Mosquito 



670 



Mehta, A. J., and M. P. O'Brien. 1973. Kennedy Space Center ocean 

 beach erosion. University of Florida, Gainesville, Coastal and 

 Oceanographic Engineering Laboratory. 66 pp. 



Discusses dune barrier erosion and possible breakthrough due to 

 storm and hurricane wave activity near Mosquito Lagoon on Kennedy 

 Space Center property. 



Cape Canaveral 



671 



Chaki, S. 1974. Study of beach ridges, Cape Canaveral, Florida. 

 Florida State University, Coastal Research Notes 4(2) : 5-7 . 



This article describes eleven distinct sets of beach ridges at 

 Cape Canaveral and discusses their morphology and formation. 



672 

 *Field, M. E. 1974. Buried strandline deposits on the central F^r- 

 ida inner continental shelf. Geological Society of America Bulle- 

 tin 85:57-60. 



Modern shoal formation may be unrelated to relict strand topog- 

 raphy. This finding is based on the occurrence and distribution 

 of intertidal clam deposits at Cape Kennedy, Florida. 



673 



Harris, W. D. , and B. C. Jones. 1964. Repeat mapping for a record 

 of shore erosion, Cape Kennedy. Shore and Beach 32(2) : 31-34. 



This article discusses a project in which tide-controlled infra- 

 red photography was used to record mean high- and low-tide lines 

 in the Cape Kennedy area. 



674 



Mehta, A. J., and H. K. Brooks. 1973. Mosquito lagoon barrier beach 

 study. Shore and Beach 41(2) :27-34. 



A study of Mosquito lagoon barrier beach on the cuspate foreland 

 of Cape Canaveral, Florida, indicated that no major barrier break- 

 throughs are likely to occur and that even in the event of such a 

 break, the resultant tidal inlet will be subsequently closed by 

 normal wave action. 



675 



Osmond, J. K. , J. P. May, and W. F. Tanner. 1970. Age of the Cape 

 Kennedy barrier-and-lagoon complex. Journal of Geophysical Re- 

 search 75(2) :469-479. 



.41 



