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
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.
Isostasy theory is a geological concept that posits that Earth's lithosphere is in gravitational equilibrium, with lighter elements floating on top of heavier materials in the mantle. This theory explains how the lithosphere adjusts vertically to maintain balance when weight is added or removed, such as from the melting of ice sheets.
Alfred Wegener discovered the theory of continental drift, proposing that the Earth's continents were once all joined together as a single supercontinent called Pangaea and have since drifted apart. This theory laid the foundation for the modern theory of plate tectonics.
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.
everything on the crust is in a state of balance
strength and weaknesses of isostasy
isostasy
Albert Einstein discovered the theory of relativity
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 balance between gravity and buoyancy is called equilibrium.
Genic balance theory is discovered by american scientist Calvin Blackman Bridges
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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).
schwarschild may be the one who has discovered it with a believable theory
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