Geological specialists explore the reason for offering a mistake in Utah to earthquakes

Its length is about 240 miles, and a mistake in Utah is running throughout the western edge of the mountains and Asch from southern Idahu to the center of Utah, and passes through the Solt Lake City and other population centers in the state. It is an active natural mistake in terms of earthquakes, which means that it is a broken Earth's crust that has moved several times in the past.

“Natural errors are observed along the various tectonic systems, where tectonic panels move from each other,” says Sercharan Sherradran, a geophysic scientist at Utah State University. “Wasatch is the eastern edge of the pelvis and the geological boycott, which has spanned and broken over millions of years.”

Crehararan, an assistant professor at the Department of Geographic Sciences at USU, says that natural errors seem to be two paintings of rocks, where one plate, the “suspended wall” moves, below for the other slab, “wall of shoes”.

“The angle of decline in the sliding surface tends to be very slope, and it often ranges between 45-90 degrees,” he says. “Wasatch's mistake, towards the west, is drowned at a high -end angle on the surface in the Salt Lake City area.”

A very slope angle can mean seismic activity that may be mitigated during an earthquake, reserve residents and buildings of many injuries and damage to the surface.

“But the Magna earthquake in 2020, which occurred about 9 kilometers deep in the west of Salt Lake City, caused injuries and led to nearly $ 50 million in property damage,” says Sharraran. “It was a awakening call.

With the professor participating in USU Alexis Out and PhD student Jordan Jensen, Sharraran has published new results about the cause of earthquakes along the WASATCH error and why societies along the mistake are more vulnerable to earthquake damage than previously thought. Their paper appeared on the April 25th version online of geology, the Journal of the Laysee review of the American Geological Association. The research is supported by the American geological survey risk program.

Using the collected rock samples, Sherraran merged experiments and analysis into a rock deformation laboratory and earthquake mechanics with AULT investigative experience in earthquake geology and rock consistency in the USU microscopic facility. Their research has revealed great evidence about the risk of a Wasatch error.

“Although the Wasatch error decreases sharply in the Salt Lake City, it bends greater gently on the depth while moving it west and may be directed at a shallow angle on the depth of the earthquake than expected,” says Sharran. “This means that the earthquake rupture may lead to stronger and more intense shaking on the surface – this means a greater chance of infection and destruction.”

Moreover, scientists have discovered the earthquake's earthquake possible along the shallow part of the WASATCH error because the rock rock themselves are much weaker – worn out and melted – of not harmful rocks.

“It turns out that this weak frictional behavior, which we described as distorting and microscopic experiences, is the product of deformation that happened more than 1.7 billion years ago when the diamond's mistake was now in greater depths inside the earth,” says Awal. “Repeated earthquakes have since modified the characteristics of the rift over time, which leads to the failure of rock rocks again in a future event.”

Sharkran says that understanding how one rock is weaker than others, says Sherradran, such as comparing the ice with sand.

“You can imagine how slow rocks can slide more easily and at an angle less than the rock with a rough surface,” he says. “This process occurs continuously, despite the very slow pace, under our feet.”

AULT ​​says that Usu, with its multidisciplinary team, is an earthquake and engineer, in a unique position to study the history of the Yutta State earthquake, future risks and help in building flexibility.

“Through our latest facilities and research synergy, we are ready to face the challenges of the state,” she says.

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