Huge Volcanic Eruptions


	Huge Volcanic Eruptions
shashtheash95
5-7-2008 10:48 AM
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<div style="margin: 12px 0px; font-family: arial; color: #333333; background: #ffffff; border: solid 4px #e5e5e5; width: 100%; clear: left;"><div class="CM_CTB_Content_Wrap" style="margin: 0px; padding: 0px;background-color: #ffffff;"><div style="border-bottom: solid 1px #dcdcdc; white-space: nowrap; margin-bottom: 8px; background-color: #eeeeee ;background-image: url(http://clipmarks.com/images/source-bg.gif); background-repeat: repeat-x; height: 24px; line-height: 24px; vertical-align: middle; padding-bottom: 4px; color: #666666; font-size: 10px;" ><a href="http://clipmarks.com/clip-to-blog/" title="see clips that are hot right now"><img src="http://content.clipmarks.com/blog_embed/713fbff0-c39d-4e03-b040-bd56b2631680/239419B3-CC52-4D60-A356-ACF0BF24BE39/" alt="" width="19" height="19" border="0" style="vertical-align: middle; margin: 0px 4px; display: inline; border: none; float:none;" /></a>clipped from <a title="http://www.unep-wcmc.org/resources/publications/MountainWatch_Bishkek/presspack/I/PINATUBO_91.jpg" href="http://www.unep-wcmc.org/resources/publications/MountainWatch_Bishkek/presspack/I/PINATUBO_91.jpg" style="font-size: 11px;">www.unep-wcmc.org</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.unep-wcmc.org/resources/publications/MountainWatch_Bishkek/presspack/I/PINATUBO_91.jpg"><div align="center"><img src="http://content9.clipmarks.com/blog_cache/www.unep-wcmc.org/img/B7478BAA-8F9F-429C-A228-5A1C578E7CDF" alt="http://www.unep-wcmc.org/resources/publications/MountainWatch_Bishkek/presspack/I/PINATUBO_91.jpg" /></div></blockquote><div style="border-bottom: solid 1px #dcdcdc; white-space: nowrap; margin-bottom: 8px; background-color: #eeeeee ;background-image: url(http://clipmarks.com/images/source-bg.gif); background-repeat: repeat-x; height: 24px; line-height: 24px; vertical-align: middle; padding-bottom: 4px; color: #666666; font-size: 10px;" ><a href="http://clipmarks.com/clip-to-blog/" title="see clips that are hot right now"><img src="http://content6.clipmarks.com/images/clip-icon.gif" alt="" width="19" height="19" border="0" style="vertical-align: middle; margin: 0px 4px; display: inline; border: none; float:none;" /></a>clipped from <a title="http://www.geology.wisc.edu/courses/g112/volcano.html" href="http://www.geology.wisc.edu/courses/g112/volcano.html" style="font-size: 11px;">www.geology.wisc.edu</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html"><div align="center"><img src="http://content7.clipmarks.com/blog_cache/www.geology.wisc.edu/img/BC5E1F3A-4A96-4A32-8697-C1ED41FE9B2D" alt="" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html"><SMALL>Mount St. Helens before the May
18, 1980 eruption</SMALL></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html"><div align="center"><img src="http://content8.clipmarks.com/blog_cache/www.geology.wisc.edu/img/37631613-69BE-4AC6-8E3A-693A297DDDE1" alt="" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html">Mount St Helens after May 18, 1980</blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html"><div align="center"><img src="http://content9.clipmarks.com/blog_cache/www.geology.wisc.edu/img/1ECE2A6F-C8AC-4101-B2CF-80D513CAB21B" alt="" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html">Mt. Fuji, Japan</blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html"><div align="center"><img src="http://content6.clipmarks.com/blog_cache/www.geology.wisc.edu/img/9E415C1E-708A-4D57-8A65-F60E4BDDCF23" alt="" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html">Mount
Pinatubo, Philippines, 1991</blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html"><div align="center"><img src="http://content7.clipmarks.com/blog_cache/www.geology.wisc.edu/img/3BEDFF08-FBF7-4CE1-841C-D19FF19BBDE4" alt="" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://www.geology.wisc.edu/courses/g112/volcano.html">
This image shows the Paricutin cinder cone of western Mexico.
This cinder cone was "born" on Feb. 20, 1943, in the field of a poor Mexican
peasant who was planting corn when he saw flames begin shooting out of
a nearby crack in the ground.  Within several years, Paricutin grew to a height of
more than 1000 feet years.  For a time, it was Mexico's main tourist attraction.
Although Paricutin's eruptions consisted mainly of cinders for several years,
it eventually emitted a lava flow that covered dozens of square miles of the
surrounding countryside.  Only nine years after eruptions initiated, Paricutin
went extinct and has remained inactive since 1952.</blockquote></div><div style="margin: 0px 6px 6px 4px;"><table style="font-size: 11px;border-spacing: 0px;padding: 0px;" cellpadding="0" cellspacing="0" width="100%"><tr><td style="background:transparent;border-width:0px;padding:0px;">&nbsp;</td><td align="right" style="background:transparent;border-width:0px;padding:0px;width:107px" width="107"><a href="http://clipmarks.com/share/239419B3-CC52-4D60-A356-ACF0BF24BE39/blog/" title="blog or email this clip"><img src="http://content8.clipmarks.com/images/c2b-foot.png" border="0" alt="blog it" width="107" height="17" style="border-width:0px;padding:0px;margin:0px;" /></a></td></tr></table></div></div>
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