The Denali Fault is a strike-slip fault, a place where two chunks of continental crust slide past each other. On Nov. 3, 2002, the fault jolted, creating a magnitude 7.9 earthquake that knocked ...
The Denali Fault is what scientists call a strike-slip fault. This is essentially a place where two chunks of the continental crust slide past each other. While this fault has been the birth of ...
"Our understanding of lithospheric growth—or plate growth—along the western margin of North America is becoming clearer, and a big part of that is related to reconstruction of strike-slip ...