acid dissolution mechanism of cave formation.
Other studies indicate that some microbes may have medicinal qualities that are beneficial to humans.
Lechuguilla Cave lies beneath a park wilderness area. The cave's passages may extend out of the park into adjacent Bureau of Land Management (BLM) land. A major threat to the cave is proposed gas and oil drilling on BLM land. Any leakage of gas or fluids into the cave's passages could kill cave life or cause explosions.
Formations in Lechuguilla Cave IncludeAnother thing that makes Lechuguilla Cave unique is its rare cave formations. The cave contains many formations that are not found in other caves. Some of these formations include:
- Chandelliers: These are delicate formations that hang from the ceiling of the cave. They are formed when water drips from the ceiling and deposits minerals on the ground.
- Gypsum flowers: These are white, flower-shaped formations that are found on the walls of the cave. They are formed when water dissolves gypsum and then redeposits it in the form of crystals.
- Cave pearls: These are round formations that are formed when water drips on sand or other small particles. The water coats the particles with minerals, which eventually build up into pearls.
- Gypsum snowdrifts: These formations look like piles of snow made of gypsum. They are often found in the lower passages of the cave.
|Annick by slenite crystals in the Chandelier Maze of Lechguilla Cave. Credit: CavePics
|Annick in Hoodoo Hall, Lechguilla Cave. Credit: CavePics
Access to Lechuguilla Cave is limited to approved scientific researchers, survey and exploration teams, and NPS management-related trips.
|Cave pearls in the Pearlsian Gulf, Lechguilla Cave. Credit: CavePics
|Aragonite bush in Land of the Lost, Lechguilla Cave. Credit: CavePics
|The Pearlsian Gulf, Lechguilla Cave. Credit: CavePics
|Cave pearls in the Pearlsian Gulf, Lechguilla Cave. Credit CavePics