Geology and Minerals

Bandelier Tuff

The Bandelier Tuff is a geologic formation exposed in and around the Jemez Mountains of northern New Mexico. It has a radiometric age of 1.85 to 1.25 million years, corresponding to the Pleistocene epoch. The tuff was erupted in a series of at least three caldera eruptions in the central Jemez Mountains. The Bandelier Tuff was one of the first ignimbrites recognized in the geologic record, and has been extensively studied by geologists seeking to understand the processes involved in volcanic supereruptions.

Also on this shelf

See also

• ▸Ashangi Basalts
• ▸Featherbed frame
• ▸BARS apparatus

Uncatalogued shelf

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