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Beach environment in Little Sister Bay, Wisconsin
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1938
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Historical GeographyCoastal ManagementHistory Of ScienceGsa Bulletin 1938EngineeringJournal Citation ReportNatural SciencesEnvironmental HistoryBeach EnvironmentBibliometricsCitation AnalysisInterdisciplinary StudiesLittle Sister BayBeach ManagementSocial SciencesCoastal Pollution
Research Article| April 01, 1938 Beach environment in Little Sister Bay, Wisconsin W. C. KRUMBEIN; W. C. KRUMBEIN Search for other works by this author on: GSW Google Scholar J. SCOTT GRIFFITH J. SCOTT GRIFFITH Search for other works by this author on: GSW Google Scholar GSA Bulletin (1938) 49 (4): 629–652. https://doi.org/10.1130/GSAB-49-629 Article history received: 23 Feb 1937 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation W. C. KRUMBEIN, J. SCOTT GRIFFITH; Beach environment in Little Sister Bay, Wisconsin. GSA Bulletin 1938;; 49 (4): 629–652. doi: https://doi.org/10.1130/GSAB-49-629 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract INTRODUCTIONThe modern viewpoint in sedimentary petrology involves the study of sets of related samples, rather than the study of a single sample and a consideration of its histogram. A natural extension of the modern point of view is the study of an entire environment of deposition, involving the analysis of samples collected at relatively short distances over the entire area of the same environment. The characteristics of each sample may then be determined in the laboratory, and, from the data so obtained, a picture of the deposit gained.1The laboratory study of the samples may include all the fundamental characteristics of sediments, such as the size-frequency distribution, the mineralogical or lithological composition, the shape of the particles, the surface texture of the particles (frosting, pitting, and the like), and finally the orientation of the individual particles in space. These fundamental data, if they are expressible as continuous functions of . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article.