FGDC-Compliant Metadata for GEOLOGY
Identification_Information:
Citation:
Originator: Cederstrand, Joel R.
Publication_Date: 1996
Publication_Time:
Title: Digitized geology of Ardmore and Sherman quadrangles, south-central Oklahoma
Edition: 1.0
Geospatial_Data_Presentation_Form: map
Series_Information:
Series_Name: Open-File Report
Issue_Identification: 96370
Publication_Information:
Publication_Place: Oklahoma City, OK
Publisher: U.S. Geological Survey
Other_Citation_Details:
Online_Linkage:
Description: Surficial geology, Ardmore and Sherman quadrangles, south-central Oklahoma
Abstract:
This data set consists of digital data and accompanying
documentation of the surficial geology of the 1:250,000-scale Ardmore
and Sherman quadrangles, Oklahoma. The original data are from the
Geologic Map, sheet 1 of 4, included in the Oklahoma Geological Survey
publication, Reconnaissance of the water resources of the Ardmore and
Sherman quadrangles, southern Oklahoma, Hydrologic Atlas 3, Hart,
1974. The geology was compiled by D.L. Hart and R.O. Fay, 1970.
Purpose:
This report provides general use information on the surficial
geologic units in the Ardmore and Sherman quadrangles, Oklahoma. It
may be inappropriate to use this data set at scales larger than
1:250,000.
This data set is intended to show the geologic contacts for the
Ardmore and Sherman quadrangles, Oklahoma. It can be used to make
geologic maps, and determine approximate areas and locations of
various geologic units. This data set can be used for studies of
water, environment, soils, sand and gravel, clay pits, gypsum salt
pollution, volcanic ash, caliche, oil and gas, flooding, archaeology,
historical geology, history, ecology, botany, paleontology, zoology,
caves, quarries, dams, farming, and other related topics. The paper
version of this data set has been used to study these topics.
Supplemental_Information:
Procedures_Used:
The black and cyan separates and mylar composite of the source map
(Hart, 1974) were obtained from the Oklahoma Geological Survey. Clear
mylar positives were made from the black and cyan separates. The
separates were scanned with a SCITEX scanner. The resulting SCITEX
files were processed with the SCITEXLINE command (ESRI, 1995) to make
ARC/INFO coverages. Ten stream and geologic contact intersections
that were on both the mylar composite and in the coverages were used
as locations for registration tics. The registration tics were used
to register the coverages to the mylar composite and to add
latitudinal/longitudinal tics from the mylar composite to the
coverages.
A Transverse Mercator projection with a central meridian of 98
degrees west is the projection of the source map. However, the tics
of the coverages were projected into Universal Transverse Mercator
projection Zone 14 because both of these projections are in the same
family of projections, and because there was a good match between the
mylar composite and the coverages.
The quadrangle boundaries were generated from the appropriate
latitudes and longitudes, and the state-line boundaries were included
from a 1:100,000 county- and state-boundary coverage (Nebert and
Negri, 1990), replacing the boundaries from the scanned coverages.
Arcs that did not form polygon boundaries, such as faults, were
removed, and each polygon was labeled. Text and single-line rivers
were removed from the hydrography coverage made from the scanned file
of the cyan separate. Lakes were added from the hydrography coverage
to the geology coverage. Polygons were checked to ensure they were
all closed, and attributes were added. The ARC/INFO command DROPLINE
(ESRI, 1995) was used to identify topology errors. A frequency check
was done on the attribute codes to ensure there were no typographical
errors.
Since alluvium and terrace formations were excluded on the original
map (Hart, 1974), they were excluded in this data set as well.
The coverage was projected into Albers Equal Area projection
(Snyder, 1987). This projection is appropriate for maps of the
conterminous United States because of the visual presentation and
equal-area characteristic, which facilitates areal analysis. This
projection frequently is used for nationwide digital map data sets.
The projection is cast on the North American Datum of 1983. Table 1
provides map projection information.
This projection slightly distorts shapes and distances (scale) in
order to maintain equal-area properties. Scale is true along the
standard parallels, which are to the north and south of Oklahoma.
Scale distortion in Oklahoma reaches a maximum of slightly less than
one percent at the northern border of the state (Snyder, 1987.)
------------------------------------------------------------------------------
Table 1. Albers Equal Area projection parameters
[GRS80, Geodetic Reference System 1980; NAD83, North American Datum 1983]
______________________________________________________________________________
Projection parameters:
Spheroid GRS80
Datum NAD83
First standard parallel 29 30 00 North
Second standard parallel 45 30 00 North
Central meridian 96 00 00 West
Latitude of projection origin 23 00 00 North
Coordinate system parameters:
False easting 0
False northing 0
Planimetric units of measure meters
______________________________________________________________________________
Revisions:
Revision Number 1.0, Joel R. Cederstrand, author.
Reviews_Applied_to_Data:
This electronic report was subjected to the same review standard
that applies to all U.S. Geological Survey reports. Reviewers were
asked to check the topological consistency, tolerances, attribute
frequencies and statistics, projection, and geographic extent.
Reviewers were given digital data sets and paper plots for checking
against the source maps to verify the linework and attributes. The
reviewers checked the metadata and a_readme.1st files for completeness
and accuracy.
Related_Spatial_and_Tabular_Data_Sets:
The ASCII approximations for the polygon attribute "FM" are stored
in "\geology.lut", which is presented in Table 2. The file
"\geology.lut" is comma delimited and there are single quotes around
text strings. There are two field types in this table: C = character
and I = integer. "FMNUM" and "FM" are attributes in both the polygon
attribute table of the coverage and "\geology.lut". "FMNUM" is stored
as the first major polygon code in the nonproprietary Digital Line
Graph (DLG) version of this data set. Each "FM" in the state
corresponds to a unique integer "FMNUM", but "\geology.lut" is only
for this data set.
---------------------------------------------------------------------
TABLE 2: "\geology.lut"
MAXIMUM
FIELD FIELD FIELD FIELD
NAME DESCRIPTION WIDTH TYPE
---------------------------------------------------------------------
FMNUM Number representing formation name 3 I
FM Formation name 6 C
---------------------------------------------------------------------
Additional surficial geology data sets are available for the rest
of Oklahoma. The source maps for the three counties of the Oklahoma
panhandle are at a scale of 1:125,000. The source maps for the data
sets for the rest of the state are at a scale of 1:250,000.
The data set "\faults.gz" contains the geologic faults for the
Ardmore and Sherman quadrangles, Oklahoma.
Other_References_Cited:
Environmental Systems Research Institute, Inc. (ESRI), 1995,
ARC/INFO Command References, ARC/INFO Version 7.0.3 ArcDoc: Redlands,
CA. [online documentation].
Hart, D.L., 1974, Reconnaissance of the water resources of the
Ardmore and Sherman quadrangles, southern Oklahoma: Oklahoma
Geological Survey Hydrologic Atlas 3, scale 1:250,000, 4 sheets.
(Geology on sheet 1 compiled by D.L. Hart and R.O. Fay, 1970.)
Nebert, D. and Negri, M., 1990, U.S. Department of Commerce,
Bureau of Census, TIGER/Line Precensus Files: U.S. Geological Survey,
Reston VA.
Snyder, J.P., 1987, Map projections--A working manual: U.S.
Geological Survey Professional Paper 1395, 383 p.
Notes:
Any use of trade, product, or firm names is for descriptive
purposes only and does not imply endorsement by the U.S. Government.
Time_Period_of_content:
Time_Period_Information:
Single Date/Time:
Calendar_Date: 1974
Currentness_Reference:
The paper map was published in 1974.
Status:
Progress: In review
Maintenance_and_Update_Frequency:
None planned
Spatial_Domain:
Bounding_Coordinates:
West_Bounding_Coordinate: -97.466753
East_Bounding_Coordinate: -96.252630
North_Bounding_Coordinate: 34.794715
South_Bounding_Coordinate: 34.149058
Keywords:
Theme:
Theme_Keyword_Thesaurus: none
Theme_Keyword:
Ardmore and Sherman quadrangles
Oklahoma
Geologic formations
Geologic units
Geology
Place:
Place_Keyword_Thesaurus: none
Place_Keyword: 1:250,000-scale Ardmore and Sherman quadrangles, south-central Oklahoma
Access_Constraints:
None
Use_Constraints:
There is uncertainty in the position of geologic contacts from the
field mapping process, the original map preparation, and the
digitizing process. The boundaries of water bodies, in particular,
were scan digitized from a different separate, and some misalignment
between those lines and the geologic contacts was indicated. This
misalignment may be as much as about 0.05 map inches. It may be
inappropriate to use this data set at scales larger than 1:250,000.
Point_of_Contact:
Contact_Information:
Contact_Person_Primary:
Contact Person: Joel R. Cederstrand
Contact_Organization: U.S. Geological Survey
Contact_Position: Geographer
Contact_Address:
Address_Type: mailing address
Address: 202 NW 66th St., Bldg. 7
City: Oklahoma City
State_or_Province: Oklahoma
Postal_Code: 73116
Country: United States of America
Contact_Voice_Telephone: (405)843-7570
Contact_Facsimile_Telephone: (405)843-7712
Contact_Electronic_Mail_Address: jrceders@usgs.gov
Contact_Instructions: none
Data_Set_Credit:
Compilation of this data set and the associated metadata was funded
under a cooperative agreement between the U.S. Geological Survey and
the State of Oklahoma, Office of the Secretary of Environment.
Security Information:
Security_Classification_System: Public
Security_Classification: UNCLASSIFIED
Security_Handling_Description: None
Native_Data_Set_Environment: Operating System: UNIX, ARC/INFO Version 7.0.3,,(Mon Mar 13 22:21:55 PST 1995)
Cross_Reference:
Originator: Nebert, D. and Negri, M.
Publication_Date: 1990
Publication_Time:
Title: TIGER/Line Precensus Files
Edition:
Geospatial_Data_Presentation_Form: map
Series_Information:
Series_Name:
Issue_Identification:
Publication_Information:
Publication_Place: Reston, VA
Publisher: U.S. Geological Survey
Other_Citation_Details:
Online_Linkage: /gis/state/us/st100k
Data_Quality_Information:
Logical_Consistency_Report: Polygon and chain-node topology present.
Completeness_Report:
Data set covers the Ardmore and Sherman quadrangles, Oklahoma.
Positional_Accuracy:
Horizontal_Positional_Accuracy:
Horizontal_Positional_Accuracy_Report:
Not available
Quantitative_Horizontal_Positional_Accuracy_Assessment:
Horizontal_Positional_Accuracy_Value: unknown
Horizontal_Positional_Accuracy_Explanation: Resolution as reported
Vertical_Positional_Accuracy:
Vertical_Positional_Accuracy_Report:
Not available
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Process_Time: 1234
Process_Description: JRCEDERS IDEDIT GEOLOGY POLY
Process_Date: 19970212
Process_Time: 1234
Process_Description: JRCEDERS IDEDIT GEOLOGY LINE
Process_Date: 19970212
Process_Time: 1234
Process_Description: JRCEDERS BUILD GEOLOGY POLY
Process_Date: 19970212
Process_Time: 1237
Process_Description: JRCEDERS BUILD GEOLOGY LINE
Process_Date: 19970212
Process_Time: 1237
Process_Description: JRCEDERS RENODE GEOLOGY
Process_Date: 19970212
Process_Time: 1237
Process_Description: JRCEDERS EXPORT COVER GEOLOGY ../GEO_ARC_DISK/GEOLOGY.E00 NONE
Process_Date: 19970212
Process_Time: 1239
Process_Description: JRCEDERS ARCDLG GEOLOGY ../GEO_PD_DISK/GEOLOGY # GEOLOGY/PRJ.ADF # #
Process_Date: 19970212
Process_Time: 1240
Process_Description: JRCEDERS BUILD GEOLOGY POLY
Process_Date: 19970310
Process_Time: 1144
Process_Description: JRCEDERS BUILD GEOLOGY LINE
Process_Date: 19970310
Process_Time: 1144
Process_Description: JRCEDERS IDEDIT GEOLOGY POLY
Process_Date: 19970310
Process_Time: 1144
Process_Description: JRCEDERS IDEDIT GEOLOGY LINE
Process_Date: 19970310
Process_Time: 1144
Process_Description: JRCEDERS BUILD GEOLOGY POLY
Process_Date: 19970310
Process_Time: 1147
Process_Description: JRCEDERS BUILD GEOLOGY LINE
Process_Date: 19970310
Process_Time: 1147
Process_Description: JRCEDERS RENODE GEOLOGY
Process_Date: 19970310
Process_Time: 1147
Process_Description: JRCEDERS EXPORT COVER GEOLOGY ../GEO_ARC_DISK/GEOLOGY.E00 NONE
Process_Date: 19970310
Process_Time: 1149
Process_Description: JRCEDERS ARCDLG GEOLOGY ../GEO_PD_DISK/GEOLOGY # GEOLOGY/PRJ.ADF # #
Process_Date: 19970310
Process_Time: 1150
Cloud_Cover:
Not applicable
Spatial_Data_Organization_Information:
Direct_Spatial_Reference_Method: Vector
Point_and_Vector_Object_Information:
SDTS_Terms_Description:
SDTS_Point_and_Vector_Object_Type: Point
Point_and_Vector_Object_Count: 1184
SDTS_Point_and_Vector_Object_Type: String
Point_and_Vector_Object_Count: 2732
SDTS_Point_and_Vector_Object_Type: GT-polygon composed of chains
Point_and_Vector_Object_Count: 1185
Spatial_Reference_Information:
Horizontal_Coordinate_System_Definition:
Horizontal_Coordinate_System_Definition:
Planar
Map_Projection:
Map_Projection_Name: 'Albers Conical Equal Area'
Albers_Conical_Equal_Area:
Standard_Parallel: 29.5
Standard_Parallel: 45.5
Longitude_of_Central_Meridian: -96
Latitude_of_Projection_Origin: 23
False_Easting: 0
False_Northing: 0
Planar_Coordinate_Information:
Planar_Coordinate_Encoding_Method: coordinate pair
Coordinate_Representation:
Abscissa_Resolution: unknown
Ordinate_Resolution: unknown
Planar_Distance_Units: METERS
Geodetic_Model:
Horizontal_Datum_Name: NAD83
Ellipsoid_Name: GRS1980
Semi-major_Axis: UNKNOWN
Denominator_of_Flattening_Ratio: UNKNOWN
Entity_and_Attribute_Information:
Detailed_Description:
Entity_Type:
Entity_Type_Label: GEOLOGY.PAT
Entity_Type_Definition: Surficial geologic units
Entity_Type_Definition_Source: Hart, 1974
Attribute:
Attribute_Label: AREA
Attribute_Definition: Area of polygon in square coverage units
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Positive real numbers
Attribute:
Attribute_Label: PERIMETER
Attribute_Definition: Perimeter of polygon in coverage units
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Positive real numbers
Attribute:
Attribute_Label: GEOLOGY#
Attribute_Definition: Internal feature number
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Sequential unique positive integer
Attribute:
Attribute_Label: GEOLOGY-ID
Attribute_Definition: User-assigned feature number
Attribute_Definition_Source: User-defined
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Integer
Attribute:
Attribute_Label: FM
Attribute_Definition: Formation name from source map
Attribute_Definition_Source: Hart, 1974
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: No restrictions
Attribute:
Attribute_Label: FMNUM
Attribute_Definition: Number representing geologic formation
Attribute_Definition_Source:
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: 1-173
Attribute:
Attribute_Label: MAJOR1
Attribute_Definition: Number representing geologic formation
Attribute_Definition_Source: FMNUM
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: 1-173
Attribute:
Attribute_Label: MINOR1
Attribute_Definition: Item used to accompany MAJOR1
Attribute_Definition_Source:
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: 0
Entity_Type:
Entity_Type_Label: GEOLOGY.AAT
Entity_Type_Definition: Geologic contacts
Entity_Type_Definition_Source: Hart, 1974
Attribute:
Attribute_Label: FNODE#
Attribute_Definition: Internal number of from-node
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Sequential unique positive integer
Attribute:
Attribute_Label: TNODE#
Attribute_Definition: Internal number of to-node
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Sequential unique positive integer
Attribute:
Attribute_Label: LPOLY#
Attribute_Definition: Internal number of polygon to left of arc
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Sequential unique positive integer
Attribute:
Attribute_Label: RPOLY#
Attribute_Definition: Internal number of polygon to right of arc
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Sequential unique positive integer
Attribute:
Attribute_Label: LENGTH
Attribute_Definition: Length of arc in coverage units
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Positive real numbers
Attribute:
Attribute_Label: GEOLOGY#
Attribute_Definition: Internal feature number
Attribute_Definition_Source: Computed
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Sequential unique positive integer
Attribute:
Attribute_Label: GEOLOGY-ID
Attribute_Definition: User-assigned feature number
Attribute_Definition_Source: User-defined
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: Integer
Attribute:
Attribute_Label: LTYPE
Attribute_Definition: Line type
Attribute_Definition_Source: Hart, 1974
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: QB FM OW SB
Attribute:
Attribute_Label: MAJOR1
Attribute_Definition: Line type
Attribute_Definition_Source: LTYPE
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: 0,1,2,3
Attribute:
Attribute_Label: MINOR1
Attribute_Definition: Item used to accompany MAJOR1
Attribute_Definition_Source:
Attribute_Domain_Values:
Enumerated_Domain:
Enumerated_Domain_Value: 0
Overview_Description:
Entity_and_Attribute_Overview:
The main polygon attribute of interest is "FM" that is an ASCII
character approximation of the map symbol for the name of geologic
unit or formation. Each "FM" in the state corresponds to a unique
integer "FMNUM". "FMNUM" and "FM" are attributes in both the polygon
attribute table of the coverage and "\geology.lut", which accompanies
the DLG version of this data set. The polygon attribute "MAJOR1" is
equivalent to "FMNUM". "MAJOR1" is found in both the DLG and ARC/INFO
versions of this data set. The polygon attribute "MINOR1" is always
zero.
An ASCII approximation of the explanation of the source document
(Hart, 1974) follows. Terms surrounded by quotation marks are
italicized in the source document. The formations are listed in order
of age, youngest first. The curly brackets and boxes shown on the
source document are approximated to help the user understand this
representation. The characters inside the boxes are equivalent to
"FM". Geologic Periods are listed on the left side as well as under
the boxes. Geologic Period subdivisions are listed on the left side
within the Geologic Periods. Geologic Groups are listed on the right
side. The stratigraphic nomenclature and age determinations used
herein are those accepted by the Oklahoma Geological Survey and do not
necessarily agree with those of the U.S. Geological Survey.
The stratigraphic nomenclature was separated into different areas
on the source document. Stratigraphic nomenclature for the entire
area covered in the source document was listed from Quaternary to
Upper Pennsylvanian Periods. The Ardmore Basin stratigraphic
nomenclature for the Middle Pennsylvanian Period was listed beside
nomenclature for the remaining area. The Arbuckle Mountains and the
Ouachita Mountains stratigraphic nomenclature for the Lower
Pennsylvanian to Middle Ordovician Periods were listed side-by-side.
The Arbuckle Mountains stratigraphic nomenclature back to the
Pre-Cambrian Era continued by itself.
The stratigraphic nomenclature cannot be listed side-by-side in
this metadata due to space limitations. This metadata will list the
general area nomenclature first. The Ardmore Basin stratigraphic
nomenclature will be listed next. The Arbuckle Mountains nomenclature
will be listed third and the Ouachita Mountains nomenclature will be
listed last. Each section will be titled to prevent confusion.
STRATIGRAPHIC NOMENCLATURE FOR ENTIRE AREA COVERED IN SOURCE
DOCUMENT (HART, 1974)
|--
| |---------|
| | Qal |
| |---------|
| QUATERNARY
Q | Alluvium
U |
A | Gravel, sand, silt, and clay, including low terraces;
T | thickness, about 25 to 100 feet. Yields moderate to large
E | amounts of water of poor to good quality along major rivers.
R-|
N | |---------|
A | | Qt |
R | |---------|
Y | QUATERNARY
| Terrace Deposits
|
| Gravel, sand, silt, clay, and volcanic ash; thickness, about 5
| to 50 feet; at various levels, as high as 160 feet above
| present flood plains. Yields moderate to large amounts of
| water of poor to good quality along major rivers.
|--
UNCONFORMITY
|--
| |--
| | |---------|
| | | Kef |
| | |---------|
| | CRETACEOUS
| | Eagle Ford Formation
| |
| | Shale, dark-gray, plastic; thickness, about 50 feet; top
| | eroded. Yields only limited amounts of water of poor quality.
| |
| | |---------|
| | | Kwt |
|U | |---------|
|p | | Kwl |
|p | |---------|
|e | | Kwr |
|r | |---------|
| -| | Kwd |
|C | |---------|
|r | CRETACEOUS
|e | Woodbine Formation
|t |
|a | Sandstone, brown to tan, fine- to coarse-grained,
|c | conglomeratic, ferruginous, moderately to weakly indurated,
|e | crossbedded, with interbedded gray shale and lignite;
|o | thickness, about 325 feet. Subdivided into 4 units:
|u | "Templeton Member," Kwt, indurated sandstone and shale, about
|s | 75 feet thick, erodes to an escarpment; "Lewisville Member,"
| | Kwl, mostly shale and weakly indurated sandstone, about 75
| | feet thick; "Red Branch Member," Kwr, indurated sandstone,
| | shale, and lignite, about 75 feet thick, erodes to an
| | escarpment; and basal "Dexter Member," Kwd, sandstone, shale,
| | and lignite, moderately to weakly indurated, about 100 feet
| | thick. Yields only small amounts of water of poor to good
| | quality.
| |--
| UNCONFORMITY
| |--
| | |----------|
| | | Kgb |
| | |----------|
| | CRETACEOUS
| | Grayson Marl and Bennington Limestone
| |
| | "Grayson Marl," marl, olive-gray, weakly indurated; thickness,
| | about 25 feet. "Bennington Limestone" at base is moderately
C | | indurated, medium bedded; thickness, about 10 feet. Yields
R | | only limited amounts of water of poor quality.
E | |
T | | |----------|
A-| | | Kb |
C | | |----------|
E | | CRETACEOUS
O | | Bokchito Formation
U | |
S | | Clay, illitic, kaolinitic, with some tan limestones and
| | sandstones. Subdivided into "Pawpaw Clay" at top, 40 to 60
| | feet thick; "Quarry Limestone," 13 feet thick; "Weno Clay,"
| | 100 to 135 feet thick; and basal "Denton Clay," 50 to 70 feet
| | thick. Yields only limited amounts of water of poor quality.
| |
| | |----------|
| | | Kc |
| | |----------|
| | CRETACEOUS
|L | Caddo Formation
|o |
|w | Limestones, marls, and shales; 150 feet thick. Subdivided
|e | into "Fort Worth Limestone" at top and "Duck Creek Limestone"
|r | below. Yields only limited amounts of water of poor quality.
| -|
|C | |----------|
|r | | Kk |
|e | |----------|
|t | CRETACEOUS
|a | Kiamichi Formation
|c |
|e | Shale, dark-gray, plastic, with oyster-shell limestones;
|o | thickness, about 30 feet. Yields only limited amounts of
|u | water of poor quality.
|s |
| | |----------|
| | | Kgw |
| | |----------|
| | CRETACEOUS
| | Goodland Limestone and Walnut Clay
| |
| | "Goodland Limestone," limestone, gray, dense, nodular to
| | massive; thickness, 20 to 30 feet. At base is "Walnut Clay,"
| | tan, about 4 feet thick. Yields only limited amounts of water
| | of poor quality.
| |
| | |----------|
| | | Ka |
| | |----------|
| | CRETACEOUS
| | Antlers Sand
| |
| | Sand, white to yellow, medium-grained, weakly indurated, with
| | varicolored clays. Contains arkosic conglomerates near
| | Arbuckle Mountains and "Baum Limestone" near Mannsville
| | anticline. Thickness, 200 to 700 feet. Yields moderate to
| | large amounts of water of good quality.
| |--
|--
UNCONFORMITY
|-- --|
| |----------| |
| | Pr | |
| |----------| |
| | Prw | |
| |----------| | W
| | Pr | | h
| |----------| | i
| PERMIAN | t
| Rush Springs Formation | e
| | h
| Sandstone, orange-brown, fine- to medium-grained, moderately | o
| indurated, with "Weatherford Gypsum Bed," Prw, 2 to 15 feet | r
| thick, near top. Thickness, about 280 feet, top eroded. | s
| Yields moderate to large amounts of water of good quality. | e
| |-
| |----------| | G
| | |-----| | | r
| | | Pmv | | | o
| | |-----| | | u
| | Pm | | p
| |----------| |
| PERMIAN |
| Marlow Formation |
| |
| Sandstone, orange-brown, fine- to medium-grained, moderately |
| indurated, with "Verden Sandstone Lentil," Pmv, 10 feet |
| thick near middle, and "Relay Creek" and "Emanuel" dolomite |
| and gypsum beds at top; thickness, 105 to 135 feet. Yields |
| only limited amounts of water of poor quality. |
| --|
| --|
| |----------| |
| | Pdc | |
| |----------| |
| PERMIAN |
| Dog Creek Shale |
| |
| Shale, red-brown, blocky, silty, weakly indurated, |
| gradational southward into "Chickasha Formation;" thickness, |
| 0 to about 130 feet. Yields only limited amounts of water |
| of poor quality. | E
| | l
| |----------| |
| | Pc | | R
| |----------| | e
| PERMIAN | n
| Chickasha Formation | o
| |-
| Mudstone conglomerate, siltstone, and sandstone, red-brown; | G
| thickness, 100 to 200 feet, decreasing southeastward. | r
| Yields only limited amounts of water of poor quality. | o
| | u
| |----------| | p
| | Pd | |
| |----------| |
P | PERMIAN |
E | Duncan Sandstone |
R | |
M-| Sandstone, white to buff, fine- to coarse-grained, |
I | moderately indurated, with interbedded mudstone |
A | conglomerates and siltstones; thickness, 100 to 400 feet, |
N | decreasing southeastward. Yields small to moderate amounts |
| of water of fair quality. |
| --|
| --|
| |----------| |
| | Pbi | |
| |----------| |
| PERMIAN |
| Bison Shale |
| |
| Shale, gray to red-brown, calcareous, blocky; thickness, 50 | H
| to 90 feet, decreasing southward. Yields only limited | e
| amounts of water of poor quality. | n
| | n
| |----------| | e
| | Pp | | s
| |----------| | s
| PERMIAN | e
| Purcell Sandstone | y
| |-
| Sandstone, red-brown to maroon and greenish-gray, fine- to | G
| coarse-grained, with some shale and mudstone conglomerate; | r
| thickness, 90 to 150 feet, decreasing southward. Yields | o
| small to moderate amounts of water of fair quality. | u
| | p
| |----------| |
| | Pfa | |
| |----------| |
| PERMIAN |
| Fairmont Shale |
| |
| Shale, red-brown, blocky; thickness, 40 to 80 feet, |
| decreasing southward. Yields only limited amounts of water |
| of poor quality. |
| --|
| |----------|
| | Pg |
| |----------|
| PERMIAN
| Garber Sandstone
|
| Sandstone, red-brown, fine- to coarse-grained; thickness,
| about 110 to 150 feet, including Fairmont Shale west of
| Elmore City, Garvin County. Yields small to moderate amounts
| of water of fair quality.
|
| |----------|
| | Pw |
| |----------|
| PERMIAN
| Wellington Formation
|
| Shale, red-brown, with several 20- to 30-foot bituminous
| sandstones at base ("Ryan"); thickness, about 100 to 200 feet,
| decreasing southeastward. Yields small to moderate amounts of
| water of fair quality.
|--
|--
| |-- --|
| | |----------| |
| | | IPo | |
| | |----------| | P
| | PENNSYLVANIAN | o
| | Oscar Group | n
| | | t
| | Shale, red-brown to gray, with arkosic sandstones and | o
| | limestone conglomerates near Arbuckle Mountains; "Hart | t
| | Limestone" at base; thickness, 300 to 500 feet, decreasing | o
| | southeastward. Yields small to moderate amounts of water of | c
| | poor to fair quality. |-
| | | G
| | |----------| | r
| | | IPv | | o
| | |----------| | u
| | PENNSYLVANIAN | p
| | Vanoss Group |
| | |
|U | Shale, maroon, arkose, and limestone conglomerate; |
|p | thickness, 250 to 900 feet (subsurface), decreasing |
|p | southward. Yields only limited amounts of water of fair to |
|e | good quality. --|
|r |
| -| |----------|
|P | | IPa |
|e | |----------|
|n | PENNSYLVANIAN
|n | Ada Formation (= Collings Ranch Conglomerate)
|s |
|y | Shale, red-brown to gray, bituminous sandstone, and limestone
|l | conglomerate; thickness, 100 to 1,400 feet (subsurface),
|v | decreasing southward. Probably will yield only limited
|a | amounts of water of fair quality.
|n |
|i | UNCONFORMITY
|a |
|n | |----------|
| | | IPva |
| | |----------|
| | PENNSYLVANIAN
| | Vamoosa Formation
| |
| | Shale, sandstone, and chert conglomerate; red-brown to buff
| | fine- to coarse-grained sandstone. Subdivided into 12
| | members, each with coarse clastics at base overlain by shale.
| | Thickness, about 125 to 260 feet (to 1,000 feet in
| | subsurface), decreasing southward. Yields small to moderate
| | amounts of water of fair quality.
| |--
| UNCONFORMITY
| |--
| | |----------|
| | | IPht |
| | |----------|
| | PENNSYLVANIAN
| | Hilltop Formation
| |
| | Shale, blue-gray to red-brown, with buff siltstones and
| | fine-grained sandstones at top; thickness, about 70 feet.
| | probably yields only limited amounts of water of fair quality.
| |
| | |----------|
| | | IPb |
| | |----------|
| | PENNSYLVANIAN
| | Belle City Formation
| |
| | Limestone, gray to buff, dense, in 2 beds each 2 to 3 feet
| | thick, with interbedded dark-gray shale, 10 to 20 feet thick.
| | Not known to yield water in this area.
| |
| | |----------|
| | | IPn |
| | |----------|
| | PENNSYLVANIAN
| | Nellie Bly Formation
| |
| | Shale, siltstone, fine-grained sandstone, chert conglomerate,
| | limestone, and limestone conglomerate, dark-gray to buff;
| | thickness, 200 to 300 feet. Probably yields only limited
| | amounts of water of poor to fair quality.
| | --|
| | |----------| |
| | | IPcf | |
| | |----------| |
| | PENNSYLVANIAN |
| | Coffeyville or Francis Formation (restricted) |
| | |
| | Shale, dark-blue, 20 to 70 feet thick, with "DeNay |
| | Limestone," yellow, massive, 2 to 6 feet thick at base, and |
| | 20 feet or more of buff fine- to coarse-grained sandstone |
| | and chert conglomerate at top. Probably yields only limited |
| | amounts of water of fair quality. |
| | | U
| | |----------| | p
| | | IPs | | p
| | |----------| | e
| | PENNSYLVANIAN | r
| | Seminole Formation |
| | | F
| | Shale, gray-green, with buff fine-grained sandstones, chert | r
| | conglomerates, and limy sandstones; thickness, about 120 | a
| | feet. Probably yields only limited amounts of water of poor | n
| | to fair quality. | k
| | | s
| | |----------| |-
| | | IPh | | C
| | |----------| | o
| | PENNSYLVANIAN | n
| | Holdenville Formation | g
| | | l
| | Shale, blue-gray, with light-brown sandstones and chert | o
| | conglomerates and 2 prominent limestones--the upper, or | m
| | "Sasakwa Limestone," white, fine-grained, 1 to 15 feet | e
| | thick, 35 feet below the top, and the lower, or "Homer | r
| | Limestone," dark-brown, sandy, 2 to 10 feet thick, 40 to 70 | a
| | feet below the Sasakwa. Thickness, 210 to 260 feet. | t
| | Probably yields only limited amounts of water of poor to | e
P | | fair quality. |
E | | |
N | | |----------| |
N | | | IPw | |
S | | |----------| |
Y | | PENNSYLVANIAN |
L-| | Wewoka Formation |
V | | |
A | | Shale, blue-gray, sandstone, chert conglomerate, and |
N | | limestone conglomerate; thickness, 400 feet. Probably |
I | | yields only limited amounts of water of poor to fair |
A | | quality. |
N | | --|
| | |----------|
| | | IPwe |
| | |----------|
| | PENNSYLVANIAN
| | Wetumka Shale
| |
| | Shale, blue-gray, with some sandstones and siltstones;
| | thickness, 120 to 250 feet. Probably yields only limited
| | amounts of water of poor to fair quality.
| |
| | |----------|
| | | IPca |
| | |----------|
|M | PENNSYLVANIAN
|i | Calvin Sandstone
|d |
|d | Sandstone, brown, medium-grained, with some gray shale;
|l | thickness, 40 to 320 feet, thinner southward. Probably
|e | yields only limited amounts of water of poor to fair quality.
| -|
|P | |----------|
|e | | IPse |
|n | |----------|
|n | PENNSYLVANIAN
|s | Senora Formation
|y |
|l | Shale, gray, and light-brown medium-grained sandstone;
|v | thickness, 150 to 500 feet, decreasing southwestward.
|a | Subdivided into lower sandstone, 350 feet thick, and upper
|n | shale, 150 feet thick. Probably yields only limited amounts
|i | of water of poor to fair quality.
|a |
|n | |----------|
| | | IPst |
| | |----------|
| | PENNSYLVANIAN
| | Stuart Shale
| |
| | Shale, blue to dark-gray, with some fine- to medium-grained
| | brown sandstones; thickness, 80 to 300 feet, decreasing
| | southwestward. Probably yields only limited amounts of water
| | of poor to fair quality.
| |
| | |----------|
| | | IPt |
| | |----------|
| | PENNSYLVANIAN
| | Thurman Sandstone
| |
| | Sandstone, brown, fine- to coarse-grained, with some gray
| | shale and basal 50-foot chert conglomerate; thickness, 80 to
| | 250 feet, decreasing southwestward. Probably yields only
| | limited amounts of water of poor to fair quality.
| |
| | |----------| --|
| | | IPbo | |
| | | | |
| | | /-------| |
| | | \ IPbj | |
| | |----------| |
| | PENNSYLVANIAN |
| | Boggy Formation |
| | |
| | Shale and sandstone, blue-gray to brown, fine- to coarse- | L
| | grained, with some thin limestone lenses and a coal bed 2.5 | o
| | feet thick about 400 feet above base. Thickness, 1,250 to | w
| | 2,800 feet. "Bluejacket Sandstone," IPbj, at base, 8 to 12 | e
| | feet thick, with 2-foot "Secor coal" 50 feet above top of | r
| | Bluejacket. Probably yields only limited amounts of water |
| | of poor to fair quality. | F
| | | r
| | |----------| | a
| | | IPsa | | n
| | |----------| | k
| | PENNSYLVANIAN | s
| | Savanna Formation |-
| | | C
| | Sandstone and shale, gray to brown, fine- to coarse- | o
| | grained, cherty, with several thin coal seams near middle; | n
| | thickness, 1,120 to 1,600 feet. Probably yields only | g
| | limited amounts of water of poor to fair quality. | l
| | | o
| | |----------| | m
| | | IPm | | e
| | |----------| | r
| | PENNSYLVANIAN | a
| | McAlester Formation | t
| | | e
| | Shale, gray, with "Upper Hartshorne coal" 1 to 50 feet |
| | above base, 500 to 600 feet thick; overlain by dark-gray |
| | shale with many buff fine-grained sandstones, 595 to 1,030 |
| | feet thick; overlain by dark-gray shale, 300 to 925 feet |
| | thick, with "McAlester coal," 1 to 3 feet thick, a few feet |
| | above base. Total thickness ranges from 1,150 to 2,420 |
| | feet. Probably yields only limited amounts of water of |
| | poor to fair quality. |
| | --|
| | |----------|
| | | IPha |
| | |----------|
| | PENNSYLVANIAN
| | Hartshorne Sandstone
| |
| | Sandstone, gray to white, medium- to coarse-grained with
| | interbedded middle gray shale and "Lower Hartshorne coal;"
| | thickness, 10 to 300 feet. Probably yields only limited
| | amounts of water of poor to fair quality.
| |
| | |----------|
| | | IPat |
| | |----------|
| | PENNSYLVANIAN
| | Atoka Formation
| |
| | Shale, dark-gray, and sandstone, buff to white, fine- to
| | coarse-grained, with some chert conglomerates; thickness, 800
| | to 3,000 feet. Probably yields only limited amounts of water
| | of poor to fair quality.
| |--
|--
UNCONFORMITY
ARDMORE BASIN STRATIGRAPHIC NOMENCLATURE
|--
| |--
| | |----------|
| | | IPho |
| | |----------|
| P | PENNSYLVANIAN
| e | Hoxbar Group (Missourian)
| n |
|M n | "Zuckerman Sandstone" (top eroded) down to base of
|i s | "Confederate Limestone;" thickness, 2,800 feet. Probably
|d y | yields only limited amounts of water of poor to fair
P |d l-| quality.
E |l v |
N |e a | |----------|
N | n | | IPd |
S | i | |----------|
Y | a | PENNSYLVANIAN
L-| n | Deese Group (Desmoinesian)
V | |
A | | Base of "Confederate Limestone" down to top of "Otterville
N | | Limestone;" thickness, 9,700 feet. Probably yields only
I | | limited amounts of water of poor to fair quality.
A | P |--
N | e |--
| n | |----------|
| n | | IPdo |
|L s | |----------|
|o y | PENNSYLVANIAN
|w l-| Dornick Hills Group (Morrowan)
|e v |
|r a | Top of "Otterville Limestone" down to base of "Lake Ardmore
| n | Sandstone;" thickness 1,800 feet. Probably yields only
| i | limited amounts of water of poor to fair quality.
| a |--
| n
|--
ARBUCKLE MOUNTAINS STRATIGRAPHIC NOMENCLATURE
|--
| |--
| | |------|-------|
| | | | IPwal |
| | | IPwa |-------|
| | | | IPwas |
| | |------|-------|
| | PENNSYLVANIAN
P | | Wapanucka Formation
E |L |
N |o | Limestone, gray to tan, fine-grained to oolitic. Mapped
N |w | separately along Lawrence uplift as IPwal, 30 to 75 feet thick
S |e | with gray shale, IPwas, below, about 160 feet thick.
Y |r | Probably yields only limited amounts of water of poor to fair
L-| -| quality.
V |P |
A |e | |----------|
N |n | | IPul |
I |n | |----------|
A |s | | IPus |
N |y | |----------|
|l | PENNSYLVANIAN
|v | Union Valley Formation
|a |
|n | Limestone, gray, fine- to medium-grained, IPul, 12 to 25 feet
|i | thick; with sandstone, IPus, below, fine- to medium-grained,
|a | about 150 to 260 feet thick. Yields small to moderate amounts
|n | of fair to good quality.
| |--
|--
|--
| |----------|
| | Mg |
| |----------|
| MISSISSIPPIAN
| Goddard Shale
|
| Mainly shale, gray, limonitic; thickness, 3,600 feet in
| Ardmore Basin, 240-450 feet on Lawrence uplift. In places
| includes "Rod Club" and "Overbrook Sandstones" and "Union
| Valley Formation-Wapanucka" shale. Probably yields only
M | limited amounts of water of poor to fair quality.
I |
S | |----------|
S | | Md |
I | |----------|
S | MISSISSIPPIAN
S-| Delaware Creek Shale
I |
P | Shale, dark-gray to black, fissile, calcareous; thickness, 160
P | to 750 feet, decreasing northward. Yields only limited
I | amounts of water of poor quality.
A |
N | |----------|
| | Msw |
| |----------|
| MISSISSIPPIAN
| Sycamore and Welden Limestones
|
| Limestone, blue-gray to tan, silty, fine-grained; thickness, 2
| to 370 feet, decreasing northeastward. Mapped separately in
| northeastern Arbuckle Mountains and Mannsville anticline;
| mapped elsewhere with underlying Woodford Shale. Probably
| yields only limited amounts of water of poor to fair quality.
|--
|--
D | |--
E | | |----------|
V | D | | Dw |
O |U e | |----------|
N |p v | DEVONIAN
I |p o-| Woodford Shale
A |e n |
N |r i | Shale, black, fissile, cherty; thickness, 160 to 560 feet,
| a | increasing southward. Yields only limited amounts of water
a | n | of poor quality.
n-| |--
d | |----------|
| | DSh |
| |----------|
S | DEVONIAN, SILURIAN
I | Hunton Group
L |
U | Marlstone, shale, and limestone, buff, ranging in age from
R | Early Silurian to Early Devonian; thickness, 100 to 700 feet,
I | with many unconformities. Probably yields only limited
A | amounts of water of poor to fair quality.
N |--
|--
|U
|p |--
|p O | |---------|
|e r | | Osfv |
|r d | |---------|
| o | ORDOVICIAN
|& v | Sylvan Shale, Fernvale Limestone, and Viola Limestone
| i-|
|M c | "Sylvan," shale, dark-greenish-gray; thickness, 60 to 325
|i i | feet. "Fernvale" and "Viola," limestone, gray, fine- to
|d a | coarse-grained; thickness, 350 to 900 feet. Probably yields
|d n | only limited amounts of water of poor to fair quality.
|l |--
|e
| |-- --|
| | |---------| |
| | | Obm | |
| | |---------| |
| | ORDOVICIAN | S
|M | Bromide, Tulip Creek, and McLish Formations | i
|i | | m
|d | Limestone, buff; shale, grayish-green; and sandstone, brown | p
|d | to white, fine- to medium-grained: approximate sequence of | s
|l | rocks in each formation, from top to bottom. Thickness, | o
|e | 750 to 1,400 feet, thinning eastward. Yields moderate to | n
| -| large amounts of water of poor to good quality. |-
|O | | G
|r | |---------| | r
|d | | Ooj | | o
O |o | |---------| | u
R |v | ORDOVICIAN | p
D |i | Oil Creek and Joins Formation |
O |c | |
V-|i | Limestone, gray to tan, granular, with greenish-gray shale |
I |a | and brown fine- to medium-grained sandstone; thickness, 600 |
C |n | to 1,100 feet, decreasing eastward. Yields moderate to |
I | | large amounts of water of poor to good quality. |
A | |-- --|
N | |-- --|
| | |-----|-----| |
| | | | Ows | |
| | | Owk |-----| |
| | | | Ok | |
| | |-----|-----| |
| | ORDOVICIAN |
|L | West Spring Creek and Kindblade Formations |
|o | |
|w | Limestone, gray to tan, fine-grained, gradational eastward |
|e | into tan fine- to coarse-grained dolomite; some tan to gray |
|r | sandstone and shale; thickness, 1,875 to 3,000 feet, |
| -| decreasing eastward. Yields moderate to large amounts of | A
|O | water of good quality. | r
|r | | b
|d | |---------| | u
|o | | Ocm | | c
|v | |---------| | k
|i | ORDOVICIAN | l
|c | Cool Creek and McKenzie Hill Formations | e
|i | |-
|a | Limestone, gray to tan, fine-grained, cherty, gradational | G
|n | eastward into dolomites and sandstones; thickness, 1,500 to | r
| | 2,300 feet, decreasing eastward. Yields moderate to large | o
| | amounts of water of good quality. | u
| |-- | p
|-- |
|-- |
| |-- |
| | |----------| |
| | | Cbf | |
| | |----------| |
| | CAMBRIAN
| | Butterfly Dolomite, Signal Mountain Limestone, |
| | Royer Dolomite, and Fort Sill Limestone |
|U | |
|p | Limestone, gray, fine-grained, gradational eastward into |
|p | tan to pink fine- to coarse-grained dolomites; thickness, |
|e | 570 to 1,600 feet, decreasing eastward. Yields moderate to |
|r | large amounts of water of good quality. |
| -| --|
|C | |----------|
|a | | Cth |
|m | |----------|
|b | CAMBRIAN
C |r | Timbered Hills Group
A |i |
M |a | "Honey Creek Limestone," above, is gray, fine grained; grades
B-|n | eastward into dolomite; thickness 90 to 250 feet. "Reagan
R | | Sandstone," at base, is brown, coarse grained; thickness,
I | | 60 to 450 feet. Probably will yield only limited amounts
A | | of water of good quality.
N | |--
|M UNCONFORMITY
|i |--
|d | |----------|
|d | | Cp |
|l | |----------|
|e | CAMBRIAN
| -| Colbert Porphyry
|C | (525 million years old)
|a |
|m | Rhyolite porphyry, red-brown, flow-banded; thickness, 7,500
|b | feet. Probably rests on 7,500 feet of metasedimentary and
|r | basaltic rocks in geosynclinal province of western Arbuckle
|i | Mountains. Probably will yield only limited amounts of
|a | water of good quality.
|n |--
|--
UNCONFORMITY
|--
P | |----------|
R | | pCt |
E | |----------|
C | PRECAMBRIAN
A | Tishomingo and Troy Granites
M-| (1.3 billion years old)
B |
R | Granite, pink, with much microcline and biotite; "Troy" is
I | fine grained; "Tishomingo" is coarse grained. Estimated
A | thickness, 10 miles. Probably will yield only limited amounts
N | of water of good quality.
|--
OUACHITA MOUNTAINS STRATIGRAPHIC NOMENCLATURE
|--
| |--
| | |----------|
| | | IPma |
| | |----------|
| | PENNSYLVANIAN
| | Morrowan-Atokan (?) rocks undifferentiated
| |
| | Shale and sandstone, gray to brown, fine- to coarse-grained;
| | thickness, 5,000 to 9,000 feet. Probably yields only
| | limited amounts of water of poor to fair quality.
| |
| | |----------|
| | | IPwc |
| | |----------|
| | PENNSYLVANIAN
| | Wapanucka Formation and Chickachoc Chert
| |
| | Limestone, gray to brown, spicular, granular to oolitic;
| | alternates with gray shale and calcareous sandstone;
| | thickness, 270 to 720 feet. Chert content increases
| | southeastward. Probably yields only limited amounts of
| | water of fair quality.
P |L |
E |o | |----------|
N |w | | IPjv |
N |e | |----------|
S |r | PENNSYLVANIAN
Y-| -| Johns Valley Formation
L |P |
V |e | Shale, dark-gray, with boulder conglomerate; thickness, 425 to
A |n | 900 feet. Yields only limited amounts of water of poor
N |n | quality.
I |s |
A |y | |----------|
N |l | | IPmo |
|v | |----------|
|a | PENNSYLVANIAN
|n | Morrowan rocks undifferentiated
|i |
|a | Shale and sandstone, gray to brown, fine- to coarse-grained;
|n | estimated thickness, 3,000 feet. Probably yields only limited
| | amounts of water of poor to fair quality.
| |
| | |----------|
| | | IPjf |
| | |----------|
| | PENNSYLVANIAN
| | Jackfork Sandstone
| |
| | Sandstone, gray, white, and tan, coarse-grained, cherty, with
| | gray shale and some boulders up to 7 feet in diameter;
| | thickness 1,150 to 5,000 feet. Probably yields only limited
| | amounts of water of poor to fair quality.
| |--
|--
|-- --|
| |----------| |
| | Mg | |
| |----------| |
| MISSISSIPPIAN |
| Goddard Shale |
M | |
I | Shale, gray, limonitic; | |----------|
S | estimated thickness, 500 | | Mst |
S | feet, but may be 2,500 | |----------|
I | feet. Probably yields | MISSISSIPPIAN
S | only limited amounts of | Stanley Shale
S-| water of poor to fair |-
I | quality. | Shale, dark-gray, siliceous,
P | | with some gray to buff fine-
P | |----------| | grained sandstones; thickness,
I | | Md | | 10,000 feet. Yields only
A | |----------| | limited amounts of water of
N | MISSISSIPPIAN | poor quality.
| Delaware Creek Shale |
| |
| Shale, dark-gray to black |
| fissile; thickness 525 |
| feet. Yields only |
| limited amounts of water |
| of poor of quality. |
|-- --|
D |--
E | |--
V | | |----------|
O | | | Da |
N | D | |----------|
N |U e | DEVONIAN
I |p v | Arkansas Novaculite
A |p o-|
N |e n | Shale, black, cherty, with much novaculite; thickness, 230 to
|r i | 375 feet. Probably yields only limited amounts of water of
a | a | fair quality.
n-| n |--
d | |----------|
| | Smb |
S | |----------|
I | SILURIAN
L | Missouri Mountain Shale and Blaylock Sandstone
U |
R | "Missouri Mountain Shale," shale, black to gray-green to red;
I | thickness, 100 feet; underlain by sandstone, several feet
A | thick, correlated as "Blaylock." Probably yields only limited
N | amounts of water of poor to fair quality.
|--
|--
|U
|p
|p
|e |--
|r | |----------|
| | | Op |
|& | |----------|
| | ORDOVICIAN
|M | Polk Creek Shale
|i |
|d | Shale, black; thickness, 175 feet. Yields only limited
|d | amounts of water of poor quality.
|l-|
|e | |----------|
O | | | Ob |
R |O | |----------|
D |r | ORDOVICIAN
O |d | Bigfork Chert
V-|o |
I |v | Limestone, gray, and dark-gray to black chert; thickness, 575
C |i | feet. Probably yields only limited amounts of water of poor
I |c | to fair quality.
A |i |--
N |a
|n
| O |--
|M r | |----------|
|i d | | Ow |
|d o | |----------|
|d v-| ORDOVICIAN
|l i | Womble Shale
|e c |
| a | Shale, black to green; thickness, 250 feet, base covered.
| n | Yields only limited amounts of water of poor quality.
| |--
|--
The arc attributes "LTYPE" and "MAJOR1" indicates the line type.
"LTYPE" is only included in the ARC/INFO version of the data set. If
"LTYPE" is "QB" then "MAJOR1" will be "0", and the line is part of the
quadrangle boundary but not part of the state boundary. If "LTYPE" is
"FM" then "MAJOR1" will be "1", and the line is a formational contact.
If "LTYPE" is "OW" then "MAJOR1" will be "2," and the line is an open
water contact. If "LTYPE" is "SB" then "MAJOR1" will be "3", and the
line is part of the Oklahoma state boundary. The arc attribute
"MINOR1" is always zero.
Distribution_Information:
Distributor:
Contact_Information:
Contact_Person_Primary:
Contact Person: Dr. Jayne Salisbury
Contact_Organization: Spatial and Environmental Information Clearinghouse, Oklahoma State University
Contact_Position: Director
Contact_Address:
Address_Type: mailing address
Address: 005A Life Science East, Oklahoma State University
City: Stillwater
State_or_Province: Oklahoma
Postal_Code: 74078
Country: United States of America
Contact_Voice_Telephone: 405-744-8974
Contact_Electronic_Mail_Address: webster@seic.lse.okstate.edu
Hours_of_Service: 9 AM to 5 PM Central Time Zone
Resource_Description: Oklahoma Aquifer Characteristics Data Sets
Distribution_Liability: None.
Standard_Ordering_Process:
Digital_Form:
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Fees: None for unassisted Internet downloads.
Custom_Order_Process: Call for information.
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Distributor:
Contact_Information:
Contact_Person_Primary:
Contact Person: Branch of Information Services
Contact_Organization: U.S. Geological Survey
Contact_Position: Branch of Information Services
Contact_Address:
Address_Type: mailing address
Address: Box 25286
City: Denver Federal Center
State_or_Province: Colorado
Postal_Code: 80225-0286
Country: United States of America
Contact_Voice_Telephone: (303)202-4210
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Fees: $10 per diskette.
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Metadata_Reference_Information:
Metadata_Date: 19970305
Metadata_Contact:
Metadata_Standard_Name:
FGDC Content Standards for Digital Geospatial Metadata
Metadata_Standard_Version: 19940608