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<table class=3DMsoNormalTable border=3D0 cellpadding=3D0 width=3D"95%"
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 <tr style=3D'mso-yfti-irow:0;mso-yfti-firstrow:yes'>
  <td colspan=3D2 style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><b>Paper No. 13-12</b><o:p></o:p></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:1'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><b>Presentation Time:</b> 5:00 PM-9:00 PM<o:p></o:p>=
</p>
  </td>
<!--abstract-->
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:2'>
  <td colspan=3D3 style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'><!--Interes=
tPaper50091-->
  <p class=3DMsoNormal><b><i><span style=3D'font-size:18.0pt;font-family:Ar=
ial'>HYDROSTRATIGRAPHIC
  CHARACTERIZATION OF THE PATOKA AND SHELBURN AQUIFER SYSTEMS IN <st1:place
  w:st=3D"on">SOUTHWESTERN INDIANA</st1:place></span></i></b><o:p></o:p></p>
  </td>
 </tr>
<!--/abstract-->
 <tr style=3D'mso-yfti-irow:3'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'><!--abstract-->
  <p class=3DMsoNormal><b><a href=3D"mailto:pdoss@usi.edu">ELPERS, Gena</a>=
</b>, WALTON,
  <span class=3DSpellE>Carly</span>, DOSS, Paul K., and MAASBERG, <span
  class=3DSpellE>Kieth</span>, Geology and Physics, <span class=3DSpellE>Un=
iv</span>
  of Southern Indiana, 8600 Univ. Blvd, Evansville, IN 47712, pdoss@usi.edu=
 <o:p></o:p></p>
  <p>The Inglefield sandstone member of the Pennsylvanian Patoka Formation =
and
  the Shelburn Formation are the primary aquifers for domestic water supply=
 in
  southwestern <st1:State w:st=3D"on"><st1:place w:st=3D"on">Indiana</st1:p=
lace></st1:State>.
  The objectives of this study were to generate conceptual models of the
  regional <span class=3DSpellE>hydrostratigraphy</span>, and to produce
  potentiometric maps of these aquifer horizons. The study used water level=
s,
  ground elevations, and stratigraphic data from logs of wells drilled over=
 a
  forty-year period in <st1:place w:st=3D"on"><st1:City w:st=3D"on">Southwe=
stern
    Vanderburgh County</st1:City>, <st1:State w:st=3D"on">Indiana</st1:Stat=
e></st1:place>
  to construct cross-sections and potentiometric maps. Map locations, well
  depths, and analyses of basal <span class=3DSpellE>stratigraphy</span>
  identified the specific aquifer horizon for each well. Water levels measu=
red
  in wells that were screened in the Patoka Formation during the ten wettest
  and ten driest years of the forty-year period were used to construct
  potentiometric maps. These maps suggest a local recharge zone that parall=
els
  the <st1:place w:st=3D"on">Ohio River</st1:place> valley, and is nearly
  coincident with areas of recent and rapid commercial development.
  Potentiometric maps need to be constructed using current and synchronous
  water-level data to verify recharge and discharge zones. Constructed
  cross-sections identified high-angle normal faults beneath the research a=
rea,
  as indicated by offsets in the West Franklin Limestone; the West Franklin
  Limestone separates the Patoka and Shelburn aquifers. In addition to pote=
ntial
  <span class=3DSpellE>hydrostratigraphic</span> implications of these faul=
ts,
  their identification may have bearing on seismic studies of the Wabash Va=
lley
  Seismic Zone. This study has provided a working conceptual model to furth=
er
  design investigations of the stratigraphic, hydrogeologic, and water-qual=
ity
  characteristics of the Patoka and Shelburn aquifer horizons in and around=
 <st1:place
  w:st=3D"on"><st1:City w:st=3D"on">Evansville</st1:City>, <st1:State w:st=
=3D"on">IN.</st1:State></st1:place>
  <!--Abstract 50091 modified by 216.135.6.140 on 12-10-2002--><!--/abstrac=
t--><o:p></o:p></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:4'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><a
  href=3D"http://gsa.confex.com/gsa/2003NC/finalprogram/index.html">North-C=
entral
  Section - 37th Annual Meeting (March 24&#8211;25, 2003)</a> <br>
  <a href=3D"http://www.geosociety.org/sectdiv/northc/03ncmtg.htm" target=
=3Dnew>General
  Information for this Meeting</a> <o:p></o:p></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:5'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'><!--info-->
  <p class=3DMsoNormal>Session No. 13--Booth# 12<br>
  <a href=3D"http://gsa.confex.com/gsa/2003NC/finalprogram/session_3541.htm=
">Showcase
  of Undergraduates (Posters)</a><br>
<st1:PlaceName w:st=3D"on">Kansas City</st1:PlaceName> <st1:PlaceType w:st=
=3D"on">Airport</st1:PlaceType>
  Hilton: <st1:City w:st=3D"on"><st1:place w:st=3D"on">Shawnee</st1:place><=
/st1:City>
  A<br>
  5:00 PM-9:00 PM, Monday, March 24, 2003<o:p></o:p></p>
<!--/info--></td>
<!--hideinscheduler-->
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
 </tr>
 <tr style=3D'mso-yfti-irow:6'>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal>&nbsp;<o:p></o:p></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
  <td style=3D'padding:3.75pt 3.75pt 3.75pt 3.75pt'>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'><o:p>&nbsp;</o:p></=
span></p>
  </td>
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  <div class=3DMsoNormal align=3Dcenter style=3D'text-align:center'>
  <hr size=3D2 width=3D"100%" align=3Dcenter>
  </div>
  <p class=3DMsoNormal><span style=3D'font-size:10.0pt'>&copy; Copyright 20=
03 The
  Geological Society of <st1:country-region w:st=3D"on"><st1:place w:st=3D"=
on">America</st1:place></st1:country-region>
  (GSA), all rights reserved. Permission <span class=3DGramE>is hereby gran=
ted</span>
  to the author(s) of this abstract to reproduce and distribute it freely, =
for
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