Lathrop Wells cone

USA / Nevada / Beatty /

A cinder cone, (or ash cone), is a deposit around a volcanic vent, formed by rock fragments or cinders that accumulate and gradually build a conical hill with a bowl-shaped crater at the top.

By studying the extent of erosion and soil development on Lathrop Wells, researchers compared this volcanic cinder cone with a similar cone in southeastern California, indirectly dated at about 15,000 to 20,000 years old.

Something else to consider while contemplating a young volcano in the desert: www.ocrwm.doe.gov/ym_repository/index.shtml
Nearby cities:
Coordinates:   36°41'20"N   116°30'39"W
This article was last modified 16 years ago