This geological process is called Mantle drag .
What is Mantle drag?
According to the first driving mechanism, known as mantle drag, plate motion is the consequence of viscous drag brought on by the lateral motion of the tops of mantle convection cells in the asthenosphere on the base of the lithosphere . Convection cells would thus be mostly absent beneath continents, rising beneath oceanic ridges, and dropping beneath trenches. This idea states that the oceanic lithosphere would be in a state of tension at the ocean ridges and compression at the trenches.
Due to their connection to accretive and destructive plate boundaries, the horizontal widths of the convection cells causing mantle drag would be projected to be around half an ocean's breadth, or 3000 km.
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The sedimentary rock cycle. This is when a lot of rocks are being pushed and pressed together.
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Earthquakes happen near those places on the map because those are where multiple tectonic plates meet. Earthquakes happen when two tectonic plates rub against each other or collide.
Explanation:
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Answer:
To move into a country without authorized access from the government
Explanation:
Answer:
AB = 5.8 units
Explanation:
The distance of line segment AB shown in the attachment below can be calculated using the distance formula, 
, assuming that each box in the graph equals 1 unit.
A(2, 4)
B(-3, 1)
Let,
Plug in the values into the distance formula
(nearest tenth)
AB = 5.8 units
