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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Because it is a habitable planet that is capable of supporting living creatures
Answer:
Most of Latin America is located in a Tropical zone that receives the Sun's direct rays yearly.
Explanation:
Latin America, as a region, has almost exclusively tropical types of climates, with Truly Cold climates lacking from the region. The closest that climates get to truly cold types are the highest parts of the Andes and the southernmost part of the region in Patagonia and Tierra del Fuego, but none of them have polar-type characteristics all year round.
This climate situation in Latin America is due to its position relative to the Equator. The Equator passes through the widest part of the region, and the vast majority of the territory north and south falls into the tropical realm, and this is also helped by the fact that north and south of the Equator the territory shrinks and the influence of the ocean is greater. The majority of the region has a tropical wet climate, savanna-like grasslands, and tropical deserts.
<span>The populations are already sparse (due to being mainly desert) added to the fact that there is a huge influx of people seeking work oppotunities in the oil industry, from Westerners to Asian communities. This swamps the local population. </span>
