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earthquakes and tsunamis
Molten magma from the mantle rises at the top oceanic ridge, cools and solidifies, continually forming a crustal plate. Hundreds to thousands of miles from the ridge the plate moves downward into the mantle at the contact with another plate and melts. The continuous process resembling a large "conveyor belt" moves the crustal plate a few centimeters each year.
the large sections of the earth's crust that move relative to each other
No, the relative sizes of the oceans change.
Crustal rock is heated inside the mantle during divergent boundaries where new crust is generated as the plates pull away from each other. In mid-ocean, this movement results in seafloor spreading and the formation of ocean ridges; on continents, crustal spreading can form rift valleys.
push into each other
when tectonic plates move toward each othe forms
earthquakes and tsunamis
Sliding Boundaries
Crustal plates are grinding past each other in a strike-slip fault.
Molten magma from the mantle rises at the top oceanic ridge, cools and solidifies, continually forming a crustal plate. Hundreds to thousands of miles from the ridge the plate moves downward into the mantle at the contact with another plate and melts. The continuous process resembling a large "conveyor belt" moves the crustal plate a few centimeters each year.
Earthquakes occur and faults are created. (Next: transform boundary) no crust is created or destroyed.
the large sections of the earth's crust that move relative to each other
It consist of large sections called tectonic plates, which move relative to each other.
No, the relative sizes of the oceans change.
Crustal rock is heated inside the mantle during divergent boundaries where new crust is generated as the plates pull away from each other. In mid-ocean, this movement results in seafloor spreading and the formation of ocean ridges; on continents, crustal spreading can form rift valleys.
the plates are moving away from each other.