The epicenter is just north of the Palisades Group of peaks on the eastern boundary of Kings Canyon National Park. They are the snowy glaciated peaks in the picture above. Big Pine is just to the left of the picture on the valley floor.
|4.8 magnitude main shock|
The fault that produced the quake shows right lateral strike slip motion. This means that the two sides of the fault moved sideways relative to each other, with the southwest side of the fault moving northwest. Since the Owens Valley is a fault graben, one might assume that the fault motion should have been vertical, i.e. lifting the mountains or dropping the valley, but the Sierra Nevada as a structural block is moving northwest relative to the rest of the continent, so this quake is consistent with that motion.
|Sierra Nevada as a "microplate" moving northwest. Big Pine is labeled BP. Source: http://tahoequarterly.com/Features/Story/ice-fire-and-granite|
The regional is seismically active. One of California's great historical earthquakes had an epicenter a short ways to the south at Lone Pine. The 1872 event had a magnitude estimated to be as high as 7.9. The quake killed 27 people, nearly a tenth of the population of the village at the time. Ground ruptures extended from Owens Lake to north of Big Pine.
|The 4.3 magnitude aftershock|
Our seismometer is a simple classroom instructional model (from Wards Scientific), but we get good results with local quakes of moderate magnitude, and larger quakes worldwide.
The U.S. Geological Survey event page for the magnitude 4.8 quake can be seen here: http://earthquake.usgs.gov/earthquakes/eventpage/nc72592670#general_executive