https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&feed=atom&action=history
Cascadia subduction zone - Revision history
2024-03-28T18:06:38Z
Revision history for this page on the wiki
MediaWiki 1.40.1
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=10882&oldid=prev
WikiMaster: Transclude intro.
2011-09-04T15:06:17Z
<p>Transclude intro.</p>
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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 08:06, 4 September 2011</td>
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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;">[</del>http://en.wikipedia.org/wiki/<del style="font-weight: bold; text-decoration: none;">Cascadia_subduction_zone </del>The Cascadia Subduction Zone] stretches from northern Vancouver Island to northern California. It is a very long sloping fault that separates the [<del style="font-weight: bold; text-decoration: none;">http</del>:<del style="font-weight: bold; text-decoration: none;">//en.wikipedia.org/wiki/Juan_de_Fuca_Plate </del>Juan de Fuca plate] and [<del style="font-weight: bold; text-decoration: none;">http</del>:<del style="font-weight: bold; text-decoration: none;">//en.wikipedia.org/wiki/North_American_Plate </del>North America plates].</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;"><section begin=Cascadia subduction zone intro /> <!-- Begins transcluded content. Please do not remove; will disrupt content transclusions to other pages. More info: </ins>http://en.wikipedia.org/wiki/<ins style="font-weight: bold; text-decoration: none;">Transclusion --></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;">[[wikipedia:Cascadia subduction zone|</ins>The Cascadia Subduction Zone<ins style="font-weight: bold; text-decoration: none;">]</ins>] stretches from northern Vancouver Island to northern California. It is a very long sloping fault that separates the [<ins style="font-weight: bold; text-decoration: none;">[wikipedia</ins>:<ins style="font-weight: bold; text-decoration: none;">Juan de Fuca Plate|</ins>Juan de Fuca plate<ins style="font-weight: bold; text-decoration: none;">]</ins>] and [<ins style="font-weight: bold; text-decoration: none;">[wikipedia</ins>:<ins style="font-weight: bold; text-decoration: none;">North American Plate|</ins>North America plates<ins style="font-weight: bold; text-decoration: none;">]</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" 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;">[http://www.ccalmr.ogi.edu/tsunami The </del>Cascadia Subduction Zone Quake<del style="font-weight: bold; text-decoration: none;">] </del>will generate two Tsunami waves, one propagating towards the coast, and the other towards the deep ocean [http://www.tsunami.org/ <del style="font-weight: bold; text-decoration: none;">and Hawaii</del>]<del style="font-weight: bold; text-decoration: none;">. </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;">A </ins>Cascadia Subduction Zone Quake will generate two Tsunami waves, one propagating towards the coast, and the other towards the deep ocean <ins style="font-weight: bold; text-decoration: none;">and Hawaii.<ref>[http://www.stccmop.org/tsunami/ Center for Coastal And Land-Margin Research] - Science for Society: Impact of tsunamis on Oregon coastal communities</ref><ref></ins>[http://www.tsunami.org/ <ins style="font-weight: bold; text-decoration: none;">Pacific Tsunami Museum</ins>]<ins style="font-weight: bold; text-decoration: none;"></ref></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" 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>It will take only minutes to reach the coasts of Oregon, Washington, southern British Columbia, and northern California with wave heights reaching close to 12m (~36ft) in some scenarios. </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>It will take only minutes to reach the coasts of Oregon, Washington, southern British Columbia, and northern California with wave heights reaching close to 12m (~36ft) in some scenarios.</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;"><section end=Cascadia subduction zone intro /> <!-- Ends transcluded content. Please do not remove; will disrupt content transclusions to other pages. More info: http://en.wikipedia.org/wiki/Transclusion --></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>[[File:Cascadia.subductionzone.jpg|center|Cascadia Subduction Zone]]</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:Cascadia.subductionzone.jpg|center|Cascadia Subduction Zone]]</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>* [http://vearthquake.calstatela.edu/edesktop/VirtApps/VirtualEarthQuake/VQuakeExecute.html Virtual Earth Quake]</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>* [http://vearthquake.calstatela.edu/edesktop/VirtApps/VirtualEarthQuake/VQuakeExecute.html Virtual Earth Quake]</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>* [http://www.isc.ac.uk/ International Seismological Centre]</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>* [http://www.isc.ac.uk/ International Seismological Centre]</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></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;"><div>* [http://earthquake.usgs.gov/earthquakes/recenteqsww/ USGS Global Quake Map]</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>* [http://earthquake.usgs.gov/earthquakes/recenteqsww/ USGS Global Quake Map]</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>* [http://wiki.openstreetmap.org/wiki/2011_Sendai_earthquake_and_tsunami OpenStreetMap: Sendai Quake]</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>* [http://wiki.openstreetmap.org/wiki/2011_Sendai_earthquake_and_tsunami OpenStreetMap: Sendai Quake]</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>* [http://www.tsunami.noaa.gov/prepare.html Tsunami Mitigation]</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>* [http://www.tsunami.noaa.gov/prepare.html Tsunami Mitigation]</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>* [http://news.google.com/news/section?pz=1&#038;cf=all&#038;ned=us&#038;hl=en&#038;q=topic:earthquake&#038;ict=clu_top/ Google Quake News]</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>* [http://news.google.com/news/section?pz=1&#038;cf=all&#038;ned=us&#038;hl=en&#038;q=topic:earthquake&#038;ict=clu_top/ Google Quake News]</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>
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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>[[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>
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WikiMaster
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=10177&oldid=prev
Lockley: cat
2011-08-26T18:10:07Z
<p>cat</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:10, 26 August 2011</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>* [http://www.tsunami.noaa.gov/prepare.html Tsunami Mitigation]</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>* [http://www.tsunami.noaa.gov/prepare.html Tsunami Mitigation]</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>* [http://news.google.com/news/section?pz=1&#038;cf=all&#038;ned=us&#038;hl=en&#038;q=topic:earthquake&#038;ict=clu_top/ Google Quake News]</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>* [http://news.google.com/news/section?pz=1&#038;cf=all&#038;ned=us&#038;hl=en&#038;q=topic:earthquake&#038;ict=clu_top/ Google Quake News]</div></td></tr>
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Lockley
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9259&oldid=prev
WikiMaster: Undo vandalism.
2011-07-26T19:22:01Z
<p>Undo vandalism.</p>
<a href="https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9259&oldid=9231">Show changes</a>
WikiMaster
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9231&oldid=prev
4.71.200.50: AaROKAMeAoM
2011-07-26T12:36:23Z
<p>AaROKAMeAoM</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 05:36, 26 July 2011</td>
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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;">This is way more heplufl than anything else I</del>'<del style="font-weight: bold; text-decoration: none;">ve looked at</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;">It</ins>'<ins style="font-weight: bold; text-decoration: none;">s really great that poeple are sharing this information</ins>.</div></td></tr>
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4.71.200.50
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9222&oldid=prev
62.156.178.29: XucmdfKDAAuGIrR
2011-07-26T11:01:50Z
<p>XucmdfKDAAuGIrR</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 04:01, 26 July 2011</td>
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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;">Yo, good lkioon out! Gonna make it work now</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;">This is way more heplufl than anything else I've looked at</ins>.</div></td></tr>
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62.156.178.29
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9204&oldid=prev
196.35.33.39: Undo revision 9116 by Samc (talk)
2011-07-26T07:16:05Z
<p>Undo revision 9116 by <a href="/Special:Contributions/Samc" title="Special:Contributions/Samc">Samc</a> (<a href="/User_talk:Samc" title="User talk:Samc">talk</a>)</p>
<a href="https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9204&oldid=9127">Show changes</a>
196.35.33.39
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Samc: /* Operational Ocean Observatories */
2011-07-17T23:07:23Z
<p><span dir="auto"><span class="autocomment">Operational Ocean Observatories</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:07, 17 July 2011</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>* [http://www.mbari.org/mars/ MBARI's MARS] and [http://www.neptunecanada.ca/ Neptune Canada] will be integrated into [http://www.oceanobservatories.org a vast global network] that is expected to move science in unforeseen directions.</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>* [http://www.mbari.org/mars/ MBARI's MARS] and [http://www.neptunecanada.ca/ Neptune Canada] will be integrated into [http://www.oceanobservatories.org a vast global network] that is expected to move science in unforeseen directions.</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> </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:Ooi6.jpg|center|Ocean Observatory Cable Pacific City]]</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>[http://en.wikipedia.org/wiki/Axial_Seamount The Axial Seamount] last erupted in 1998. It's 3,600 ft high, in 4,600 ft of water, just 300 mi west of Cannon Beach, Oregon. [http://interactiveoceans.washington.edu/rsn/story/Axial+Caldera+Seafloor It will be wired up]. [http://www.astrobiology.com/news/viewpr.html?pid=12337 Microbes scooped from hydrotermal vents] and other [http://en.wikipedia.org/wiki/Extremophile extreme environments] can create new enzymes [http://www.astrobio.net/pressrelease/4092/record-breaking-heat-tolerant-enzyme for extreme industrial processes], like the production of biofuels from cellulose or DNA amplification ([http://www.npr.org/player/v2/mediaPlayer.html?action=1&t=1&islist=false&id=15233498&m=15233537 NPR: Science Friday]). </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>[http://en.wikipedia.org/wiki/Axial_Seamount The Axial Seamount] last erupted in 1998. It's 3,600 ft high, in 4,600 ft of water, just 300 mi west of Cannon Beach, Oregon. [http://interactiveoceans.washington.edu/rsn/story/Axial+Caldera+Seafloor It will be wired up]. [http://www.astrobiology.com/news/viewpr.html?pid=12337 Microbes scooped from hydrotermal vents] and other [http://en.wikipedia.org/wiki/Extremophile extreme environments] can create new enzymes [http://www.astrobio.net/pressrelease/4092/record-breaking-heat-tolerant-enzyme for extreme industrial processes], like the production of biofuels from cellulose or DNA amplification ([http://www.npr.org/player/v2/mediaPlayer.html?action=1&t=1&islist=false&id=15233498&m=15233537 NPR: Science Friday]). </div></td></tr>
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Samc
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9126&oldid=prev
Samc: /* Cyber Infrastructure */
2011-07-17T23:06:55Z
<p><span dir="auto"><span class="autocomment">Cyber Infrastructure</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:06, 17 July 2011</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>[http://www.oceanleadership.org/2011/consortium-for-ocean-leadership-selects-sea-bird-electronics-ooi/ Three Implementing Organizations] are responsible for construction and development of the overall program. The [http://uwnews.org/article.asp?articleID=51819 University of Washington] is responsible for cabled seafloor systems and moorings on the Juan de Fuca tectonic plate.</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>[http://www.oceanleadership.org/2011/consortium-for-ocean-leadership-selects-sea-bird-electronics-ooi/ Three Implementing Organizations] are responsible for construction and development of the overall program. The [http://uwnews.org/article.asp?articleID=51819 University of Washington] is responsible for cabled seafloor systems and moorings on the Juan de Fuca tectonic plate.</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><del style="font-weight: bold; text-decoration: none;">== Cyber Infrastructure ==</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> </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 [http://www.calit2.net/newsroom/release.php?id=1593 University of California, San Diego] is implementing the cyberinfrastructure component ([http://www.dtic.mil/cgi-bin/GetTRDoc?Location=U2&doc=GetTRDoc.pdf&AD=ADA527748 pdf]). [http://coastwatch.pfeg.noaa.gov/erddap/index.html NOAA standardizes different data sets] into a common file format to make graphs and maps. [https://www.facebook.com/Unidata?sk=app_4949752878 Unidata], funded primarily by the [http://en.wikipedia.org/wiki/National_Science_Foundation National Science Foundation], is one of eight programs in the [http://en.wikipedia.org/wiki/University_Corporation_for_Atmospheric_Research University Corporation for Atmospheric Research](UCAR). It [http://www.unidata.ucar.edu/ provides streaming observational data to university classrooms] world-wide.</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 [http://www.calit2.net/newsroom/release.php?id=1593 University of California, San Diego] is implementing the cyberinfrastructure component ([http://www.dtic.mil/cgi-bin/GetTRDoc?Location=U2&doc=GetTRDoc.pdf&AD=ADA527748 pdf]). [http://coastwatch.pfeg.noaa.gov/erddap/index.html NOAA standardizes different data sets] into a common file format to make graphs and maps. [https://www.facebook.com/Unidata?sk=app_4949752878 Unidata], funded primarily by the [http://en.wikipedia.org/wiki/National_Science_Foundation National Science Foundation], is one of eight programs in the [http://en.wikipedia.org/wiki/University_Corporation_for_Atmospheric_Research University Corporation for Atmospheric Research](UCAR). It [http://www.unidata.ucar.edu/ provides streaming observational data to university classrooms] world-wide.</div></td></tr>
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Samc
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9125&oldid=prev
Samc: /* Ocean Observatory Initiative */
2011-07-17T23:06:20Z
<p><span dir="auto"><span class="autocomment">Ocean Observatory Initiative</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:06, 17 July 2011</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>Initial capacity of the RSN system will be delivery of up to 200kW of power and 240Gbps of TCP/IP Internet data communications to the seven primary science nodes.</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>Initial capacity of the RSN system will be delivery of up to 200kW of power and 240Gbps of TCP/IP Internet data communications to the seven primary science nodes.</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></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:Ooi6.jpg|center|Ocean Observatory Cable Pacific City]]</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>== Oceanographer John Delany ==</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>== Oceanographer John Delany ==</div></td></tr>
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Samc
https://portlandwiki.org/index.php?title=Cascadia_subduction_zone&diff=9124&oldid=prev
Samc: /* Oceanographer John Delany */
2011-07-17T23:04:08Z
<p><span dir="auto"><span class="autocomment">Oceanographer John Delany</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:04, 17 July 2011</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>== Oceanographer John Delany ==</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>== Oceanographer John Delany ==</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:Johnd.jpg|left|John Delany]][http://ooi.washington.edu/rsn/jrd/ John Delany] has apparently managed to steer this thing though a minefield of conflicting interests, including the DOD, scientists, government bureaucrats and funding agencies. </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> </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>[[File:Johnd.jpg|left|John Delany]] <ins style="font-weight: bold; text-decoration: none;">[http://www.ooi.washington.edu/ The regional cabled ocean observatory] was nurtured and developed at UW, by [http://ooi.washington.edu/rsn/jrd/ oceanographer John Delany]. </ins>[http://ooi.washington.edu/rsn/jrd/ John Delany] has apparently managed to steer this thing though a minefield of conflicting interests, including the DOD, scientists, government bureaucrats and funding agencies. </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>Whether the military has negatively impacted public safety with data restrictions may never be known for sure. Delany's vision has clearly been persuasive.</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>Whether the military has negatively impacted public safety with data restrictions may never be known for sure. Delany's vision has clearly been persuasive.</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>[http://www.oceanleadership.org/2011/consortium-for-ocean-leadership-selects-sea-bird-electronics-ooi/ Three Implementing Organizations] are responsible for construction and development of the overall program. The [http://uwnews.org/article.asp?articleID=51819 University of Washington] is responsible for cabled seafloor systems and moorings on the Juan de Fuca tectonic plate. </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>[http://www.oceanleadership.org/2011/consortium-for-ocean-leadership-selects-sea-bird-electronics-ooi/ Three Implementing Organizations] are responsible for construction and development of the overall program. The [http://uwnews.org/article.asp?articleID=51819 University of Washington] is responsible for cabled seafloor systems and moorings on the Juan de Fuca tectonic plate.</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>== Cyber Infrastructure ==</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>== Cyber Infrastructure ==</div></td></tr>
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Samc