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Friedman, G.M., 1962, On sorting, sorting coefficients and the lognormality of the grain-size distribution of sandstones: Journal of Sedimentary Petrology, v.70, p.737-753. Gibeaut, J.C., White, W.A., Smyth, R.C., Andrews, J.R., Trembley, T.A., Gutierrez, R., Hepner, T.L. and Neuenschwander, A., 2003, Topographic variation of barrier island subenvironments and associated habitats: in Coastal Sediments 2003: Crossing Disciplinary Boundaries: Proceedings 5 th International Symposium on Coastal Engineering and Science of Coastal Sediment Processes, Clearwater Beach, Florida, May 18-23, 10 p. CD-ROM. Gilbert, G.K., 1885, The topographic feature of lake shores: U.S. Geological Survey 5 th Annual Report, p.69-123. Godwin, H., Suggate, R.P. and Willis, E.H., 1958, Radiocarbon dating of the eustatic rise in ocean-level: Nature, v.181, p.1518-1519. Granlund, E., 1932, De svenska hogmossarnas geologi: Sveriges Geologiska Underskning., eries C, v. 373, 193 p. Haan, C.T., 1977, Statistical methods in hydrology: Iowa State University Press, Ames, Iowa, 378 p. Harari, Z., 1996, Ground-penetrating radar for imaging stratigraphic features and groundwater in sand dunes: Journal of Applied Geophysics, v.36, p.43-52. Hodell, D.A., Brenner, M, Curtis, J.H. and Guilderson, T., 2001, Solar forcing of drought frequency in the Maya lowlands: Science, v.292, p.1367-1370. Hoyt, J.H., 1967, Barrier island formation: Geological Society of America Bulletin, v.78, p.1125-1135. Huntley, D. J., 1985, On the zeroing of the thermoluminescence of sediments: Physics and Chemistry of Minerals, v. 12, p.122-127. Huntley, D.J, Godfrey-Smith, D.I. and Thewalt, M.L.W., 1985, Optical Dating of Sediments: Nature, v.313, p.105-107. Huntley, D. J., and Lian, O. B., 1999, Using optical dating to determine when a sediment was last exposed to sunlight: Geological Society of Canada Bulletin, v. 534, p.211-215. Hutt, G. I., and Raukas, A., 1995, Thermoluminescence dating of sediments: in Rutter, N. W., and Catto, N. R., eds., Dating Methods for Quaternary Deposits: Newfoundland, Geological Association of Canada. p.73-79. Johnson, D.W., 1919, Shore Processes and Shoreline Development: Wiley and Sons, New York. 584 p. 261
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THE FLORIDA STATE UNIVERSITY COLLEG
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ACKNOWLEDGEMENTS I would like to th
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4. RESULTS Laboratory Analyses ....
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LIST OF FIGURES 1.1 Location map of
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preheating is carried out on a heat
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4.17 Site SVI 023. a) Trench. b) Sa
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4.38 Location relative to the Apala
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A.37 Granplot analysis of sample 05
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A.83 Granplot analysis of sample 05
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ABSTRACT The goal of this investiga
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4) To further develop Optically Sti
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the rate of erosion or deposition a
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esult of the buildup of offshore ba
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Recent studies of barriers using Gr
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and, therefore, sea level) (Dorsey,
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Holocene Sea Level Over 900 Holocen
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first is that sea level rose steadi
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Figure 1.2. Beach ridge sets on St.
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-100 Figure 1.4. Pleistocene glacia
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Figure 1.6. The Apalachicola River
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Figure 1.8. Global sea-level histor
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K and L have crest elevations of ap
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Geoarchaeology The earliest inhabit
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Oyster Pond Figure 2.1. Infrared or
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Figure 2.3. St. Vincent Island shor
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Pickalene Middens Paradise Point Si
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At each vibracore or trench locatio
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luminescence signal equivalent to t
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Application of OSL to Coastal Studi
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atio between the first and the fift
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Topographic Surveying Topographic s
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time elapsed between when this ener
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a) b) Figure 3.1. a) Collecting a v
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Increasing energy T CONDUCTION BAND
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Figure 3.5. Sample removed from lar
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Figure 3.7. Location of samples col
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Figure 3.9. Basis of airborne LIDAR
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Sample Sites CHAPTER 4 RESULTS A to
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SVI005 This site is located just we
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collapsed the trench. Therefore, a
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SVI025 This site is located within
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m and 3.7 m respectively. A cross s
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Vincent Island has changed little o
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(sorting). Standard deviation decre
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4,100 and 3,500 years ago. The corr
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Table 4.1 Continued Site Samples Be
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Table 4.3. Measured elevations of S
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Table 4.5. Application of Tanner’
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Table 4.7. OSL age calculations usi
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Table 4.9. Paleosealevel position e
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Figure 4.2. Example of a trench thr
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Figure 4.5. Site SVI 003. Trench ex
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a) b) 050505-01E 050505-01K 050505-
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a) b) 050505-04C 050505-04A Figure
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Figure 4.13. Site SVI 015. Vibracor
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a) b) 011006-15 011006-16 Figure 4.
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a) b) 011106-08 011106-07 011106-10
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Figure 4.21. Dutch gouge-auger core
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Figure 4.23. Line A-A’ represents
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Elevation (m) NAVD 88 5.00 4.50 4.0
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1200 +/- 100 yr 102 Figure 4.27. GP
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0.65 Set C 0.6 0.55 0.5 Set A 0.45
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6 Set B Set C Set E 5 Set A Set F S
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0.7 Set C 0.6 Set A 0.5 Set E Set F
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ENVIRONMENTS OF DEPOSITION -- SKEWN
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mean grain size (phi) 3 2.5 2 1.5 1
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SVI 015 SVI 002 SVI 003 114 SVI 004
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CHAPTER 5 DISCUSSION The beach ridg
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vibracore or trench, both of which
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Skewness can be used to identify th
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island. Another is a C-14 date of 2
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sea level. It was at this point tha
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The fourth hypothesis was that sea-
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APPENDIX A INDIVIDUAL SIEVE ANALYSI
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Page 277 and 278: Berger, G., 1988, Dating quaternary
Page 279: Douglas, B., Kearney, M. and Leathe
Page 283 and 284: Northwest Florida Water Management
Page 285 and 286: Stapor, F.W. and Tanner, W.F., 1977
Page 287 and 288: BIOGRAPHICAL SKETCH Beth Margaret F
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