T H D V D D D D D D D ! D D D D D # # # # # # # # # # # D D D # # H H H H H H H H! D D D D D D D D D D D D D D D D D D D D D D D D D D D D DD D D DD D D D D D D D D D D D D D DD D ª ª D V V V V V V V V V V V V J T T T T T TT T T H H H H T T ! ª ª D ª V V V V V V V V V D D D H H H H D D D T T D D D D D # 0 # 0 # 0 # 0 # 0 k G k k k k G G G G G G k k k k k k k k G C C _ A A' South Florida Basin Bahamas Basin Blake Plateau Basin Apalachicola Basin Bahamas Fracture Zone Sunniland Fracture Zone Cuba Fracture Zone 3-km 2-km 5- k m 3 .5 - k m 8 - k m 6 - k m 5 .5- km 4.5- k m 4 -k m 1 . 5- k m 1 0 - k m 1 - k m 12 - km 4-km 6-km 4 - k m 5 - k m 1. 5 - k m 3- k m 2-km 5 - k m 3. 5 - k m 8 - k m 6 - k m 5 . 5 - k m 4 . 5- k m 4 -k m 1 . 5 -km 1 0 - k m 1 - k m 1 2 - k m 1 . 5 - k m 6-km 4- k m 5 - k m 4 -k m Pre-Cretaceous Surface and Types of Basement Terrane Figure 2.5.1-212 LEGEND File path: S:\11100\11151.001\figures\2_5_1_figures\LNP_FSAR_FIG02_05_01_212.mxd; Date: [06/09/2008]; User: [sbozkurt] Progress Energy Florida Rev 0 Levy Nuclear Plant Units 1 and 2 Part 2, Final Safety Analysis Report _ LNP Site 320-km (200-mi.) Radius from Site A-A' Profile (see Figure 2.5.1-213) Drill Holes Not Penetrating Basement R Deep See Drilling k Lower Cretaceous carbonate rocks G Upper Jurassic anhydrite – carbonate rocks overlaying basal – clastics (Wood River formation) C Wood River formation underlain by Jurassic salt Drill Holes Penetrating Basement # Jurassic volcanics and volcaniclastics # 0 Jurassic volcanics overlain by Wood River formation T Paleozoic (?) rhyolites and felsic volcanics J Paleozoic (?) rhyolites and overlain by marine clastics ! Paleozoic diorites and mafic plutonic H Paleozoic granites D Paleozoic marine clastics ª Paleozoic marine clastics overlain by Eagle Mills formation or intruded with diabase dikes and sills V Triassic red beds-clastics (Eagle Mill formation) and diabase dikes or sills Source: Klitgord et al. (1984); Base Map: ETOPO2v2 (2006), and SRTM (2005) 0 40 80 Kilometers / 0 30 60 Miles LNP COL 2.5-1

V H V m V T H TT A T H V T V H T VV V VVª V J H H T H V ª ... · ª Paleozoic marine clastics overlain by Eagle Mills formation or intruded with diabase dikes and sills V Triassic

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Page 1: V H V m V T H TT A T H V T V H T VV V VVª V J H H T H V ª ... · ª Paleozoic marine clastics overlain by Eagle Mills formation or intruded with diabase dikes and sills V Triassic

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SouthFloridaBasin

BahamasBasin

BlakePlateauBasin

ApalachicolaBasin

Bahamas Fracture Zone

Sunniland Fracture Zone Cuba Fracture Zone

3-km

2-km

5-km

3.5-km

8-km

6-km

5.5-km

4.5-km

4-km

1.5-k m

10-km

1-km

12-km

4-km

6-km

4-km

5-km1.5

-km

3-km

2-km

5-km

3.5-km

8-km

6-km

5.5-km4.5-km

4-km

1.5-km

10-km

1-km

12-km

1.5

-km

6-km

4-km

5-km

4-km

Pre-Cretaceous Surface andTypes of Basement Terrane

Figure 2.5.1-212

LEGEND

File path: S:\11100\11151.001\figures\2_5_1_figures\LNP_FSAR_FIG02_05_01_212.mxd; Date: [06/09/2008]; User: [sbozkurt]

Progress Energy Florida

Rev 0

Levy Nuclear PlantUnits 1 and 2Part 2, Final Safety Analysis Report

_ LNP Site

320-km (200-mi.) Radius from SiteA-A' Profile (see Figure 2.5.1-213)

Drill Holes Not Penetrating BasementR Deep See Drillingk Lower Cretaceous carbonate rocksG Upper Jurassic anhydrite – carbonate rocks overlaying basal – clastics (Wood River formation)C Wood River formation underlain by Jurassic salt

Drill Holes Penetrating Basement# Jurassic volcanics and volcaniclastics#0 Jurassic volcanics overlain by Wood River formationT Paleozoic (?) rhyolites and felsic volcanicsJ Paleozoic (?) rhyolites and overlain by marine clastics! Paleozoic diorites and mafic plutonicH Paleozoic granitesD Paleozoic marine clasticsª Paleozoic marine clastics overlain by Eagle Mills formation or intruded with diabase dikes and sillsV Triassic red beds-clastics (Eagle Mill formation) and diabase dikes or sills

Source: Klitgord et al. (1984); Base Map: ETOPO2v2 (2006), and SRTM (2005)

0 40 80

Kilometers

/0 30 60

Miles

LNP COL 2.5-1

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