GORDA PLATE STRUCTURE & TECTONICS
Investigators: Jason Chaytor, Chris Goldfinger & Robert Dziak
 

June 14th 2005 Magnitude 7.2 & June 16th 2005 Magnitude 6.7
Gorda Plate Earthquakes

Click here to read OSU Press Release

Bathymetry compilation and structural interpretation by Jason Chaytor
OSU Active Tectonics and Seafloor Mapping Lab,
Earthquake locations from USGS NEIC, centroid moment tensors from Harvard CMT database (dates are local).
Updated June 20, 2005



Preliminary comparison of the moment tensors to the known structures within the Gorda
plate strongly suggest the earthquakes occurred on a NE-trending left-lateral strike-slip faults.  It appears from the bathymetry
that the causitive faults are buried by sediments and situated along the trends of mapped strike-slip faults in the epicentral areas.




3-Dimensional view of the Gorda plate shaded-bathymetry looking toward the northeast from the location
of the Gorda Ridge - Mendocino Fracture Zone intersection, showing the location of the June 2005
Magnitude 7.2 and 6.7 earthquakes




Where is the Gorda Plate?
Results of Gorda Plate Structural Mapping

Home     Contact Us

Oregon State University
College of Oceanic and Atmospheric Sciences
Marine Geology and Geophysics
104 COAS Admin. Building
 
Corvallis, OR 97331, USA

ph +1 541.737.5214
fax +1 541.737.2064
email gold@coas.oregonstate.edu
  Back to the Active Tectonics Home Page