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Geologic map of the Walnut, Miss.-Tenn., 7.5' Quadrangle Geology by Charles T. Swann, R.P.G. Mississippi Mineral Resources Institute 2002 SCALE; 1:48,000 0 0 1 Mi. 1 Km N Projection is Transverse Mercator MS U D Tpc Qal Sand, silt, clay: flood plain deposits associated with existing fluvial system Porters Creek Formation Clay: micaceous, locally silty, massive to laminated, conchoidal to blocky fracture, spiculitic, sparse bivalve fossils; becomes sandy, glauconitic, bedded in lower part of section; becomes massive upon weathering Fault: Approximately located; upthrown and downthrown blocks indicated by "U" and "D" U D Fault: Measured location Tertiary Quaternary Owl Creek Formation Clay, silt, sand: typically silty clay, sandy, very micaceous, fossiliferous; sand beds fine-grained, thin; unit often carbonaceous at top; weathers to sandy clay Axis of anticlinal feature Hydrocarbon well - dry hole Clayton Formation; Chalybeate Member Sand: medium- to fine-grained, poorly bedded, minor clay beds, fossiliferous; at base is discontinuous limestone, glauconitic, phosphatic, fossiliferous; upper unit weathers to massive argillaceous sand; entire unit assigned to Chalybeate Member Cretaceous Tcl Koc LEGEND Unconformity Tmr Meridian Sand Sand: medium- to coarse-grained, cross-bedded, minor clay beds, silicified wood locally common Tna Naheola Formation Sand, clay, lignite: sand beds typically medium-grained and argillaceous, may be well sorted, may locally contain granules; clays are gray to yellowish-gray, thinly bedded to laminated; base is locally channeled and may contain angular clay boulders, often has a "mealy" texture R 3 E R 4 E R 3 E R 4 E T 2 S T 1 S T 2 S T 1 S 15 15 HOLLY SPRINGS NATIONAL FOREST I L LIN O IS C ENTRAL GULF RAILROAD WALNUT 72 72 354 101 301 301 Brownsfield Tiplersville U U U U U D U D U U D D D D D D Tpc Tpc Tpc Tpc Tpc Tpc Tpc HARDEMAN CO. TIPPAH CO. TENNESSEE MMRI-Martindale No. 1 MISSISSIPPI Tpc Tna Tna Tna Tna Tna Tmr Tmr Tmr Tmr Tmr Tmr Tmr Tmr Qal Koc Tcl Tcl Tcl CREEK MUDDY CREEK CREEK CREEK BRANCH BRANCH BRANCH YOPP DRY BIG CREEK MIX BRANCH CANE BRANCH WATKINS BRANCH BRANCH PRESSLEY SOUTH NORTH SPICEWOOD HURRICANE CREEK CREEK BLUFF MUDDY TURKEY BRUSH DREWERY CREEK CREEK CREEK Smackco Ltd., Blackwell No. 1 Memphis Equiptment Co., Melton No. 1 R E G I S T E R E D P R O F E SS I O N A L G E O L O G I S T C H A R L E S T . S W A N N T H E G R E A T S E A L O F T H E S T A T E O F M I S S I S S I P P I MS 0003

N MS Geology by Charles T. Swann, R.P.G. Mississippi ...Geology by Charles T. Swann, R.P.G. Mississippi MineralT Resources Institute 2002 SCALE; 1:48,000 0 0 1 Mi. 1 Km N Projection

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Page 1: N MS Geology by Charles T. Swann, R.P.G. Mississippi ...Geology by Charles T. Swann, R.P.G. Mississippi MineralT Resources Institute 2002 SCALE; 1:48,000 0 0 1 Mi. 1 Km N Projection

Geologic map of the Walnut, Miss.-Tenn., 7.5' QuadrangleGeology by Charles T. Swann, R.P.G.Mississippi Mineral Resources Institute

2002

SCALE; 1:48,000

0

0

1 Mi.

1 Km

N

Projection is Transverse Mercator

MS

U

D

Tpc

Qal Sand, silt, clay: flood plain deposits associated withexisting fluvial system

Porters Creek FormationClay: micaceous, locally silty, massive to laminated,conchoidal to blocky fracture, spiculitic, sparse bivalvefossils; becomes sandy, glauconitic, bedded in lowerpart of section; becomes massive upon weathering

Fault: Approximately located;upthrown and downthrownblocks indicated by "U" and "D"

UD Fault: Measured location

Ter

tiary

Qua

tern

ary

Owl Creek FormationClay, silt, sand: typically silty clay, sandy, verymicaceous, fossiliferous; sand beds fine-grained, thin;unit often carbonaceous at top; weathers to sandy clay

Axis of anticlinal feature

Hydrocarbon well - dry hole

Clayton Formation; Chalybeate MemberSand: medium- to fine-grained, poorly bedded, minorclay beds, fossiliferous; at base is discontinuouslimestone, glauconitic, phosphatic, fossiliferous; upperunit weathers to massive argillaceous sand; entireunit assigned to Chalybeate Member

Cre

tace

ous

Tcl

Koc

LEGEND

Unconformity

Tmr Meridian SandSand: medium- to coarse-grained, cross-bedded, minorclay beds, silicified wood locally common

Tna Naheola FormationSand, clay, lignite: sand beds typically medium-grainedand argillaceous, may be well sorted, may locally contain granules; clays are gray to yellowish-gray, thinly beddedto laminated; base is locally channeled and may containangular clay boulders, often has a "mealy" texture

R 3 E R 4 E

R 3 E R 4 ET

2 S

T 1

S

T 2

ST

1 S

15

15

HOLLY SPRINGS NATIONAL FOREST

ILLI

NO

IS C

EN

TRA

L G

ULF

RA

ILR

OA

D

WALNUT

72

72

354

101

301

301

Brownsfield

Tiplersville

UU

U

U

U

D

UD

U

U

D

D

D

D

D

D

Tpc

Tpc

Tpc

Tpc

Tpc

TpcTpc

HARDEMAN CO.

TIPPAH CO.TENNESSEE

MMRI-MartindaleNo. 1

MISSISSIPPI

Tpc

Tna

Tna

Tna

Tna

Tna

Tmr

Tmr

Tmr

Tmr

Tmr

Tmr

Tmr

Tmr

Qal

Koc

Tcl

Tcl

Tcl

CR

EE

K

MU

DD

Y

CR

EEK

CREEK

CREEK

BRANCH

BR

AN

CH B

RA

NC

H

YO

PP

DRY

BIG

CR

EEKMIX

BRANCH

CANE

BRANCH

WA

TKIN

S

BRANCH

BRANCH

PRESSLEY

SOUTH

NO

RTH

SPICEWOOD

HURRICANE

CREEK

CREEK

BLUFF

MU

DD

Y

TURKEY

BRU

SHD

RE

WE

RY

CR

EE

K

CR

EE

K

CREEK

Smackco Ltd.,Blackwell No. 1

MemphisEquiptment Co.,Melton No. 1

RE

GIS

TERED PROFESSIONAL GEO

LOG

IST

CHARLES T. SWANN

THE GR

EA

T S

EAL O

F THE STATE OF M

ISSISSIPPI

MS0003