Discuss the isostatic balance at global level.
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It can be thought that the crustal parts have a tendency to rise or sink gradually until they are balanced by their weight of the displaced mantle rocks. This concept of vertical movement to reach equilibrium is called as Global Isostatic adjustment.
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It can be thought that the crustal parts have a tendency to rise or sink gradually until they are balanced by their weight of the displaced mantle rocks. This concept of vertical movement to reach equilibrium is called as Global Isostatic adjustment.
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