<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Leslie J. Crain</dc:contributor>
  <dc:contributor>Richard C. Shipley</dc:contributor>
  <dc:contributor>James B. Hood Jr.</dc:contributor>
  <dc:creator>William J. Shampine</dc:creator>
  <dc:date>1966</dc:date>
  <dc:description>&lt;p&gt;This report contains a tabulation of data collection sites established by the U.S. Geological Survey in the Western Oswego River basin. Information on the types of data collected at each site is also provided.&lt;/p&gt;
&lt;p&gt;Statistical summaries are furnished for selected stream-gaging stations in the form of duration, flood frequency, and low-flow frequency curves.&lt;/p&gt;
&lt;p&gt;Climatological data on long-term average precipitation is provided in the form of an isohyetal map of the study area.&lt;/p&gt;
&lt;p&gt;Selected results of computerized data on flow passing Mud Lock and. on Cayuga Lake levels are presented.&lt;/p&gt;
&lt;p&gt;Data being collected in the course of the ground-water studies includes test borings, information on existing wells, and geologic mapping. Preliminary analysis of this data indicates that the areas with the greatest potential for development of large ground-water supplies are portions of the basin underlain by carbonate rocks, the unconsolidated deposits in the northern portion of the basin, and the unconsolidated deposits south of the four lakes.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr66122</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Water resources of the Western Oswego River basin, N.Y. -interim report</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>