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Summary Theory of isostacy

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  • May 20, 2023
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Theory of Isostasy | Airy and Pratt | World Physical Geography |Geomorphology |



Understanding Isostasy: The Concept of Balance

Isostasy is a fundamental concept in earth’s system sciences based on opposing influences of two main
forces, buoyancy and gravity. In this state of gravitational equilibrium between the earth’s crust and
mantle, we will understand how this balance is maintained between the different masses, and the top
most important eight theories of isostasy.



What is Isostasy?

Isostasy is the ideal theoretical balance of all large portions of the earth’s lithosphere as though they
were floating on the denser underlying layer that is asthenosphere. It is the balance between buoyant
forces and the gravity forces. The crust floats at an elevation that depends upon its thickness and
density. It is the idea that lighter crust must be floating on the denser underlying material.



The Theories of Isostasy

There are eight important concepts or theories related to the isostasy concept:



The theory of Sir George Erie in 1854

The theory of Pratt in 1859

The returns concept in 1889

The theory of Heford and Bobby in the 1920s

The theory of Jolly at the same time

The Waning Men’s regional model, also called the flexural model

The theory of Heskinin

The theory of Holmes

Theories of Isostasy

The concept of isostasy refers to the balance of the Earth’s crust, and it is an important concept in
geology. There are several theories of isostasy that have been developed over time, each with its unique
perspective. Here are the major eight theories of isostasy:



The Airy Model: This model studied uniform density with varying depth. It assumes that the surface of
the Earth has the same depth, but different densities. Higher elevations indicate lesser dense rock.

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