01801oam 2200457 450 991070653630332120171208082152.0(CKB)5470000002457086(OCoLC)892425305(OCoLC)995470000002457086(EXLCZ)99547000000245708620141006d1965 ua 0engurmn|||||||||txtrdacontentcrdamediacrrdacarrierPostglacial drainage evolution and stream geometry in the Ontonagon area, Michigan /by John T. HackWashington :United States Department of the Interior, Geological Survey,1965.1 online resource (iii, B40 pages) illustrations, maps +1 plateGeological Survey professional paper ;504-BShorter contributions to general geologyTitle from title screen (viewed September 30, 2014).Includes bibliographical references (pages B39-B40)."A parallel drainage network controlled by glacial grooves provides data for the study of fluvial geomorphic phenomena, especially the geometry of stream bifurcations."DrainageMichiganOntonagon CountyGeologyMichiganOntonagon CountyPhysical geographyMichiganOntonagon CountyDrainageGeologyPhysical geographyHack John T(John Tilton),1913-1991,1400331Geological Survey (U.S.),COPCOPOCLCOGPOBOOK9910706536303321Postglacial drainage evolution and stream geometry in the Ontonagon area, Michigan3500956UNINA