- Earthscope
The EarthScope project is an undertaking funded by the
National Science Foundation in partnership with theUSGS andNASA to characterize the geology ofNorth America . EarthScope is composed of three projects:USARRAY , thePlate Boundary Observatory PBO and theSan Andreas Fault Observatory at Depth (SAFOD).The instrumentation of
USARRAY consists of a series of portable and permanent seismometers that are being installed over a 10 year period beginning in2004 . The goal of USARRAY is primarily to gain a better understanding of the structure and evolution of thecontinental crust ,lithosphere , and mantle underneath North America.The
Plate Boundary Observatory PBO consists of a series ofgeodetic instruments:Global Positioning System (GPS) receivers and borehole strainmeters that are being installed to help understand the boundary between the North American and Pacific plates. The backbone includes a network of more than 130 GPS receivers that will cover, when completed, the western continental US, includingAlaska , at a receiver spacing of 200 km and the eastern US at a receiver spacing of 500 km. A series of focused dense clusters of 775 permanent GPS receivers and 175 strainmeters are being installed along fault zones andvolcanoes in westernNorth America andAlaska . These permanent networks are supplemented by a pool of portable GPS receivers that can be deployed for temporary networks, to measure the crustal motion at a specific target or in response to a geologic event. The Plate Boundary Observatory portion of EarthScope is operated by UNAVCO, Inc, a non-profit organization that supports research applications of high-precisiongeodesy .The San Andreas Fault Observatory at Depth (SAFOD) consists of drilling a hole across the active
San Andreas Fault at a depth of approximately 3 km. Samples collected during drilling, as well as data from instruments installed in the hole, will help to better understand the process that control the behavior of theSan Andreas Fault .Some scientific questions that are being addressed by the EarthScope project and the PBO include [National Research Council, "Review of EarthScope Integrated Science" (Washington D.C., National Academy Press, 2001). ] :
* How does accumulated strain lead toearthquakes ?
* Are there recognizable precursors to earthquakes?
* How does the evolution of thecontinent influence the motions that are happening today?
* What happens togeologic structures at depth?
* What influences the location of features such as faults andmountain ranges ?
* Is it inherited from earlier tectonic events or related to deeper processes in the mantle?
* How ismagma generated? How does it travel from the mantle to reach the surface?
* What are the precursors to avolcanic eruption ?External links
Information on EarthScope
* [http://www.earthscope.org The EarthScope web page]
References
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