. Beach profile changes - east coast of Lake Michigan, 1970-72. Beach erosion; Coast changes. Geomorphology. Beach at Stevensville, Michigan, has a shoreline orientation of °E. and is the site of the time-series study by Fox and Davis (1970a, b). Foredune terrace is adjacent to small vegetated dunes. One mile or more to the north (updrift) is an extensive stretch of high bluffs of glacial till. Bench Mark Location (5 August 1970) (NW cor., sec. 20, N. , ). About ^-mile north of village of Chalet-on-the-Lake. Just south of second house in village on grassy bank. Azimuths (from nor
. Beach profile changes - east coast of Lake Michigan, 1970-72. Beach erosion; Coast changes. Geomorphology. Beach at Stevensville, Michigan, has a shoreline orientation of °E. and is the site of the time-series study by Fox and Davis (1970a, b). Foredune terrace is adjacent to small vegetated dunes. One mile or more to the north (updrift) is an extensive stretch of high bluffs of glacial till. Bench Mark Location (5 August 1970) (NW cor., sec. 20, N. , ). About ^-mile north of village of Chalet-on-the-Lake. Just south of second house in village on grassy bank. Azimuths (from north) : 96°50', television antenna just behind dune crest; 206°40', western peak of westernmost part of village. June 1970. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Davis, Richard A. (Richard Albert), 1937-; Fingleton, W. G; Pritchett, P. C; Coastal Engineering Research Center (U. S. ); Western Michigan University. Ft. Belvoir, Va. : U. S. Dept. of Defense, Dept. of the Army, Corps of Engineers, Coastal Engineering Research Center ; Springfield, Va. : for sale by the National Technical Information Service
Size: 1468px × 1701px
Photo credit: © Library Book Collection / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookcollectionameri, bookcollectionbiodiversity
