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- W4231742009 abstract "The extended development of southeast drainage transverse to the structural belts of the Appalachians is pictured. In explanation of this phenomenon a new theory of Appalachian geomorphic evolution is presented for discussion. According to this theory, a southeast-flowing consequent drainage system was originally superposed on Appalachian structures from an ancient coastal plain cover which extended from 125 to 200 miles northwest of the present inner margin of the Atlantic coastal plain and rested on a peneplane much older than the Schooley or Kittatinny erosion surfaces. A full discussion of the theory, of the considerations which seem to support it, and of the consequences which would follow its acceptance, will be published in book form at an early date." @default.
- W4231742009 created "2022-05-12" @default.
- W4231742009 date "1931-09-01" @default.
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- W4231742009 doi "https://doi.org/10.1086/jg.1931.39.issue-6" @default.
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