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Carr, J.E.; and Bergman, D.L., 1976, Reconnaissance of the water resources of the
Clinton Quadrangle, west-central Oklahoma: Oklahoma Geological Survey
Hydrological Atlas 5, 1:250,000, 4 sheets.
Davis, L.V., 1955, Geology and ground-water resources of Grady and northern
Stephens Counties, Oklahoma: Oklahoma Geological Survey Bulletin 73, 184 p.
Donovan, R.N.; and Ditzell, C., 1986, Stop 3—Geologic highlights at Zodletone
(”Stinking Mountain”), Donovan, R.N. (ed.), The Slick Hills of Southwestern
Oklahoma—Fragments of an Aulacogen?: Oklahoma Geological Survey Guidebook
24, p. 96-99.
in
Howery, S.D., 1960, Areal geology of northeastern Caddo County, Oklahoma:
University of Oklahoma unpublished M.S. thesis, 78 p.
Fay, R.O.; and Hart, D.L., 1978, Geology and mineral resources (exclusive of
petroleum) of Custer County, Oklahoma: Oklahoma Geological Survey Bulletin 114, 88
p.
Miser, H.D.; and others, 1954, Geologic map of Oklahoma: U.S. Geological Survey and
the Oklahoma Geological Survey, 1:500,000, 1 sheet.
O’Brien, B.E., 1963, Geology of east-central Caddo County, Oklahoma: University of
Oklahoma unpublished M.S. thesis, 72 p.
Tanaka, H.H.; and Davis, L.V., 1963, Ground-water resources of the Rush Springs
Sandstone in the Caddo County area, Oklahoma: Oklahoma Geological Survey
Circular, 61, 63 p.
Trapnell, D.E., 1961, Areal geology of southwestern Canadian County, Oklahoma:
University of Oklahoma unpublished M.S. thesis, 63 p.
8
APPROXIMATE MEAN DECLINATION
MAGNETIC NORTH
TRUE NORTH
GEOLOGIC MAP OF THE ANADARKO 30 60 QUADRANGLE,
CADDO, CANADIAN, CUSTER, GRADY, KIOWA
AND WASHITA COUNTIES, OKLAHOMA
X
Compiled by Galen W. Miller and Thomas M. Stanley
Cartography by G. Russell Standridge
2004
Qal
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UNCONFORMITY
UNCONFORMITY
DESCRIPTION OF UNITS
ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river
channels on modern flood plains
DUNE SAND—Unconsolidated windblown sand formed into definite dune
structures and ridges
COVER SHEET SAND—Featureless sheet of windblown silt and sand
CLOUD CHIEF FORMATION—Reddish-brown to orange-brown shale, locally
interbedded with thin, reddish-brown, fine-grained sandstone and siltstone in
middle of formation, and some dolomite in lower parts. Base of the formation is
the base of the Moccasin Creek Gypsum Bed. Thickness from 60–120 meters
DOXEY SHALE—Reddish-brown, moderately indurated siltstone and silty
shale. Only basal 10-20 m exposed in map area
WHITEHORSE GROUP, Undifferentiated—Reddish-brown and orange-brown,
fine-grained sandstone and minor siltstone of the Marlow Formation (below) and
the Rush Springs Formation (above). Units undifferentiated in southwestern
part of map area due to absence of the Emanuel gypsum bed at the top of the
Marlow Formation
DUNCAN SANDSTONE—Light-gray to reddish-brown, fine-grained, cross-bedded
sandstone, with interbeds of yellowish gray and reddish-brown shale,
and local occurrences of mudstone conglomerate. Total thickness is 15 60
meters
–
HENNESSEY FORMATION—Reddish-brown shale, with some reddish-brown
and greenish-gray siltstone beds. Only upper 15–45 m is exposed
OLDER ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and
river channels, mainly between 0–12 m above modern flood plains
TERRACE GRAVEL—Unconsolidated gravel, sand, silt, and clay laid down at
several levels along former courses of present-day rivers and streams
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MARLOW FORMATION—Orangish-brown, fine-grained, massive sandstone
with local interbeds of siltstone. Top mapped at the top of the Emanuel Gypsum
Bed. Thickness varies from 30 to 40 meters
EL RENO GROUP, Undifferentiated—Reddish-brown silty shale, with local
interbeds of thin gypsum and dolomite beds. Consists of the Dog Creek and
Flowerpot Shales in areas where the Blaine Formation has pinched out due to
off-lap
ARBUCKLE AND TIMBERED HILLS GROUPS, Undifferentiated—Outliers of
Timbered Hills Group, consisting in descending order the Honey Creek
Limestone and upper Reagan Sandstone; overlain by the lower section of the
Arbuckle Group, consisting of in descending order the lower part of the Signal
Mountain Formation, and the Fort Sill Limestone. Total thickness about 200-225
meters
CARLTON RHYOLITE GROUP—Rhyolite flows and tuffs. Less than 50 m
exposed
DOG CREEK SHALE—Reddish-brown, silty shale. Contains thin interbeds of
greenish-gray shale and several thin layers of light-gray dolomite. Thickness,
about 60 meters
BLAINE FORMATION—Anywhere from a maximum of 9, to a minimum of 2,
thick beds of white, massive gypsum, each typically underlain by a thin bed of
dolomite and thin to thick beds of reddish-brown shale. Unit pinches out to the
east of map area. Thickness varies from 0–55 meters
FLOWERPOT SHALE—Reddish-brown, silty shale, with locally occurring thin
interbeds of greenish-gray shale and several thin layers of gypsum and dolomite
in the upper part. Unit varies between 30–50 m thick
RUSH SPRINGS FORMATION—Reddish-brown locally orange-brown, cross-bedded,
fine- to very fine-grained sandstone with local occurrences of dolomite
and gypsum. Weatherford Gypsum Bed (Prw) occurring from 9 to 18 m below
top of unit. Thickness varies between 60 m in west to 90 m in central and east
parts of quad
UNCONFORMITY
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_
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Middle Upper Leonardian Guadalupian Ochoan Pleistocene
QUATERNARY
PALEOZOIC CENOZOIC
CAMBRIAN PERMIAN
UNCONFORMITY
UNCONFORMITY
UNCONFORMITY
CORRELATION OF UNITS
Holocene
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OKLAHOMA GEOLOGICAL SURVEY
Charles J. Mankin, Director
OKLAHOMA GEOLOGICAL SURVEY
1908 CENTENNIAL 2008
Base Map Credits
Geologic Map Credits
The base map was compiled by the U.S. Geological Survey from 1:24,000-scale
topographic maps dated 1967-1985. Planimetry revised from aerial photographs taken
1981. Map edited 1986. Universal Transverse Mercator (UTM) projection. 1927 North
American Datum. 25,000-foot grid ticks based on Oklahoma coordinate system, north
zone. 10,000-meter UTM grid, zone 14.
Geology compiled and field checked by Galen W. Miller and Thomas M. Stanley, 2003 -
2004. Research supported by the U.S. Geological Survey, National Cooperative
Geologic Mapping Program, under Assistance Award Number 03HQAG0014. 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. Originally published as Open-File Report OF4-2005.
Map revised and published as OGQ-58. Cartography and layout prepared by G.
Russell Standridge, 2004.
Boise City Guymo n Beaver Buffalo
Fo ss
Reservoir
Elk City
Altus
Watonga
Anadarko
Lawton Pauls Valley
Ardmore
Gainesville
Burkburnett
Wichita Falls
Ponca City Pawhuska Bartlesville
Tul sa
Mu skogee S tilwell
Eufa ula Fort Smith
McAlester Mena
Antlers
Paris
De Queen
Ida be l
Bristow
Shawnee
A da
Tishomingo
Sherm an
Keystone
Lake
Woodwar d Fairview Enid
Oklahoma
City North
Oklahoma
City South
Alva
103° 102° 101° 100° 99° 98° 97° 96° 95° 37°
36°
35°
34°
Neosho
Fayetteville
Map of Oklahoma showing the locations of the 30 X 60
quadrangles. Red shaded quadrangle represents the current
map
Vernon
Unit contact; approximately located
Axial trace of synclinal structure, dashed where approximate
Fault, dotted where covered; ball and spike on downthrown
side. All faults are normal faults, dipping 60–65°
SYMBOLS
Oklahoma Geologic Quadrangle OGQ-58
Geologic Map of the Anadarko
30 X 60 Quadrangle
(previously Open-File Report OF4-2005)
Object Description
Description
| Title | OGQ-58_Anadarko_100K 1 |
| Full text | Pdx Qal Qao Qao Qao Pcc Prs Pcc Qao Qao Pcc Qal Pcc Qao Qao Qal Pcc Pcc Pwh Prs Pwh Pmw Pdc Pdc Pbl Pbl Pfp Pfp Pbl Pfp Pdn Qcs Qcs Pbl Qcs Pfp Qcs Qcs Pdn Qal Phy Qcs Qcs Qcs Qcs Phy Phy Phy Qcs Qcs Pdn Pdn Pdn Pdn Ccr Cat Phy Qao Pfp Qcs Pbl Qao Qcs Qao Qao Prs Pmw Pbl Pdc Qcs Qcs Qcs Qcs Pfp Qao Pdc Pmw Pdc Pfp Pbl Prs Pdn Phy Pmw Qal Prs Pcc Qao Prs Pmw Qao Qtg Pmw Prs Qtg Qal Pmw Qtg Qtg Pel Pel Pel Qal Qao Pel Pel Qao Qal Pel Pel Pmw Pel Pel Pel Pmw Pel Prs Prs Prs Pmw Prs Pmw Qtg Pmw Pmw Prs Prs Qtg Qtg Qtg Pmw Pel Pmw Pel Qcs Pmw Prs Pmw Qal Qtg Pmw Qtg Qtg Pcc Prs Qds Qtg Pmw Pmw Pel Qal Qao Qds Qds Qao Pmw Pel Qds Qal Pel Prs Pmw Pel Pmw Prs Prs Qal Pel Pel Qds Qds Qcs Qtg Qds Qds Qds Qtg Prs Pcc Pcc Pcc Qds Qds Qtg Qds Pcc Pcc Prs Qtg Qtg Prs Pdx Prw Pmw Qal Pbl Prw Prw Prw Prw Prw Prw Qal Qal Qal Qal Qal Prw Prw Qal Prw Prw Prw Prw Prw Prw Prw Prw Prw Pcc Prw Prw Prw Prw Prw Prw Qds Prw Qal Prw Prw Qal Qal Qal Prw Prw Prw Prw Pel Qal Qal Pmw Qtg Prw Prw Prs Prw Prw Carr, J.E.; and Bergman, D.L., 1976, Reconnaissance of the water resources of the Clinton Quadrangle, west-central Oklahoma: Oklahoma Geological Survey Hydrological Atlas 5, 1:250,000, 4 sheets. Davis, L.V., 1955, Geology and ground-water resources of Grady and northern Stephens Counties, Oklahoma: Oklahoma Geological Survey Bulletin 73, 184 p. Donovan, R.N.; and Ditzell, C., 1986, Stop 3—Geologic highlights at Zodletone (”Stinking Mountain”), Donovan, R.N. (ed.), The Slick Hills of Southwestern Oklahoma—Fragments of an Aulacogen?: Oklahoma Geological Survey Guidebook 24, p. 96-99. in Howery, S.D., 1960, Areal geology of northeastern Caddo County, Oklahoma: University of Oklahoma unpublished M.S. thesis, 78 p. Fay, R.O.; and Hart, D.L., 1978, Geology and mineral resources (exclusive of petroleum) of Custer County, Oklahoma: Oklahoma Geological Survey Bulletin 114, 88 p. Miser, H.D.; and others, 1954, Geologic map of Oklahoma: U.S. Geological Survey and the Oklahoma Geological Survey, 1:500,000, 1 sheet. O’Brien, B.E., 1963, Geology of east-central Caddo County, Oklahoma: University of Oklahoma unpublished M.S. thesis, 72 p. Tanaka, H.H.; and Davis, L.V., 1963, Ground-water resources of the Rush Springs Sandstone in the Caddo County area, Oklahoma: Oklahoma Geological Survey Circular, 61, 63 p. Trapnell, D.E., 1961, Areal geology of southwestern Canadian County, Oklahoma: University of Oklahoma unpublished M.S. thesis, 63 p. 8 APPROXIMATE MEAN DECLINATION MAGNETIC NORTH TRUE NORTH GEOLOGIC MAP OF THE ANADARKO 30 60 QUADRANGLE, CADDO, CANADIAN, CUSTER, GRADY, KIOWA AND WASHITA COUNTIES, OKLAHOMA X Compiled by Galen W. Miller and Thomas M. Stanley Cartography by G. Russell Standridge 2004 Qal Qao Qcs Qtg Pcc Pdx Pdn Phy UNCONFORMITY UNCONFORMITY DESCRIPTION OF UNITS ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river channels on modern flood plains DUNE SAND—Unconsolidated windblown sand formed into definite dune structures and ridges COVER SHEET SAND—Featureless sheet of windblown silt and sand CLOUD CHIEF FORMATION—Reddish-brown to orange-brown shale, locally interbedded with thin, reddish-brown, fine-grained sandstone and siltstone in middle of formation, and some dolomite in lower parts. Base of the formation is the base of the Moccasin Creek Gypsum Bed. Thickness from 60–120 meters DOXEY SHALE—Reddish-brown, moderately indurated siltstone and silty shale. Only basal 10-20 m exposed in map area WHITEHORSE GROUP, Undifferentiated—Reddish-brown and orange-brown, fine-grained sandstone and minor siltstone of the Marlow Formation (below) and the Rush Springs Formation (above). Units undifferentiated in southwestern part of map area due to absence of the Emanuel gypsum bed at the top of the Marlow Formation DUNCAN SANDSTONE—Light-gray to reddish-brown, fine-grained, cross-bedded sandstone, with interbeds of yellowish gray and reddish-brown shale, and local occurrences of mudstone conglomerate. Total thickness is 15 60 meters – HENNESSEY FORMATION—Reddish-brown shale, with some reddish-brown and greenish-gray siltstone beds. Only upper 15–45 m is exposed OLDER ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river channels, mainly between 0–12 m above modern flood plains TERRACE GRAVEL—Unconsolidated gravel, sand, silt, and clay laid down at several levels along former courses of present-day rivers and streams Prs Pmw Pdc Pbl Pfp MARLOW FORMATION—Orangish-brown, fine-grained, massive sandstone with local interbeds of siltstone. Top mapped at the top of the Emanuel Gypsum Bed. Thickness varies from 30 to 40 meters EL RENO GROUP, Undifferentiated—Reddish-brown silty shale, with local interbeds of thin gypsum and dolomite beds. Consists of the Dog Creek and Flowerpot Shales in areas where the Blaine Formation has pinched out due to off-lap ARBUCKLE AND TIMBERED HILLS GROUPS, Undifferentiated—Outliers of Timbered Hills Group, consisting in descending order the Honey Creek Limestone and upper Reagan Sandstone; overlain by the lower section of the Arbuckle Group, consisting of in descending order the lower part of the Signal Mountain Formation, and the Fort Sill Limestone. Total thickness about 200-225 meters CARLTON RHYOLITE GROUP—Rhyolite flows and tuffs. Less than 50 m exposed DOG CREEK SHALE—Reddish-brown, silty shale. Contains thin interbeds of greenish-gray shale and several thin layers of light-gray dolomite. Thickness, about 60 meters BLAINE FORMATION—Anywhere from a maximum of 9, to a minimum of 2, thick beds of white, massive gypsum, each typically underlain by a thin bed of dolomite and thin to thick beds of reddish-brown shale. Unit pinches out to the east of map area. Thickness varies from 0–55 meters FLOWERPOT SHALE—Reddish-brown, silty shale, with locally occurring thin interbeds of greenish-gray shale and several thin layers of gypsum and dolomite in the upper part. Unit varies between 30–50 m thick RUSH SPRINGS FORMATION—Reddish-brown locally orange-brown, cross-bedded, fine- to very fine-grained sandstone with local occurrences of dolomite and gypsum. Weatherford Gypsum Bed (Prw) occurring from 9 to 18 m below top of unit. Thickness varies between 60 m in west to 90 m in central and east parts of quad UNCONFORMITY Cat Ccr _ _ Pel Pwh Qds Cat Qal Qao Pdx Pcc Pwh Prs Pmw Pdc Pbl Prw Pfp Pdn Phy Qcs Qtg Middle Upper Leonardian Guadalupian Ochoan Pleistocene QUATERNARY PALEOZOIC CENOZOIC CAMBRIAN PERMIAN UNCONFORMITY UNCONFORMITY UNCONFORMITY CORRELATION OF UNITS Holocene Cat Ccr _ _ Pel Qds Cat OKLAHOMA GEOLOGICAL SURVEY Charles J. Mankin, Director OKLAHOMA GEOLOGICAL SURVEY 1908 CENTENNIAL 2008 Base Map Credits Geologic Map Credits The base map was compiled by the U.S. Geological Survey from 1:24,000-scale topographic maps dated 1967-1985. Planimetry revised from aerial photographs taken 1981. Map edited 1986. Universal Transverse Mercator (UTM) projection. 1927 North American Datum. 25,000-foot grid ticks based on Oklahoma coordinate system, north zone. 10,000-meter UTM grid, zone 14. Geology compiled and field checked by Galen W. Miller and Thomas M. Stanley, 2003 - 2004. Research supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program, under Assistance Award Number 03HQAG0014. 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. Originally published as Open-File Report OF4-2005. Map revised and published as OGQ-58. Cartography and layout prepared by G. Russell Standridge, 2004. Boise City Guymo n Beaver Buffalo Fo ss Reservoir Elk City Altus Watonga Anadarko Lawton Pauls Valley Ardmore Gainesville Burkburnett Wichita Falls Ponca City Pawhuska Bartlesville Tul sa Mu skogee S tilwell Eufa ula Fort Smith McAlester Mena Antlers Paris De Queen Ida be l Bristow Shawnee A da Tishomingo Sherm an Keystone Lake Woodwar d Fairview Enid Oklahoma City North Oklahoma City South Alva 103° 102° 101° 100° 99° 98° 97° 96° 95° 37° 36° 35° 34° Neosho Fayetteville Map of Oklahoma showing the locations of the 30 X 60 quadrangles. Red shaded quadrangle represents the current map Vernon Unit contact; approximately located Axial trace of synclinal structure, dashed where approximate Fault, dotted where covered; ball and spike on downthrown side. All faults are normal faults, dipping 60–65° SYMBOLS Oklahoma Geologic Quadrangle OGQ-58 Geologic Map of the Anadarko 30 X 60 Quadrangle (previously Open-File Report OF4-2005) |
| Date created | 2014-01-07 |
| Date modified | 2014-01-07 |