73 



Hoyt, J. H., and V. J. Henry, Jr. 1967. Influence of island migration on 



barrier island sedimentation. Geological Society of America Bulletin 78 



(l):77-86. 



This article discussess the migration of barrier islands along some 

 coastal areas in the direction of dominant sediment transport. 



74 

 *Hoyt, J. H. 1968. Barrier island formation: reply. Geological Society of 

 America Bulletin 79:947. 



This a response to C. II. Cooke's article on barrier island formation 

 which is found in the same issue. 



75 



Hoyt, J. H. 1971. Field guide to beaches. American Geological Institute, 

 Earth Science Curriculum Project Pamphlet Series PS-7. 46 pp. 



Describes beach processes such as tsunamis, tides, swash, longshore 

 current, and undertow. Most beaches on the Atlantic and Gulf coasts are 

 on barrier islands, which were dunes at a lower sea level. 



76 



Hoyt, J. H. 1972. Shoreline processes. Journal of Geoloaical Education 

 20(1) :16-22. 



Reviews shoreline development in relation to sea level, deltaic deposi- 

 tion, inlet migration, storms, and surf base. 



77 



Hoyt, J. H. 1973. Erosional and depositional estuarine "terraces," south- 

 eastern United States. Pages 465-474 i_n_ B. W. Nelson, ed. Environmental 

 framework of coastal plain estuaries. Geological Society of America 

 Memoir No. 132. 



Discusses sediment accumulation in the lagoon after the formation of 

 barrier islands, which produces two major surfaces concurrently at the 

 base and top of estuarine deposits. 



78 



Klein, G. D. 1974. Estimating water depths from analysis of barrier island 

 and deltaic sedimentary sequences. Geology 2(8) :409-412. 



Describes proposed model for estimating water depths from thickness of 

 prograding coarsening-upward barrier island and deltaic sequences. 



79 

 *Kraft, J. C. 1971. Sedimentary facies patterns and geologic history of a 

 Holocene marine transgression. Geological Society of America Bulletin 

 82:2131-2158. 



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