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Plate motion during an earthquake can range from a few centimeters to several meters per year, depending on the specific fault. However, during the actual seismic event, the plates can move much faster, reaching speeds of several meters per second.

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AnswerBot

1y ago

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Related Questions

What happens to plates when they slide underneath each other?

earthquake.


What happen when plates slide past each other?

An Earthquake occurs.


What can happen when 2 plates slide against each other?

an earthquake


When earth plates slide past each other does that cause a earthquake?

Yes ♥The tectonic plates.


Which type of earthquake is the result of the release of pressure from when two plates slide past each other in opposing directions?

When two plates slide past each other in opposing directions, an interplate earthquake occurs. It occurs at the boundary between two tectonic plates.


How a earthquake begins?

It happens when two stressed plates slide pass each other


When 2 plates slide past each other it is called?

It is called transform boundaries.An earthquake


What happens when the two plates slide past each other deep inside the Earth's crust?

An earthquake.


A possible result of plates moving along a transform boundary is?

earthquakes occurring as the plates slide past each other in opposite directions.


When two plates slip pass each other is called?

When two tectonic plates slide past each other, it is called transform boundary. This movement can create earthquakes along the boundary where the plates are in contact.


Are earthquakes caused by plates sliding past each other?

Yes, earthquakes are primarily caused by the movement of tectonic plates. When two plates slide past each other, get stuck, and then suddenly release, it generates seismic waves that we feel as earthquakes.


What happens to lithospheric plates when an earthquake occurs?

When an earthquake occurs, lithospheric plates either slide past each other, collide, or move apart along their boundaries. The stress accumulated along the plate boundaries is released suddenly, causing the plates to deform and generate seismic waves that we feel as an earthquake.