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.
Answer:
I really don't know if this is what your looking for. Or what kind of speed review your talking about. Sorry if this is wrong. I tried
The trajectory path is the path that a moving object follows through space as a function of time. Mathematically, a trajectory can be defined by the geometry of the path through which it traveled or by by the position of the object over time.
The geometry definition involves the vertical and the horizontal distances of the object from the ground.
Answer:
2_opposite sides are equal in
parallelogram