the florida state university college of arts and sciences evolution of ...

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Gulf of Mexico High-angle, seaward dipping reflectors Pleistocene/Holocene Contact Figure 4.28. Close-up of the section of the 100 MHz GPR survey that covered site SVI 009. Site location is shown in Figure 4.1 and 4.27. South (seaward) is to left. 103 SVI 009 St. Vincent Sound 0 m 4 m 8 m
0.65 Set C 0.6 0.55 0.5 Set A 0.45 Set E Set L 104 Set F 0.4 Set Standard Deviation (phi units) Set J Set K Set H Set I Set D Set G Set B 0.35 0.3 2.05 2.10 2.15 2.20 2.25 2.30 2.35 Set Mean Diameter (phi units) Figure 4.29. Suite mean versus suite standard deviation
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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
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 and 100: Table 4.9. Paleosealevel position e
Page 101 and 102: Figure 4.2. Example of a trench thr
Page 103 and 104: Figure 4.5. Site SVI 003. Trench ex
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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: 1200 +/- 100 yr 102 Figure 4.27. GP
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
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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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