by U.S. Dept. of the Interior, U.S. Geological Survey in [Reston, Va.? .
Written in English
|Other titles||Water level changes, 1980 to 1997, and saturated thickness, 1996-97, in the High Plains aquifer|
|Series||USGS fact sheet -- 124-99, Fact sheet (Geological Survey (U.S.)) -- FS-99-124|
|Contributions||Geological Survey (U.S.)|
|The Physical Object|
|Pagination|| p. :|
High Plains Aquifer Water-Level Monitoring Study Water-Level Changes, to , and Saturated Thickness, , in the High Plains Aquifer. By V.L. McGuire, C.P. Stanton, and B.C. Fischer. U.S. Geological Survey Fact Sheet FS Lincoln, Nebraska This report is also available in Adobe PDF format (2 Meg PDF). Introduction. The map of water-level changes in the High Plains aquifer from predevelopment to (fig. 1) is based on water levels from 4, wells (table 1). The area-weighted average water-level change was a decline of feet, and the water removed from the aquifer through . Get this from a library! Water-level changes, to , and saturated thickness, , in the High Plains aquifer.. [Geological Survey (U.S.);]. WATER-LEVEL CHANGES, TO AND TO Ninety-nine percent of all water-level changes from to were from a rise of feet to a decline of feet. The average area-weighted water-level change in the High Plains aquifer was a decline of foot from to based on measurements from 7, wells (table 1).
This map is published in the web report "Water-level changes, to , and saturated thickness, , in the High Plains aquifer" and USGS Fact Sheet , "Water-level changes, to , and saturated thickness, , in the High Plains aquifer". Water Flow in the High Plains Aquifer in Northwestern Oklahoma The High Plains is a major agricultural area, supported the land surface. In , the saturated thickness (the vertical thickness of an aquifer that is filled with water) ranged from McGuire, V.L., and Fischer, B.C., , Water-level changes, to , and saturated. Water Flow in the High Plains Aquifer in Northwestern Oklahoma. Water-level changes, to , and saturated thickness, , in the High Plains. This digital data set consists of saturated thickness contours for the High Plains aquifer in Central United States, The High Plains aquifer extends from south of 32 degrees to almost 44 degrees north latitude and from 96 degrees 30 minutes to degrees west h Year:
Knowledge Systems for Sustainable Development Article Literature Review (PDF Available) in Proceedings of the National Academy of Sciences (14) July with 1, Reads. Water-level changes, to , and saturated thickness, , in the High Plains aquifer by Geological Survey (U.S.) 1 edition - first published in Not in Library. This bibliography includes a majority of references used in the Colorado Ground Water Atlas along with pertinent entries gathered in the updating process. Values of saturated thickness, aquifer thickness, and during –97 to determine aquifer properties. Supply well LUV23 was used as the pumped well during a 72– pumped wells during through Water-level measurements in pumped wells and nearby observation.