Assessing Seismic Tomography Models of Alaska
Aracely Garcia
2101
Alaska is positioned on a convergent plate boundary, where the Pacific Plate is being subducted underneath the North American Plate, with a convergence rate of 7.8 to 5.5 cm/yr from Near Islands region to the Gulf of Alaska along the Aleutian-Alaska Trench. The plate movement has resulted in Alaska’s mountains, volcanos, and frequently occurring earthquakes at high magnitudes. Seismic tomography images of the upper mantle’s seismic structure of Alaska are used to better understand the geological processes in subduction zones, including earthquakes, volcanoes, and crustal deformation in Alaska. By comparing multiple seismic velocity models in this region, we will be able to better understand the earth structure under Alaska to better assess earthquake and volcano hazards.
S. Shawn Wei
Enter the password to open this PDF file.
-
-
-
-
-
-
-
-
-
-
-
-
-
-