Presentation Title
Using GPS to model slip rate of the San Andreas Fault and other faults within a transect across the plate boundary passing through San Gorgonio Pass
Presentation Type
Poster Presentation/Art Exihibt
College
College of Natural Sciences
Major
Geological Sciences
Location
Event Center A & B
Faculty Mentor
Dr. Sally McGill
Start Date
5-19-2016 1:00 PM
End Date
5-19-2016 2:30 PM
Abstract
Using Global Positioning System (GPS) observations along with a model of elastic motion, the slip rates for the San Andreas Fault (SAF), San Jacinto fault (SJF), and many other faults on the Pacific-North America plate boundary were determined in the vicinity of San Gorgonio Pass. After testing 414,722 slip rate combinations, the slip rate for the San Andreas Fault was determined to be between 4 and 16 mm/yr., with the best fitting slip rate being 8 mm/yr. The slip rate of the San Jacinto fault was determined to be between 6 and 18 mm/yr. with the best fitting slip rate being 18 mm/ yr. Other faults passing through the San Gorgonio Pass transect had slip rates ranging from 0 mm/yr. to 6 mm/yr.
Using GPS to model slip rate of the San Andreas Fault and other faults within a transect across the plate boundary passing through San Gorgonio Pass
Event Center A & B
Using Global Positioning System (GPS) observations along with a model of elastic motion, the slip rates for the San Andreas Fault (SAF), San Jacinto fault (SJF), and many other faults on the Pacific-North America plate boundary were determined in the vicinity of San Gorgonio Pass. After testing 414,722 slip rate combinations, the slip rate for the San Andreas Fault was determined to be between 4 and 16 mm/yr., with the best fitting slip rate being 8 mm/yr. The slip rate of the San Jacinto fault was determined to be between 6 and 18 mm/yr. with the best fitting slip rate being 18 mm/ yr. Other faults passing through the San Gorgonio Pass transect had slip rates ranging from 0 mm/yr. to 6 mm/yr.