- 420 



1 \ 1 r— 



88<» a?" 86" 85° 



LEGEND 



1. Geomorphology { Hands, 1970) 



2. Extreme Storms ( Resio and Vincent, 1976c) 



3. 3-yr Hindcast (Soville, 1953) 



4. LEO Currents { Weggel , 1979 ) 



5. LEO Waves (Weggel, 1979) 



e. Section III Reports (U.S. Army Engineer 

 District, Detroit, 1975a, b; 1976a, b,c) 



7. Sediment Characteristics ( Hulsey, 1962) 



8. Sediment Characteristics (Saylor and Hands, 1970) 



a ri i.s t e e 



Sable Point 



ington 



mmit Park 

 twoter 



ttle Sable Point 

 nert Pork 

 hite Lake 



Mulakegon 

 Grand Haven 



Indicotes Direction of Net 

 Tronsport 



Indicates o Bolonce Between 

 Longs))ore Tronsport Directions 

 420 . 



20 40 60 80 lOO(km) 



Gory 



88° 



87« 

 I 



20 40 60(mi) 



85" 



Figure 15. Direction of net longshore transport along the eastern shore. Not 

 all sources are in agreement, but most support the hypothesis that 

 there are areas of longshore divergence beyond the study area both 

 to the north and south, and that longshore transport within the 

 study area converges near Little Sable Point. 



33 



