<?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:creator>J. M. Kernodle</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>As part of a multidisciplinary regional aquifer-system &#13;
analysis, a three-dimensional steady-state ground-water-flow &#13;
model was constructed for the San Juan Basin in parts of New &#13;
Mexico, Colorado, Arizona, and Utah. The model simulated ground-&#13;
water flow in 12 hydrostratigraphic units representing all of the &#13;
major sources of ground water from aquifers of Jurassic and &#13;
younger age.&#13;
&#13;
     Ten map reports in the U.S. Geological Survey Hydrologic &#13;
Investigations Atlas 720 series were prepared in conjunction with &#13;
this investigation. The units that were described in the atlases &#13;
were the San Jose, Nacimiento, and Animas Formations; Ojo Alamo &#13;
Sandstone; Kirtland Shale and Fruitland Formation; Pictured &#13;
Cliffs Sandstone; Cliff House Sandstone; Menefee Formation; Point &#13;
Lookout Sandstone; Gallup Sandstone; Dakota Sandstone; and &#13;
Morrison Formation. Additional descriptions of the alluvial and &#13;
landslide deposits, Chuska and Crevasse Canyon Sandstones, Lewis &#13;
and Mancos Shales, Wanakah Formation, and Entrada Sandstone are &#13;
included in this report. Much of the information in the HA-720 &#13;
series was generated from digital computer data bases that were &#13;
directly usable by the computer for compilation of input data for &#13;
the model. In essence, the major components of the ground-water-&#13;
flow model were described and documented in the series of &#13;
hydrologic atlases.&#13;
&#13;
     The primary finding resulting from the ground-water-flow &#13;
simulation was that boundary conditions and internal geometry of &#13;
the aquifers are the major controls of steady-state ground-water &#13;
flow and hydraulic heads in the San Juan Basin. Another &#13;
significant finding was that the computed steady-state ground-&#13;
water flux is a very minor component (about 1 percent) of the &#13;
total water budget of the basin.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/wri954187</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey, [Water Resources Division, New Mexico District] ;&#13;
Can be purchased from U.S.G.S., Branch of Information Services,</dc:publisher>
  <dc:title>Hydrogeology and steady-state simulation of ground-water flow in the San Juan Basin, New Mexico, Colorado, Arizona, and Utah</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>