Geologic Map of the Catoosa 7.5' Quadrangleogs.ou.edu/docs/OGQ/OGQ-64-color.pdf · 2008. 2. 6. ·...
1
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 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 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 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 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 D D D D D D D D D D D ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! IPog IPlb Qal Qts IPsn Qal IPsn IPfs b IPlb fs,b IPlb fs,b IPlb fs,b IPfs IPlb IPfs b IPsn IPsn L L L v L L L L L L v L L L L v L v v L L Qal IPsn IPsnc IPsnc IPsnc IPsn c,t c,t c,t c t c t Qal c IPsn IPsn t t t c t c Qal c t IPsnc t c c t IPsn c t c,t c,t c t c t Qal IPsn IPsnc IPsnc IPsn IPsnc IPsnc IPsnc IPsn IPsn Qal v v L L v L L b b Qtg b IPfs b IPfs b B'''' B''''' af af IPsnc af IPlb c B'''' Feet 800 600 400 200 0 -200 -400 B''''' Feet 800 600 400 200 0 -200 -400 lPlb Qal lPsn Qal lPsnc lPsn Qal lPbg (Boggy Formation) Verdigris Limestone Tiawah Limestone Inola Limestone Sallie McAauly #1; proj. 3100 ft South E. Dodd #1; proj. 2500 ft South C.E. Dearston Leach #1; proj. 300 ft North L.W. Hoover Hias #1; proj. 4600 ft North Morgan and Flynn Robson #1; proj. 4200 ft North Adkins Drilling Co. Geo Patrick #1; proj. 1600 ft North Duck Lake Toague #1; proj. 1600 ft South Mulligan and Parker Geo Patrick #1; proj. 300 ft North G.W. Webster Baker #1; proj. 5700 ft North Sooner Oil and Gas Co. lPfs Savanna and Older Formations Cross section drawn by T.M. Stanley Vertical exaggeration: x10 OKLAHOMA GEOLOGICAL SURVEY Charles J. Mankin, Director O K L A H O M A G E O L O G I C A L S U R V E Y 1 90 8 C E N T E N N I A L 2 0 0 8 SCALE 1:24 000 ° 7 APPROXIMATE MEAN DECLINATION M A G N E T I C N O R T H T R U E N O R T H GEOLOGIC MAP OF THE CATOOSA 7.5 QUADRANGLE, ROGERS AND WAGONER COUNTIES, OKLAHOMA Thomas M. Stanley and Galen W. Miller 2006 ′ DESCRIPTION OF UNITS* ARTIFICIAL FILL (Holocene) - ALLUVIUM (Holocene) - Clay, silt, sand, and gravel in channels and on flood plains of modern streams. Includes terrace deposits of similar composition located directly above and adjacent to modern channels and flood plains. Thickness: 0 to about 30 ft. TERRACE GRAVELS (Pleistocene(?)) - Concentrations of locally and distally derived sediment, mostly rounded and subrounded chert and limestone pebbles mixed with a medium-grained quartz sand sediment. Pebbles typically dusky yellow (5Y6/4) to light olive brown (5Y5/6) color; quartz sand sediment more of a light brown (5YR5/6) color. May represent former course of Verdigris River. Thickness: 5 ft or less. OOLOGAH FORMATION UPPER TERRACE SANDS (Holocene and Pleistocene(?)) - Consists mostly of unconsolidated fine- to medium-grained quartz sand, silt, and clay; little to no gravel-sized material observed. Situated just above modern flood plains and drainages. Thickness: 0 ft to as much as 20 ft; averages closer to 8 ft thick. (Pennsylvanian, Desmoinesian) - Limestone characterized by a medium gray (N5) to medium dark gray, medium bluish gray (5B5/1), to locally yellowish gray (5Y7/2), thin- to medium bedded, wavy, skeletal and whole-fossil, algal mudstones and wackestones; bedding varies between 1”-16” thick, with thicker beds more common at the base of formation. Fossils dominated by numerous species of brachiopod, phylloid algal, and crinoid debris; fenestrate and ramose bryozoans present in thicker beds, while bivalve-filled burrows also common in some sections with a large compliment of argillaceous limestone. The upper half of exposed Oologah tends to be more regular, thin-bedded, slightly argillaceous, fossiliferous mudstones; bedding planar to slightly wavy, ranging from 2-5” thick; fossils similar to lower part, except less of a phylloid algal content. The Anna Shale and underlying Childers School Member were not observed in the quadrangle. Only lower 50 to 60 ft of the Oologah Formation exposed in quad. LABETTE FORMATION (Pennsylvanian, Desmoinesian) - Medium light gray (N6) to dusky yellow (5Y6/4), occasionally light olive gray (5Y5/2), laminated, very silty to sandy, micaceous, concretionary clayshale; concretions dusky red (5R4/2) to moderate red (5R5/4), composed of hematite and/or siderite(?), and usually occur sporadically throughout formation as 1-3” diameter discoid-shaped clasts. Clayshale predominantly non-calcareous, although some narrow horizons are weakly calcareous (particularly those associated with abundant concretions). Locally, various non-descript very sandy shale or sandstone horizons occur; mostly these sand horizons are planar laminated to thin-bedded. Overall, formation becomes increasingly silty and sandy toward the top. Within the upper 50 ft. of the formation a sequence of interbedded sandstones and shales (Peru sandstones). The Peru sandstones consist of between 2 to 4 intervals of dusky yellow (5Y6/4), moderately indurated, thin- to medium-, trough-cross-bedded, fine-grained, non-calcareous sandstones; sandstone intervals vary between 5 to as much as 15 ft thick, where the thicker intervals have been variably termed the Upper and Lower Peru sandstones by previous investigations. Each sandstone separated by 7 to 10 ft thick interval of well-laminated, flaser-bedded, calcareous, interbedded mudshale and siltstone. The Sageeyah limestone was not observed in this quadrangle. Formation about 220 ft thick. FORT SCOTT FORMATION (Pennsylvanian, Desmoinesian) - In the Catoosa Quadrangle the formation consists of only two members, in descending order: 1) the Little Osage Shale; and 2) the Blackjack Creek Limestone. Thickness of the formation is about 7 to 12 ft, averaging closer to 10 ft thick. : Similar to the Excello Shale of the Senora Formation, a medium dark gray (N4) to dark gray (N3), well-laminated to fissile, phosphatic clayshale; upper 5-8” a light brownish gray (5YR6/1), blocky-bedded, silty, calcareous, fossiliferous clayshale. Phosphate nodules throughout lower part of member, occurring as 0.25-0.5”, ovoid-shaped clasts. Thickness usually 5 ft, but may be as thin as 2 ft thick locally. : Light gray (N7), medium light gray (N6), light brownish gray (5YR6/1), to moderate orange pink (5YR8/4), thin, planar to wavy bedded, skeletal to whole-fossil wackestone. Bedding varies from 2” to 5” thick; wavy bedding contacts due (in part) to stromatolitic bedding; limestone in upper 1-3 ft of member exhibiting wavy laminated bedding and more fragmentary bioclasts compared to lower parts of member. Fossils dominated by spirifer and productid brachiopods, and crinoid debris; algae and fusulinids common in some intervals. Thickness from 5 to 10 ft, averaging close to 7 ft. Little Osage Shale Blackjack Creek Limestone Natural or artificial talus, slumps, and tailings covering formally exposed areas around active and inactive mining operations. Qal Qtg IP IP IP fs lb og Qts af af SENORA FORMATION (Pennsylvanian, Desmoinesian) - Complex sequence of silty and concretionary clayshale interbedded with a number of mappable limestone and sandstone members (including: b, Breezy Hill Limestone; L, Lagonda Sandstone; v, Verdigris Limestone; lPsnc, Chelsea Sandstone); and various minor sandstone intervals and coal beds (including: Oowala sandstone; and the Iron Post, Croweburg, and Mineral coal beds). Thickness of formation about 500 ft. A silty to sandy clayshale, interlaminated with 0.16-1” thick very fine-grained sandstone and siltstone beds is the predominant lithology of the formation, silt and sand content increasing adjacent to significant sandstone intervals (such as the Chelsea or Lagonda sandstones); clayshale bedding laminated, becoming blocky where deeply weathered; color variable, ranging, from the most frequent to infrequent: medium light gray (N6), brownish gray (5YR4/1), grayish orange (10YR7/4), very pale orange (10YR8/2), dark yellowish orange (10YR6/2), pale brown (5YR5/2), light brown (5YR5/6), grayish yellow (5Y8/4), and yellowish gray (5Y7/2); typically, shale associated with concretionary zones tend to be more orange or brown, instead of gray in hue; clay is predominant cement, calcite rare. Clayshales immediately above coal seams tends to be harder, silt-free, slightly phosphatic, with slightly thicker laminated bedding, and are weakly calcareous; color usually a medium dark gray (N4). The interlaminated sandstones and siltstones are friable to poorly indurated, usually a very pale orange (10YR8/2), pale orange (10YR8/2), or dark yellowish orange (10YR6/2); sandstone more common than siltstone, typically fine- to very fine-grained; predominant cement is clay, with a possible weak silica. Ironstone concretions occur sporadically throughout the shale section, but concentrations may occur just above the Verdigris Limestone; concretions composed predominately of hematite, may occur as 0.5-2” thick, dense discontinuous beds in the concentrated horizons, but normally occur as small (between 1-2”) individual, hollow, ovoid-shaped clasts; color a light red (5R6/6) to moderate red (5R5/4). A number of prominent stratigraphic horizons occur in the Senora Formation, these are in descending order: : Predominantly a medium dark gray (N4) to dark gray (N3), well-laminated to fissile, phosphatic clayshale; however, upper 2-5” a light brownish gray (5YR6/1) to pale brown (5YR5/2), laminated, slightly silty, calcareous, fossiliferous clayshale. Phosphate nodules throughout lower part of member, occurring as 0.25-0.5”, ovoid-shaped clasts. Thickness from 3-6 ft, averaging 4 ft. (b; fs,b): Grayish orange (10YR7/4), yellowish gray (5Y7/2), pale olive (10Y6/2), to medium light gray (N6), with local dark yellowish orange streaks along bedding contacts and fractures, alternating thin to medium, wavy bedded, whole-fossil and skeletal wackestone. Bedding varies from 3-16” thick, with thinner bedding characterized by skeletal textures, and medium bedding a characteristically whole-fossil texture. Large linoproductuids, other small productids ( ) and mesolobids are the most common fossils; chaetetid sponges and large crinoid stems also present. Skeletal material usually consists of sub-angular crinoid debris (ossicles and plates), and nondescript brachiopod shell fragments. Some exposures contain casts of weathered out pyrite crystals, which have subsequently turned to goethite and hematite. Overall, the Breezy Hill is thicker and more wavy bedded than the overlying Blackjack Creek Limestone. Thickness of the unit about 7 to 8 ft. : Moderate yellowish brown (10YR5/4) to medium light gray (N6), fissile to well- laminated, fossiliferous silty clayshale. Silt and sand increasing toward top of member. Base occurs at the top of the Iron Post coal. Due to extreme thickness of the underlying Lagonda Sandstone this shale interval rarely exceeds 1 ft, and averages closer to 8 inches in thickness. : Where observed, coal is a single bed, black (N1) to grayish black (N2), having well- developed 2 directional cleats. Associated underclay not well-developed. Thickness about 6 to 8 inches. (L): Grayish orange (10YR7/4), dark yellowish orange (10YR6/6), to very pale orange (10YR8/2), friable to moderately indurated, thin- to medium-bedded, sometimes wavy laminated, trough-cross-bedded, fine- to very fine-grained, slightly siliceous sandstone; shale partings may occur between cross-bed sets; sandstone mostly very clean, with rounded to well- rounded quartz grains, but it does become more argillaceous and micaceous toward top; calcite cement rare. Bedding varies from less than 1/16” thick to as much as 24” thick, thicker bedded material more common at the basal two-thirds of the member; ripple-bedded surfaces associated with internal tabular cross-lamination common in upper one-third of member. Molds of and may occur locally. Thickness ranges from 20 to as much as 60 ft. (v): medium dark gray (N4) skeletal mudstone; but may weather to a medium light gray (N6), grayish red (5R4/2), or grayish orange (10YR7/4) color. Represented either by a single massive bed, or by a couple of 9-12” thick, wavy, skeletal mudstone beds; top 3-4” becoming a wavy laminated whole-fossil mudstone to wackestone, with large productid brachiopods and large crinoid stems. Chert pods, or silica replacement of limestone along bedding surfaces common. Thickness about 2 to 3 ft. : Poorly exposed in map area; where observed in old mine workings represented by a black (N1) to grayish black (N2), 0.5-2’ thick coal bed overlying a comparably thick very light gray (N8) to light bluish gray (5B7/1) underclay. Locally, a pair of 9-12” thick, whole-fossil mudstones separated by a 6” thick clayshale interval, informally named the McNabb limestone by some geologists, occurs immediately below the underclay. (IPsnc; c; c,t): Variable sandstone unit that can be loosely segregated into two zones. Lower zone well exposed, consisting of a pale reddish brown (10YR4/2), dark yellowish brown (10YR7/4), grayish orange (10YR8/2), to locally moderate yellow (5Y7/6), pale greenish yellow (10Y8/2), or pale olive (10Y6/2), moderately indurated, medium- to thin-bedded, fine- to medium- grained, calcareous trough-cross-bedded sandstone. Trough cross-bed sets vary from 0.5” to 3’ thick, average 5” thick; locally graded, with siltstone, sandstone, and limestone pebble conglomerate set within a medium-grained sand matrix at base, that grades upward into a fine-grained sandstone. Thickness of basal Chelsea varies from 20-60 ft, but averages closer to 35 ft. Upper zone of the Chelsea poorly exposed, evidenced often times only by the presence of a sandy loam soil as opposed to a clay loam; where exposed, consists of a pale yellowish brown (10YR6/2) to light brown (5YR6/4), friable, thin-bedded to often planar laminated, weakly calcareous, micaceous, fine-grained sandstone. Thickness varying from 15-40 ft thick, averaging closer to 20 ft. Typically, base of the Chelsea resides 20-25 ft above the Tiawah Limestone; locally it may be as high as 30 ft above. Where the Chelsea was mapped in close proximity to the Tiawah, base of the sandstone labeled with a ‘c,t’. Average thickness of the Chelsea Sandstone is 110 ft. (t; c,t): Similar to the Verdigris Limestone in texture and thickness, usually a grayish orange pink (5YR7/2) to very pale orange (10YR7/2), locally light brownish gray (5YR6/1) to pale yellowish brown (10YR6/2), with dark yellowish orange (10YR6/6) splotches; generally a massive bed of whole-fossil mudstone in lower half, grading into a wavy laminated skeletal wackestone in upper half. Fossils usually large crinoid stems with large productid and spirifirid brachiopods. Thickness varies from 2 to 4 ft thick. Where the Tiawah was mapped in close proximity to the Chelsea, base of the limestone labeled with a ‘c,t’. : Rarely observed; black (N1) to grayish black (N2), 1-2” thick coal seam, with a 2-3” thick underclay immediately below. : Normally a yellowish gray (5Y7/2) to pale greenish yellow (10Y8/2) color, but can be a very pale orange (10YR8/2) to pale yellowish orange (10YR8/6) in deeply weathered exposures; moderately indurated, fine-grained, slightly micaceous, siliceous sandstone. Bedding planar, medium, varying from 11-16” thick; some tabular cross-bedding observed at the base of unit in some exposures. Thickness from 2-4 ft thick. : Overall, a grayish orange (10YR7/4), becoming dark yellowish orange (10YR6/6) in upper third, moderately indurated, medium- to thin-bedded, fine- to very fine-grained, micaceous, calcareous sandstone, with shale interbeds and partings. Interval can be segregated into 3 general lithologic zones: basal zone usually 23” thick, consists of medium to thin planar bedding, with bedding ranging from 0.5-4” thick, shale partings common, sandstone is slightly calcareous; middle zone consists of about 3.2’ of alternating beds of sandstone and shale, each about 3-4” thick, sandstone slightly calcareous and indurated; the upper sandstone zone is moderately indurated, siliceous, and thin- to medium-trough-cross-bedded. Upper Taft sandstone about 5 to 7 ft thick. Excello Shale Breezy Hill Limestone Desmoinesia Kinnison Shale Iron Post coal Lagonda Sandstone Linoproductus Juresania Verdigris Limestone Croweburg coal Chelsea Sandstone Tiawah Limestone Tebo coal White sandstone Upper Taft sandstone *Detailed descriptions only include mappable units observed in the field. Formal member and bed names are indicated by capitalization (i.e., Chelsea Sandstone), while informal names are given in lowercase (i.e., Peru sandstone). Color of units based on fresh surfaces, unless stated otherwise. IPsn Qal Qtg af UNCONFORMITY HOLOCENE PLEISTOCENE? DESMOINESIAN QUATERNARY PENNSYLVANIAN IP IP IP IP IP fs og lb b v L sn snc CORRELATION OF MAP UNITS af Qts t Base Map Credits Geologic Map Credits Base map compiled by the U.S. Geological Survey. Topography by photogrammetric methods from aerial photographs taken 1962. Field checked 1963. Photorevised from aerial photographs taken 1978. Map edited 1980. Universal Transverse Mercator (UTM) projection. 1927 North American Datum. 10,000-foot grid ticks based on Oklahoma coordinate system, north zone. UTM 1,000-meter grid ticks, zone 15. Geology by Thomas M. Stanley and Galen W. Miller, 2005-2006. Research supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program, under Assistance Award Number 05HQAG0048. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. Cartography and layout prepared by G. Russell Standridge, 2006. Oklahoma Geologic Quadrangle OGQ-64 Geologic Map of the Catoosa 7.5 Quadrangle Unit contact; dashed where approximate SYMBOLS Outcrop, geologic observation Petroleum well. Includes oil, gas, oil and gas, dry service (water supply or injection), junked and abandoned, unknown. Modified from Natural Resources Information System database 44 44 244 44 75 412 75 51 51 96°15’ 35°52’30” D’’’’’ D’’’’ 36°22’30” A A’ A’’ A’’’ A’’’’ Tulsa Tulsa Creek Wagoner Wagoner Rogers Tulsa Broken Arrow Sand Springs Sapulpa Jenks Collinsville Skiatook Claremore CLAREMORE SAGEEYAH SPERRY COLLINSVILLE Owasso Sperry Catoosa Kiefer Bixby A rk a ns a s Ri ve r V e rdi g ris R i v e r MINGO TULSA JENKS BIXBY LEONARD KELLYVILLE SAPULPA NORTH SAPULPA SOUTH LAKE SAHOMA SAND SPRINGS BROKEN ARROW CATOOSA 35°52’30” 36°22’30” 96°00’ 95°30’ 95°37’30” WEKIWA ONETA COWETA Coweta B B’ B’’ B’’’ B’’’’ B’’’’’ C’’’’ C’’’’’ Tulsa Osage Current Map Quadrangles Proposed for Mapping Major Cities Expanding Suburbs and Communities 5 Miles EXPLANATION North Mapped Quadrangles
Transcript of Geologic Map of the Catoosa 7.5' Quadrangleogs.ou.edu/docs/OGQ/OGQ-64-color.pdf · 2008. 2. 6. ·...
-
DD
D
D
D
D
D
D
D
D
D
D
D
D
D
DD
DD D
D
D
DD D
D
D
DD
DD
D
D D D
D
DD
D
D
D
D
D
DD
D
D
D
D D
D
D
D
D
D
D
D
D D DD
D
D
D
D
D
D
D
D
D
D
D
D D
D
D
D
D
D
DD
D
DDD
D
D
D
D
D
D
DD
D
D
D
D
DDD DD
D
DDD
D
DDD
D
D
D
D
D
D
D DDD
D
D
D
DD
D
D
D
DD
DD DD D
DD
DD
D D
D
D D
D
D
D D
D
D D
!
!
!
!! !
!
!
!
!
!
!
!
!
!
!
!
!
!!
!
! !
!
!
!
!
!
!
!
!
!
!
!!
!
! !! !!
!
!
!
!!
!
! !!
!
!
!
!
!
!
!
!
!
!
!
!
!
!
!
!
!
!
!
!!
!
!
! !
!
!
!
!
!
!
!!
!
!
!
!
!
!
!
!
!
!
!
!!
!
!
!
!
!
!
!
!
!!
!
!!
!
!
IPog
IPlb
Qal
Qts
IPsn
Qal
IPsn
IPfs
b
IPlb
fs,b
IPlbfs,b
IPlb
fs,b
IPfs
IPlb
IPfs
b
IPsn
IPsnL
L
Lv
L
L
L
L
L
L
vL
L
L
L
v
L
v
v
L
L
Qal
IPsn
IPsnc
IPsnc
IPsnc
IPsn
c,t
c,t
c,tc
tc
t
QalcIPsn
IPsn
tt t
c
tc
Qal
c
t
IPsnct c
c
t
IPsn
c
t
c,t
c,t
c
t
c
t
Qal
IPsn
IPsnc
IPsnc
IPsnIPsnc
IPsnc
IPsnc
IPsn
IPsn
Qal
v
v
L
L
v
L
L
b
b
Qtg
bIPfs
b
IPfsb
B'''' B'''''
af
af
IPsnc
af
IPlb
c
B''''Feet800
600
400
200
0
-200
-400
B'''''Feet800
600
400
200
0
-200
-400
lPlb
Qal lPsn Qal
lPsnclPsn
Qal
lPbg (Boggy Formation)
Verdigris Limestone
Tiawah Limestone
Inola Limestone
Sal
lie M
cAau
ly #
1; p
roj.
3100
ft S
outh
E. D
odd
#1; p
roj.
2500
ft S
outh
C.E
. Dea
rsto
n
Leac
h #1
; pro
j. 30
0 ft
Nor
thL.
W. H
oove
r
Hia
s #1
; pro
j. 46
00 ft
Nor
thM
orga
n an
d Fl
ynn
Rob
son
#1; p
roj.
4200
ft N
orth
Adk
ins
Dril
ling
Co.
Geo
Pat
rick
#1; p
roj.
1600
ft N
orth
Duc
k La
ke
Toag
ue #
1; p
roj.
1600
ft S
outh
Mul
ligan
and
Par
ker
Geo
Pat
rick
#1; p
roj.
300
ft N
orth
G.W
. Web
ster
Bak
er #
1; p
roj.
5700
ft N
orth
Soo
ner O
il an
d G
as C
o.
lPfs
Savanna and Older Formations
Cross section drawn by T.M. StanleyVertical exaggeration: x10
OKLAHOMA GEOLOGICAL SURVEYCharles J. Mankin, DirectorO
KL
AH
OM
A G
EOLOGICAL SU
RV
EY
1908 CENTENNIAL
200
8
SCALE 1:24 000°7
APPROXIMATE MEAN DECLINATION
MA
GN
ETIC
NO
RTH
TRU
E N
OR
TH
GEOLOGIC MAP OF THE CATOOSA 7.5 QUADRANGLE,ROGERS AND WAGONER COUNTIES, OKLAHOMA
Thomas M. Stanley and Galen W. Miller2006
′
DESCRIPTION OF UNITS*
ARTIFICIAL FILL (Holocene) -
ALLUVIUM (Holocene) - Clay, silt, sand, and gravel in channels and on flood plains of modern streams. Includes terrace deposits of similar composition located directly above and adjacent to modern channels and flood plains. Thickness: 0 to about 30 ft.
TERRACE GRAVELS (Pleistocene(?)) - Concentrations of locally and distally derived sediment, mostly rounded and subrounded chert and limestone pebbles mixed with a medium-grained quartz sand sediment. Pebbles typically dusky yellow (5Y6/4) to light olive brown (5Y5/6) color; quartz sand sediment more of a light brown (5YR5/6) color. May represent former course of Verdigris River. Thickness: 5 ft or less.
OOLOGAH FORMATION
UPPER TERRACE SANDS (Holocene and Pleistocene(?)) - Consists mostly of unconsolidated fine- to medium-grained quartz sand, silt, and clay; little to no gravel-sized material observed. Situated just above modern flood plains and drainages. Thickness: 0 ft to as much as 20 ft; averages closer to 8 ft thick.
(Pennsylvanian, Desmoinesian) - Limestone characterized by a medium gray (N5) to medium dark gray, medium bluish gray (5B5/1), to locally yellowish gray (5Y7/2), thin- to medium bedded, wavy, skeletal and whole-fossil, algal mudstones and wackestones; bedding varies between 1”-16” thick, with thicker beds more common at the base of formation. Fossils dominated by numerous species of brachiopod, phylloid algal, and crinoid debris; fenestrate and ramose bryozoans present in thicker beds, while bivalve-filled burrows also common in some sections with a large compliment of argillaceous limestone. The upper half of exposed Oologah tends to be more regular, thin-bedded, slightly argillaceous, fossiliferous mudstones; bedding planar to slightly wavy, ranging from 2-5” thick; fossils similar to lower part, except less of a phylloid algal content.
The Anna Shale and underlying Childers School Member were not observed in the quadrangle.Only lower 50 to 60 ft of the Oologah Formation exposed in quad.
LABETTE FORMATION (Pennsylvanian, Desmoinesian) - Medium light gray (N6) to dusky yellow (5Y6/4), occasionally light olive gray (5Y5/2), laminated, very silty to sandy, micaceous, concretionary clayshale; concretions dusky red (5R4/2) to moderate red (5R5/4), composed of hematite and/or siderite(?), and usually occur sporadically throughout formation as 1-3” diameter discoid-shaped clasts. Clayshale predominantly non-calcareous, although some narrow horizons are weakly calcareous (particularly those associated with abundant concretions). Locally, various non-descript very sandy shale or sandstone horizons occur; mostly these sand horizons are planar laminated to thin-bedded. Overall, formation becomes increasingly silty and sandy toward the top.
Within the upper 50 ft. of the formation a sequence of interbedded sandstones and shales (Peru sandstones). The Peru sandstones consist of between 2 to 4 intervals of dusky yellow (5Y6/4), moderately indurated, thin- to medium-, trough-cross-bedded, fine-grained, non-calcareous sandstones; sandstone intervals vary between 5 to as much as 15 ft thick, where the thicker intervals have been variably termed the Upper and Lower Peru sandstones by previous investigations. Each sandstone separated by 7 to 10 ft thick interval of well-laminated, flaser-bedded, calcareous, interbedded mudshale and siltstone.
The Sageeyah limestone was not observed in this quadrangle.Formation about 220 ft thick.
FORT SCOTT FORMATION (Pennsylvanian, Desmoinesian) - In the Catoosa Quadrangle the formation consists of only two members, in descending order: 1) the Little Osage Shale; and 2) the Blackjack Creek Limestone. Thickness of the formation is about 7 to 12 ft, averaging closer to 10 ft thick.
: Similar to the Excello Shale of the Senora Formation, a medium dark gray (N4) to dark gray (N3), well-laminated to fissile, phosphatic clayshale; upper 5-8” a light brownish gray (5YR6/1), blocky-bedded, silty, calcareous, fossiliferous clayshale. Phosphate nodules throughout lower part of member, occurring as 0.25-0.5”, ovoid-shaped clasts. Thickness usually 5 ft, but may be as thin as 2 ft thick locally.
: Light gray (N7), medium light gray (N6), light brownish gray (5YR6/1), to moderate orange pink (5YR8/4), thin, planar to wavy bedded, skeletal to whole-fossil wackestone. Bedding varies from 2” to 5” thick; wavy bedding contacts due (in part) to stromatolitic bedding; limestone in upper 1-3 ft of member exhibiting wavy laminated bedding and more fragmentary bioclasts compared to lower parts of member. Fossils dominated by spirifer and productid brachiopods, and crinoid debris; algae and fusulinids common in some intervals. Thickness from 5 to 10 ft, averaging close to 7 ft.
Little Osage Shale
Blackjack Creek Limestone
Natural or artificial talus, slumps, and tailings covering formally exposed areas around active and inactive mining operations.
Qal
Qtg
IP
IP
IP
fs
lb
og
Qts
afafSENORA FORMATION (Pennsylvanian, Desmoinesian) - Complex sequence of silty and concretionary clayshale interbedded with a number of mappable limestone and sandstone members (including: b, Breezy Hill Limestone; L, Lagonda Sandstone; v, Verdigris Limestone; lPsnc, Chelsea Sandstone); and various minor sandstone intervals and coal beds (including: Oowala sandstone; and the Iron Post, Croweburg, and Mineral coal beds). Thickness of formation about 500 ft.
A silty to sandy clayshale, interlaminated with 0.16-1” thick very fine-grained sandstone and siltstone beds is the predominant lithology of the formation, silt and sand content increasing adjacent to significant sandstone intervals (such as the Chelsea or Lagonda sandstones); clayshale bedding laminated, becoming blocky where deeply weathered; color variable, ranging, from the most frequent to infrequent: medium light gray (N6), brownish gray (5YR4/1), grayish orange (10YR7/4), very pale orange (10YR8/2), dark yellowish orange (10YR6/2), pale brown (5YR5/2), light brown (5YR5/6), grayish yellow (5Y8/4), and yellowish gray (5Y7/2); typically, shale associated with concretionary zones tend to be more orange or brown, instead of gray in hue; clay is predominant cement, calcite rare.
Clayshales immediately above coal seams tends to be harder, silt-free, slightly phosphatic, with slightly thicker laminated bedding, and are weakly calcareous; color usually a medium dark gray (N4).
The interlaminated sandstones and siltstones are friable to poorly indurated, usually a very pale orange (10YR8/2), pale orange (10YR8/2), or dark yellowish orange (10YR6/2); sandstone more common than siltstone, typically fine- to very fine-grained; predominant cement is clay, with a possible weak silica.
Ironstone concretions occur sporadically throughout the shale section, but concentrations may occur just above the Verdigris Limestone; concretions composed predominately of hematite, may occur as 0.5-2” thick, dense discontinuous beds in the concentrated horizons, but normally occur as small (between 1-2”) individual, hollow, ovoid-shaped clasts; color a light red (5R6/6) to moderate red (5R5/4).
A number of prominent stratigraphic horizons occur in the Senora Formation, these are in descending order:
: Predominantly a medium dark gray (N4) to dark gray (N3), well-laminated to fissile, phosphatic clayshale; however, upper 2-5” a light brownish gray (5YR6/1) to pale brown (5YR5/2), laminated, slightly silty, calcareous, fossiliferous clayshale. Phosphate nodules throughout lower part of member, occurring as 0.25-0.5”, ovoid-shaped clasts. Thickness from 3-6 ft, averaging 4 ft.
(b; fs,b): Grayish orange (10YR7/4), yellowish gray (5Y7/2), pale olive (10Y6/2), to medium light gray (N6), with local dark yellowish orange streaks along bedding contacts and fractures, alternating thin to medium, wavy bedded, whole-fossil and skeletal wackestone. Bedding varies from 3-16” thick, with thinner bedding characterized by skeletal textures, and medium bedding a characteristically whole-fossil texture. Large linoproductuids, other small productids ( ) and mesolobids are the most common fossils; chaetetid sponges and large crinoid stems also present. Skeletal material usually consists of sub-angular crinoid debris (ossicles and plates), and nondescript brachiopod shell fragments. Some exposures contain casts of weathered out pyrite crystals, which have subsequently turned to goethite and hematite. Overall, the Breezy Hill is thicker and more wavy bedded than the overlying Blackjack Creek Limestone. Thickness of the unit about 7 to 8 ft.
: Moderate yellowish brown (10YR5/4) to medium light gray (N6), fissile to well-laminated, fossiliferous silty clayshale. Silt and sand increasing toward top of member. Base occurs at the top of the Iron Post coal. Due to extreme thickness of the underlying Lagonda Sandstone this shale interval rarely exceeds 1 ft, and averages closer to 8 inches in thickness.
: Where observed, coal is a single bed, black (N1) to grayish black (N2), having well-developed 2 directional cleats. Associated underclay not well-developed. Thickness about 6 to 8 inches.
(L): Grayish orange (10YR7/4), dark yellowish orange (10YR6/6), to very pale orange (10YR8/2), friable to moderately indurated, thin- to medium-bedded, sometimes wavy laminated, trough-cross-bedded, fine- to very fine-grained, slightly siliceous sandstone; shale partings may occur between cross-bed sets; sandstone mostly very clean, with rounded to well-rounded quartz grains, but it does become more argillaceous and micaceous toward top; calcite cement rare. Bedding varies from less than 1/16” thick to as much as 24” thick, thicker bedded material more common at the basal two-thirds of the member; ripple-bedded surfaces associated with internal tabular cross-lamination common in upper one-third of member. Molds of and
may occur locally. Thickness ranges from 20 to as much as 60 ft. (v): medium dark gray (N4) skeletal mudstone; but may weather to a medium
light gray (N6), grayish red (5R4/2), or grayish orange (10YR7/4) color. Represented either by a single massive bed, or by a couple of 9-12” thick, wavy, skeletal mudstone beds; top 3-4” becoming a wavy laminated whole-fossil mudstone to wackestone, with large productid brachiopods and large crinoid stems. Chert pods, or silica replacement of limestone along bedding surfaces common. Thickness about 2 to 3 ft.
: Poorly exposed in map area; where observed in old mine workings represented by a black (N1) to grayish black (N2), 0.5-2’ thick coal bed overlying a comparably thick very light gray (N8) to light bluish gray (5B7/1) underclay. Locally, a pair of 9-12” thick, whole-fossil mudstones separated by a 6” thick clayshale interval, informally named the McNabb limestone by some geologists, occurs immediately below the underclay.
(IPsnc; c; c,t): Variable sandstone unit that can be loosely segregated into two zones. Lower zone well exposed, consisting of a pale reddish brown (10YR4/2), dark yellowish brown (10YR7/4), grayish orange (10YR8/2), to locally moderate yellow (5Y7/6), pale greenish yellow (10Y8/2), or pale olive (10Y6/2), moderately indurated, medium- to thin-bedded, fine- to medium-grained, calcareous trough-cross-bedded sandstone. Trough cross-bed sets vary from 0.5” to 3’ thick, average 5” thick; locally graded, with siltstone, sandstone, and limestone pebble conglomerate set within a medium-grained sand matrix at base, that grades upward into a fine-grained sandstone. Thickness of basal Chelsea varies from 20-60 ft, but averages closer to 35 ft. Upper zone of the Chelsea poorly exposed, evidenced often times only by the presence of a sandy loam soil as opposed to a clay loam; where exposed, consists of a pale yellowish brown (10YR6/2) to light brown (5YR6/4), friable, thin-bedded to often planar laminated, weakly calcareous, micaceous, fine-grained sandstone. Thickness varying from 15-40 ft thick, averaging closer to 20 ft. Typically, base of the Chelsea resides 20-25 ft above the Tiawah Limestone; locally it may be as high as 30 ft above. Where the Chelsea was mapped in close proximity to the Tiawah, base of the sandstone labeled with a ‘c,t’. Average thickness of the Chelsea Sandstone is 110 ft.
(t; c,t): Similar to the Verdigris Limestone in texture and thickness, usually a grayish orange pink (5YR7/2) to very pale orange (10YR7/2), locally light brownish gray (5YR6/1) to pale yellowish brown (10YR6/2), with dark yellowish orange (10YR6/6) splotches; generally a massive bed of whole-fossil mudstone in lower half, grading into a wavy laminated skeletal wackestone in upper half. Fossils usually large crinoid stems with large productid and spirifirid brachiopods. Thickness varies from 2 to 4 ft thick. Where the Tiawah was mapped in close proximity to the Chelsea, base of the limestone labeled with a ‘c,t’.
: Rarely observed; black (N1) to grayish black (N2), 1-2” thick coal seam, with a 2-3” thick underclay immediately below.
: Normally a yellowish gray (5Y7/2) to pale greenish yellow (10Y8/2) color, but can be a very pale orange (10YR8/2) to pale yellowish orange (10YR8/6) in deeply weathered exposures; moderately indurated, fine-grained, slightly micaceous, siliceous sandstone. Bedding planar, medium, varying from 11-16” thick; some tabular cross-bedding observed at the base of unit in some exposures. Thickness from 2-4 ft thick.
: Overall, a grayish orange (10YR7/4), becoming dark yellowish orange (10YR6/6) in upper third, moderately indurated, medium- to thin-bedded, fine- to very fine-grained, micaceous, calcareous sandstone, with shale interbeds and partings. Interval can be segregated into 3 general lithologic zones: basal zone usually 23” thick, consists of medium to thin planar bedding, with bedding ranging from 0.5-4” thick, shale partings common, sandstone is slightly calcareous; middle zone consists of about 3.2’ of alternating beds of sandstone and shale, each about 3-4” thick, sandstone slightly calcareous and indurated; the upper sandstone zone is moderately indurated, siliceous, and thin- to medium-trough-cross-bedded. Upper Taft sandstone about 5 to 7 ft thick.
Excello Shale
Breezy Hill Limestone
Desmoinesia
Kinnison Shale
Iron Post coal
Lagonda Sandstone
LinoproductusJuresania
Verdigris Limestone
Croweburg coal
Chelsea Sandstone
Tiawah Limestone
Tebo coal
White sandstone
Upper Taft sandstone
*Detailed descriptions only include mappable units observed in the field. Formal member and bed names are indicated by capitalization (i.e., Chelsea Sandstone), while informal names are given in lowercase (i.e., Peru sandstone). Color of units based on fresh surfaces, unless stated otherwise.
IPsn
Qal
Qtg
af
UNCONFORMITY
HO
LOC
ENE
PLE
ISTO
CE
NE?
DES
MO
INE
SIAN
QU
ATER
NA
RY
PEN
NSY
LVAN
IAN
IP
IP
IP
IPIP
fs
og
lb
b
vL
snsnc
CORRELATION OF MAP UNITS
af
Qts
t
Base Map Credits
Geologic Map Credits
Base map compiled by the U.S. Geological Survey. Topography by photogrammetric methods from aerial photographs taken 1962. Field checked 1963. Photorevised from aerial photographs taken 1978. Map edited 1980. Universal Transverse Mercator (UTM) projection. 1927 North American Datum. 10,000-foot grid ticks based on Oklahoma coordinate system, north zone. UTM 1,000-meter grid ticks, zone 15.
Geology by Thomas M. Stanley and Galen W. Miller, 2005-2006. Research supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program, under Assistance Award Number 05HQAG0048. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. Cartography and layout prepared by G. Russell Standridge, 2006.
Oklahoma Geologic Quadrangle OGQ-64Geologic Map of the Catoosa
7.5 Quadrangle
Unit contact; dashed where approximate
SYMBOLS
Outcrop, geologic observation
Petroleum well. Includes oil, gas, oil and gas, dry service (water supply or injection), junked and abandoned, unknown. Modified from Natural Resources Information System database
44
44
244
44
75
412
75
51
51
96°15’35°52’30”
D’’’’’D’’’’
36°22’30”
A A’ A’’ A’’’ A’’’’
Tulsa
Tulsa
Creek
Wagoner
Wagoner
Rogers
Tulsa
BrokenArrow
Sand Springs
Sapulpa
Jenks
CollinsvilleSkiatook
Claremore
CLAREMORESAGEEYAHSPERRY COLLINSVILLE
Owasso
Sperry
Catoosa
Kiefer
Bixby
ArkansasRiver
Verdigris River
MINGOTULSA
JENKS
BIXBY LEONARDKELLYVILLE
SAPULPANORTH
SAPULPASOUTH
LAKESAHOMA
SANDSPRINGS
BROKENARROW
CATOOSA
35°52’30”
36°22’30”96°00’ 95°30’
95°37’30”
WEKIWA
ONETA
COWETA
Coweta
B B’ B’’ B’’’ B’’’’ B’’’’’
C’’’’ C’’’’’
Tulsa
Osage
Current Map
Quadrangles Proposed for Mapping
Major Cities
Expanding Suburbs and Communities
5 Miles
EXPLANATION
North
Mapped Quadrangles
/ColorImageDict > /JPEG2000ColorACSImageDict > /JPEG2000ColorImageDict > /AntiAliasGrayImages false /DownsampleGrayImages true /GrayImageDownsampleType /Bicubic /GrayImageResolution 300 /GrayImageDepth -1 /GrayImageDownsampleThreshold 1.50000 /EncodeGrayImages true /GrayImageFilter /DCTEncode /AutoFilterGrayImages true /GrayImageAutoFilterStrategy /JPEG /GrayACSImageDict > /GrayImageDict > /JPEG2000GrayACSImageDict > /JPEG2000GrayImageDict > /AntiAliasMonoImages false /DownsampleMonoImages true /MonoImageDownsampleType /Bicubic /MonoImageResolution 1200 /MonoImageDepth -1 /MonoImageDownsampleThreshold 1.50000 /EncodeMonoImages true /MonoImageFilter /CCITTFaxEncode /MonoImageDict > /AllowPSXObjects false /PDFX1aCheck false /PDFX3Check false /PDFXCompliantPDFOnly false /PDFXNoTrimBoxError true /PDFXTrimBoxToMediaBoxOffset [ 0.00000 0.00000 0.00000 0.00000 ] /PDFXSetBleedBoxToMediaBox true /PDFXBleedBoxToTrimBoxOffset [ 0.00000 0.00000 0.00000 0.00000 ] /PDFXOutputIntentProfile () /PDFXOutputCondition () /PDFXRegistryName (http://www.color.org) /PDFXTrapped /Unknown
/Description >>> setdistillerparams> setpagedevice
