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Search Earthquake Catalog Time Zone. Display event dates and times using this time zone.
An earthquake – also called a quake, tremor, or temblor – is the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves.
Apr 25, 2023 · SINGAPORE – A 7.3-magnitude earthquake that struck west of Sumatra in Indonesia early on Tuesday morning was also felt in neighbouring Singapore and Malaysia.
3 days ago · Estimation of the earthquake magnitude may differ from other centres, due to varying factors in its determination. All maps are to be used solely for displaying meteorological/geophysical information, and not for other purpose.
Jun 12, 2024 · Earthquake, any sudden shaking of the ground caused by the passage of seismic waves through Earth’s rocks. Earthquakes occur most often along geologic faults, narrow zones where rock masses move in relation to one another. Learn more about the causes and effects of earthquakes in this article.
Nov 8, 2022 · For example, a magnitude 6.2 earthquake in Sumatra in February 2022 was widely felt throughout the Republic. More research is needed to assess the activity of geological faults and seismic hazard...
Feb 6, 2023 · February 6, 2023. • 7 min read. Earthquakes, also called temblors, can be so tremendously destructive that it’s hard to imagine they occur by the thousands every day around the world, usually ...
EMSC (European Mediterranean Seismological Centre) provides real time earthquake information for seismic events with magnitude larger than 5 in the European Mediterranean area and larger than 7 in the rest of the world.
Oct 19, 2023 · Hundreds of earthquakes occur on Earth everyday. Most of them are small, barely detectable by most people. But occasionally there is a much more significant quake. On average, a major earthquake —one with a magnitude of 7.0-7.9—strikes somewhere on the planet more than once a month.
An earthquake is caused by a sudden slip on a fault. The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.
