The bedrock topography is shown as 50-foot (15-meter) contours of bedrock elevation above mean sea level (msl). Bedrock elevations range from less then 250 feet (76 meters) in southern Illinois to more than a 1000 feet (300 meters) in the northwestern part of the state. Several major bedrock valleys are found across the state.
The greatest control for the present bedrock surface configuration was probably the preglacial surface configuration. The interpretations of bedrock topography have been modified since the 1950's. Horberg contoured his map with the philosophy that the bedrock surface map represented the preglacial topography modified by glacial erosion, which formed U-shaped valleys. The current map, showing narrow valley channels and bedrock knobs in wide channels, indicates complex preglacial and glacial erosion primarily from running water. The major valleys were formed before the minor valleys that appear as tributaries. Streams that formed during successive glaciations probably eroded to bedrock and produced the small tributary valleys to the main channels. The bedrock surface was less likely to be eroded as sediments accumulated during each successive glaciation.
Herzog, B.L.. B.J. Stiff, C.A. Chenoweth, K.L, 1994, Buried Bedrock Surface of Illinois: ISGS GIS Database GISDB_BEDGEO.IL_Bedrock_Topography_1994_Ln, Illinois State Geological Survey, Champaign, Illinois.
This is a Vector data set. It contains the following vector data types (SDTS terminology):
Horizontal positions are specified in geographic coordinates, that is, latitude and longitude. Latitudes are given to the nearest 0.000001. Longitudes are given to the nearest 0.000001. Latitude and longitude values are specified in Decimal degrees.
The horizontal datum used is NAD27.
The ellipsoid used is CLARKE1866.
The semi-major axis of the ellipsoid used is 6378206.4 meters.
The flattening of the ellipsoid used is 1/294.98.
CONTOUR The elevation above msl in Lambert feet. Values range from 200 to 1000 with a contour interval of 50 feet. A value of zero (0) is used to indicate the state boundary or areas where bedrock is at or near the surface.
Sequential unique whole numbers that are automatically generated.
Coordinates defining the features.
Applications are regional or statewide studies, preferably at a scale of 1:500,000.The Buried Bedrock Surface of Illinois will be useful in fields such as groundwater resource planning, engineering geology and earthquake hazard mapping. Data shown on this map were compiled from geologic data from drill holes, samples, surface observations and geophysical data from downhole logging and surface studies.
The data are not appropriate as a geodetic, legal or engineering base. The data set was not and is not intended as a substitute for surveyed locations, such as can be determined by a registered Public Land Surveyor. Although useful in a GIS as a reference base layer for maps, the data set has no legal basis in the definition of boundaries or property lines.
Herzog, B.L.. B.J. Stiff, C.A. Chenoweth, K.L, 1994, Buried Bedrock Surface of Illinois: ISGS Illinois Map series 5, Illinois State Geological Survey, Champaign, Illinois.
Herzog, B.L.. B.J. Stiff, C.A. Chenoweth, K.L, 1994, Original mylar separates for map of Buried Bedrock Surface of Illinois: Illinois State Geological Survey, Champaign, Illinois.
Anderson, R.C., 1980, Geology for Planning in Rock Island County, Illinois: ISGS Circular 510, Illinois State Geological Survey, Champaign, Illinois.
Berg, R.C., J.P. Kempton, A. Stecyk, 1984, Geology for Planning in Boone and Winnebago Counties: ISGS Circular 531, Illinois State Geological Survey, Champaign, Illinois.
Bristol, B.B. and P.R. Seaber, 1973, Ordovician Galena Group of Illinois-Structure and Oil Fields, Plate 1: Illinois State Geological Survey, Champaign, Illinois.
Curry, B.B. and P.R. Seaber, 1990, Hydrogeology of Shallow Groundwater Resources, Kane County, Illinois: Contract/Grant Report 1990-1, Illinois State Geological Survey, Champaign, Illinois.
Greasse, A.M., R.A. Bauer, B.B. Curry, R.C. Va, 1988, Geological-Geotechnical Studies for Siting Superconducting Super Collider in Illinois: ISGS Environment notes 123, Illinois State Geological Survey, Champaign, Illinois.
Heigold, P.C. and R.W. Ringler, 1979, A seismic Refraction Survey of the Lower Illinois Valley Bottomlands: ISGS Circular 507, Illinois State Geological Survey, Champaign, Illinois.
Horberg, L., 1950, Bedrock Topography of Illinois: ISGS Bulletin 73, Illinois State Geological Survey, Champaign, Illinois.
Horberg, L., 1957, Bedrock Surface of Illinois: Illinois State Geological Survey, Champaign, Illinois.
Hunt, C.S. and J.P. Kempton, 1971, Geology for Planning in DeWitt County, Illinois: ISGS Environmental Geology Notes 83, Illinois State Geological Survey, Champaign, Illinois.
Jacobs, A.M. (compiler), 1971, Geology for Planning in St. Clair County, Illinois: ISGS Circular 465, Illinois State Geological Survey, Champaign, Illinois.
Kempton, J.P., W.H. Johnson, P.C. Heigold and , 1991, Mahomet Bedrock Valley in east-central Illinois: Geological Society of America (GSA) Special Paper 285.
Kempton, J.P., W.H. Morse, and A.P. Visocky, 1982, Hydrogeologic Evaluation of Sand and Gravel Aquifers and Municipal Groundwater Supplies in east-central Illinois: Cooperative Groundwater/Resources Report 8, Illinois State Geological Survey, Champaign, Illinois.
Kempton, J.P., R.W. Ringler, P.C. Heigold, K. , 1981, Groundwater Resources of Northern Vermillion County, Illinois: Environmental Groundwater/Resources Report 13, Illinois State Geological Survey, Champaign, Illinois.
Kempton, J.P. A.P. Visocky, 1992, Regional Groundwater Resources in East McLean and Tazewell County: Mahomet Bedrock Valley: Cooperative Groundwater/Resources Report 13, Illinois State Geological Survey, Champaign, Illinois.
Kolata, D.R., T.C. Buschbach and J.D. Treworg, 1978, The Sandwich Fault Zone of Northern Illinois: ISGS Circular 505, Illinois State Geological Survey, Champaign, Illinois.
Larsen, J.I, 1973, Geology for Planning in Lake County, Illinois: ISGS Circular 481, Illinois State Geological Survey, Champaign, Illinois.
Larson, D.R., B.L. Herzog, R.C. Vaiden, C.A. , 1994, Hydrogeology of the Green River Lowland and Associated Bedrock Valleys of Northwest Illinois: Illinois State Geological Survey, Champaign, Illinois.
Larson T.H. and V.L. Poole, 1989, Geophysical Exploration of Potential Groundwater Resources near Bloomington, Illinois: ISGS Contract/Grant Report 1989-2, Illinois State Geological Survey, Champaign, Illinois.
Lineback, J.A., 1979, Quaternary Deposits of Illinois: ISGS map same as title, Illinois State Geological Survey, Champaign, Illinois.
Palmer, R.A. (compiler), 1983, The Decade of North American Geology (DNAG) 1983 Geologic Time Scale: Geology, v 11 no. 9.
Piskin, K. and R.E. Bergstrom, 1975, Glacial Drift in Illinois: Thickness and Character: ISGS Circular 490, Illinois State Geological Survey, Champaign, Illinois.
Richmond, M.R. and D.S. Fullerton, 1986, Introduction to Quaternary Glaciation in the United States of America: Quaternary Science Review v5.
Walker W.H., R.E. Bergstrom and W.C. Walton, 1965, Report on the Groundwater Reservoir of the Havana Region in West-Central Illinois: Cooperative Groundwater/Resources Report 3, Illinois State Geological Survey, Champaign, Illinois.
H. B. Willman, John C. Frye, Jake A. Simon, Kenneth, 1967, Geologic Map of Illinois: ISGS map same as title, Williams and Heintz Map Corp., Capitol Heights, MD.
Willman, H.B., and J.C. Frye, 1980, The Glacial Boundary in Southern Illinois: ISGS Circular 511, Illinois State Geological Survey, Champaign, Illinois.
The features were imported into the ISGS SDE enterprise database following steps outlined in ISGS procedure GISDB_0009.
Metadata updated.
Person who carried out this activity:
The published geological map (ISGS Illinois Map 5, 1994) was the source for feature attributes. Attribute code assignments were reviewed by both the ISGS and the USGS and are believed to be fully representative of the source document.
Horizontal positional accuracy of this data with respect to the source map was verified by ISGS and USGS personnel by visual comparison (manual overlay) of source mylars and hard-copy plots. Arcs within one line-width of source mylars were deemed acceptable.
This data set depicts the buried bedrock surface of Illinois. Areas where the bedrock surface is exposed at the surface are not shown (e.g. the northwest Illinois driftless area, and much of southern Illinois).
When in coverage format, this data set was checked for complete chain-node topology (no dangling arcs, except where appropriate), boundary values appropriate for map projection and map units, and appropriate "fuzzy" tolerances. There are no known arc attribute values outside the appropriate value domains.
Are there legal restrictions on access or use of the data?
- Access_Constraints: none
- Use_Constraints:
- This coverage should be used at 1:500,000 scale or smaller (ie: 1:1,000,000).
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The Illinois Department of Natural Resources (DNR) provides these geographic data "as is." DNR makes no guarantee or warranty concerning the accuracy of information contained in the geographic data. DNR further makes no warranties, either expressed or implied as to any other matter whatsoever, including, without limitation, the condition of the product, or its fitness for any particular purpose. The burden for determining fitness for use lies entirely with the user. Although these data have been processed successfully on computers of DNR, no warranty, expressed or implied, is made by DNR regarding the use of these data on any other system, nor does the fact of distribution constitute or imply any such warranty.In no event shall the DNR have any liability whatsoever for payment of any consequential, incidental, indirect, special, or tort damages of any kind, including, but not limited to, any loss of profits arising out of use of or reliance on the geographic data or arising out of the delivery, installation, operation, or support by DNR.
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The data are intended for use with GIS software. The ISGS uses ESRI ArcGIS software, however, the ESRI shapefile format can be imported into many different GIS software packages.It is expected that customers who order this data have the technical expertise to use GIS software. The ISGS does not provide software support of any kind.
Illinois Natural Resources Geospatial Data Clearinghouse
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