Abstract
THERE are strong reasons for believing that the earth was wholly fluid at an early stage of its history. My present topic is the manner in which such a fluid earth would solidify and afterwards cool to its present state.
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References
Jour. Wash. Acad. Sci., 1924.
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JEFFREYS, H. The Cooling of the Earth1. Nature 115, 876–878 (1925). https://doi.org/10.1038/115876a0
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DOI: https://doi.org/10.1038/115876a0
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