ΒιΆΉΣ³»­

Thousands of 2015 ΒιΆΉΣ³»­ Earthquakes

ΒιΆΉΣ³»­ earthquake expertise spans the globe

1915 Pleasant Valley Earthquake

This 1915 photo shows an earthquake fault rift crossing a stream at Pearce Ranch, showing old and new fault scarps. The 1915 surface rupture crossed a stream here and formed a waterfall 10 feet high behind the man. The stream was flowing four times its normal flow because of some new springs that were opened by the earthquake. (Jones, 1915)

Thousands of 2015 ΒιΆΉΣ³»­ Earthquakes

ΒιΆΉΣ³»­ earthquake expertise spans the globe

This 1915 photo shows an earthquake fault rift crossing a stream at Pearce Ranch, showing old and new fault scarps. The 1915 surface rupture crossed a stream here and formed a waterfall 10 feet high behind the man. The stream was flowing four times its normal flow because of some new springs that were opened by the earthquake. (Jones, 1915)

1915 Pleasant Valley Earthquake

This 1915 photo shows an earthquake fault rift crossing a stream at Pearce Ranch, showing old and new fault scarps. The 1915 surface rupture crossed a stream here and formed a waterfall 10 feet high behind the man. The stream was flowing four times its normal flow because of some new springs that were opened by the earthquake. (Jones, 1915)

More than 17,500 earthquakes were recorded in 2015 by the ΒιΆΉΣ³»­'s ΒιΆΉΣ³»­ Seismological Laboratory. That includes the 231 recent quakes in south Reno and the magnitude 4.8 in Caliente that shook Las Vegas in January 2015.

"While the Reno shaking is fresh in our minds, what's really bumping the number up from the background rates is the energetic sequence in far northwestern ΒιΆΉΣ³»­, the Sheldon sequence," Graham Kent, director of the said.

Through 2015 there have been 4,511 earthquakes recorded in the remote Sheldon Wildlife Refuge near Vya, east of Cedarville, California. The earthquake activity that began there in July 2014 has produced 234 earthquakes greater than magnitude 3.0, and 24 earthquakes of magnitude 4.0 or larger, including the largest, a magnitude 4.8 on Sept. 14 and a magnitude 4.6 just before Christmas this year.

That leaves more than 13,000 other ΒιΆΉΣ³»­ and eastern California earthquakes, including swarms as well as less prolonged mainshock-aftershock sequences in Caliente, Carson City and Virginia City. Outside of the persistent Sheldon sequence, ΒιΆΉΣ³»­ was hit with 54 magnitude 3 or greater earthquakes or about one per week.

Overall, there have been 19 earthquakes of magnitude 4.0 and larger and the University's seismological lab has reported 160 earthquakes between magnitude 3.0 and 3.9.  

"The south Reno swarm that just happened produced about 30 earthquakes in two days and about 200 more in the days that followed," Kent said. "For our entire network, we are averaging about 50 located earthquakes a day."

They aren't all part of identifiable swarms like Sheldon, South Reno or Virginia City.

"Many of the earthquake clusters in the Walker Lake area in 2015 were more typical sequences and not like Sheldon that has now continued for more than a year," Ken Smith, associate director of the ΒιΆΉΣ³»­ Seismological Lab said. "Just as the Caliente 4.8 that startled Las Vegas in May or the 4.8 at Scotty's Castle at Death Valley in February with their fairly extensive aftershocks, in ΒιΆΉΣ³»­ we wouldn't be surprised to see a significant event anywhere."

The ΒιΆΉΣ³»­ Seismological Lab is a public service and research department in the University's tasked by the State of ΒιΆΉΣ³»­ to operate a monitoring network and report earthquake information for activity throughout the state. The Seismology Lab's data are provided to the USGS, other national data centers and shared with adjacent network operators in California, Utah, Washington and Oregon.

"All of our earthquake data are fed to the USGS," Smith said. "We work with the ΒιΆΉΣ³»­ Department of Emergency Management, county emergency managers, FEMA and even the California Office of Emergency Services. We have special reporting requirements for magnitude 3 and higher quakes. We had 179 earthquakes of magnitude 3.0 and larger in 2015, the most of any seismic network operation in the lower 48."

The lab operates, maintains and monitors 185 real-time seismograph stations across ΒιΆΉΣ³»­ and along the Sierra ΒιΆΉΣ³»­ mountain range of eastern California. The seismological lab crew has been upgrading and expanding the network, including adding 15 broadband stations in southern ΒιΆΉΣ³»­ this year and are looking for funding to match or exceed that expansion rate in 2016.

"We're looking to the USGS, State of ΒιΆΉΣ³»­ and others for support to bring seismograph coverage to more of the state," Kent said. "What we've done for the Vegas area already has been critical for our response capabilities in southern ΒιΆΉΣ³»­ Despite the number of earthquakes we track - compared to other western states - support for statewide earthquake monitoring in ΒιΆΉΣ³»­ is far below that of similar western U.S. seismic networks. That said, we've added new analysts and reorganized our 24/7 monitoring team to keep up with the volume. But maintaining this level of effort isn't really sustainable without additional funding."

Worldwide Research
The Seismological Lab, a 24/7/365 operation, has about 30 faculty, researchers and graduate students who support the earthquake monitoring as well as conduct outreach and research in ΒιΆΉΣ³»­, nationally and internationally to better inform disaster managers, policymakers and the general public about seismic hazards.

In addition to numerous geophysical studies of faults in ΒιΆΉΣ³»­, the researchers have projects in California, the Pacific Northwest, Japan, New Zealand, Australia and the Himalayas.

They've tracked and studied fault lines throughout the west, including pioneering work defining underwater fault systems in Lake Tahoe, the Salton Sea and Pyramid Lake and along the entire Pacific coastline from Mexico to Canada using a high-resolution, state-of-the-art seismic imaging system.

In May of this year, following the April 25 Gorka earthquake in Nepal, ΒιΆΉΣ³»­ Seismological Lab researcher and professor Steve Wesnousky was one of the first scientists to enter the region to search for geophysical signs of the 7.8 earthquake. He is one of the world's leading scientists on the hundreds-of miles-long Himalayan fault, having studied it for more than 15 years.

College of Science Dean Jeff Thompson and Kent cobbled together some funding and sent Wesnousky's two graduate students to Nepal to assist him in the studies.

"This was a unique window to understand what a surface rupture might look like 'fresh' as compared to a trench looking at paleoearthquakes," Kent said. "The information they gathered helps us understand other thrust faults around the world, such as in the Los Angeles basin, and what the surface deformation associated with these large earthquakes might look like."

The seismological lab team met with colleagues from the local university and spent two weeks searching for surface ruptures and other geophysical signs. Their work and travels were chronicled in a daily blog on the College of Science website.

"We have a variety of research projects underway here in ΒιΆΉΣ³»­ that helps inform the world as well," Kent said. "With the Sierra ΒιΆΉΣ³»­ range extending away from us, and the unique structures we find in the Great Basin, it's not surprising ΒιΆΉΣ³»­ is the third most seismically active state in the country."

Though the third most seismically active state behind California and Alaska, ΒιΆΉΣ³»­ has not had a magnitude 7.0 earthquake in 60 years.

Great ΒιΆΉΣ³»­ Earthquake
This year marks the 100-year anniversary of the largest recorded earthquake in ΒιΆΉΣ³»­, with a magnitude 7.3 that left a 35-mile-long surface scar with a vertical offset as high as 19 feet in one area and numerous large cracks in the earth.

"The Pleasant Valley earthquake caused damage to multiple communities that were as far as 50 miles away," Craig dePolo, an earthquake geologist with the ΒιΆΉΣ³»­'s ΒιΆΉΣ³»­ Bureau of Mines and Geology, said. "This illustrates that large earthquakes cause widespread damage and can affect many communities at the same time. It was felt throughout ΒιΆΉΣ³»­ but the most damage was in Winnemucca, the closest town; with nearly half the chimneys damaged, walls collapsed and windows broken."

The Great ΒιΆΉΣ³»­ Earthquake ushered in a period of significant quakes that hasn't been matched in 60 years.

"The first 54 years of the 20th century we had seven earthquakes of magnitude 6.5 or larger and haven't had one since," Kent said. "We haven't had the big one since the Dixie Valley/Fairview Peak sequence in 1954 east of Fallon, which was two magnitude 7s four minutes apart. Since then, ΒιΆΉΣ³»­'s population has grown 13-fold."

The magnitude 6.0 Wells, ΒιΆΉΣ³»­, earthquake in 2008 has been the largest event in ΒιΆΉΣ³»­ in 42 years. Historically, ΒιΆΉΣ³»­ can expect to have three magnitude 7.0 earthquakes per century and one magnitude 6.0 or larger every decade, Kent said.

The lab also runs the Great ΒιΆΉΣ³»­ ShakeOut, a statewide "drop, cover and hold-on" earthquake drill, and helped grow participation by more than 60,000 in 2015, with some 630,000 ΒιΆΉΣ³»­ns participating in this year's sixth annual drill.

Although earthquake monitoring is a critical part of the lab's mission, the hope during the next several years is to help ΒιΆΉΣ³»­ become a more economically resilient community to earthquakes and other natural disasters such as wildfire, Kent said. Examples of this new focus are the AlertTahoe and BLM fire camera programs that leverage multi-hazard early-warning strategies to help detect wildfire ignition at its inception to help knock down fires before they become large. The ΒιΆΉΣ³»­ Seismological Lab was involved with more than 25 fires in 2015 providing either discovery and/or early intel to fire response managers.

This expansion into fire detection will ultimately help build out the earthquake network into critical areas of the state.

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