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  1. Dictionary
    earthquake
    /ˈəːθkweɪk/

    noun

    • 1. a sudden violent shaking of the ground, typically causing great destruction, as a result of movements within the earth's crust or volcanic action.

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  2. Nov 10, 2024 · earthquake, any sudden shaking of the ground caused by the passage of seismic waves through Earth ’s rocks. Seismic waves are produced when some form of energy stored in Earth’s crust is suddenly released, usually when masses of rock straining against one another suddenly fracture and “slip.”. Earthquakes occur most often along geologic ...

  3. en.wikipedia.org › wiki › EarthquakeEarthquake - Wikipedia

    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. Earthquakes can range in intensity, from those so weak they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, ...

  4. Earthquakes can have various effects, including ground shaking, damage to man-made structures, fires and hazardous chemical spills, landslides and avalanches and the generation of tsunamis in coastal areas. The severity of these effects depends on factors such as the earthquake’s magnitude, depth and local geology. Q6.

  5. Nov 8, 2024 · An earthquake is the sudden movement of Earth’s crust at a fault line. This photograph shows the San Andreas Fault, a 750-mile-long fault in California. Credit: Public Domain. The location where an earthquake begins is called the epicenter. An earthquake’s most intense shaking is often felt near the epicenter. However, the vibrations from an earthquake can still be felt and detected hundreds, or even thousands of miles away from the epicenter.

  6. Nov 22, 2022 · Earthquake is a natural phenomenon that manifests itself as a sudden shaking or trembling of the earth that lasts just a few seconds. It occurs as a result of disruption deep within the earth’s crust or as a result of disturbances within the earth’s crust. Earthquakes often occur deep inside the earth, but they are not visible from the surface.

  7. 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.In California ...

  8. Nov 28, 2023 · Earthquakes are natural geological phenomena that occur when there is a sudden release of energy in the Earth’s crust, resulting in seismic waves.These waves cause the ground to shake, often leading to the displacement of the Earth’s surface. Earthquakes can range in size and intensity, from small tremors that go unnoticed to massive quakes that cause widespread devastation.

  9. www.phivolcs.dost.gov.ph › index › earthquakeIntroduction to Earthquake

    2 days ago · An earthquake is a weak to violent shaking of the ground produced by the sudden movement of rock materials below the earth’s surface. The earthquakes originate in tectonic plate boundary. The focus is point inside the earth where the earthquake started, sometimes called the hypocenter, and the point on the surface of the earth directly above ...

  10. Nov 24, 2023 · An earthquake is the shaking caused by the rupture (breaking) and subsequent displacement of rocks (one body of rock moving with respect to another) beneath the Earth’s surface. Most earthquakes are a result of the stresses placed on rocks in areas where adjacent tectonic plates are moving in different directions.

  11. An earthquake is what happens when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. The location below the earth’s surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter. Sometimes an earthquake has foreshocks. These are smaller earthquakes that happen in the same place as the larger earthquake that follows.

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