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Further explanation:How do seismic waves work?
When materials suddenly move within the Earth, such as when they slip along a fault during an earthquake, seismic waves are produced. Seismic waves can also be produced by volcanic eruptions, explosions, landslides, avalanches, and even swiftly flowing rivers. Seismometers can record seismic waves as they pass through and around the Earth.
Seismic Wave Types
Seismic waves come in a variety of varieties and behave in various ways. Body waves and surface waves are the two primary forms of waves. Surface waves can only move over the Earth's surface like water ripples, whereas body waves can pass through the planet's core layers. Both body waves and surface waves are produced by earthquakes.
Earthquakes: Where Do They Happen?
Every day around the globe, tectonic plate interiors and margins experience earthquakes. Faults, which are cracks in the rock that allow the blocks to move in relation to one another, are where earthquakes happen. The bumping and sliding that plates perform result in faults, which are more prevalent close to the borders of the plates.
Motion, Plates, Faults, and Energy Release
Most earthquakes happen around the boundaries of the tectonic plates that make up the Earth's crust, the planet's outer layer. Oceanic plates are the plates that lie beneath the oceans. Continental plates are those that are not submerged in the ocean. The motion of the mantle, a layer of the earth beneath the crust, and the weight of oceanic plates, which drag the plates down beneath oceanic plates, are what move the plates. The rate at which these plates move apart, collide, or slide past one another is roughly equal to how quickly your fingernails develop. Earthquakes often happen when two plates collide or slide past one another.
Learn more about seismic waves here: https://brainly.ph/question/167440#
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