Why are there so many earthquakes at Yellowstone?
Almost all earthquakes at Yellowstone are brittle-failure events caused when rocks break due to crustal stresses. Though we've been looking at Yellowstone for years, no one has yet identified "long-period (LP) events" commonly attributed to magma movement. If LP events are observed, that will NOT mean Yellowstone is getting ready to erupt. LP earthquakes commonly occur at other volcanoes in the world, including volcanoes in California, that have not erupted for centuries or millennia. One variety of ground shaking called “tremor” is observed at Yellowstone's geothermal areas whenever water boils in a geyser.
The largest historic earthquake in the Rocky Mountains was a magnitude 7.3 earthquake at Hebgen Lake northwest of Yellowstone in 1959. It was caused by the extension--or stretching--of the Earth's crust. The earthquake displaced a 40-km-long fault (25 miles) that rose vertically up to 12 meters (40 feet).
Shaking from earthquakes can also change the way that Yellowstone's hydrothermal system behaves. The interval between eruptions of Old Faithful Geyser increased significantly following the 1959 earthquake.
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Yellowstone Volcano Observatory 2019 annual report
The Yellowstone Volcano Observatory (YVO) monitors volcanic and hydrothermal activity associated with the Yellowstone magmatic system, conducts research into magmatic processes occurring beneath Yellowstone Caldera, and issues timely warnings and guidance related to potential future geologic hazards. This report summarizes the activities and...
Yellowstone Volcano Observatory
History of surface displacements at the Yellowstone Caldera, Wyoming, from leveling surveys and InSAR observations, 1923-2008
Modern geodetic studies of the Yellowstone caldera, Wyoming, and its extraordinary tectonic, magmatic, and hydrothermal systems date from an initial leveling survey done throughout Yellowstone National Park in 1923 by the U.S. Coast and Geodetic Survey. A repeat park-wide survey by the U.S. Geological Survey (USGS) and the University of Utah...
Dzurisin, Daniel; Wicks, Charles W.; Poland, Michael P.
Protocols for geologic hazards response by the Yellowstone Volcano Observatory
The Yellowstone Plateau hosts an active volcanic system, with subterranean magma (molten rock), boiling, pressurized waters, and a variety of active faults with significant earthquake hazards. Within the next few decades, light-to-moderate earthquakes and steam explosions are certain to occur. Volcanic eruptions are less likely, but are ultimately...
Volcano and Earthquake Monitoring Plan for the Yellowstone Volcano Observatory, 2006-2015
To provide Yellowstone National Park (YNP) and its surrounding communities with a modern, comprehensive system for volcano and earthquake monitoring, the Yellowstone Volcano Observatory (YVO) has developed a monitoring plan for the period 2006-2015. Such a plan is needed so that YVO can provide timely information during seismic, volcanic, and...
Steam explosions, earthquakes, and volcanic eruptions -- what's in Yellowstone's future?
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Tracking changes in Yellowstone's restless volcanic system
No abstract available.
Stauffer, Peter H.
The Hebgen Lake, Montana, earthquake of August 17, 1959
Old Faithful Geyser, Yellowstone
Old Faithful Geyser erupts on a clear winter day in Yellowstone National Park
Inside USGS, No. 6, Ken Pierce, Heavy Breathing of Yellowstone Caldera
Dr. Kenneth Pierce studied the geology and geomorphology of the greater Yellowstone area for nearly his entire career with the U.S. Geological Survey. From 1965 to present, Dr. Pierce has mapped glacial deposits, pioneered Quaternary dating techniques, conducted research on the Yellowstone Hot Spot, studied the geothermal areas, explored the geology of archaeological sites
Inside USGS, No. 4, Robert B. Smith
Robert B. Smith of the University of Utah has been collaborating with USGS scientists on Yellowstone geologic topics since the 1960’s. In this interview Bob describes nuances of the Yellowstone volcano story. He shares details of his past and present work and explains how the University of Utah and USGS have a long history of working together on Yellowstone geology.
The Yellowstone Volcano: Past, Present and Future
Public Lecture on Yellowstone Volcano by Jake Lowenstern at Menlo Park, CA on January 23, 2014. The Q&A at the end of the talk can be found on the original source video (Source URL).
Yellowstone Volcano Observatory (Part 2 of 3)
USGS Scientist-in-Charge of Yellowstone Volcano Observatory, Jake Lowenstern, answers
the following questions to provide a tour of the Yellowstone Volcano Observatory: "What is YVO?", "How
do you monitor volcanic activity at Yellowstone?", "How are satellites used to study deformation?", "Do
you monitor geysers or any other aspect of the Park?", "Are
Yellowstone Eruptions (Part 3 of 3)
USGS Scientist-in-Charge of Yellowstone Volcano Observatory, Jake Lowenstern, answers
the following questions to explain volcanic eruptions at Yellowstone: When was the last supereruption at
Yellowstone?", "Have any eruptions occurred since the last supereruption?", "Is Yellowstone overdue for
an eruption?", "What does the magma below indicate about a
Yes! Yellowstone is a Volcano (Part 1 of 3)
USGS Scientist-in-Charge of Yellowstone Volcano Observatory, Jake Lowenstern, answers
the following questions to explain volcanic features at Yellowstone: "How do we know Yellowstone is a
volcano?", "What is a Supervolcano?", "What is a Caldera?","Why are there geysers at Yellowstone?",
and "What are the other geologic hazards in Yellowstone?"
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Seismographs at the U.S. Geological Survey
Seismographs at the U.S. Geological Survey record (1) north-south horizontal, (2) east-west horizontal, and (3) vertical components of the earthquake.