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B
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SS
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SS
SS
SSSS
SS
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SS
SS
SSSS
SS
SS
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SS
SS
SSSS
SS
SS
SS
SSSS
SSSS
SS
SS
SS
SS
SS
SS
SSSS
SSSS
SS
SS
SS
SSSS
SS
SS
SS
SS
SS
SS
SS
SS
SS
SS
SS
SS
SSSS
SS
SS Fl
FlR
FlR F C
R
FlR C
R
R FFl
R FFl
R FFl
R
R Fl
R
R Fl F C
R
R
R Fl F
R Fl F C
R
R
R Fl F
R Fl
Fl
R Fl
R
R
Fl F
Fl F
Fl F
R
Fl F
Fl F
R
Fl
Fl
R
R
Fl
R Fl Cl
R
Fl F
RRs Fl F
R Fl F
R Fl F
R Fl F
R Fl
R Fl
Fl F
R Rs
Fl
R Rs
Fl
FlR
Fl
R Rs
F
Fl
Fl
Fl
R
Fl
Fl
Fl
R Rs Fl
R Rs Fl F
Fl
Fl
R
Fl
Fl
Fl
R Fl A
R Fl F
R Fl F
R Fl
R Fl
R
FlR
FFlR
R
Fl F
R Rs Fl F C
R Fl
R Rs Fl F
Rs
R Rs Fl F
R
R Fl F
R Fl
SS
No
data
III
III
II
II
II
II
II
II
II
II
II
II
II
II
II
II
II
II
IIIIII
II
IV
I
I
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I
IV
I
I
IV
I
IV
I
I
I
I
II
II
IV
I
II
II
II
II
Uppe
r
Flor
idan
aq
uife
r M
iddl
e
se
mic
onfin
ing
unit
1 DS
AP3
DS A
P2
1,070
1,075
1,145
1,130
1,120
1,115
1,110
1,080
1,085
1,090
1,095
1,100
1,105
1,125
1,135
1,140
1,150
1,155
1,160
1,165
1,170
1,175
1,180
1,185
1,190
1,195
1,265
1,250
1,240
1,235
1,230
1,200
1,205
1,210
1,215
1,220
1,225
1,245
1,255
1,260
1,270
1,275
1,280
1,285
1,290
1,295
1,300
1,305
Avon
Park
Fo
rmat
ion
Grain types
Percent pore type
m w p g f r b
Grain size and texture
Drill
er's
dep
th, i
n fe
et b
elow
gro
und
leve
l
Ichn
ofac
ies
Trac
e fo
ssils
and
se
dim
enta
ry
feat
ures
frac
i ii mol
d
fene
irv
Ichnofabricindex
1 2 3 4 5ND
mc s vfs vcsfs ms cs G P C
Lost
circ
ulat
ion
zone
s
Max
imum
vis
ual
est.
poro
sity
Flowmeter rate, in gallons per minute
0 147L S
Geol
ogic
unit
Bor
ehol
e w
all i
mag
e
RSM
HFC
type
Dep
ositi
onal
se
quen
ce
Hyd
rolo
gic
unit
DESu
rfac
es
Max
imum
est
. pe
rmea
bilit
yFl
ow
zone
s
Scientific Investigations Report 2017–5109Plate 5 of 21
U.S. Department of the InteriorU.S. Geological Survey
Prepared in cooperation with the
Broward County Environmental Planning and Community Resilience Division
Detailed Graphical Lithologic Log of the Avon Park Formation in the G–2984 Test CoreholeBy
Kevin J. Cunningham, Jared W. Kluesner, Richard L. Westcott, Edward Robinson, Cameron Walker, and Shakira A. Khan2017
EXPLANATION
Abbreviations
Mudstonem
Wackestonew
Packstonep
Grainstoneg
Floatstonef
Rudstoner
Boundstoneb
i Interparticleii Intraparticle
mold Particle moldicirv Irregular vug
frac Fracturefene Fenestral
Clayc
CobbleC
Mudm
Silts
Very fine sandvfs
Fine sandfs
Medium sandms
Coarse sandcs
GranuleG
PebbleP
Very coarse sandvcs
Depositional environmentDEHigh frequency cycle HFCRelative shoreline movementRSMNot determinedND
LandwardL
SeawardS
Estimated permeabilityEst. perm.Estimatedest.
General Grain size Texture Pore type
Depositional sequences
Depositional sequence AP3DS AP3High frequency cycle type
I Microbial-laminite-capped, grain-rich, peritidal cycle
II Rhizolith- and mud-capped, micrite-rich peritidal cycleIII Aggradational grain-rich subtidal cycleIV Glossifungites-capped subtidal cycle
High frequency cycle
Depositional-sequence boundary
No recovery/no data
Flooding surface FirmgroundKarst
Miscellaneous symbols
FS
K
FG
FG
FG
FG
FG
K
FG
K
FS
K
K
K
K
Ichnofacies
Lithofacies
Porosity and permability
High-energy inner shelf, shallow subtidal
High-energy event, marine subtidal High-energy inner shelf, shallow subtidalLow-energy inner shelf, shallow subtidal
Low-energy restricted lagoon inner shelf, subtidal
Low-energy restricted inner shelf, low-energy tidal flat
Low-energy restricted inner shelf, intertidal to supratidal
Avon Park FormationDepositional environment (DE)
Grain types, trace fossils, and sedimentary features
Gastropod
Ostracod
Larger benthic foraminifera undifferentiated
Smaller benthic foraminifera undifferentiated
Planktic foraminifera
Miliolid
FabulariaF
FallotellaFl
CoskinolinaC
Peloid
Small echinoid
Echinoid fragments
Microcodium
Unidentified skeletal grain
Bivalve
R Rotaliid
Rs Reussella
AmphisteginaA
Dasycladacean algae
RhodolithColeiconusCl
Charophytes
Intraclast
B Breccia Laminae
Desiccation cracksFenestrae
Planolites
Burrowed mottled
Thalassinoides-domintated Glossifungites firmground
Psilonichnus
Ophiomorpha
Rhizocorallium
Thalassanoides
Root traces
Asterosoma
Grain types Trace fossils
Sedimentary features
SS
Percent pore type
Maximum estimated permeability
Maximum visual estimated porosity
Floatstone and rudstone
Glossifungites
Mudstone
Skolithos Not determined
Carbonate
Floatstone
1–2%0% >10–25%>2–10% >25 –50%
>10–25%>1–10% >25 –50%
Grainstone
Cruziana
PackstoneWackestone and packstone
Packstone and grainstone
Mudstone and wackestone
Low Medium
Psilonichnus
Autochthonous breccia
Microbial laminite
0%
No
Data
ISSN 2328-0328 (online)https://doi.org/10.3133/sir20175109
Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government
This map was printed on an electronic plotter directly from digital files. Dimensional calibration may vary between electronic plotters and between X and Y directions on the same plotter, and paper may change size due to atmospheric conditions; therefore, scale and proportions may not be true on plots of this map.
For sale by U.S. Geological Survey, Information Services, Box 25286, Federal Center, Denver, CO 80225, 1–888–ASK–USGS
Suggested citation: Cunningham, K.J., Kluesner, J.W., Westcott, R.L., Robinson, Edward, Walker, Cameron, and Khan, S.A., 2017, Sequence stratigraphy, seismic stratigraphy, and seismic structures of the lower intermediate confining unit and most of the Floridan aquifer system, Broward County, Florida: U.S. Geological Survey Scientific Investigations Report 2017–5109, 71 p., 21 pls., https://doi.org/10.3133/sir20175109.