https://www.conservapedia.com/index.php?action=history&feed=atom&title=Talc 2026-09-26T08:25:33Z Revision history for this page on the wiki MediaWiki 1.35.14 https://www.conservapedia.com/index.php?title=Talc&diff=1261013&oldid=prev 2016-07-13T20:03:05Z

<p><span dir="auto"><span class="autocomment">References: </span>clean up &amp; uniformity</span></p> <table class="diff diff-contentalign-left diff-editfont-monospace" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <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 20:03, July 13, 2016</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l2" >Line 2:</td> <td colspan="2" class="diff-lineno">Line 2:</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>Phyllosilicates occur when the silica tetrahedra join together to form flat sheets.  These sheets are held together by weak bonding between the free oxygen on the tetrahedra and so cleave easily.  Phyllosilicates include both micas (biotite &amp; muscovite), talc, and clay minerals.&lt;ref&gt;[http://www.museums.udel.edu/mineral/mineral_site/education/silicate/phyllo.html]&lt;/ref&gt;</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>Phyllosilicates occur when the silica tetrahedra join together to form flat sheets.  These sheets are held together by weak bonding between the free oxygen on the tetrahedra and so cleave easily.  Phyllosilicates include both micas (biotite &amp; muscovite), talc, and clay minerals.&lt;ref&gt;[http://www.museums.udel.edu/mineral/mineral_site/education/silicate/phyllo.html]&lt;/ref&gt;</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;"></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;"></td></tr> <tr><td class='diff-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 class="diffchange diffchange-inline">Reference</del>==</div></td><td class='diff-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 class="diffchange diffchange-inline">References</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>&lt;references/&gt;</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>&lt;references/&gt;</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>[[Category:Geology]]</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>[[Category:Geology]]</div></td></tr> <tr><td class='diff-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 class="diffchange diffchange-inline">category</del>:Minerals]]</div></td><td class='diff-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 class="diffchange diffchange-inline">Category</ins>:Minerals]]</div></td></tr> </table>

DavidB4-bot https://www.conservapedia.com/index.php?title=Talc&diff=292704&oldid=prev 2007-09-13T23:31:19Z

<p>start</p> <p><b>New page</b></p><div>'''Talc''' is number '''1''' on [[Mohs Hardness Scale|Mohs hardness scale]], is a phyllosilicate.&lt;br&gt;<br /> Phyllosilicates occur when the silica tetrahedra join together to form flat sheets. These sheets are held together by weak bonding between the free oxygen on the tetrahedra and so cleave easily. Phyllosilicates include both micas (biotite &amp; muscovite), talc, and clay minerals.&lt;ref&gt;[http://www.museums.udel.edu/mineral/mineral_site/education/silicate/phyllo.html]&lt;/ref&gt;<br /> <br /> ==Reference==<br /> &lt;references/&gt;<br /> [[Category:Geology]]<br /> [[category:Minerals]]</div>

Samwell