Earthquake error near Tonoba still active after aftershocks 6,500 | Carson City Nevada News

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The surface rupture, drawn by the University of Nevada by Reno Field teams, extends approximately six miles west of Interstate 95.

Reno – An earthquake of 6.5 magnitude in Monte Cristo near Tonoba is still renewed. Two weeks after Nevadans woke up, the Nevada Seismic Laboratory tracked 6,500 massive aftershocks – four at a strength of 5.0 and greater, from the quake sequence.

“The aftershocks may last for years and a decade,” said Ken Smith, director of the Seismic Network and assistant director of the Nevada Seismology Laboratory at the University’s College of Science. “The major earthquakes of 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 “Activity progress that may indicate another major event. However, keep in mind that each of these series of active aftershocks after major earthquakes in Nevada is evolving in its unique ways.”

The U.S. Geological Survey, which partners with the Nevada Seismological Laboratory to monitor seismic sequences, estimates that in the week to June 6, there is a 99 percent chance of a 3 or higher earthquake with up to 22-49 events like this, a chance of a magnitude of 5 and more Above it is 39 percent with an opportunity for up to three of these, its strength is 6 and above 6 percent with a possibility of having two in this range and a chance of 7 or greater is 1 in 100 such an earthquake is possible but with a low probability.

Within minutes of 4:03 am the Monte Cristo earthquake on May 15, members of the University of Nevada, the seismology laboratory in Reno, were at full speed. The lab began validating their automatic notification of 6.5 shaker, the largest in Nevada in 65 years, 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.

Installation of temporary seismographs Eight temporary seismographs and a local microwave telemetry system were installed, starting from the first day, which returns data directly to the university via the microwave network at the state-level 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, four earthquakes of magnitude 5 or higher, which are large enough to cause damage and the rate of aftershocks higher and slow down than the average of aftershocks in similar areas around the world.

University geologists also draw error after a 6.5-magnitude earthquake early in the Monte Cristo earthquake on May 15, geologists from the University’s Nevada Mines and Geology office quickly prepared for a road trip. Led by the office’s Rich Koller, geologists, seismologists from the office, the Nevada Seismology Laboratory, the USGS, and the California Geological Survey mobilized field teams and traveled to the earthquake epicenter in a remote area southeast of the small town of Mina and about 35 miles from Tonopah.

Teams identified and recorded surface tears, displacements, and other field observations. Geologists looked forward to a description and a map of how rupture affected the Earth’s surface: by taking measurements, images, and GPS points from cracks along the fault lines across the desert.

“The surface torn by the field teams runs 10 km west of Interstate 95,” Koehler said. “It is interesting that only minor surface cracks were observed just east of Interstate 95 near the epicenter. Efforts are under way to better determine the eastern end of the surface rupture. The lateral left compensation ranged from about 5-15 cm, but an average of about 10 cm. Note a vertical displacement of up to 10 cm in some traces of the malfunction.

Kohler joined Geologists Seth D. and Craig DePulo, also from the Nevada Bureau of Mines and Geology, Steve Wisnowski of the Nevada Seismology Laboratory and Ian Pearce Geologist recently completed a PhD in the Department of Geosciences and Engineering.

“I was in the central area before 3:30 pm,” Kohler said. “We camped out during the entire field response just above the epicenter of the earthquake. Not only was the epicenter more than 20 miles from the nearest hotel, but camping provided a better position to preserve the social dimension that the university requires. Plus, it was great to feel and hear Hundreds of aftershocks beneath us. “

The Office of Mines and Geology collects observations from different teams in a comprehensive map of surface rupture.

Use of GPS satellites to track the movement of the Earth’s crust The Nevada Geodetic Laboratory, a unit at the University’s Nevada Mines and Geology office, continues to measure the continuous deformation of crustaceans in the region. 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 logged data into the area when the event happened, and captured it in action. So far, they have seen a permanent movement of the Earth 120 miles from the epicenter.

“The Nevada Geodetic Laboratory was constantly observing the event during our survey and was on the ground deploying temporary stations a few days after the event,” Kohler said. “Geological field efforts have been greatly assisted by the rapid availability of InSAR data processed by USGS, JPL and other researchers and shared with real-time field survey teams. This has helped us focus on areas that have been torn off by the surface.”

The lab is deploying additional GPS stations at about 30 locations around the epicenter and the sequence of aftershocks of the Monte Cristo Ring M6.5 earthquake on May 15, 2020. All of these stations will be visited several times in the coming months to download continuous notes.

“This 6.5 magnitude earthquake happened well inside this dense network of stations,” Beloit said. “Without this dense network, we will not be able to learn as much as we learn from this earthquake. We have about 50 mobile GPS units, so we transfer units to collect data at all stations.”

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 mines and geology of Nevada, College of Science. “It happened for millions of years in Walker Lane.”

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