1963
DOI: 10.1098/rspa.1963.0151
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On the origin of mountains

Abstract: The hypothesis is adopted that the Earth began as an entirely solid body and gradually became melted in its central regions. The incompressibilities of both the liquid and solid regions are linear functions of the pressure, and this enables an integral pressure-density relation to be found and also the effective uncom pressed densities of the different regions. The equations for hydrostatic equilibrium can be reduced to a standard mathematical form, while Earth-models can be related to their solution by homolo… Show more

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Cited by 15 publications
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