This report covers the archeology, cultural geography, botany, coastal 

 morphology, and geology of the Cape Hatteras area, North Carolina. 



394 



Chang, Y. M., and R. L. Kaesler. 1974. Morphological variation of the fora- 

 minifer Ammonia beccarii (Linne) from the Atlantic coast of the United 

 States. University of Kansas, Paleontological Contributions 69:1-23. 



The foraminifer A. beccarii is discussed in terms of various Holocene 

 environments of the Atlantic coast north and south of Cape Hatteras. 



395 

 *Cooke, C. W. 1968. Barrier island formation: discussion. Geological 

 Society of America Bulletin 79(7) :945-946. 



This article describes the various ways in which a barrier island may 

 be produced. Areas discussed include Cape Hatteras, Sapelo Island, Padre 

 Island, and the Florida Keys. 



396 



Cooke, C. W. 1971. Holocene evolution of a portion of the North Carolina 



coast: discussion. Geological Society of America Bulletin 82(8):2369- 



2370. 



This article discusses the part played by the configuration of the sea 

 bottom and the activity of waves in progradation in Hatteras Banks area 

 during the Pleistocene. 



397 



Dolan, R. 1970. Sand waves-Cape Hatteras, North Carolina. Shore and Beach 

 38(1) :23-25. 



This paper discusses shoreline changes caused by the migration of sand 

 waves along the beach at Cape Hatteras, North Carolina. 



398 

 *Dolan, R. 1971. Coastal landforms: crescentic and rhythmic. Geological 

 Society of America Bulletin 82:177-180. 



This article discusses rhythmic shoreline landforms along the coast of 

 North Carolina. Emphasis is made on the Cape Hatteras area. 



399 

 *Dolan, R. 1973. Barrier islands: natural and controlled. Pages 263-278 



j_n_ D. R. Coates, ed. Coastal geomorphology. State University of New York, 

 Binghamton. 



Compares the upper section of the Outer Banks, around Cape Hatteras, 

 man-manipulated for many years, to the southern segment including Core 

 Banks, which remains in a natural state. The latter prove much better 

 adapted to natural processes and extreme events. Also compares the effects 

 of Hurricane Ginger in both areas. 



83 



