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Mapping Kamchatka Earthquake Displacement
Earth’s surface may seem stable and unchanging, but it is anything but static. The tectonic plates that make up the planet’s rigid outer layer are like puzzle pieces that squeeze and grind against each other—often slowly but sometimes in violent, shuddering jolts that we know as earthquakes.
After an earthquake, seismometers are among the first tools scientists look to for information. Global networks of these ground-based sensors measure vibrations in the Earth’s crust and upper mantle and are used to identify the location of the epicenter and the intensity of the shaking. However, seismic networks have limits. In some cases, they cannot measure the extent of a rupture with great accuracy, especially in areas where local seismic networks are sparse.
7.4-magnitude earthquake strikes near the east coast of Russia’s Kamchatka region
MOSCOW — A powerful 7.4-magnitude earthquake struck early Saturday near the east coast of Russia’s Kamchatka region, the U.S. Geological Survey reported.
The quake’s epicenter was 69.3 miles east of Petropavlovsk-Kamchatsky, and had a depth of 39 kilometers, according to the USGS.
The Pacific Tsunami Warning System briefly said there was a threat of a possible tsunami from the earthquake but then changed it to no tsunami threat or warning on its website.
Russia’s Kamchatka Peninsula was hit by at least five powerful quakes — the largest with a magnitude of 7.4 — on July 20. Days later, a powerful 8.8-magnitude earthquake in the region triggered tsunami warnings in Japan, the U.S. and Russia.
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