





 |
 Ubehebe
Crater. Can you see the students that hiked to the bottom of the
crater? Didn't think so.

Paula and Andy point out the some of the perils of volcanology. |
by Rachel B.
Ubehebe Crater was formed when rising magma met
water-saturated bedrock and alluvial fan sediments. This resulted in an
explosion powered by steam which essentially blasted the confining rock
away, exposing layers of strata. This powerful type of volcanism is known as
maar volcanism, and is characterized by the formation and release of steam
as violent eruptions. This particular eruption is believed to have taken
place about 2000 years ago, making it a relatively young volcanic feature of
Death Valley. It is the largest crater in a region characterized by similar
formations making up the Ubehebe crater system. |