The Time of Glacial Loess Accumulation in Its Relation to the Climatic Implications of the Great Loess Deposits: Did They Chiefly Accumulate during Glacial Retreat?

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Previous articleNext article FreeThe Time of Glacial Loess Accumulation in Its Relation to the Climatic Implications of the Great Loess Deposits: Did They Chiefly Accumulate during Glacial Retreat?Stephen Sargent VisherStephen Sargent Visher Search for more articles by this author PDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmail SectionsMoreDetailsFiguresReferencesCited by The Journal of Geology Volume 30, Number 6Aug. - Sep., 1922 Article DOIhttps://doi.org/10.1086/622934 Views: 111Total views on this site Citations: 4Citations are reported from Crossref PDF download Crossref reports the following articles citing this article:Hugh French The development of periglacial geomorphology: 1- up to 1965, Permafrost and Periglacial Processes 14, no.11 (Jan 2003): 29–60.https://doi.org/10.1002/ppp.438John J. Alford Glacial Outwash Loess as a Climatic Indicator, Annals of the Association of American Geographers 72, no.11 (Mar 2010): 138–140.https://doi.org/10.1111/j.1467-8306.1982.tb01390.xJOHN KERR ROSE STEPHEN SARGENT VISHER, 1887–1967, Annals of the Association of American Geographers 61, no.22 (Jun 1971): 394–406.https://doi.org/10.1111/j.1467-8306.1971.tb00791.xI.J. Smalley “In-situ” theories of loess formation and the significance of the calcium-carbonate content of loess, Earth-Science Reviews 7, no.22 (Apr 1971): 67–85.https://doi.org/10.1016/0012-8252(71)90082-1