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According to the process of isostatic adjustment, a. Thick sections of crustal material float higher than thinner slabs. Crustal slabs adjust very rarely. Thin sections of crustal material float higher than thicker slabs.
According to the process of isostatic adjustment, a. Thin sections of crustal material float higher than thicker slabs. b. Crustal slabs adjust very rarely. Thick sections of crustal material float higher than thinner slabs. Mountains are lowered as they become older. Dipietro, in geology and landscape evolution (second edition), 2018 isostasy, the equalizer. Isostasy is perhaps the least appreciated of the forcing agents, but it is extremely important in landscape development. We will explain isostasy in chapter 7. for now, we can say that isostasy, like tectonic activity, is a process that emanates from the earth’s interior, and as. The land rising under the reduced weight ( isostatic adjustment) takes very much longer and will not counteract the additional water in the oceans.
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