University of Utah
University of Utah
 
Bob Smith's Home Page
An Interdisciplinary Academic Program in Earth Science
Bob Smith's research interests are in seismology, tectonophysics, crustal deformation using GPS (Global Positioning System), and active tectonics. Current research projects include: 1) geodynamics of and evolution of the Yellowstone hotspot and the Yellowstone caldera, 2) seismicity and volcanic hazards of Yellowstone and operation of the Yellowstone seismograph network, and 3) crustal deformation and earthquake hazards of the Wasatch and Teton faults using GPS and fault modeling. Teaching includes tectonophysics and elastic waves, theoretical seismology, earthquake seismology and earthquake hazards, and introductory earthquakes and volcanoes. See detailed information on my courses and research below.


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Teton Range, Wasatch Range & Fault, Steamboat Geyser, Teton Scarp
Above, from left to right: Teton Range, Wasatch Range, Steamboat Geyser, and Teton fault scarp



Yellowstone Rising

Accelerated Uplift and Magmatic Intrusion of the Yellowstone Caldera, 2004 to 2006

by Wu-Lung Chang, Bob Smith, Chuck Wicks, Jamie Farrell, and Christine Puskas

Published in Science on November 09 2007

The Yellowstone caldera began an extraordinary episode of ground rising in mid-2004, revealed by GPS (Global Positioning System) and InSAR (Interferometric Synthetic Aperture Radar) measurements, at rates up to 7 cm/yr that is over three times faster than previously observed inflation rates. The caldera-wide accelerated upli ft is interpreted as magmatic recharge of the Yellowstone magma body. While the geodetic observations and mo dels do not imply an impending volcanic eruption or hydrothermal explosion, they are important evidence of on going processes of a large caldera that was produced by a super volcano eruption.

More Information:

 

Yellowstone Volcano Observatory

The Yellowstone Volcano Observatory (YVO) was established in May 2001 to study and monitor the Yellowstone Volcanic Field. The Observatory is a collaboration between the University of Utah, the U.S. Geological Survey, and Yellowstone National Park. For more information, visit


Book Announcement

Smith, R. B. and L. Siegel, 2000, Windows into the Earth: The Geologic Story of Yellowstone and Grand Teton National Parks, Oxford University Press, New York.

Millions of years ago, the North American continent was dragged over the world's largest continental hotspot, a huge column of hot and molten rock rising from the Earth's interior that traced a 50-mile wide, 500-mile-long path northeastward across Idaho. Generating cataclysmic volcanic eruptions and large earthquakes, the hotspot helped lift the Yellowstone Plateau to more than 7,000 feet, creating the jewel of the U.S. national park system: Yellowstone. At the same time, forces stretching apart the western U.S. created the mountainous glory of Grand Teton National Park.

This book offers expert guidance through this awe-inspiring terrain, bringing to life the forces that have shaped--and continue to shape--the greater Yellowstone-Teton region. Over seventy illustrations--including fifty-two in full color--illuminate the breathtaking beauty of the landscape, while two final chapters provide driving tours of the parks to help visitors enjoy and understand the region's wonders. Fascinating and informative, this book affords us a striking new perspective on Earth's creative forces.

YSRP Thumbnail Map of the Yellowstone-Snake River Plain volcanic system and the Yellowstone hotspot showing topography (in color), earthquakes and silicic volcanic centers (Old Yellowstone's, by age in millions of years) (from Smith and Siegel, 2000).

Book Thumbnail Space view of Grand Teton and Yellowstone national parks from satellite images overlaid on digital elevation maps. The 8,000-foot-high Yellowstone caldera was produced by a giant volcanic eruption 630,000 years ago. The caldera occupies a 45- by 30-mile-wide area of central Yellowstone. The Teton fault bounds the east side of the Teton Range and raised the mountains high above Jackson Hole's valley floor (from Smith and Siegel, 2000).


Bob Smith may be contacted at:
Department of Geology and Geophysics
University of Utah
Room 702
135 South 1460 East
Salt Lake City, Utah 84112-0111

phone: 801 581 7129
email: rbsmith@mines.utah.edu


©&nbsp2000 Robert B. Smith