000272679 000__ 01741cam\a22003614a\45e0 000272679 001__ 272679 000272679 005__ 20210513103010.0 000272679 008__ 031023s2003\\\\kyuab\\\\b\\\f000\0\eng\d 000272679 010__ $$a 2003479869 000272679 035__ $$a(OCoLC)ocm53274949 000272679 035__ $$a272679 000272679 040__ $$aDLC$$beng$$cDLC$$dBTCTA$$dGPO$$dAGL$$dTXJ$$dOCLCA$$dKMS 000272679 043__ $$an-us-ky 000272679 049__ $$aISEA 000272679 05000 $$aGB701$$b.W375 no.03-4180 000272679 074__ $$a0624-B 000272679 0860_ $$aI 19.42/4:03-4180 000272679 1001_ $$aHodgkins, Glenn. 000272679 24510 $$aEstimating the magnitude of peak flows for streams in Kentucky for selected recurrence levels /$$cby Glenn A. Hodgkins and Gary R. Martin. 000272679 260__ $$aLouisville, Ky. :$$bU.S. Dept. of Interior, U.S. Geological Survey,$$c2003. 000272679 300__ $$aiv, 68 p. :$$bill., maps (some col.) ;$$c28 cm. 000272679 4901_ $$aWater-resources investigations report ;$$v03-4180 000272679 500__ $$aOne folded map in pocket. 000272679 500__ $$aShipping list no.: 2004-0005-P. 000272679 504__ $$aIncludes bibliographical references (p. 29-31). 000272679 650_0 $$aStream measurements$$zKentucky. 000272679 650_0 $$aStreamflow$$zKentucky. 000272679 7102_ $$aGeological Survey (U.S.) 000272679 7101_ $$aKentucky.$$bDepartment of Highways. 000272679 77608 $$iOnline version:$$aHodgkins, Glenn.$$tEstimating the magnitude of peak flows for streams in Kentucky for selected recurrence intervals.$$dLouisville, Ky. : U.S. Dept. of the Interior, U.S. Geological Survey ; Denver, CO : U.S. Geological Survey, Information Services [distributor], 2003$$w(OCoLC)622489311 000272679 830_0 $$aWater-resources investigations report ;$$v03-4180. 000272679 85200 $$bgen$$hGB701$$i.W375$$ino.03-4180 000272679 85640 $$zOnline access via PURL$$uhttp://purl.access.gpo.gov/GPO/LPS98247 000272679 85640 $$zOnline access via HathiTrust Digital Library$$uhttp://catalog.hathitrust.org/api/volumes/oclc/54392875.html 000272679 909CO $$ooai:library.usi.edu:272679$$pGLOBAL_SET 000272679 980__ $$aBIB 000272679 980__ $$aBOOK 000272679 983__ $$aOnline