Plan of study for the regional aquifer-system analysis of the Appalachian Valley and Ridge, Piedmont, and Blue Ridge physiographic provinces of the eastern and southeastern United States, with a description of study-area geology and hydrogeology

Swain, Lindsay A.; Hollyday, E. F.; Daniel, Charles C.; Zapecza, Otto S.

doi:10.3133/wri914066

Cited by 5 publications

References 18 publications

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USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW¹

Hinaman¹

1993

J American Water Resour Assoc

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A Geographic Information System (GIS) was used to expedite assembly of input‐data sets for a model of ground‐water flow in the Middle Patuxent River basin in Howard County, Maryland. The model grid was developed with GIS and used to select attributes from GIS data coverages. These attributes were then output from GIS into the input‐data sets, which included model boundaries, regolith thickness, bedrock‐surface altitude, stream locations, stream length, stream‐bottom altitude, and trans‐missivity. The ability to change large sets of spatial data quickly and accurately with GIS enhances the model‐calibration process. (KEY TERMS: GIS; ground water; Piedmont; Maryland; MODFLOW.)

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USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW¹

Hinaman¹

1993

J American Water Resour Assoc

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Ground-water resources of the Upper Chattahoochee River basin in Georgia and Subarea 1 of the Apalachicola-Chattahoochee-Flint and Alabama-Coosa-Tallapoosa river basins

Chapman¹,

Peck²

1997

Open-File Report

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Ground-water resources of the middle Chattahoochee River basin in Georgia and Alabama, and upper Flint River basin in Georgia - Subarea 2 of the Apalachicola-Chattahoochee-Flint and Alabama-Coosa-Tallapoosa river basins

Chapman¹,

Peck²

1997

Open-File Report

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The error occurs in table 7. Station number 02341070 Mulberry Creek at State Route 85, near Waverly Hall, Ga. The drainage area of 123 square miles is incorrect the correct drainage area is 12.3 square miles. The unit-area discharge is still correct as shown (zero cubic feet per second per square mile), because the measured stream discharge on the indicated day (10-21-54) was zero cubic feet per second. Because the measured stream discharge was zero, the stream discharge exiting the Chartahoochee River basin in Subarea 2 (shown as 679 cubic feet per second, on page 31) also is still correct. We apologize for any inconvenience this error may have caused.

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Plan of study for the regional aquifer-system analysis of the Appalachian Valley and Ridge, Piedmont, and Blue Ridge physiographic provinces of the eastern and southeastern United States, with a description of study-area geology and hydrogeology

Cited by 5 publications

References 18 publications

USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW¹

USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW¹

Ground-water resources of the Upper Chattahoochee River basin in Georgia and Subarea 1 of the Apalachicola-Chattahoochee-Flint and Alabama-Coosa-Tallapoosa river basins

Ground-water resources of the middle Chattahoochee River basin in Georgia and Alabama, and upper Flint River basin in Georgia - Subarea 2 of the Apalachicola-Chattahoochee-Flint and Alabama-Coosa-Tallapoosa river basins

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Plan of study for the regional aquifer-system analysis of the Appalachian Valley and Ridge, Piedmont, and Blue Ridge physiographic provinces of the eastern and southeastern United States, with a description of study-area geology and hydrogeology

Cited by 5 publications

References 18 publications

USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW1

USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW1

Ground-water resources of the Upper Chattahoochee River basin in Georgia and Subarea 1 of the Apalachicola-Chattahoochee-Flint and Alabama-Coosa-Tallapoosa river basins

Ground-water resources of the middle Chattahoochee River basin in Georgia and Alabama, and upper Flint River basin in Georgia - Subarea 2 of the Apalachicola-Chattahoochee-Flint and Alabama-Coosa-Tallapoosa river basins

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Resources

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USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW¹

USE OF A GEOGRAPHIC INFORMATION SYSTEM TO ASSEMBLE INPUT‐DATA SETS FOR A FINITE‐DIFFERENCE MODEL OF GROUND‐WATER FLOW¹