Geology of the Jemez Mountains and Valles Caldera

ID : 80267   
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The Jemez Mountains are only one of a number of volcanic features located along the Rio Grande Rift zone – a north-south corridor throughout central New Mexico and part of the Basin and Range Province of the southwestern United States. The Jemez Mountains are what is known as a caldera or a collapsed volcano. It is one of three “supervolcanoes” in North America, including the Long Valley caldera in California and Yellowstone caldera in Wyoming. The Jemez volcanic field has been active for the past 15 million years, and the rhyolite flow that makes up Kasha-Katuwe Tent Rocks National Monument formed about 6.7 million years ago. The Jemez caldera exploded two times: once at 1.62 million years and then again 1.25 million years – that last and greatest explosion creating the Bandelier Tuff. In this class we will learn about the geology of the Valles Caldera, Bandelier National Monument and Kasha-Katuwe Tent Rocks National Monument. We will also discover a “little Yellowstone” right in our own Jemez Mountains.

Class Details

2 Sessions
Weekly - Wed

Location
CE South Building

Instructor
Carol A. Hill 

Notice
Please read: UNM Tuition Remission eligible, Personal Enrichment

Tuition: 

$29.00


Registration Closes On
Wednesday, May 3, 2017 @ 11:59 PM

Schedule Information

Date(s) Class Days Times Location Instructor(s)
5/3/2017 - 5/10/2017 Weekly - Wed 10:00 AM - 12:00 PM Albuquerque, CE South Building  Map, Room: 108 Carol A. Hill