continent: Floating Continents and Isostasy

Evidence indicates that part of the mantle below the crust consists of semifluid rocks on which the continents and ocean basins, in effect, are floating. A condition of gravitational balance, called isostasy, exists between different parts of the earth's crust. The theory of isostasy claims that the continental crust floats higher than the oceanic crust because the former is composed of a thick layer of lower density rocks while the latter is composed of a thin layer of higher density rocks. Isostatic adjustments to changes in mass distribution on the earth's surface associated with plate interactions may occur through flow of semifluid materials deep in the earth. These materials cause a compensatory uplift of mountains and plateau areas as erosion wears them down. The mass of eroded material is added to and thus depresses the continental shelves and the ocean floor. Adjustments also accompany such changes as the growth and melting of continental ice sheets.

Sections in this article:

• Introduction
• Theories of Continental Formation
• Floating Continents and Isostasy
• Plateaus, Shields, and Mountains
• Geology and Topography of the Continents
• Geographic Distribution of the Continents

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