Students installing a broadband seismometer. |
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Continous recording and temporary deployments of Global Positioning Systems (GPS) receivers and bench marks on solid monuments are employed at Yellowstone to precisely record their positions (horizontal and vertical coordinates). The time variations over days, months, years, etc. provide the velocity (in cm per year) of the site relative to the rest of the points in Yellowstone and to the rest of the North American continent. The velocity fields thus map spatial variations of the ground due to such volcanic processes as magma and hydrothermal transport and fault motions related to earthquakes. Measurements of ground motions using GPS at Yellowstone thus provides a method of monitoring its active volcanic and tectonic processes that are necessary for understanding the properties and locations of the sources as well as providing information on possible premonitory motions that precede a volcanic or earthquake event.
The continuously recorded GPS data are telemetered via radio and satellite links to the University of Utah for recording and processing.
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A GPS campaign survey at Yellowstone. |
River-Discharge and Chloride-Concentration Data
Analysis of long-term river discharge and chloride concentrations in major rivers in Yellowstone provide a quantitative estimate of the total heat discharge from the Yellowstone volcanic system and can also be examined for temporal trends associated with magmatic and tectonic activity. Learn more.
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Tantalus gauging site. |
Thermal-Feature Data
Leveling survey at Yellowstone. |
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Descriptions of volcano-monitoring techniques |