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Barclay, J.E.; and Burton, L.C., 1953, Ground-water resources of the terrace deposits
and alluvium of western Tillman County, Oklahoma: Oklahoma Planning and
Resources Board, Division of Water Resources Bulletin, 12, 71p.
Havens, J.S., 1977, Reconnaissance of the water resources of the Lawton Quadrangle,
southwestern Oklahoma: Oklahoma Geological Survey Hydrologic Atlas, HA-6,
1:250,000, 4 sheets.
Johnson, K.S.; and Ham, W.E., 1966, Geology and mineral resources of the Permian
Blaine Formation and associated strata in southwestern Oklahoma: Oklahoma
Geological Survey unpublished maps.
Miser, H.D.; and others, 1954, Geologic map of Oklahoma: U.S. Geological Survey and
the Oklahoma Geological Survey, 1:500,000, 1 sheet.
8°
APPROXIMATE MEAN DECLINATION
MAGNETIC NORTH
TRUE NORTH
GEOLOGIC MAP OF THE OKLAHOMA PART OF THE VERNON 30 60 QUADRANGLE,
JACKSON AND TILLMAN COUNTIES, OKLAHOMA
X
Compiled by Thomas M. Stanley
Cartography by G. Russell Standridge
2004
′ ′
OKLAHOMA GEOLOGICAL SURVEY
Charles J. Mankin, Director
OKLAHOMA GEOLOGICAL SURVEY
1908 CENTENNIAL 2008
Oklahoma Geologic Quadrangle OGQ-60
Geologic Map of the Vernon
30 X 60 Quadrangle ′′
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Leonardian Guadalupian Pleistocene
QUATERNARY
PALEOZOIC CENOZOIC
PERMIAN
UNCONFORMITY
CORRELATION OF UNITS
Holocene
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UNCONFORMITY
DESCRIPTION OF UNITS
ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river
channels on modern flood plains
ARTIFICIAL FILL—Natural or artificial talus, slumps, and tailings covering
formally exposed areas around active and inactive mining operations
DUNE SAND—Unconsolidated windblown sand formed into definite dune
structures and ridges
COVER SHEET SAND—Featureless sheet of windblown silt and sand
DOG CREEK SHALE—Reddish-brown, silty shale. Contains thin interbeds of
greenish-gray shale. Less than 5 meters exposed.
BLAINE FORMATION—Nine thick beds of white, massive gypsum, each
typically underlain by a thin bed of dolomite and thin to thick beds of reddish-brown
shale. Typically 45 55 meters thick. Formation divided into the lower
Elm Fork Member (Pbe) and the upper Van Vacter Member (Pbv)
VAN VACTER MEMBER
–
–
–
–
– –
—Six beds of gypsum, each typically 1 5 m thick (each
is thinner or absent to east). Dolomite and shale beds are 3 cm to 1.2 m thick.
Total thickness is 20 25 meters. Base mapped at the base of the Mangum
Dolomite Bed
ELM FORK MEMBER—Three beds of gypsum, each typically 1.5 10 m thick
(each is thinner to east). Dolomite beds typically 3 cm to 1 m thick; shale
intervals typically 3 10 m thick. Total thickness is 25 30 meters. Base mapped
at the base of the Haystack Gypsum Bed
FLOWERPOT SHALE—Reddish-brown, silty shale. Contains thin interbeds of
greenish-gray shale and several thin layers of gypsum and dolomite in the upper
part; thickness, about 30-40 meters
SAN ANGELO SANDSTONE—Light-gray to reddish-brown, fine-grained,
cross-bedded sandstone, with local interbeds of yellowish-gray and reddish-brown
shale; thickness, about 20–30 meters
HENNESSEY FORMATION—Reddish-brown shale, with some reddish-brown
siltstone beds. Top 15–45 meters are 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
Pbv
Pbe
EL RENO GROUP
Unit contact; approximately located
SYMBOLS
Axial trace of synclinal structure, dashed where approximate
Boise City Guymon Beaver Buffalo
Foss
Reservoir
Elk City
Altus
Watonga
Anadarko
Lawton Pauls Valley
Ardmore
Gainesville
Burkburnett
Wichita Falls
Ponca City Pawhuska Bartlesville
Tul sa
Muskogee Stilwell
Eufaula Fort Smith
McAlester Mena
Antlers
Paris
De Queen
Idabe l
Bristow
Sh awne e
Ada
Tis homingo
Sher man
Keyston e
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
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 1983-1985. Planimetry revised from aerial photographs taken
1984. 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 Thomas M. Stanley, 2003. 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.
2004.
Originally published as Open-File Report OF6-2005. Map revised and published as
OGQ-60. Cartography and layout prepared by G. Russell Standridge,
Object Description
Description
| Title | OGQ-60_Vernon_100K 1 |
| Full text | Pbv Qal Pbv Qtg Qds Qds Qao Pbv Pbe Qao Qds Qal Pdc Qtg Qtg Qtg Pbv Pbv Qal Qtg Pbv Qds Qtg Pbe Pbv Pbe Pbv Qds af Pfp Qao Qds Pbe Pbv Pfp Pfp Psa Psa Qds Qtg Qal Qds Psa Phy Qtg Phy Qtg Qds Qtg Qds Qal Qds Qds Qtg Qao Qds Qds Qao Qds Qds Qao Qal Qds Qds Qao Qtg Qtg Qal Phy Qds Qcs Qds Qds Qds Qds Qal Qtg Qao Qds Qds Qao Barclay, J.E.; and Burton, L.C., 1953, Ground-water resources of the terrace deposits and alluvium of western Tillman County, Oklahoma: Oklahoma Planning and Resources Board, Division of Water Resources Bulletin, 12, 71p. Havens, J.S., 1977, Reconnaissance of the water resources of the Lawton Quadrangle, southwestern Oklahoma: Oklahoma Geological Survey Hydrologic Atlas, HA-6, 1:250,000, 4 sheets. Johnson, K.S.; and Ham, W.E., 1966, Geology and mineral resources of the Permian Blaine Formation and associated strata in southwestern Oklahoma: Oklahoma Geological Survey unpublished maps. Miser, H.D.; and others, 1954, Geologic map of Oklahoma: U.S. Geological Survey and the Oklahoma Geological Survey, 1:500,000, 1 sheet. 8° APPROXIMATE MEAN DECLINATION MAGNETIC NORTH TRUE NORTH GEOLOGIC MAP OF THE OKLAHOMA PART OF THE VERNON 30 60 QUADRANGLE, JACKSON AND TILLMAN COUNTIES, OKLAHOMA X Compiled by Thomas M. Stanley Cartography by G. Russell Standridge 2004 ′ ′ OKLAHOMA GEOLOGICAL SURVEY Charles J. Mankin, Director OKLAHOMA GEOLOGICAL SURVEY 1908 CENTENNIAL 2008 Oklahoma Geologic Quadrangle OGQ-60 Geologic Map of the Vernon 30 X 60 Quadrangle ′′ Qal af Qao Pdc Pbl Pbv Pbe Pfp Psa Phy Qds Qcs Qtg Leonardian Guadalupian Pleistocene QUATERNARY PALEOZOIC CENOZOIC PERMIAN UNCONFORMITY CORRELATION OF UNITS Holocene Qal af Qao Qds Qcs Qtg Pdc Pfp Psa Phy Pbl UNCONFORMITY DESCRIPTION OF UNITS ALLUVIUM—Unconsolidated sand, silt, clay, and gravel in stream and river channels on modern flood plains ARTIFICIAL FILL—Natural or artificial talus, slumps, and tailings covering formally exposed areas around active and inactive mining operations DUNE SAND—Unconsolidated windblown sand formed into definite dune structures and ridges COVER SHEET SAND—Featureless sheet of windblown silt and sand DOG CREEK SHALE—Reddish-brown, silty shale. Contains thin interbeds of greenish-gray shale. Less than 5 meters exposed. BLAINE FORMATION—Nine thick beds of white, massive gypsum, each typically underlain by a thin bed of dolomite and thin to thick beds of reddish-brown shale. Typically 45 55 meters thick. Formation divided into the lower Elm Fork Member (Pbe) and the upper Van Vacter Member (Pbv) VAN VACTER MEMBER – – – – – – —Six beds of gypsum, each typically 1 5 m thick (each is thinner or absent to east). Dolomite and shale beds are 3 cm to 1.2 m thick. Total thickness is 20 25 meters. Base mapped at the base of the Mangum Dolomite Bed ELM FORK MEMBER—Three beds of gypsum, each typically 1.5 10 m thick (each is thinner to east). Dolomite beds typically 3 cm to 1 m thick; shale intervals typically 3 10 m thick. Total thickness is 25 30 meters. Base mapped at the base of the Haystack Gypsum Bed FLOWERPOT SHALE—Reddish-brown, silty shale. Contains thin interbeds of greenish-gray shale and several thin layers of gypsum and dolomite in the upper part; thickness, about 30-40 meters SAN ANGELO SANDSTONE—Light-gray to reddish-brown, fine-grained, cross-bedded sandstone, with local interbeds of yellowish-gray and reddish-brown shale; thickness, about 20–30 meters HENNESSEY FORMATION—Reddish-brown shale, with some reddish-brown siltstone beds. Top 15–45 meters are 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 Pbv Pbe EL RENO GROUP Unit contact; approximately located SYMBOLS Axial trace of synclinal structure, dashed where approximate Boise City Guymon Beaver Buffalo Foss Reservoir Elk City Altus Watonga Anadarko Lawton Pauls Valley Ardmore Gainesville Burkburnett Wichita Falls Ponca City Pawhuska Bartlesville Tul sa Muskogee Stilwell Eufaula Fort Smith McAlester Mena Antlers Paris De Queen Idabe l Bristow Sh awne e Ada Tis homingo Sher man Keyston e 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 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 1983-1985. Planimetry revised from aerial photographs taken 1984. 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 Thomas M. Stanley, 2003. 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. 2004. Originally published as Open-File Report OF6-2005. Map revised and published as OGQ-60. Cartography and layout prepared by G. Russell Standridge, |
| Date created | 2014-01-08 |
| Date modified | 2014-01-08 |