Watch the waves from the M5.7 Utah earthquake roll across seismic stations in North America! This animation, called a Ground Motion Visualization (GMV), shows the motion of the ground as detected on seismometers across North America - each dot is a seismic station and when the ground moves up it turns red and when it moves down it turns blue. Waves generated by an earthquake travel around and through the earth, but they get smaller (attenuate) as they move away from the earthquake location, just
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Watch the waves from the M5.7 Utah earthquake roll across seismic sta…
360.5K viewsMar 18, 2020
FacebookEarthScope Consortium
Watch the waves from the M6.1 earthquake in Alaska roll across seismic stations in North America. This animation, called a Ground Motion Visualization (GMV), shows the motion of the ground as detected on seismometers across North America - each dot is a seismic station and when the ground moves up it turns red and when it moves down it turns blue. Waves generated by an earthquake travel around and through the earth, but they get smaller (attenuate) as they move away from the earthquake location,
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FacebookEarthScope Consortium
Watch the waves from the M6.0 earthquake near the California / Nevada border roll across seismic stations in North America. This animation, called a Ground Motion Visualization (GMV), shows the motion of the ground as detected on seismometers across North America - each dot is a seismic station and when the ground moves up it turns red and when it moves down it turns blue. Waves generated by an earthquake travel around and through the earth, but they get smaller (attenuate) as they move away fro
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FacebookEarthScope Consortium
Watch seismic waves from the M7.7 earthquake in Myanmar ripple across North America. This animation, called a Ground Motion Visualization (GMV), shows how the ground moved as detected by seismometers across the continent. Each dot is a seismic station—red 🔴 means the ground moved up, blue 🔵 means it moved down. Seismic waves from earthquakes travel both through and around the Earth. Far from the source, these motions aren’t felt by people, but sensitive seismic instruments still pick them up.
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