aftershocks
The measurement of how likely an area is to have damaging earthquakes is called seismic hazard. It assesses the probability of ground shaking exceeding a certain intensity within a specific timeframe.
Earthquakes at convergent boundaries occur at greater depths because of the intense pressure from the overriding tectonic plates, which drives the descending plate deeper into the mantle where it eventually triggers seismic activity. In contrast, earthquakes at divergent boundaries are generally shallower due to the tensional forces pulling the plates apart, causing them to fracture closer to the surface.
Earthquakes are internal forces of change caused by tectonic plate movement and stress release along faults within the Earth's crust. They are not considered external forces as they originate from within the Earth.
Shallow focus earthquakes are associated with divergent and transform plate boundaries. These earthquakes typically occur within the top 70 kilometers of the Earth's crust and are caused by the movement of tectonic plates against each other.
Deposition itself does not cause earthquakes. Earthquakes are typically caused by tectonic forces within the Earth's crust, such as the movement of tectonic plates or the release of built-up stress along faults. Deposition, which is the process of laying down sediment or rock by natural forces like water or wind, does not directly trigger earthquakes.
in cahokia
California
Earthquakes associated with convergent plate boundaries typically occur in the subduction zones where one tectonic plate is forced beneath another. These earthquakes are known as megathrust earthquakes and can have very high magnitudes due to the intense tectonic forces involved in the subduction process.
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Faults
arthquake hazard
Seismic waves are associated with earthquakes.
earthquakes
The measurement of how likely an area is to have damaging earthquakes is called seismic hazard. It assesses the probability of ground shaking exceeding a certain intensity within a specific timeframe.
Earthquakes at convergent boundaries occur at greater depths because of the intense pressure from the overriding tectonic plates, which drives the descending plate deeper into the mantle where it eventually triggers seismic activity. In contrast, earthquakes at divergent boundaries are generally shallower due to the tensional forces pulling the plates apart, causing them to fracture closer to the surface.
yes
it is when forces create new things like volcano, and earthquakes