Publisher's Synopsis
Excerpt from Bulletin of the Scientific Laboratories of Denison University, Vol. 16: 1910 1911
In this paper the term metamorphism includes all alterations concerned in the transition from degradational products to solid rock again.6 It is not possible to observe many stages in this cycle because of the fact that so far as present investigation goes, the glacial periods are separated by long lapses of time, and because of the further fact that most phases of metamorphism require a physical environment that precludes observation.
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