fatter platter
Fatter platter
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Coastal plates can become thicker due to the accumulation of sediments from erosion of the land deposited at the coastline, increasing the overall thickness of the plate. Additionally, the process of subduction, where one plate is forced beneath another, can also contribute to the thickening of coastal plates by adding material to the edge of the plate.
Denser plate refers to a lithospheric plate that is heavier and thicker than surrounding plates. These plates are often associated with subduction zones, where one plate is forced beneath another due to differences in density.
Continental plates are generally thicker than oceanic plates. Continental plates can range from 20-200 km thick, while oceanic plates are typically around 5-10 km thick.
In the proses of a subduction, one plate (normally an oceanic plate) is formed beneath another into the solid but fluid mantle below. When the subducted plate is thicker, less dense continental plate, it resists being pushed into the thicker rock, and pushes upward on the overlying plate. This buckles the overlying crust and increases its elevation. It should not be noted that mountains are "built" almost as slowly as they are eroded the proses taking place over tens of millions of years.
It is called a 'charger'.
To provide an accurate answer, I would need specific details about "plate a" and "plate b," such as their characteristics or context. Generally, if plate a is an oceanic plate, it would be denser and thinner compared to plate b, which might be a continental plate, characterized by being thicker and less dense. The classification is based on geological features and tectonic activity.
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The oceanic crust consists of heavier rock, mostly Basalt, so that if a oceanic plate collides with a continental plate the oceanic plate will be forced down below the continental plate, forming island arcs.continental plates are thicker than oceanic plates.