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A Geoscience Digital Image Library

526.jpg
TitleSpeleothems in Lehman Cave
DescriptionLehman Cave extends about a quarter mile into the base of the Snake Range in Great Basin National Park. The cave is in the Pole Canyon Limestone of Cambrian age. The limestone has been slightly metamorphosed, and so some geologists call it a low grade marble. Speleothems (cave formations) in the cave formed by the action of flowing groundwater. This photo shows popcorn precipitated on a large stalagmite.
ChronostratigraphyCambrian
LithostratigraphyPole Canyon Limestone
Geologic provinceGreat Basin
LocationUSA ▹ Nevada ▹ White Pine. Near Ely. Great Basin National Park.
PhotographerDexter Perkins. 2001-05-22.
CollectionE15102199-8.
Key wordsLehman Cave, stlagmite, popcorn
Tech details258 KB. Outcrop.
GeoDIL number526