ML083030250

Copper Nuclear Station, License Renewal Application, Environmental Report, Figure 2.1-1 - Figure 2.3.3

ML083030250
Person / Time
Site:	Cooper
Issue date:	09/24/2008
From:	Nebraska Public Power District (NPPD)
To:	Office of Nuclear Reactor Regulation
References
NLS2008071
Download: ML083030250 (12)

Text

Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage2-129Figure 2.1-1Location of CNS, 6-Mile Radius Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage2-130Figure 2.1-2Location of CNS, 50-Mile Radius Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage 2-131Figure 2.1-3CNS Levee Map Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage2-132Figure 2.1-4Topographic Map Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage2-133Figure 2.1-5Major State and Federal, and Native American Lands, 6-Mile Radius Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage2-134Figure 2.1-6Major State, Federal, and Native American Lands, 50-Mile Radius Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage2-135Figure 2.1-7CNS Exclusion Area Boundary Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage 2-136Figure 2.2-1Missouri River Drainage Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage2-137Figure 2.3-1Stratigraphic Chart Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage 2-138Figure 2.3-2Surficial Aquifers Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage 2-139Notes for Figure 2.3-2Coarse-grained, unconsolidated deposits, mostly of quaternary age, compose the surficial aquifer system and provide water for many shallow wells. Alluvium along major stream valleys, a broad blanket of alluvium in southeastern Missouri, and glacial outwash (buried in some places beneath fine-grained sediments) form productive aquifers. Till, loess, and fine-grained glacial-lake deposits a re widespread in areas of the segment that were covered by continental glaciers; these deposits generally yield only small amounts of water and are not considered to be principal aquifers. Modified fromAmerican Association of Petroleum Geologists, 1984, Geological Highway Map, Northern Great Plains Region-North Dakota, South Dakota, Iowa, Nebraska, Minnesota: American Association of Petroleum Geologists, scale 1:900,000, 1 sheet.American Association of Petroleum Geologists, 1988, Geological Highway Map, Mid-Continent Region: Kansas, Missouri, Oklahoma, Arkansas: American Association of Petroleum Geologists, scale 1:900,000, 1 sheet.Lugn, A.L. and Wenzel, L.K., 1938, Geology and ground-water resources of south-central Nebraska: U.S. Geological Survey Water-Supply Paper 779,242P.

D.R. Soller, U.S. Geological Survey, written communication, 1989.

Cooper Nuclear StationApplicant's Environmental ReportOperating License Renewal Stage 2-140Figure 2.3-3Nemaha Natural Resources District