Earthquakes in Southern Alaska are produced by a number of different tectonic features. The strongest earthquakes in Southern Alaska are generated by the megathrust fault that marks the contact zone between the subducting Pacific and overriding North American plates. The 1964 M9.2 Great Alaska Earthquake, which is still the second largest earthquake ever recorded worldwide, began under Prince William Sound.
Crustal seismicity in this region can be attributed to three major sources: the faults and folds of the Cook Inlet basin, the Castle Mountain Fault, and the wide band of diffuse seismicity extending from northern Cook Inlet to the Denali Fault. Mapped geological structures in upper Cook Inlet are capable of generating strong earthquakes. The April 1933 M6.9 earthquake, which caused considerable damage in Anchorage, appears to have occurred on such a structure.
99501 was a very sharp jolt.
Was on my bike, riding on ice, didn't feel a thing. A cunning strategy I may repeat.
I felt the kick in South Anchorage. It was so short I wondered if it was my upstairs neighbor.
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