Isostatiset
Isostatiset is a term that can refer to several related concepts, primarily in the fields of geology and geophysics. In its most common geological context, isostasy describes the state of gravitational equilibrium between the Earth's lithosphere and asthenosphere. Imagine large, rigid blocks of the Earth's crust and upper mantle floating on a denser, more fluid layer beneath. The thickness and density of these blocks determine how high they stand. Thicker, less dense blocks will float higher, forming mountains and plateaus, while thinner, denser blocks will be lower, forming ocean basins.
This concept helps explain why the Earth's surface isn't uniformly smooth. When significant mass is added to
The principles of isostasy are crucial for understanding various geological phenomena, including the formation of mountain