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SVI 005 SVI 028 SVI 029 SVI 011 SVI 006 SVI 021 SVI 022 SVI 009 SVI 020 SVI 023 SVI 010 SVI 026 SVI 025 Figure 4.1. Sample sites on St. Vincent Island. The blue circles represent sites where a vibracore was collected. The black circles represent sites where samples were collected from the vertical wall of a trench. The approximate locations of Roads 4 and 5 are shown in red. 81 SVI 008 SVI 012 SVI 007 SVI 016 SVI 002 SVI 003 SVI 014 SVI 004 SVI 013 SVI 024 SVI 001 SVI 018 SVI 027 SVI 015 Stapor’s dutch auger core
Figure 4.2. Example of a trench through a beach ridge on St. Vincent Island. The trench axis is perpendicular to the shoreline. Seaward direction is to the left. Note the seaward dipping beds at all levels in the ridge, shown by the solid black line and the dashed lines. Vertical structures in the upper section are root casts. White circles indicate sediment sample locations. 82
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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
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
Page 59 and 60: atio between the first and the fift
Page 61 and 62: Topographic Surveying Topographic s
Page 63 and 64: time elapsed between when this ener
Page 65 and 66: a) b) Figure 3.1. a) Collecting a v
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
Page 87 and 88: (sorting). Standard deviation decre
Page 89 and 90: 4,100 and 3,500 years ago. The corr
Page 91 and 92: Table 4.1 Continued Site Samples Be
Page 93 and 94: Table 4.3. Measured elevations of S
Page 95 and 96: Table 4.5. Application of Tanner’
Page 97 and 98: Table 4.7. OSL age calculations usi
Page 99: Table 4.9. Paleosealevel position e
Page 103 and 104: Figure 4.5. Site SVI 003. Trench ex
Page 105 and 106: a) b) 050505-01E 050505-01K 050505-
Page 107 and 108: a) b) 050505-04C 050505-04A Figure
Page 109 and 110: Figure 4.13. Site SVI 015. Vibracor
Page 111 and 112: a) b) 011006-15 011006-16 Figure 4.
Page 113 and 114: a) b) 011106-08 011106-07 011106-10
Page 115 and 116: Figure 4.21. Dutch gouge-auger core
Page 117 and 118: Figure 4.23. Line A-A’ represents
Page 119 and 120: Elevation (m) NAVD 88 5.00 4.50 4.0
Page 121 and 122: 1200 +/- 100 yr 102 Figure 4.27. GP
Page 123 and 124: 0.65 Set C 0.6 0.55 0.5 Set A 0.45
Page 125 and 126: 6 Set B Set C Set E 5 Set A Set F S
Page 127 and 128: 0.7 Set C 0.6 Set A 0.5 Set E Set F
Page 129 and 130: ENVIRONMENTS OF DEPOSITION -- SKEWN
Page 131 and 132: mean grain size (phi) 3 2.5 2 1.5 1
Page 133 and 134: SVI 015 SVI 002 SVI 003 114 SVI 004
Page 135 and 136: CHAPTER 5 DISCUSSION The beach ridg
Page 137 and 138: vibracore or trench, both of which
Page 139 and 140: Skewness can be used to identify th
Page 141 and 142: island. Another is a C-14 date of 2
Page 143 and 144: sea level. It was at this point tha
Page 145 and 146: The fourth hypothesis was that sea-
Page 147 and 148: 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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