The theory of secular marine planation
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ID: 309046
1955
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Abstract
Concludes that the hypothesis of marine planation during extensive periods in which no significant changes of sea level took place may be applicable to shore-line development in the geologic past, but cannot be applied to existing coasts. Erosion at successively lower levels, accompanying gradual subsidence, is considered a more valid explanation of the shore-line features cited by Johnson and others as examples of a single cycle of marine planation at constant sea level.
| Reference Key |
openalex_W2063556058
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|---|---|
| Authors | C. A. Cotton |
| Journal | american journal of science |
| Year | 1955 |
| DOI |
10.2475/ajs.253.10.580
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| URL | |
| Keywords | Keywords not found |
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