Excavated trenches reveal two faults that bound the eastern flank of the Sierra Nevada in Antelope Valley, California and the Carson Range in Reno, Nevada; a new model changes predictions of amplified ground motion in Seattle basin.
Excavated trenches reveal two faults that bound the eastern flank of the Sierra Nevada in Antelope Valley, California and the Carson Range in Reno, Nevada; a new model changes predictions of amplified ground motion in Seattle basin.