Monitor non -joke signals on the Yellowston earthquake network

Yellowstone Caldera Chronicles is a weekly column written by scientists and collaborators at the Yellowston Berkano Observatory. The contribution of this week is Jimmy Farrell, a professor of research in university stations at Utah University, and a chief earthquake at the Yellowstone Observatory.

It is known that the 1500 and 2500 earthquakes are one of the most active areas in the western United States, a Yellowstone seismic network designed to record the land shakes these earthquakes and sends data again to Utah University in real time For analysis. There are many other things that cause the earth to be shaken, and this shaking is recorded by and around the seismic stations in Yellowston. Most of the time, it is easy to distinguish between these signals from those in real earthquakes.

So, what is on the side of earthquakes that make the earth shake in Yellowston?

Webicorders for YMR YMR (Western Entrance Road) and YNM (Norris Geyser) show traffic lights (left) and visitors walk (right) during daylight hours. Both records run 24 hours from July 23, 2024, MDT.

Some of the most common reasons for shaking the non -earthly earth are the humans and the compounds they lead. As a general guidance principle, seismic stations are located away from the roads to avoid these signals, but some are close enough to record each car/truck/bus that drives them. A seismic station is located near the Madison West entrance road, which was appointed in YMR, is famous for recording the road noise. In addition, a seismic station located in the Norris Geyser Basin Museum (appointed YNM) is recorded thousands of visitors who walk every day during the summer. Signs related to human activity can be identified through their spread during daylight hours and their absence during the night hours.

Signals registered at the YDD station at Yellowstone National Park of the Honga Tonga -Honga Volcano Puriture. The YDD earthquake scored both the direct seismic stage (the top of the left) as well as the wave of the sheep in the atmosphere associated with the Earth when it spreads (the top right). The microphone under the infection of the YDD infection recorded the atmosphere of the sheep wave (the bottom of the right) that arrived in Yellowston ~ 9 hours after the explosion. Seismic waves are transmitted across the Earth much faster than the audio waves that are transmitted across the air, explaining the long delay in the timing between when the signals were recorded.

Significance can be seen signals related to non -alitori geological events that are far from Yellowstone. An example of this is the Hunga -Hunga -Hunga Haʻapai 2022 in the South Pacific. Volcano is about 9742 km (6,053 miles) from Yellowston National Park, but signals from this violent explosion are clearly seen in many stations in the Yellowstone seismic network. In fact, this explosion produced two clear signals in the Yellowstone earthquake record. The first sign is the direct P (seismic stage) that traveled across the ground from the eruption site to Yellowon-and the wave reached about 27 minutes after the eruption. The eruption also produced waves in the atmosphere. The most of these waves in the atmosphere were something called the wave of sheep, which traveled across the atmosphere but along the surface of the earth. Mutlaws traveled from the explosion around the Earth 4 times over a period of 6 days. The first of them arrived in Yellowston ~ after 9 hours of the explosion – which extends the sound speed, which is much slower than the earthquake velocity across the ground – and it is clear on both the earthquake measuring devices and lower microphones. This indicates that with the widespread wave of the sheep along the surface of the earth, it did not only cause an atmosphere disorder (as the microphone recorded under the red) but the energy was also transferred to the ground (as the earthquake scale recorded). In this sense, the wave was similar to a sound mutation or Thunderclap.

Sometimes other signs other than Erthquake are recorded on earthquake measuring devices around rivers due to the earth's vibration of large floods in Yellowston, such as those that occurred in June 2022. Near Yeloston Lake, “ice” earthquakes are recorded from breaking the ice cover during the winter season And when the lake is free of snow during the summer months, shaking can be due to the movement of the wave on the lake during daylight hours. In addition, earthquake records related to thermal activity and even water explosions.

Although these erthquake references are not what was originally designed by the SYMONSTONE seismic network for recording, it still provides valuable visions in the volcanic Yellowstone and Tiktouni system. Scientists are increasingly used this data to better understand the dynamic nature of the geological activity in the Yellowston region.

Signs of the suspected icequaked on the Yellowstone Lake in the YLASTON Ceal Network stations on the Butte (TOP) and YTP in Parthat (3 pieces below). The plot appears about two minutes of data from January 24, 2022, starting at about 7:43:34 pm MST.

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