https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&feed=atom&action=history
Caseyville Formation - Revision history
2024-03-29T06:34:47Z
Revision history for this page on the wiki
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https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=19629&oldid=prev
Jennifer.Obrad: /* Primary source */
2022-02-09T16:31:49Z
<p><span dir="auto"><span class="autocomment">Primary source</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:31, 9 February 2022</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Primary source==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Primary source==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Nelson, W.J., <del style="font-weight: bold; text-decoration: none;">2020</del>, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey Bulletin (in press)<del style="font-weight: bold; text-decoration: none;">. <br></del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Nelson, W.J., <ins style="font-weight: bold; text-decoration: none;">P.H. Heckel and J.M. Obrad, 2022</ins>, Pennsylvanian Subsystem in Illinois: Illinois State Geological Survey<ins style="font-weight: bold; text-decoration: none;">, </ins>Bulletin (in press).</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Edited and figures drafted by Jennifer M. Obrad</del>.</div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Contributing author&#40;s&#41;==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Contributing author&#40;s&#41;==</div></td></tr>
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=19036&oldid=prev
Jennifer.Obrad at 21:40, 24 November 2020
2020-11-24T21:40:27Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 21:40, 24 November 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-2.jpg|250px|{{file:Penn_caseyville_2-2.jpg}}|left|thumb]]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-2.jpg|250px|{{file:Penn_caseyville_2-2.jpg}}|left|thumb]]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Railroad cuts on the Canadian National (formerly Illinois Central Gulf) Railroad from the NW¼ SW¼ SE¼, <del style="font-weight: bold; text-decoration: none;">Sec</del>. 31, T11S, R5E to NE¼ SE¼ NE¼, <del style="font-weight: bold; text-decoration: none;">Sec</del>. 18, T12S, R5E, Pope County, Illinois.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Railroad cuts on the Canadian National (formerly Illinois Central Gulf) Railroad from the NW¼ SW¼ SE¼, <ins style="font-weight: bold; text-decoration: none;">sec</ins>. 31, T11S, R5E to NE¼ SE¼ NE¼, <ins style="font-weight: bold; text-decoration: none;">sec</ins>. 18, T12S, R5E, Pope County, Illinois.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Roadcuts on Interstate 24 just south of Exit 7, in <del style="font-weight: bold; text-decoration: none;">Secs</del>. 8, 9, 16, and 17, T12S, R3E, Johnson County, Illinois.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Roadcuts on Interstate 24 just south of Exit 7, in <ins style="font-weight: bold; text-decoration: none;">secs</ins>. 8, 9, 16, and 17, T12S, R3E, Johnson County, Illinois.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Roadcuts on Interstate 57 beginning just south of Exit 36, in <del style="font-weight: bold; text-decoration: none;">Secs</del>. 24 and 25, T11S, R1E, Johnson County, Illinois.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Roadcuts on Interstate 57 beginning just south of Exit 36, in <ins style="font-weight: bold; text-decoration: none;">secs</ins>. 24 and 25, T11S, R1E, Johnson County, Illinois.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-3.jpg|250px|{{file:Penn_caseyville_2-3.jpg}}|thumb]]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-3.jpg|250px|{{file:Penn_caseyville_2-3.jpg}}|thumb]]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>A core that represents the entire Caseyville Formation is ISGS #1 Berry, drilled in <del style="font-weight: bold; text-decoration: none;">Sec</del>. 8, T9S, R3W, Jackson County, Illinois (ISGS county #26246). The Caseyville is 285.2 ft (86.9 m) thick in the Berry core, extending through a depth range from 105.1 to 390.3 ft (32 to 119 m; Figure 2-3). The upper contact is an abrupt change from clay- and iron-rich sublitharenite above to white, pure quartz arenite below. The lower contact is unconformable between conglomerate of the Caseyville and the Mississippian Kinkaid Limestone below.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>A core that represents the entire Caseyville Formation is ISGS #1 Berry, drilled in <ins style="font-weight: bold; text-decoration: none;">sec</ins>. 8, T9S, R3W, Jackson County, Illinois (ISGS county #26246). The Caseyville is 285.2 ft (86.9 m) thick in the Berry core, extending through a depth range from 105.1 to 390.3 ft (32 to 119 m; Figure 2-3). The upper contact is an abrupt change from clay- and iron-rich sublitharenite above to white, pure quartz arenite below. The lower contact is unconformable between conglomerate of the Caseyville and the Mississippian Kinkaid Limestone below.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference author&#40;s&#41;===</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=19012&oldid=prev
Jennifer.Obrad: /* Primary source */
2020-07-20T21:32:47Z
<p><span dir="auto"><span class="autocomment">Primary source</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 21:32, 20 July 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Primary source==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Primary source==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Nelson, W.J., <del style="font-weight: bold; text-decoration: none;">2018</del>, Pennsylvanian Subsystem in Illinois. Edited and figures drafted by Jennifer M. Obrad<del style="font-weight: bold; text-decoration: none;">. Illinois State Geological Survey Bulletin (in press)</del>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Nelson, W.J., <ins style="font-weight: bold; text-decoration: none;">2020</ins>, Pennsylvanian Subsystem in Illinois<ins style="font-weight: bold; text-decoration: none;">: Illinois State Geological Survey Bulletin (in press)</ins>. <ins style="font-weight: bold; text-decoration: none;"><br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Edited and figures drafted by Jennifer M. Obrad.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Contributing author&#40;s&#41;==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Contributing author&#40;s&#41;==</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=18947&oldid=prev
Jennifer.Obrad at 19:31, 16 July 2020
2020-07-16T19:31:18Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 19:31, 16 July 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-1.jpg|<del style="font-weight: bold; text-decoration: none;">right</del>|<del style="font-weight: bold; text-decoration: none;">thumb|Figure 2-1. Map showing the type area of the Caseyville Formation and several of its members. Map drafted by Alan Myers. Base is a U.S. Geological Survey Dekoven 7.5-minute topographic map. Base map courtesy of the U.S. Geological Survey.]]</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-1.jpg|<ins style="font-weight: bold; text-decoration: none;">250px</ins>|<ins style="font-weight: bold; text-decoration: none;">{{</ins>file:Penn_caseyville_2-<ins style="font-weight: bold; text-decoration: none;">1</ins>.jpg<ins style="font-weight: bold; text-decoration: none;">}}</ins>|thumb]]</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[[</del>file:Penn_caseyville_2-<del style="font-weight: bold; text-decoration: none;">2</del>.jpg<del style="font-weight: bold; text-decoration: none;">|right</del>|thumb<del style="font-weight: bold; text-decoration: none;">|Figure 2-2. Graphic columns of the Caseyville type section and three reference sections. Column 1 after Lee (1916). Used courtesy of the Kentucky Geological Survey. Columns 2 to 4 from Kosanke et al. (1960); Palmer and Dutcher (1979) and unpublished field notes by W.J. Nelson and J.T. Popp; and Nelson and Weibel (1996) and unpublished field notes by W.J. Nelson, respectively. Copyright © 1960, 1979, and 1996 University of Illinois Board of Trustees.</del>]]</div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Reference section (1)==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Reference section (1)==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[file:Penn_caseyville_2-2.jpg|250px|{{file:Penn_caseyville_2-2.jpg}}|left|thumb]]</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Railroad cuts on the Canadian National (formerly Illinois Central Gulf) Railroad from the NW¼ SW¼ SE¼, Sec. 31, T11S, R5E to NE¼ SE¼ NE¼, Sec. 18, T12S, R5E, Pope County, Illinois.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Railroad cuts on the Canadian National (formerly Illinois Central Gulf) Railroad from the NW¼ SW¼ SE¼, Sec. 31, T11S, R5E to NE¼ SE¼ NE¼, Sec. 18, T12S, R5E, Pope County, Illinois.</div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Reference section (4)==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Reference section (4)==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-3.jpg|<del style="font-weight: bold; text-decoration: none;">thumb</del>|<del style="font-weight: bold; text-decoration: none;">Figure 2</del>-3. <del style="font-weight: bold; text-decoration: none;">Graphic log based on continuous core from Illinois State Geological Survey #1 Berry test hole in Sec. 8, T9S, R3W, Jackson County, Illinois. This is a reference section for the Caseyville Formation. QA = quartz arenite</del>]]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-3.jpg|<ins style="font-weight: bold; text-decoration: none;">250px</ins>|<ins style="font-weight: bold; text-decoration: none;">{{file:Penn_caseyville_2</ins>-3.<ins style="font-weight: bold; text-decoration: none;">jpg}}|thumb</ins>]]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Reference location===</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A core that represents the entire Caseyville Formation is ISGS #1 Berry, drilled in Sec. 8, T9S, R3W, Jackson County, Illinois (ISGS county #26246). The Caseyville is 285.2 ft (86.9 m) thick in the Berry core, extending through a depth range from 105.1 to 390.3 ft (32 to 119 m; Figure 2-3). The upper contact is an abrupt change from clay- and iron-rich sublitharenite above to white, pure quartz arenite below. The lower contact is unconformable between conglomerate of the Caseyville and the Mississippian Kinkaid Limestone below.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A core that represents the entire Caseyville Formation is ISGS #1 Berry, drilled in Sec. 8, T9S, R3W, Jackson County, Illinois (ISGS county #26246). The Caseyville is 285.2 ft (86.9 m) thick in the Berry core, extending through a depth range from 105.1 to 390.3 ft (32 to 119 m; Figure 2-3). The upper contact is an abrupt change from clay- and iron-rich sublitharenite above to white, pure quartz arenite below. The lower contact is unconformable between conglomerate of the Caseyville and the Mississippian Kinkaid Limestone below.</div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Extent and thickness==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Extent and thickness==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-4.jpg|<del style="font-weight: bold; text-decoration: none;">left|thumb</del>|<del style="font-weight: bold; text-decoration: none;">Figure 2</del>-4. <del style="font-weight: bold; text-decoration: none;">Isopach map of Morrowan Stage, which essentially corresponds to the Caseyville Formation in the Illinois Basin. From Nelson et al. (2013), after McKee and Crosby (1975), Gray et al. (1987), Greb et al. (1992), and Droste and Furer (1995). Copyright permission granted by Micropress, 2020.</del>]]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-4.jpg|<ins style="font-weight: bold; text-decoration: none;">250px</ins>|<ins style="font-weight: bold; text-decoration: none;">{{file:Penn_caseyville_2</ins>-4.<ins style="font-weight: bold; text-decoration: none;">jpg}}|left|thumb</ins>]]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Owing to the difficulty of identifying the top of the Caseyville Formation in the subsurface, the thickness and lithofacies of the formation have not been mapped in detail from well data. Small-scale maps that depict the thickness of roughly the Caseyville interval appear in McKee and Crosby (1975, Plate 3A), Greb et al. (1992, Figure 15), Droste and Furer (1995, Figure 4), and Droste and Horowitz (1998, Figure 4). Compiled from these sources, the map shown here (Figure 2-4) is essentially an isopach map of the Caseyville.<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Owing to the difficulty of identifying the top of the Caseyville Formation in the subsurface, the thickness and lithofacies of the formation have not been mapped in detail from well data. Small-scale maps that depict the thickness of roughly the Caseyville interval appear in McKee and Crosby (1975, Plate 3A), Greb et al. (1992, Figure 15), Droste and Furer (1995, Figure 4), and Droste and Horowitz (1998, Figure 4). Compiled from these sources, the map shown here (Figure 2-4) is essentially an isopach map of the Caseyville.<br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Quad Cities outlier is called Caseyville Formation because its lithology and age are similar to the type Caseyville (Ravn et al. 1984; Ravn 1986; Isbell 1985). Outcrops occur within and west of the Quad Cities in Mercer and Rock Island Counties, Illinois, and Muscatine and Scott Counties, Iowa. As in the southern part of the basin, Caseyville sandstones of the northwestern outlier are quartz arenites; however, quartz granules are rare. Shale, siltstone, and at least three coal layers make up the rest of the formation. These rocks have a maximum observed thickness of 100 ft (30 m) and are overlain unconformably by lower Desmoinesian rocks of the upper [[Tradewater Formation]]. The Caseyville of the Quad Cities area has been established as Morrowan age via palynology of its coal beds (Ravn and Fitzgerald 1982; Ravn et al. 1984).<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Quad Cities outlier is called Caseyville Formation because its lithology and age are similar to the type Caseyville (Ravn et al. 1984; Ravn 1986; Isbell 1985). Outcrops occur within and west of the Quad Cities in Mercer and Rock Island Counties, Illinois, and Muscatine and Scott Counties, Iowa. As in the southern part of the basin, Caseyville sandstones of the northwestern outlier are quartz arenites; however, quartz granules are rare. Shale, siltstone, and at least three coal layers make up the rest of the formation. These rocks have a maximum observed thickness of 100 ft (30 m) and are overlain unconformably by lower Desmoinesian rocks of the upper [[Tradewater Formation]]. The Caseyville of the Quad Cities area has been established as Morrowan age via palynology of its coal beds (Ravn and Fitzgerald 1982; Ravn et al. 1984).<br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-5.jpg|<del style="font-weight: bold; text-decoration: none;">thumb</del>|<del style="font-weight: bold; text-decoration: none;">Figure 2</del>-5. <del style="font-weight: bold; text-decoration: none;">Map showing where the Caseyville Formation crops out in Illinois and where the formation has been identified in the subsurface. Map drafted by Alan Myers.</del>]]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[file:Penn_caseyville_2-5.jpg|<ins style="font-weight: bold; text-decoration: none;">250px</ins>|<ins style="font-weight: bold; text-decoration: none;">{{file:Penn_caseyville_2</ins>-5.<ins style="font-weight: bold; text-decoration: none;">jpg}}|thumb</ins>]]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A few authors have described Caseyville strata in the subsurface of Illinois. Lowenstam (1951, p. 45–46) reported Caseyville sandstone and quartz-pebble conglomerate occupying what is now known to be a paleochannel cut into the Mississippian surface in the Bible Grove area of Clay County (Figure 2-5). Winslow (1959) identified Caseyville-age fossil spores in drill cores from the Allendale oil field in northern Wabash County (Figure 2-5). Although not identified as “Caseyville,” the quartz-rich sandstone serving as an oil reservoir in the Hardinville field of Crawford County (Figure 2-5) probably represents this formation. Sealed by overlying shale, the productive sandstone lies at the bottom of a sub-Pennsylvanian paleovalley (Howard and Whitaker 1988). Using limited palynological control, Droste et al. (2000) published a series of generalized maps and cross sections showing Morrowan (Caseyville age) depositional patterns in part of the Illinois Basin.<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A few authors have described Caseyville strata in the subsurface of Illinois. Lowenstam (1951, p. 45–46) reported Caseyville sandstone and quartz-pebble conglomerate occupying what is now known to be a paleochannel cut into the Mississippian surface in the Bible Grove area of Clay County (Figure 2-5). Winslow (1959) identified Caseyville-age fossil spores in drill cores from the Allendale oil field in northern Wabash County (Figure 2-5). Although not identified as “Caseyville,” the quartz-rich sandstone serving as an oil reservoir in the Hardinville field of Crawford County (Figure 2-5) probably represents this formation. Sealed by overlying shale, the productive sandstone lies at the bottom of a sub-Pennsylvanian paleovalley (Howard and Whitaker 1988). Using limited palynological control, Droste et al. (2000) published a series of generalized maps and cross sections showing Morrowan (Caseyville age) depositional patterns in part of the Illinois Basin.<br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=18946&oldid=prev
Jennifer.Obrad: Undo revision 18931 by IlLex (talk)
2020-07-16T18:52:53Z
<p>Undo revision 18931 by <a href="/wiki/Special:Contributions/IlLex" title="Special:Contributions/IlLex">IlLex</a> (<a href="/index.php?title=User_talk:IlLex&action=edit&redlink=1" class="new" title="User talk:IlLex (page does not exist)">talk</a>)</p>
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<tr class="diff-title" lang="en">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 18:52, 16 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l35">Line 35:</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[file:Penn_caseyville_2-1.jpg|right|thumb|Figure 2-1. Map showing the type area of the Caseyville Formation and several of its members. Map drafted by Alan Myers. Base is a U.S. Geological Survey Dekoven 7.5-minute topographic map. Base map courtesy of the U.S. Geological Survey.]]</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[file:Penn_caseyville_2-2.jpg|right|thumb|Figure 2-2. Graphic columns of the Caseyville type section and three reference sections. Column 1 after Lee (1916). Used courtesy of the Kentucky Geological Survey. Columns 2 to 4 from Kosanke et al. (1960); Palmer and Dutcher (1979) and unpublished field notes by W.J. Nelson and J.T. Popp; and Nelson and Weibel (1996) and unpublished field notes by W.J. Nelson, respectively. Copyright © 1960, 1979, and 1996 University of Illinois Board of Trustees.]]</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The type section was “measured from outcrops on the Illinois shore of the Ohio River between the mouth of the Saline River and Gentry’s Landing below Battery Rock” in Hardin County, Illinois (Lee 1916, p. 15; Figure 2-1).</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The type section was “measured from outcrops on the Illinois shore of the Ohio River between the mouth of the Saline River and Gentry’s Landing below Battery Rock” in Hardin County, Illinois (Lee 1916, p. 15; Figure 2-1).</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"><center></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">{| class="wikitable" style="text-align: center;"</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">|-</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">|<gallery caption="" widths=250px heights=250px perrow=4></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-1.jpg|{{file:Penn_caseyville_2-1.jpg}}</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-2.jpg|{{file:Penn_caseyville_2-2.jpg}}</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></gallery></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">|}</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></center></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type author&#40;s&#41;===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type author&#40;s&#41;===</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=18931&oldid=prev
Jennifer.Obrad: /* Type section */
2020-07-16T17:26:35Z
<p><span dir="auto"><span class="autocomment">Type section</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 17:26, 16 July 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[[file:Penn_caseyville_2-1.jpg|right|thumb|Figure 2-1. Map showing the type area of the Caseyville Formation and several of its members. Map drafted by Alan Myers. Base is a U.S. Geological Survey Dekoven 7.5-minute topographic map. Base map courtesy of the U.S. Geological Survey.]]</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[[file:Penn_caseyville_2-2.jpg|right|thumb|Figure 2-2. Graphic columns of the Caseyville type section and three reference sections. Column 1 after Lee (1916). Used courtesy of the Kentucky Geological Survey. Columns 2 to 4 from Kosanke et al. (1960); Palmer and Dutcher (1979) and unpublished field notes by W.J. Nelson and J.T. Popp; and Nelson and Weibel (1996) and unpublished field notes by W.J. Nelson, respectively. Copyright © 1960, 1979, and 1996 University of Illinois Board of Trustees.]]</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The type section was “measured from outcrops on the Illinois shore of the Ohio River between the mouth of the Saline River and Gentry’s Landing below Battery Rock” in Hardin County, Illinois (Lee 1916, p. 15; Figure 2-1).</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The type section was “measured from outcrops on the Illinois shore of the Ohio River between the mouth of the Saline River and Gentry’s Landing below Battery Rock” in Hardin County, Illinois (Lee 1916, p. 15; Figure 2-1).</div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><center></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">{| class="wikitable" style="text-align: center;"</ins></div></td></tr>
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<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">|<gallery caption="" widths=250px heights=250px perrow=4></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-1.jpg|{{file:Penn_caseyville_2-1.jpg}}</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-2.jpg|{{file:Penn_caseyville_2-2.jpg}}</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"></gallery></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">|}</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"></center></ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type author&#40;s&#41;===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type author&#40;s&#41;===</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=18930&oldid=prev
Jennifer.Obrad: /* Type section */
2020-07-16T17:21:22Z
<p><span dir="auto"><span class="autocomment">Type section</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 17:21, 16 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l35">Line 35:</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-1.jpg|{{</del>file:Penn_caseyville_2-1.jpg<del style="font-weight: bold; text-decoration: none;">}}</del>|thumb|<del style="font-weight: bold; text-decoration: none;">right</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[</ins>file:Penn_caseyville_2-1.jpg<ins style="font-weight: bold; text-decoration: none;">|right</ins>|thumb|<ins style="font-weight: bold; text-decoration: none;">Figure 2-1. Map showing the type area of the Caseyville Formation and several of its members. Map drafted by Alan Myers. Base is a U.S. Geological Survey Dekoven 7.5</ins>-<ins style="font-weight: bold; text-decoration: none;">minute topographic map. Base map courtesy of the U.S. Geological Survey</ins>.<ins style="font-weight: bold; text-decoration: none;">]]</ins></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Penn_caseyville_2</del>-<del style="font-weight: bold; text-decoration: none;">2</del>.<del style="font-weight: bold; text-decoration: none;">jpg|{{</del>file:Penn_caseyville_2-2.jpg<del style="font-weight: bold; text-decoration: none;">}}</del>|thumb|<del style="font-weight: bold; text-decoration: none;">right</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[</ins>file:Penn_caseyville_2-2.jpg<ins style="font-weight: bold; text-decoration: none;">|right</ins>|thumb|<ins style="font-weight: bold; text-decoration: none;">Figure 2-2. Graphic columns of the Caseyville type section and three reference sections. Column 1 after Lee (1916). Used courtesy of the Kentucky Geological Survey. Columns 2 to 4 from Kosanke et al. (1960); Palmer and Dutcher (1979) and unpublished field notes by W.J. Nelson and J.T. Popp; and Nelson and Weibel (1996) and unpublished field notes by W.J. Nelson, respectively. Copyright © 1960, 1979, and 1996 University of Illinois Board of Trustees.]]</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=18929&oldid=prev
Jennifer.Obrad: /* Type section */
2020-07-16T17:20:50Z
<p><span dir="auto"><span class="autocomment">Type section</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 17:20, 16 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l35">Line 35:</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Type section==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[[</del>file:Penn_caseyville_2-1.jpg<del style="font-weight: bold; text-decoration: none;">|right</del>|thumb|<del style="font-weight: bold; text-decoration: none;">Figure </del>2<del style="font-weight: bold; text-decoration: none;">-1</del>. <del style="font-weight: bold; text-decoration: none;">Map showing the type area of the Caseyville Formation and several of its members. Map drafted by Alan Myers. Base is a U.S. Geological Survey Dekoven 7.5-minute topographic map. Base map courtesy of the U.S. Geological Survey.]]</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-1.jpg|{{</ins>file:Penn_caseyville_2-1.jpg<ins style="font-weight: bold; text-decoration: none;">}}</ins>|thumb|<ins style="font-weight: bold; text-decoration: none;">right</ins></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[[</del>file:Penn_caseyville_2-2.jpg<del style="font-weight: bold; text-decoration: none;">|right</del>|thumb|<del style="font-weight: bold; text-decoration: none;">Figure 2-2. Graphic columns of the Caseyville type section and three reference sections. Column 1 after Lee (1916). Used courtesy of the Kentucky Geological Survey. Columns 2 to 4 from Kosanke et al. (1960); Palmer and Dutcher (1979) and unpublished field notes by W.J. Nelson and J.T. Popp; and Nelson and Weibel (1996) and unpublished field notes by W.J. Nelson, respectively. Copyright © 1960, 1979, and 1996 University of Illinois Board of Trustees.]]</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-</ins>2.<ins style="font-weight: bold; text-decoration: none;">jpg|{{</ins>file:Penn_caseyville_2-2.jpg<ins style="font-weight: bold; text-decoration: none;">}}</ins>|thumb|<ins style="font-weight: bold; text-decoration: none;">right</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Type location===</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=18925&oldid=prev
Jennifer.Obrad: /* Extent and thickness */
2020-07-15T22:18:54Z
<p><span dir="auto"><span class="autocomment">Extent and thickness</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:18, 15 July 2020</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l106">Line 106:</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Quad Cities outlier is called Caseyville Formation because its lithology and age are similar to the type Caseyville (Ravn et al. 1984; Ravn 1986; Isbell 1985). Outcrops occur within and west of the Quad Cities in Mercer and Rock Island Counties, Illinois, and Muscatine and Scott Counties, Iowa. As in the southern part of the basin, Caseyville sandstones of the northwestern outlier are quartz arenites; however, quartz granules are rare. Shale, siltstone, and at least three coal layers make up the rest of the formation. These rocks have a maximum observed thickness of 100 ft (30 m) and are overlain unconformably by lower Desmoinesian rocks of the upper [[Tradewater Formation]]. The Caseyville of the Quad Cities area has been established as Morrowan age via palynology of its coal beds (Ravn and Fitzgerald 1982; Ravn et al. 1984).<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Quad Cities outlier is called Caseyville Formation because its lithology and age are similar to the type Caseyville (Ravn et al. 1984; Ravn 1986; Isbell 1985). Outcrops occur within and west of the Quad Cities in Mercer and Rock Island Counties, Illinois, and Muscatine and Scott Counties, Iowa. As in the southern part of the basin, Caseyville sandstones of the northwestern outlier are quartz arenites; however, quartz granules are rare. Shale, siltstone, and at least three coal layers make up the rest of the formation. These rocks have a maximum observed thickness of 100 ft (30 m) and are overlain unconformably by lower Desmoinesian rocks of the upper [[Tradewater Formation]]. The Caseyville of the Quad Cities area has been established as Morrowan age via palynology of its coal beds (Ravn and Fitzgerald 1982; Ravn et al. 1984).<br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[file:Penn_caseyville_2-5.jpg|thumb|Figure 2-5. Map showing where the Caseyville Formation crops out in Illinois and where the formation has been identified in the subsurface. Map drafted by Alan Myers.]]</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A few authors have described Caseyville strata in the subsurface of Illinois. Lowenstam (1951, p. 45–46) reported Caseyville sandstone and quartz-pebble conglomerate occupying what is now known to be a paleochannel cut into the Mississippian surface in the Bible Grove area of Clay County (Figure 2-5). Winslow (1959) identified Caseyville-age fossil spores in drill cores from the Allendale oil field in northern Wabash County (Figure 2-5). Although not identified as “Caseyville,” the quartz-rich sandstone serving as an oil reservoir in the Hardinville field of Crawford County (Figure 2-5) probably represents this formation. Sealed by overlying shale, the productive sandstone lies at the bottom of a sub-Pennsylvanian paleovalley (Howard and Whitaker 1988). Using limited palynological control, Droste et al. (2000) published a series of generalized maps and cross sections showing Morrowan (Caseyville age) depositional patterns in part of the Illinois Basin.<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A few authors have described Caseyville strata in the subsurface of Illinois. Lowenstam (1951, p. 45–46) reported Caseyville sandstone and quartz-pebble conglomerate occupying what is now known to be a paleochannel cut into the Mississippian surface in the Bible Grove area of Clay County (Figure 2-5). Winslow (1959) identified Caseyville-age fossil spores in drill cores from the Allendale oil field in northern Wabash County (Figure 2-5). Although not identified as “Caseyville,” the quartz-rich sandstone serving as an oil reservoir in the Hardinville field of Crawford County (Figure 2-5) probably represents this formation. Sealed by overlying shale, the productive sandstone lies at the bottom of a sub-Pennsylvanian paleovalley (Howard and Whitaker 1988). Using limited palynological control, Droste et al. (2000) published a series of generalized maps and cross sections showing Morrowan (Caseyville age) depositional patterns in part of the Illinois Basin.<br></div></td></tr>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></gallery></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></center></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>During the 1990s, Russell Jacobson and I constructed a network of subsurface cross sections of Caseyville and [[Tradewater Formation|Tradewater]] strata in southern Illinois. Starting from the outcrop and the few available cores, we tried to extend correlations into the deep Fairfield basin by using geophysical logs supplemented by sample studies in which special attention was paid to the character of the sandstone. T. Michael Whitsett carried out a similar investigation in western Kentucky with the cooperation of the Kentucky Geological Survey. Through our collective efforts, we determined that with sufficient attention to samples, the Caseyville–Tradewater contact could be approximated in the subsurface and that depositional packages or sequences could be correlated across distances of 5 to 10 mi (~8 to 16 km) and occasionally farther. We were unable to develop any means for distinguishing the Caseyville from the Tradewater solely from geophysical logs, and we failed to trace any named members of the Caseyville or lower Tradewater more than a few miles from their type localities. The cross sections we developed remain unpublished in ISGS archives.<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>During the 1990s, Russell Jacobson and I constructed a network of subsurface cross sections of Caseyville and [[Tradewater Formation|Tradewater]] strata in southern Illinois. Starting from the outcrop and the few available cores, we tried to extend correlations into the deep Fairfield basin by using geophysical logs supplemented by sample studies in which special attention was paid to the character of the sandstone. T. Michael Whitsett carried out a similar investigation in western Kentucky with the cooperation of the Kentucky Geological Survey. Through our collective efforts, we determined that with sufficient attention to samples, the Caseyville–Tradewater contact could be approximated in the subsurface and that depositional packages or sequences could be correlated across distances of 5 to 10 mi (~8 to 16 km) and occasionally farther. We were unable to develop any means for distinguishing the Caseyville from the Tradewater solely from geophysical logs, and we failed to trace any named members of the Caseyville or lower Tradewater more than a few miles from their type localities. The cross sections we developed remain unpublished in ISGS archives.<br></div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Caseyville_Formation&diff=18923&oldid=prev
Jennifer.Obrad: /* Extent and thickness */
2020-07-15T22:15:16Z
<p><span dir="auto"><span class="autocomment">Extent and thickness</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:15, 15 July 2020</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Extent and thickness==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Extent and thickness==</div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[file:Penn_caseyville_2-4.jpg|left|thumb|Figure 2-4. Isopach map of Morrowan Stage, which essentially corresponds to the Caseyville Formation in the Illinois Basin. From Nelson et al. (2013), after McKee and Crosby (1975), Gray et al. (1987), Greb et al. (1992), and Droste and Furer (1995). Copyright permission granted by Micropress, 2020.]]</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Owing to the difficulty of identifying the top of the Caseyville Formation in the subsurface, the thickness and lithofacies of the formation have not been mapped in detail from well data. Small-scale maps that depict the thickness of roughly the Caseyville interval appear in McKee and Crosby (1975, Plate 3A), Greb et al. (1992, Figure 15), Droste and Furer (1995, Figure 4), and Droste and Horowitz (1998, Figure 4). Compiled from these sources, the map shown here (Figure 2-4) is essentially an isopach map of the Caseyville.<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Owing to the difficulty of identifying the top of the Caseyville Formation in the subsurface, the thickness and lithofacies of the formation have not been mapped in detail from well data. Small-scale maps that depict the thickness of roughly the Caseyville interval appear in McKee and Crosby (1975, Plate 3A), Greb et al. (1992, Figure 15), Droste and Furer (1995, Figure 4), and Droste and Horowitz (1998, Figure 4). Compiled from these sources, the map shown here (Figure 2-4) is essentially an isopach map of the Caseyville.<br></div></td></tr>
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<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Penn_caseyville_2-4.jpg|{{file:Penn_caseyville_2-4.jpg}}</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>These maps indicate that the Caseyville Formation and equivalent strata lie largely southeast of a line that runs from Vigo County in west-central Indiana to Randolph County in southwestern Illinois. Northwest of this line, Caseyville rocks are largely confined to paleovalleys on the sub-Pennsylvanian surface. A sizeable outlier of the Caseyville occurs in the Quad Cities area in northwestern Illinois and adjacent Iowa.<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>These maps indicate that the Caseyville Formation and equivalent strata lie largely southeast of a line that runs from Vigo County in west-central Indiana to Randolph County in southwestern Illinois. Northwest of this line, Caseyville rocks are largely confined to paleovalleys on the sub-Pennsylvanian surface. A sizeable outlier of the Caseyville occurs in the Quad Cities area in northwestern Illinois and adjacent Iowa.<br></div></td></tr>
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Jennifer.Obrad