Geomorphology . Beach at Stevensville, 

 Michigan, has a shoreline orientation 

 of N.28°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, T.5 N. , R.19W.). 

 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 



11 August 1971 

 Figtire 21. Location and geomorphology of profile site 16. 



44 



