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Heiskanen hypothesis
geology
Also known as: Heiskanen model
Learn about this topic in these articles:
application to isostasy
- In isostasy
The Heiskanen hypothesis, developed by Finnish geodesist Weikko Aleksanteri Heiskanen, is an intermediate, or compromise, hypothesis between Airy’s and Pratt’s. This hypothesis says that approximately two-thirds of the topography is compensated by the root formation (the Airy model) and one-third by Earth’s crust above the boundary…
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