They undergo extension, tear in two and move away from each other.
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^ is wrong...
Real answer: Normal falts form. Earthquakes occure, and streams and rivers flow in the cracks. Forming new lakes as a result.
^is the right answer.
At a divergent plate boundary, the crust is growing from the solidification of molten material that is rising from the mantle. As the plates on either side of the DPB are moving away from each other, the void is filled by hot, buoyant new crust.
Divergence occurs due to extensional or tensile stress. This leads to the formation of normal faults. If the extensional stress is maintained then tensile strain will continue leading to the formation of horst and graben structures and if this continues the formation of a rift valley. Ultimately this can lead to the formation of a new mid ocean ridge.
a way to remember convergent boundaries are: c is for crashes which is the same letter....
it may be a tsunami, a huge giant wave.
Convergent boundary.
Convergent boundary.
Yes. It is a convergent boundary where both masses consist of continental crust.
A convergent plate boundary. a piece of continental crust and a piece of oceanic crust meeting at a convergent boundary.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
No. New crust is created along a divergent boundary. Crust is destroyed at a convergent boundary.
Convergent boundary.
Convergent boundary
Convergent boundary.
Yes. It is a convergent boundary where both masses consist of continental crust.
A convergent plate boundary. a piece of continental crust and a piece of oceanic crust meeting at a convergent boundary.
The type of boundary that forms when the crust of one plate is pushed down under another plate and turned into molten rock is referred to as a convergent boundary. Convergent boundaries form when oceanic crust slides beneath continental crust.
Convergent BoundariesGO middle school
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
The two types of Crust is the Continental Crust and the Oceanic Crust.
Convergent plate boundaries.
Crust is destroyed at the convergent plate boundary. This is usually between the oceanic and continental plates. This is where subduction of the more dense crust occurs.