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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Answer:
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Explanation:
Answer:Lake Ara Shetan (Butajiri-Silti Volcanic Field)
1st O'a Caldera, with Lake Shala and the smaller Chitu water-filled maar
2nd Bilate River Volcanic Field (several water-filled maars)
3nd El Sod (small salt lake), South Omo Valley
Explanation: i no it
You can find the elevations by finding the contour interval and each line up count up