https://ilstratwiki.web.illinois.edu/index.php?title=Stewartville_Member&feed=atom&action=history
Stewartville Member - Revision history
2024-03-29T12:07:47Z
Revision history for this page on the wiki
MediaWiki 1.38.4
https://ilstratwiki.web.illinois.edu/index.php?title=Stewartville_Member&diff=16692&oldid=prev
Jennifer.Obrad: IlLex moved page Stewartsville Member to Stewartville Member without leaving a redirect
2018-02-08T21:57:26Z
<p>IlLex moved page <a href="/index.php?title=Stewartsville_Member&action=edit&redlink=1" class="new" title="Stewartsville Member (page does not exist)">Stewartsville Member</a> to <a href="/wiki/Stewartville_Member" title="Stewartville Member">Stewartville Member</a> without leaving a redirect</p>
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<td colspan="1" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="1" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 21:57, 8 February 2018</td>
</tr><tr><td colspan="2" class="diff-notice" lang="en"><div class="mw-diff-empty">(No difference)</div>
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Stewartville_Member&diff=16690&oldid=prev
Jennifer.Obrad at 21:55, 8 February 2018
2018-02-08T21:55:55Z
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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 21:55, 8 February 2018</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>|tree3=Kimmswick Subgroup</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>|tree3=Kimmswick Subgroup</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>|tree4=Wise Lake Formation</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>|tree4=Wise Lake Formation</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>|tree5=<del style="font-weight: bold; text-decoration: none;">Stewartsville </del>Member</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>|tree5=<ins style="font-weight: bold; text-decoration: none;">Stewartville </ins>Member</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>|tree21=Paleozoic Erathem</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>|tree21=Paleozoic Erathem</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>===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" 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>The type section of the <del style="font-weight: bold; text-decoration: none;">Stewartsville </del>Member is located half a mile west of Stewartville, Olmstead County, Minnesota, in a quarry on the north side of the Root River, where 28 feet of dolomite in the lower part of the member is exposed (Kay, 1935a, p. 567).</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>The type section of the <ins style="font-weight: bold; text-decoration: none;">Stewartville </ins>Member is located half a mile west of Stewartville, Olmstead County, Minnesota, in a quarry on the north side of the Root River, where 28 feet of dolomite in the lower part of the member is exposed (Kay, 1935a, p. 567).</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>
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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>==Lithology==</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>==Lithology==</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>The <del style="font-weight: bold; text-decoration: none;">Stewartsville </del>Member is largely thick-bedded, pure dolomite, and many samples from the lower 10-15 feet (the Upper ''Receptaculites'' Zone) contain almost no insoluble residue. The bedding becomes thinner upward as a gradual transition to the shaly Dubuque Formation above takes place. The top of the Stewartville is placed at the lowest definitely argillaceous or shaly bedding plane. Above this position is the first occurrence of ''Pseudolingula iowensis'', which is common in the higher, more shaly part of the Dubuque Formation. The Stewartville Member is the ''Maclurea'' bed of early reports.</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>The <ins style="font-weight: bold; text-decoration: none;">Stewartville </ins>Member is largely thick-bedded, pure dolomite, and many samples from the lower 10-15 feet (the Upper ''Receptaculites'' Zone) contain almost no insoluble residue. The bedding becomes thinner upward as a gradual transition to the shaly Dubuque Formation above takes place. The top of the Stewartville is placed at the lowest definitely argillaceous or shaly bedding plane. Above this position is the first occurrence of ''Pseudolingula iowensis'', which is common in the higher, more shaly part of the Dubuque Formation. The Stewartville Member is the ''Maclurea'' bed of early reports.</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>==Core&#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>==Core&#40;s&#41;==</div></td></tr>
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Stewartville_Member&diff=15423&oldid=prev
Jennifer.Obrad at 16:45, 12 January 2017
2017-01-12T16:45:59Z
<p></p>
<p><b>New page</b></p><div>{{Editwithform}}<br />
{{Tree<br />
|category1=Paleozoic Erathem<br />
|category2=Ordovician System<br />
|category3=Trentonian Stage<br />
|category4=Tippecanoe Sequence<br />
|category5=Ottawa Limestone Megagroup<br />
|category6=Champlainian Series<br />
|category7=Galena Group<br />
|category8=Kimmswick Subgroup<br />
|category9=Wise Lake Formation<br />
|tree1=Ottawa Limestone Megagroup<br />
|tree2=Galena Group<br />
|tree3=Kimmswick Subgroup<br />
|tree4=Wise Lake Formation<br />
|tree5=Stewartsville Member<br />
|tree21=Paleozoic Erathem<br />
|tree22=Ordovician System<br />
|tree23=Champlainian Series<br />
|tree24=Trentonian Stage<br />
|tree31=Tippecanoe Sequence<br />
}}<br />
==Primary source==<br />
Willman, H. B., Elwood Atherton, T. C. Buschbach, Charles Collinson, John C. Frye, M. E. Hopkins, Jerry A. Lineback, and Jack A. Simon, 1975, Handbook of Illinois Stratigraphy: Illinois State Geological Survey Bulletin 95, 261 p.<br />
<br />
==Contributing author&#40;s&#41;==<br />
H. B. Willman and T. C. Buschbach<br />
<br />
==Name==<br />
<br />
===Original description===<br />
The Stewartville Member of the Wise Lake Formation (Ulrich, 1911, pl. 27)(originally the Stewartville Formation).<br />
<br />
===Derivation===<br />
Named for Stewartville, Olmstead County, Minnesota, which is half a mile east of the type section.<br />
<br />
===Other names===<br />
<br />
===History&#47;background===<br />
<br />
==Type section==<br />
<br />
===Type location===<br />
The type section of the Stewartsville Member is located half a mile west of Stewartville, Olmstead County, Minnesota, in a quarry on the north side of the Root River, where 28 feet of dolomite in the lower part of the member is exposed (Kay, 1935a, p. 567).<br />
<br />
===Type author&#40;s&#41;===<br />
<br />
===Type status===<br />
<br />
==Reference section==<br />
<br />
===Reference location===<br />
<br />
===Reference author&#40;s&#41;===<br />
<br />
===Reference status===<br />
<br />
==Stratigraphic relationships==<br />
The Stewartville Member is the upper member of the Wise Lake Formation.<br />
<br />
==Extent and thickness==<br />
The Stewartville Member is about 60 feet thick in the type locality, but only 30-35 feet thick in northern Illinois.<br />
<br />
==Lithology==<br />
The Stewartsville Member is largely thick-bedded, pure dolomite, and many samples from the lower 10-15 feet (the Upper ''Receptaculites'' Zone) contain almost no insoluble residue. The bedding becomes thinner upward as a gradual transition to the shaly Dubuque Formation above takes place. The top of the Stewartville is placed at the lowest definitely argillaceous or shaly bedding plane. Above this position is the first occurrence of ''Pseudolingula iowensis'', which is common in the higher, more shaly part of the Dubuque Formation. The Stewartville Member is the ''Maclurea'' bed of early reports.<br />
<br />
==Core&#40;s&#41;==<br />
<br />
==Photograph&#40;s&#41;==<br />
<br />
==Contacts==<br />
<br />
==Well log characteristics==<br />
<br />
==Fossils==<br />
<br />
==Age and correlation==<br />
<br />
==Environments of deposition==<br />
<br />
==Economic importance==<br />
<br />
==Remarks==<br />
<br />
==References==<br />
KAY, MARSHALL, 1935a, Ordovician Stewartville-Dubuque problems: Journal of Geology, v. 43, p. 541-590.<br><br />
ULRICH, E. O., 1911, Revision of the Paleozoic systems: Geological Society of America Bulletin, v. 22, p. 281-680.<br />
<br />
{{Codes<br />
|membercode=7590<br />
|geo_unit=--<br />
}}</div>
Jennifer.Obrad