This earthquake is located just north of the aftershock zone of the September 12, 1966 Truckee earthquake. That 1966 earth- quake had a magnitude of 6.0.
The data reported here are preliminary. For more information, contact the Seismological Laboratory at (702) 784-4975, or at the WWW site http://www.seismo.unr.edu . The free pamphlet Earthquakes in Nevada and How to Survive Them, is available on request.
We received a number of reports from people who felt the explosion. Probably what most people felt is the air wave which the explosion generated. This air wave shook the ground also, and at our stations the signal from the air wave is larger than the waves that traveled through the earth. This is typical of explosions above the ground surface. The air wave travels relatively slowly, taking about 5 seconds to travel a mile. It was recorded at least as far away as our station south of Gardnerville, as well as all stations closer to the explosion. In the air wave, we see two distinct pulses separated by about three seconds.
The data reported here are preliminary. For more information, contact the Seismological Laboratory at (702) 784-4975, or at the WWW site http://www.seismo.unr.edu . The free pamphlet Earthquakes in Nevada and How to Survive Them, is available on request.