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Figure 1.7. Model of beach ridge formation. (Source: Tanner et al., 1989). 21
Figure 1.8. Global sea-level history from 400,000 years to present, based on dated shoreline indicators from Barbados and New Guinea (symbols) and oxygen isotope data from marine sediments (solid line). (Source: Lea et al., 2002). 22
Page 1 and 2: THE FLORIDA STATE UNIVERSITY COLLEG
Page 3 and 4: ACKNOWLEDGEMENTS I would like to th
Page 5 and 6: 4. RESULTS Laboratory Analyses ....
Page 7 and 8: LIST OF FIGURES 1.1 Location map of
Page 9 and 10: preheating is carried out on a heat
Page 11 and 12: 4.17 Site SVI 023. a) Trench. b) Sa
Page 13 and 14: 4.38 Location relative to the Apala
Page 15 and 16: A.37 Granplot analysis of sample 05
Page 17 and 18: A.83 Granplot analysis of sample 05
Page 19 and 20: ABSTRACT The goal of this investiga
Page 21 and 22: 4) To further develop Optically Sti
Page 23 and 24: the rate of erosion or deposition a
Page 25 and 26: esult of the buildup of offshore ba
Page 27 and 28: Recent studies of barriers using Gr
Page 29 and 30: and, therefore, sea level) (Dorsey,
Page 31 and 32: Holocene Sea Level Over 900 Holocen
Page 33 and 34: first is that sea level rose steadi
Page 35 and 36: Figure 1.2. Beach ridge sets on St.
Page 37 and 38: -100 Figure 1.4. Pleistocene glacia
Page 39: Figure 1.6. The Apalachicola River
Page 43 and 44: K and L have crest elevations of ap
Page 45 and 46: Geoarchaeology The earliest inhabit
Page 47 and 48: Oyster Pond Figure 2.1. Infrared or
Page 49 and 50: Figure 2.3. St. Vincent Island shor
Page 51 and 52: Pickalene Middens Paradise Point Si
Page 53 and 54: At each vibracore or trench locatio
Page 55 and 56: luminescence signal equivalent to t
Page 57 and 58: Application of OSL to Coastal Studi
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Page 61 and 62: Topographic Surveying Topographic s
Page 63 and 64: time elapsed between when this ener
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Page 67 and 68: Increasing energy T CONDUCTION BAND
Page 69 and 70: Figure 3.5. Sample removed from lar
Page 71 and 72: Figure 3.7. Location of samples col
Page 73 and 74: Figure 3.9. Basis of airborne LIDAR
Page 75 and 76: Sample Sites CHAPTER 4 RESULTS A to
Page 77 and 78: SVI005 This site is located just we
Page 79 and 80: collapsed the trench. Therefore, a
Page 81 and 82: SVI025 This site is located within
Page 83 and 84: m and 3.7 m respectively. A cross s
Page 85 and 86: Vincent Island has changed little o
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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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Berger, G., 1988, Dating quaternary
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Douglas, B., Kearney, M. and Leathe
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Jol, H.M., Peterson, C.D., Vanderbu
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Northwest Florida Water Management
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Stapor, F.W. and Tanner, W.F., 1977
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BIOGRAPHICAL SKETCH Beth Margaret F
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