Answer:
isostasy
Explanation:
Of iso, same; stasy, state; word derived from the Greek; its meaning speaks of the equilibrium state of the portions of the earth's crust and how they are permanently compensated. It is not a static equilibrium but a dynamic one, its behavior implies the recognition of erosion and sedimentation phenomena as exogenous factors and the rearrangement of cortical blocks as endogenous factors.
The earth's crust, having a lower density than the underlying layer (outer mantle), will submerge in it and float, in a measure proportional to the height, that is to say that the mountains will have deeper roots than the plains, the lowlands or the bottoms sailors
The theory has been widely known in some cases as "Plate Tectonics" and in others as "Continental Drift". Today, the first title conforms more to the scientific truth since the continents travel as passengers on the tectonic plates whose areal dimension is much greater.
In The Tropics can i please have brainiest answer :D
Sedimentary rock is the correct answer
Answer:
The easiest way to differentiate them is to remember that the site of an area is its exact location and the situation describes its surrounding areas and physical features. Favorable features of site and situation will ensure that the city will be able to thrive and survive.