everything on the crust is in a state of balance
strength and weaknesses of isostasy
Isostasy theory was developed by the American geologist Clarence Edward Dutton in the late 19th century. He proposed that the Earth's crust is in equilibrium, with less dense crust floating on top of the denser mantle.
isostasy
The theory of isostasy states that the Earth's lithosphere floats on the denser, semi-fluid layer beneath it (the asthenosphere) in gravitational equilibrium, causing adjustments in the elevation of the Earth's surface due to variations in crustal thickness and density. Isostatic equilibrium occurs when the weight of the lithosphere is balanced by the buoyancy provided by the asthenosphere.
An isostatic is something that pertains to or is characterized by isostasy. Isostasy is the equilibrium of the Earths crust.
Three principal models of isostasy are:The Airy-HeiskanenModel- where different topographic heights are accommodated by changes in crustal thickness, in which the crust has a constant density The Pratt-HayfordModel- where different topographic heights are accommodated by lateral changes in rock density. The Vening Meinesz, or Flexural Model- where the lithosphere acts as an elastic plate and its inherent rigidity distributes local topographic loads over a broad region by bending.
The principle is called isostasy, which states that the Earth's crust floats on the semi-fluid upper mantle because of differences in density and thickness. This balance of floating is what helps maintain the stability and equilibrium of the Earth's crust.
Because the theory of Isostasy states that the crust floats over the Mantel like a large piece of ice in water, so when a large piece of the crusts deteriorates, like when a extensive glacier melts, the Earth will raise up where the large piece of Earth deteriorate.
The balance between gravity and buoyancy is called equilibrium.
Alfred Wegener was a scientist who proposed the theory of continental drift and the idea of isostasy. The idea of isostasy stated that continental blocks drifted upon oceanic blocks (continental blocks had a lower density than oceanic blocks, which explained why it was higher than oceanic blocks).
Monkey
isostasy