<?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>David T. Poynter</dc:contributor>
  <dc:creator>Paul W. Westerfield</dc:creator>
  <dc:date>1994</dc:date>
  <dc:description>Water-level maps of the Mississippi River Valley alluvial aquifer are presented for spring 1992 in this map report.  The alluvial aquifer consists of sand and gravel in flood-plain and terrace deposits of Quaternary age and supplies much of the water used for irrigation and aquaculture in eastern Arkansas. The map of the potentiometric surface, 5-year water-level change, and depth to water illustrates the effects of large with- drawals for irrigation on water levels in the aquifer. One large area of depression in the potentiometric surface, caused by large with- drawals of ground water for irrigation, occurs in Arkansas, Lonoke, and Prairie Counties, and another extends from Monroe County to western Craighead County.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr93374</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, spring 1992</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>