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Most Recent Earthquakes Worldwide
earthquake.usgs.govMagnitudeLocationTimeM5.65 hours agoM5.88 hours agoM58 hours agoM510 hours agoM5.113 hours agoM513 hours agoM5.11 day agoM5.11 day agoView the map of the latest earthquakes around the world, updated in real time by the USGS. See the magnitude, location, time and depth of each earthquake, and click on the marker for more details.
Sep 19, 2022 · View real-time and near-real-time information for magnitude 2.5+ earthquakes in the U.S. and 4.5+ earthquakes around the world. Use the interactive tool to fine-tune the display and access detailed data and products for each event.
- Overview
- Causes of earthquakes
Over the centuries, earthquakes have been responsible for millions of deaths and an incalculable amount of damage to property. Depending on their intensity, earthquakes (specifically, the degree to which they cause the ground’s surface to shake) can topple buildings and bridges, rupture gas pipelines and other infrastructure, and trigger landslides, tsunamis, and volcanoes. These phenomena are primarily responsible for deaths and injuries. Very great earthquakes occur on average about once per year.
What are earthquake waves?
Earthquake waves, more commonly known as seismic waves, are vibrations generated by an earthquake and propagated within Earth or along its surface. There are four principal types of elastic waves: two, primary and secondary waves, travel within Earth, whereas the other two, Rayleigh and Love waves, called surface waves, travel along its surface. In addition, seismic waves can be produced artificially by explosions.
How is earthquake magnitude measured?
Magnitude is a measure of the amplitude (height) of the seismic waves an earthquake’s source produces as recorded by seismographs. Seismologist Charles F. Richter created an earthquake magnitude scale using the logarithm of the largest seismic wave’s amplitude to base 10. Richter’s scale was originally for measuring the magnitude of earthquakes from magnitudes 3 to 7, limiting its usefulness. Today the moment magnitude scale, a closer measure of an earthquake’s total energy release, is preferred.
Where do earthquakes occur?
Earth’s major earthquakes occur mainly in belts coinciding with the margins of tectonic plates. This has long been apparent from early catalogs of felt earthquakes and is even more readily discernible in modern seismicity maps, which show instrumentally determined epicentres. The most important earthquake belt is the Circum-Pacific Belt, which affects many populated coastal regions around the Pacific Ocean—for example, those of New Zealand, New Guinea, Japan, the Aleutian Islands, Alaska, and the western coasts of North and South America. It is estimated that 80 percent of the energy presently released in earthquakes comes from those whose epicentres are in this belt. The seismic activity is by no means uniform throughout the belt, and there are a number of branches at various points. Because at many places the Circum-Pacific Belt is associated with volcanic activity, it has been popularly dubbed the “Pacific Ring of Fire.”
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A second belt, known as the Alpide Belt, passes through the Mediterranean region eastward through Asia and joins the Circum-Pacific Belt in the East Indies. The energy released in earthquakes from this belt is about 15 percent of the world total. There also are striking connected belts of seismic activity, mainly along oceanic ridges—including those in the Arctic Ocean, the Atlantic Ocean, and the western Indian Ocean—and along the rift valleys of East Africa. This global seismicity distribution is best understood in terms of its plate tectonic setting.
View earthquakes around the world as circles sized by magnitude on a map. Click or tap on a circle to see more details, or use Did You Feel It? to report your experience and damage.
Find information on recent or historic earthquakes, maps, lists, statistics, and resources by state or worldwide. Learn about earthquake hazards, effects, and how to report or get notified of earthquakes.
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Terminology. An earthquake is the shaking of the surface of Earth resulting from a sudden release of energy in the lithosphere that creates seismic waves. Earthquakes may also be referred to as quakes, tremors, or temblors. The word tremor is also used for non-earthquake seismic rumbling .
Oct 19, 2023 · Learn what causes earthquakes, how they happen, and how to measure them. Find out the difference between major and great earthquakes, and the types of faults and plate boundaries where they occur. Explore the history and examples of earthquakes around the world, from ancient times to modern events.