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OKLAHOMA GEOLOGICAL SURVEY
Charles J. Mankin, Director
OKLAHOMA GEOLOGICAL SURVEY
1908 CENTENNIAL 2008
7 °
APPROXIMATE MEAN DECLINATION
MAGNETIC NORTH
TRUE NORTH
GEOLOGIC MAP OF THE OKLAHOMA PART OF THE BURKBURNETT 30 X 60 QUADRANGLE,
COMANCHE, COTTON, JEFFERSON, STEPHENS, AND TILLMAN COUNTIES, OKLAHOMA
Compiled by Galen W. Miller and Thomas M. Stanley
Cartography by G. Russell Standridge
2006
′ ′
Oklahoma Geologic Quadrangle OGQ-65
Geologic Map of the Burkburnett
30 X 60 Quadrangle ′′
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LEONARDIAN PLEISTOCENE
QUATERNARY
PALEOZOIC CENOZOIC
PERMIAN
UNCONFORMITY
CORRELATION OF UNITS
HOLOCENE
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DESCRIPTION OF UNITS
ARTIFICIAL FILL—Natural or artificial talus, slumps, and tailings covering formally exposed
areas around large spillways.
ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river channels on
modern flood plains.
OLDER ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river channels,
mainly between 0–12 m above modern flood plains.
DUNE SAND—Unconsolidated windblown sand formed into definite dune structures and
ridges.
COVER SHEET SAND—Thin, featureless sheet of windblown silt and sand; thickness varies in
relation to underlying topography.
TERRACE GRAVEL—Unconsolidated gravel, sand, silt, and clay laid down at several levels
along former courses of present-day rivers and streams.
HENNESSEY FORMATION—Mostly a reddish-brown silty mudstone, with siltstone, and thin
sandstone intervals; very thin dolomite and limestone beds locally. Unit correlates with the Clear
Fork Group of north-central Texas. Only lower 15–45 meters are exposed in quad.
WAGGONER RANCH FORMATION—Interbedded reddish-brown laminated silty mudstones
and thin limestone and dolomite beds; locally, thin intervals of siltstone and sandstone occur, but
are rare. Limestone and dolomite beds typically medium to coarsely crystalline texture,
particularly in upper half of formation; where original depositional texture is observed,
carbonates consist of an argillaceous, algal lime mudstone. The Lake Kemp Limestone, a 2-3
meter thick coarsely crystalline limestone, occurs at the top of the formation; base mapped at the
top of the stratigraphically highest occurring sandstone or conglomerate bed of the Petrolia
Formation. Thickness varies between 40–60 meters.
PETROLIA FORMATION—Interbedded reddish-brown, unstratified silty mudstones, and
lenticular, trough cross-bedded, medium- to fine-grained sandstones, soft sediment
deformation common; locally, conglomeratic beds consisting of siltstone and limestone clasts
set within a medium- to coarse-grain matrix occur, particularly in the upper half of the formation.
Mudstones are blocky bedded, with local occurrences of calcareous nodules and paleosol
development. Thickness varies between 110–122 meters.
POST OAK FORMATION—Generally unconsolidated to weakly consolidated unit, consisting of
well-rounded cobbles, sand, silt, and clay. Lithology of cobbles reflects the provence of bedrock
terraine from which the formation was derived, either limestone, granitic, or anorthositic. Post
Oak derived from more mafic provences locally contains zeolite-opal, termed Teepee Creek
facies. Laterally, the Post Oak interfingers with the Hennessey, Waggoner Ranch and Petrolia
Formations. Surficial thickness in quad only about 10 meters; however, in subsurface formation
extends into Pennsylvanian rocks occurring at depths of 700 meters.
Unit contact; dashed where approximate
SYMBOLS
Base Map Credits
Geologic Map Credits
The base map was compiled by the U.S. Geological Survey from 1:24,000 and
1:62,500-scale topographic maps dated 1962-1985. Planimetry revised from aerial
photographs taken 1983 and other source data. Map edited 1985. Universal
Transverse Mercator (UTM) projection. 1927 North American Datum. 25,000-foot grid
ticks based on Oklahoma coordinate system, north zone. 10,000-meter grid, zone 14.
Geology compiled and field checked by Galen W. Miller and Thomas M. Stanley, 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.
Boise City Guymon Beaver B uffalo
Foss
Reser voi r
Elk City
Altus
Watonga
Anadarko
Lawton Pauls Valley
Ardmore
Gainesville
Burkburnett
Wichita Falls
Ponca City P aw huska Bartle sville
Tulsa
Muskogee Stilwell
Eufaula Fort Smith
McA lester Mena
An tlers
Paris
D e Queen
Idabel
Bristow
Shawnee
Ada
Tishomingo
Sherman
Keystone
Lake
Woodward 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
Hentz, T.F.; and Brown, L.F., 1987, Geologic atlas of Texas: Wichita Falls-Lawton
sheet. Bureau of Economic Geology and the University of Texas at Austin, 1:250,000
scale.
Miser, H.D.; and others, 1954, Geologic map of Oklahoma: U.S. Geological Survey and
the Oklahoma Geological Survey, 1:500,000 scale.
1.
2.
Object Description
Description
| Title | OGQ-65_Burkburnett_100K 1 |
| Full text | Phy Qal Pwr Phy Pwr Qtg Phy Qtg Phy Pwr Qtg Qcs Phy Qtg Qal Qal Qds Qal Qds Qtg Qtg Qds Ppt Qal Qds Qtg Ppt Ppt Qal Ppt Ppt Qtg Qtg Pwr Pwr Pwr Qcs Qao Qao Ppt Qao Qcs Qcs Qtg Ppo Ppt Qal Qtg Qtg Qtg Qal Qcs Qcs Qtg Ppt Ppt Qao Qds Qtg Qal Qtg Qao Qds Qal Qao Ppt Qal Qtg Qao Qds Ppt Qcs Qal Ppt Qcs Qcs af Qtg Qtg Qao Qds Qao Ppt Qcs Qds Qds Qal Ppt Qtg Qtg Qao Qcs Ppt Qal Qao Qao Qao Qao Qao Qds Qtg Qao Qtg Qtg Qtg Qal Qds Qal Qao Qao Qal Qal Ppt Qal Qal Qtg Qal Qal Qal Qal Qal Qcs Qal Qal Ppt Ppt Ppt Ppt Pwr Pwr Qal Qal Ppt OKLAHOMA GEOLOGICAL SURVEY Charles J. Mankin, Director OKLAHOMA GEOLOGICAL SURVEY 1908 CENTENNIAL 2008 7 ° APPROXIMATE MEAN DECLINATION MAGNETIC NORTH TRUE NORTH GEOLOGIC MAP OF THE OKLAHOMA PART OF THE BURKBURNETT 30 X 60 QUADRANGLE, COMANCHE, COTTON, JEFFERSON, STEPHENS, AND TILLMAN COUNTIES, OKLAHOMA Compiled by Galen W. Miller and Thomas M. Stanley Cartography by G. Russell Standridge 2006 ′ ′ Oklahoma Geologic Quadrangle OGQ-65 Geologic Map of the Burkburnett 30 X 60 Quadrangle ′′ Qal af Qao Phy Qds Qcs Qtg LEONARDIAN PLEISTOCENE QUATERNARY PALEOZOIC CENOZOIC PERMIAN UNCONFORMITY CORRELATION OF UNITS HOLOCENE Pwr Ppt Ppo DESCRIPTION OF UNITS ARTIFICIAL FILL—Natural or artificial talus, slumps, and tailings covering formally exposed areas around large spillways. ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river channels on modern flood plains. OLDER ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river channels, mainly between 0–12 m above modern flood plains. DUNE SAND—Unconsolidated windblown sand formed into definite dune structures and ridges. COVER SHEET SAND—Thin, featureless sheet of windblown silt and sand; thickness varies in relation to underlying topography. TERRACE GRAVEL—Unconsolidated gravel, sand, silt, and clay laid down at several levels along former courses of present-day rivers and streams. HENNESSEY FORMATION—Mostly a reddish-brown silty mudstone, with siltstone, and thin sandstone intervals; very thin dolomite and limestone beds locally. Unit correlates with the Clear Fork Group of north-central Texas. Only lower 15–45 meters are exposed in quad. WAGGONER RANCH FORMATION—Interbedded reddish-brown laminated silty mudstones and thin limestone and dolomite beds; locally, thin intervals of siltstone and sandstone occur, but are rare. Limestone and dolomite beds typically medium to coarsely crystalline texture, particularly in upper half of formation; where original depositional texture is observed, carbonates consist of an argillaceous, algal lime mudstone. The Lake Kemp Limestone, a 2-3 meter thick coarsely crystalline limestone, occurs at the top of the formation; base mapped at the top of the stratigraphically highest occurring sandstone or conglomerate bed of the Petrolia Formation. Thickness varies between 40–60 meters. PETROLIA FORMATION—Interbedded reddish-brown, unstratified silty mudstones, and lenticular, trough cross-bedded, medium- to fine-grained sandstones, soft sediment deformation common; locally, conglomeratic beds consisting of siltstone and limestone clasts set within a medium- to coarse-grain matrix occur, particularly in the upper half of the formation. Mudstones are blocky bedded, with local occurrences of calcareous nodules and paleosol development. Thickness varies between 110–122 meters. POST OAK FORMATION—Generally unconsolidated to weakly consolidated unit, consisting of well-rounded cobbles, sand, silt, and clay. Lithology of cobbles reflects the provence of bedrock terraine from which the formation was derived, either limestone, granitic, or anorthositic. Post Oak derived from more mafic provences locally contains zeolite-opal, termed Teepee Creek facies. Laterally, the Post Oak interfingers with the Hennessey, Waggoner Ranch and Petrolia Formations. Surficial thickness in quad only about 10 meters; however, in subsurface formation extends into Pennsylvanian rocks occurring at depths of 700 meters. Unit contact; dashed where approximate SYMBOLS Base Map Credits Geologic Map Credits The base map was compiled by the U.S. Geological Survey from 1:24,000 and 1:62,500-scale topographic maps dated 1962-1985. Planimetry revised from aerial photographs taken 1983 and other source data. Map edited 1985. Universal Transverse Mercator (UTM) projection. 1927 North American Datum. 25,000-foot grid ticks based on Oklahoma coordinate system, north zone. 10,000-meter grid, zone 14. Geology compiled and field checked by Galen W. Miller and Thomas M. Stanley, 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. Boise City Guymon Beaver B uffalo Foss Reser voi r Elk City Altus Watonga Anadarko Lawton Pauls Valley Ardmore Gainesville Burkburnett Wichita Falls Ponca City P aw huska Bartle sville Tulsa Muskogee Stilwell Eufaula Fort Smith McA lester Mena An tlers Paris D e Queen Idabel Bristow Shawnee Ada Tishomingo Sherman Keystone Lake Woodward 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 Hentz, T.F.; and Brown, L.F., 1987, Geologic atlas of Texas: Wichita Falls-Lawton sheet. Bureau of Economic Geology and the University of Texas at Austin, 1:250,000 scale. Miser, H.D.; and others, 1954, Geologic map of Oklahoma: U.S. Geological Survey and the Oklahoma Geological Survey, 1:500,000 scale. 1. 2. |
| Date created | 2014-01-08 |
| Date modified | 2014-01-08 |