The UNRWA Laboratory tracks 6,500 aftershocks

Two weeks after the Monte Cristo earthquake woke up to 6.5 on the Nevada scale, the Nevada Earthquake Laboratory said it tracked 6,500 aftershocks, including four degrees of magnitude 5.0 or more.

“The aftershocks can last for years and a decade,” said Ken Smith, director of the Seismic Network and associate director of the Nevada Seismology Laboratory at the University of Nevada, College of Science in Reno. “The major earthquakes that occurred in 1954 in December of that year preceded a series of earthquakes of great magnitude and following the aftershocks that started in July. So this may be an indication that this is not over.

“Fortunately, today we have real-time data to monitor the progress of activity that may indicate another major event. However, keep in mind that each series of these active aftershocks after large earthquakes in Nevada is evolving in its unique ways.”

The U.S. Geological Service, which partnered with the Nevada Seismology Laboratory to monitor seismic sequences, estimated that in the week ending June 6 there was a 99% chance of a 3 or higher earthquake with up to 22-49 events and a 1% chance of a 7 earthquake or Larger.

Within minutes of 4:03 am in the Monte Cristo earthquake on May 15, the lab began checking the automatic notification of the largest earthquake in Nevada 65 years ago and worked with USGS to communicate data to the public. It also started to move a series of activities to bring lab members to the event site to develop additional seismometers to better monitor the activity.

Eight makeshift temporary seismographs and a local microwave telemetry system were installed, starting from day one, which returns data directly to the university on a state-level microwave network at the seismic laboratory. Other partnership agencies, including USGS, Mission Support and Test Services from Nevada National Security, have installed additional hardware.

“The addition of additional tools is very important,” Smith said. “We are trying to obtain optimal coverage to achieve the best event locations. The area of ​​the aftershocks is about 12 miles, and the tools are now located inside and outside the aftershocks area, to get the best coverage.”

So far in this sequence, there have been 284 earthquakes of magnitude 3 or higher, which are strong enough to feel, and four earthquakes of magnitude 5 or higher, which are large enough to cause damage and the rate of aftershocks higher and slow below average for aftershocks in similar areas around the world.

The Nevada Geodesic Laboratory, a unit at the University’s Nevada Mines and Geology office, continues to measure continuous deformation in the Earth’s crust. They use GPS satellites and earth stations to study tectonic motion. Because of the work they did weeks ago, they had sensors on the ground and logging data into the area when the event happened. So far they have seen a permanent movement of the Earth more than 120 miles from the epicenter.

The lab is deploying additional GPS stations in 30 locations around the epicenter and following the earthquake regression. All of these stations will be visited several times in the coming months to download continuous notes.

Nevada is the third most seismically active state in the country after Alaska and California. The Walker Lane is a seismically active area 60 miles wide and bordering Nevada and California. Walker Lane starts in the Mojave desert in southern California and extends east from Sierra Nevada, north through western Nevada in the Reno region, and then to northeastern California.

“We can expect earthquakes in Nevada,” said Jim Foulds, director of Nevada Mines and Geology at the College of Science. “It happened for millions of years in Walker Lane.”

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