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<br />000070 <br /> <br />I-/e II~.!;~)_~ <br />.-- <br /> <br /> <br />United States Department of the <br /> <br />GEOLOGICAL SURVEY <br />Box 25046 <br />Denver Federal Center <br />Denv'Ba~ota'l09 '9225 <br /> <br />Interior <br /> <br />Water Resources Division <br />Colorado District <br />Mail Stop 415 <br />l' 01' '\ '-f\'~ <br />0\ \~.,g. <br />,-- ,,~ <br /> <br />~.'oJ <br />Is -\\AI" <br />\I A..& <br /> <br />IN REPLY REFER TO: <br /> <br />INFORMATION FOR THE PRESS: <br /> <br />Subject: <br /> <br /> <br />Release Date: <br /> <br /> <br />For additional information, contact: <br /> <br />R. U. Grozier, Acting District Chief <br />U.S. Geological Survey, Water Resources <br />Box 25046, Mail Stop 415 <br />Denver Federal Center <br />Lakewood, CO 80225 <br />Telephone: (303) 234-5091 <br /> <br />A hydrologic reconnaissance of a 74-kilometer reach of the Yampa River in <br />Dinosaur National ,Monument was made by personnel of the U.S. Geological Survey <br />during low flow, in mid-August 1976. Stream discharge, which waS measured along <br />this reach every 16 to 24 kilometers, ranged from 9.4 to 10.6 cubic meters per <br />second. Variations in streamflow were explained, in part, by underflow, loss <br />to ground water, and evaporation. Specific conductance was measured about <br />every 2 kilometers and indicated a downstream increase on the order of 11 to <br />12 percent for the reach. Except for mercury, bottom-sediment trace-element <br />concentrations in the study reach were less than maximum concentrations deter- <br />mined during August-September 1976 for bottom sediments at unperturbed sites <br />upstream in the Yampa River basin. At one of five sampling sites, the mercury <br />concentration in bottom sediments was 0.35 microgram per gram, which exceeded <br />the maximum measured upstream level. <br /> <br />The results of the hydrologic reconnaissance are summarized in U.S. Geo- <br />logical Survey Open-File Report 78-226, "Hydrologic reconnaissance of the Yampa <br />River during low flow, Dinosaur National Monument, northwestern Colorado," by <br />Timothy D. Steele, Dennis A. Wentz, and James W. Warner. The report is not <br />available for general distribution, but it may be purchased from: Open-File <br />Services Section, Branch of, Distribution, U.S. Geological Survey, Box 25425, <br />Denver Federal Center, Lakewood, CO 80225. (Telephone: 303-234-5888.) Or, <br />the report may be examined only at the following U.S. Geological Survey offices: <br /> <br />1. Colorado District Office, Water Resources Division, Room H-2103, <br />Building 53, Denver Federal Center, Lakewood, Colo. (Mailing address: Box <br />25046, Mail Stop 415, Denver Federal Center, Lakewood, CO 80225.) <br /> <br />(Continued on back) <br /> <br />~ <br /> <br />~ <br />'I <br />" <br />,I <br /> <br />~ <br /> <br />I <br /> <br />