The Reno earthquakes of 2008, also known as the "Mogul-Somersett Earthquake Sequence", are an unusual swarm of earthquakes which are occurring in or near the western Reno, Nevada suburbs of Mogul and Somersett. The quakes began in February 2008, but the first significant quake of the series occurred on April 15, 2008, registering a 3.6 magnitude. On April 24, 2008, two quakes in the same area registered 4.1 and 4.2. On April 25, 2008, the quake of largest magnitude occurred, registering 4.7 on the Richter scale and causing damage in the immediate area around the epicenter, including destroying 200 feet of a wooden flume suppling water from the Highland Ditch, also known as the Highland Ditch flume. The flume carried up to 50 million US gallons (190,000 m3) a day from the Highland Ditch to Reno's Chalk Bluff Water Treatment Facility and another 5 million US gallons (19,000 m3) to area irrigation users. In addition to these significant quakes, hundreds of smaller ones have also occurred in the same area. This event is significant because no known dominant fault line has been responsible for the earthquake swarm occurring in the region. It is also highly unusual because the quakes have, for the most part, been limited to a three mile area. The USGS estimates that over 620 earthquakes have occurred in the general three mile vicinity since the swarm has been monitored.
Seismologists with the USGS as well as the Nevada Seismological Laboratory expressed concern that the increasing magnitude of the felt quakes may indicate that a larger earthquake is imminent. As yet, they have not identified the particular tectonics involved with these earthquakes. However, they have stated categorically that volcanic activity is not involved.[1]
The last "major" earthquake in the Reno area in occurred on April 24, 1914, registering 6.1; the state's most powerful quake to date was a magnitude 7.4 quake south of Winnemucca, in 1915. [2]
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