A pair of earthquake sequences, in September 2018 and April 2019, focused scientists' attention on the Black Rock Desert. The sequences, which included the main quakes and their aftershocks, were very different from the Magna earthquake that shook the Wasatch Front in 2020 and other Utah earthquakes. The Black Rock sequences were captured by the Utah Regional Seismic Network and by nearby temporary seismic equipment deployment that was monitoring a geothermal well. Earthquakes in the Black Rock Desert are rare and capturing the seismic recordings from these earthquakes provides a glimpse into the volcanic system of the Black Rock Desert that, while not showing any signs of erupting, is still active. A study of the earthquake sequences is published in Geophysical Research Letters.

"The results showed us that we should give more attention to the Black Rock area," says Maria Mesimeri, a postdoctoral research associate with the University of Utah Seismograph Stations. "We need to improve seismic and volcanic monitoring in this area, so that we are aware of small changes that may occur."

Not your typical earthquakes

The earthquake sequences, with main shocks of magnitude 4.0 and 4.1 respectively, were picked up by both the Utah Regional Seismic Network and a dense temporary network of seismometers deployed as part of Utah FORGE, an experimental geothermal project funded by the U.S. Department of Energy and operated by the University of Utah, located about 19 miles south of the Black Rock Desert near Milford, Utah. The temporary network allowed researchers to detect more aftershocks than usual. For example, the regional network detected 19 earthquakes as part of the April 2019 sequence. But the dense temporary network detected an additional 35 quakes. Each additional aftershock provided a bit more information for seismologists studying the sequence.

The Black Rock sequences showed some interesting features that set them apart from the 2020 Magna sequence and other Utah earthquake sequences. While the initial Magna quake occurred at a depth of about six miles below the surface, a typical depth for Utah earthquakes, the Black Rock quakes were much shallower -- around 1.5 miles below the surface.

"Because these earthquakes were so shallow," Mesimeri says, "we could measure surface deformation [due to the quakes] using satellites, which is very unusual for earthquakes this small."

Also, Mesimeri and her colleagues found, the quakes produced much lower-frequency seismic energy than usually seen in Utah quakes. And one of the main types of seismic waves, shear waves or S-waves, wasn't detected in the Black Rock sequences.

Volcanoes? In Utah?

All of these signs point to the Black Rock sequences having a very different origin than the Magna sequence, which was generated by movement of the Wasatch Fault. The Black Rock quakes, on the other hand, may have been generated by ongoing activity in the Black Rock volcanic field.

What are volcanoes doing in the middle of Utah? The Wasatch Mountains (and Wasatch Fault) form the eastern margin of a region called the Basin and Range province that stretches west to the Sierra Nevada. The province is being stretched apart by plate tectonics, and that stretching thins the crust, allowing more heat to rise up from the Earth's interior. In the Black Rock area, that heat resulted in eruption of basalt lava up until around 9,000 to 12,000 years ago.

So what do these earthquake sequences mean for the volcanoes of the Black Rock Desert?

"Our findings suggest that the system is still active and that the earthquakes were probably the result of fluid-related movement in the general area," Mesimeri says, referring to potentially magma or heated water. "The earthquakes could be the result of the fluid squeezing through rock or the result of deformation from fluid movement that stressed the surface faults."

Activity in a volcanic field does not mean eruption, and Mesimeri says that there's no evidence that any eruption is imminent in the Black Rock Desert. But, she says, it's an area that geoscientists may want to monitor a little more closely.

Story Source:

Materials provided by University of Utah. Original written by Paul Gabrielsen. Note: Content may be edited for style and length.

Journal Reference:

1. Maria Mesimeri, Kristine L. Pankow, William D. Barnhart, Katherine M. Whidden, J. Mark Hale. Unusual Seismic Signals in the Sevier Desert, Utah Possibly Related to the Black Rock Volcanic Field. Geophysical Research Letters, 2021; 48 (5) DOI: 10.1029/2020GL090949