<?xml version="1.0" encoding="UTF-8"?>
<?xml-stylesheet href="/style/rss/rss_feed.xsl" type="text/xsl" media="screen"?><?xml-stylesheet href="/style/rss/rss_feed.css" type="text/css" media="screen" ?><rss version="2.0"><channel><title>Clipmarks | Tectonic movements Clips</title><link>http://clipmarks.com/tags/tectonic+movements/</link><feedUrl>http://rss.clipmarks.com/tags/tectonic+movements/</feedUrl><ttl>15</ttl><description>Clip, tag and save information that's important to you. Bookmarks save entire pages...Clipmarks save the specific content that matters to you!</description><language>en-us</language><item><title>Top 33 volcanoes on Earth</title><link>http://clipmarks.com/clipmark/CF65A97D-EFE1-499D-9B04-4D0F5D5C2071/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/hitchhiker08/"&gt;hitchhiker08&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://news.softpedia.com/news/Top-33-Volcanoes-83849.shtml" title="http://news.softpedia.com/news/Top-33-Volcanoes-83849.shtml"&gt;news.softpedia.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H1 id="hot_title"&gt;Top 33 Volcanoes &lt;/H1&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;
			&lt;DIV&gt;&lt;A title="Picture of Vesuvius blast in 73AD" href="http://news.softpedia.com/newsImage/Top-33-Volcanoes-2.jpg" target="_blank"&gt;&lt;IMG border="0" alt="Picture of Vesuvius blast in 73AD" src="http://news.softpedia.com/images//newsrsz/Top-33-Volcanoes-2.jpg" /&gt;&lt;/A&gt;&lt;BR /&gt;&lt;SPAN class="rightcellcontent"&gt;&lt;A href="http://news.softpedia.com/newsImage/Top-33-Volcanoes-2.jpg" target="_blank" class="small"&gt;Enlarge picture&lt;/A&gt;&lt;/SPAN&gt;&lt;/DIV&gt;Volcanoes are the result of the tectonic movements of the Earth's crust, when magma from the entrails of the planet goes out as lava. They became present in the legends and mythology of all people living around them, which venerated and feared them at the same time. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://news.softpedia.com/newsImage/Top-33-Volcanoes-2.jpg" title="http://news.softpedia.com/newsImage/Top-33-Volcanoes-2.jpg"&gt;news.softpedia.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/hitchhiker08/512/7CFE9207-6425-44AD-8E04-80C87E735223.jpg" alt="Picture of Vesuvius blast in 73AD" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://news.softpedia.com/newsImage/Top-33-Volcanoes-3.jpg" title="http://news.softpedia.com/newsImage/Top-33-Volcanoes-3.jpg"&gt;news.softpedia.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/hitchhiker08/512/CA31B374-3785-4E2D-9DC9-8EC26F2B0AC7.jpg" alt="The peak of Cotopaxi" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://news.softpedia.com/news/Top-33-Volcanoes-83849.shtml" title="http://news.softpedia.com/news/Top-33-Volcanoes-83849.shtml"&gt;news.softpedia.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;
Amongst the hundreds of active or non-active volcanoes, here is a list that we should all know, about the most significant volcanoes on Earth. They are not aligned by size or importance. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;DIV&gt;
1.The most important volcano in North America is Mount Saint Helens, located in Skamania County, Washington, in the Pacific Northwest region of the US, at 96 miles (154 km) south of the city of Seattle and 53 miles (85 km) northeast of Portland, Oregon. This active volcano is located in the Cascade Range and is part of the Cascade Volcanic Arc, a segment of the Pacific Ring of Fire that includes over 160 active volcanoes. St Helens is the fourth volcanic peak in the Cascade Range. &lt;/DIV&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/volcanoes/" rel="tag"&gt;volcanoes&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/tectonic+movements/" rel="tag"&gt;tectonic movements&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/phenomena/" rel="tag"&gt;phenomena&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/vesuvius/" rel="tag"&gt;vesuvius&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/mount+saint+helens/" rel="tag"&gt;mount saint helens&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/lava/" rel="tag"&gt;lava&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/eruption/" rel="tag"&gt;eruption&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://news.softpedia.com/news/Top-33-Volcanoes-83849.shtml</clipSource><pubDate>Mon, 21 Apr 2008 06:04:55 GMT</pubDate></item><item><title>Quakes Under Pacific Ocean Floor Reveal Unexpected Circulation System</title><link>http://clipmarks.com/clipmark/D029D488-23D2-42E2-8899-C4CF6B30FBA8/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/amgumen/"&gt;amgumen&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.nsf.gov/news/mmg/media/images/vents_h1.jpg" title="http://www.nsf.gov/news/mmg/media/images/vents_h1.jpg"&gt;www.nsf.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;img src="http://clipmarks.com/image_cache/amgumen/512/EAE59129-7305-43A5-82C8-AA316A9A37A3.jpg" alt="http://www.nsf.gov/news/mmg/media/images/vents_h1.jpg" /&gt;&lt;br /&gt;&lt;/div&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.nsf.gov/discoveries/disc_summ.jsp?cntn_id=110976&amp;org=NSF" title="http://www.nsf.gov/discoveries/disc_summ.jsp?cntn_id=110976&amp;org=NSF"&gt;www.nsf.gov&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;Zigzagging some 60,000 kilometers across the ocean floor, Earth's system of mid-ocean ridges plays a pivotal role in many workings of the planet: in plate-tectonic movements, heat flow from the interior, and the chemistry of rock, water and air. &lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;The systems pull in cold water, superheat it, then spit it back out from seafloor vents--a process that brings up not only hot water, but dissolved substances from rocks below. Unique life forms feed off the vents' stew, and valuable minerals including gold may pile up.&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;water moves a lot faster than previously thought--perhaps a billion gallons per year--through these systems. The water appears to descend instead through a buried 200-meter-wide chimney atop the ridge studied on the East Pacific Rise, run below the ridge along its axis through a tunnel just above a magma chamber, then bubble back up through a series of vents further along the ridge.&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/geology/" rel="tag"&gt;geology&lt;/a&gt;, &lt;a href="http://clipmarks.com/tags/ocean/" rel="tag"&gt;ocean&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.nsf.gov/news/mmg/media/images/vents_h1.jpg</clipSource><pubDate>Thu, 17 Jan 2008 01:32:02 GMT</pubDate></item><item><title>Back-seat toilet to end mishaps in traffic jams</title><link>http://clipmarks.com/clipmark/5374638F-3826-42E5-A457-323721D6182B/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/tabsey/"&gt;tabsey&lt;/a&gt;&lt;br&gt;&lt;b&gt;clipper's remarks:&lt;/b&gt;  Beep, beep! Just using the bathroom. Beep, beep, WHAT? &lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.abc.net.au/news/stories/2007/10/24/2069280.htm" title="http://www.abc.net.au/news/stories/2007/10/24/2069280.htm"&gt;www.abc.net.au&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P class="first"&gt;A Japanese manufacturer has developed a new portable toilet for cars, equipped with a curtain for privacy and a plastic bag to collect waste.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;The Kaneko Sangyo Co, a manufactuer of plastic car accessories, unveiled its new design to help people stuck in traffic when nature calls.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;"The commode will come in handy during major disasters such as earthquakes or when you are caught in a traffic jam," a company official told reporters, according to Kyodo News.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;Japan is situated on the Pacific "Ring of Fire" and accounts for about 20 per cent of the world's earthquakes of magnitude 6 or greater.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;Drivers stranded by tectonic movements or stuck in traffic jams simply assemble the cardboard toilet bowl, fit a water-absorbent sheet inside and draw round the curtain.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;The product is small enough to fit inside a suitcase, the company said.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;But prospective customers will have to hang on until November 15 when the firm begins selling the new product online.&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/offbeat/" rel="tag"&gt;offbeat&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.abc.net.au/news/stories/2007/10/24/2069280.htm</clipSource><pubDate>Wed, 24 Oct 2007 11:34:12 GMT</pubDate></item><item><title>Gravitational bumpiness exaggerated.</title><link>http://clipmarks.com/clipmark/D1C9287E-CFE4-473C-A02F-2D3B665479DC/</link><description>&lt;b&gt;clipped by:&lt;/b&gt; &lt;a href="http://clipmarks.com/clipper/shankargallery/"&gt;shankargallery&lt;/a&gt;&lt;br&gt;&lt;div border="2" style="margin-top: 10px; border:#000000 1px solid;" width="90%"&gt;&lt;div style="background-color:"&gt;&lt;div align="center" width="100%" style="padding:4px;margin-bottom:4px;background-color:#666666;overflow:hidden;"&gt;&lt;span style="color:#FFFFFF;font-weight:bold;"&gt;Clip Source: &lt;a style="color:#FFFFFF;" href="http://www.solstation.com/stars/earth.htm" title="http://www.solstation.com/stars/earth.htm"&gt;www.solstation.com&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;P&gt;
&lt;FONT face="Arial" color="#000000"&gt;&lt;FONT face="Arial" color="#000000"&gt;&lt;A href="http://www.solstation.com/stars/ear1grav.jpg"&gt;
&lt;IMG hspace="12" align="left" src="http://www.solstation.com/stars/ear-grav.jpg" /&gt;&lt;/A&gt;
&lt;SMALL&gt;&lt;I&gt;&lt;DIV&gt;NASA -- &lt;A href="http://www.solstation.com/stars/ear1grav.jpg"&gt;Larger&lt;/A&gt; image&lt;/DIV&gt;
&lt;BR /&gt;&lt;DIV&gt;
Gravitational bumpiness exaggerated.  &lt;/DIV&gt;
&lt;BR /&gt;
&lt;BR /&gt;
While Earth is a fairly uniform sphere, &lt;BR /&gt;
its gravitational field does vary by small &lt;BR /&gt;
fractions of a percent from place to place. &lt;BR /&gt;
Not only is the planet bumpy as the result &lt;BR /&gt;
of slow geological processes such as &lt;BR /&gt;
tectonic plate movements or polar ice cap &lt;BR /&gt;
changes, but these processes also create &lt;BR /&gt;
mass density variations that affect the &lt;BR /&gt;
local gravitational field 
(more from 
&lt;A href="http://science.nasa.gov/headlines/y2001/ast30oct_1.htm"&gt;NASA&lt;/A&gt; &lt;BR /&gt;
and 
&lt;A href="http://antwrp.gsfc.nasa.gov/apod/ap011113.html"&gt;Astronomy 
Picture of the Day&lt;/A&gt;).  &lt;BR clear="left" /&gt;&lt;/I&gt;&lt;/SMALL&gt;&lt;/FONT&gt;&lt;/FONT&gt;&lt;/P&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;H1&gt;Earth&lt;/H1&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;FONT size="1" face="Verdana, Arial" color="#ffffff"&gt;  
&lt;A  href="http://www.solstation.com/stars/../index.html"&gt;&lt;B&gt;Home&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/../stars.htm"&gt;&lt;B&gt;Stars&lt;/B&gt;&lt;/A&gt;  |   
&lt;A  href="http://www.solstation.com/stars/../orbits.htm"&gt;&lt;B&gt;Orbits&lt;/B&gt;&lt;/A&gt;  |   
&lt;A  href="http://www.solstation.com/stars/../habitable.htm"&gt;&lt;B&gt;Habitability&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/../life.htm"&gt;&lt;B&gt;Life&lt;/B&gt;&lt;/A&gt;  | &lt;/FONT&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;FONT size="1" face="Verdana, Arial" color="#ffffff"&gt;  
          |  
&lt;A  href="http://www.solstation.com/stars/sol-sum.htm"&gt;&lt;B&gt;System Summary&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/4planets.htm"&gt;&lt;B&gt;Rocky Inner Planets&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/asteroid.htm"&gt;&lt;B&gt;Main Asteroid Belt&lt;/B&gt;&lt;/A&gt;  | 
&lt;A  href="http://www.solstation.com/stars/jovians.htm"&gt;&lt;B&gt;Gas Giants&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/kuiper.htm"&gt;&lt;B&gt;E-K Belt &amp; Dust Disk&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/oort.htm"&gt;&lt;B&gt;Oort Cloud&lt;/B&gt;&lt;/A&gt;  | 
&lt;/FONT&gt;&lt;/div&gt;&lt;/div&gt;&lt;hr size="2" color="#666666" /&gt;&lt;div style="padding: 10px;"&gt;&lt;div style="text-align:left;"&gt;&lt;table background="undefined" bgcolor="#ffffff"&gt;&lt;tr&gt;&lt;TD valign="middle" nowrap="NOWRAP" height="20" bgcolor="#0000ff" colspan="4"&gt;
&lt;FONT size="1" face="Verdana, Arial" color="#ffffff"&gt;  
          |  
&lt;A  href="http://www.solstation.com/stars/sol.htm"&gt;&lt;B&gt;Sol&lt;/B&gt;&lt;/A&gt;  |   
&lt;A  href="http://www.solstation.com/stars/mercury.htm"&gt;&lt;B&gt;Mercury&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/venus.htm"&gt;&lt;B&gt;Venus&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/earth.htm"&gt;&lt;B&gt;Earth&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/mars.htm"&gt;&lt;B&gt;Mars&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/jupiter.htm"&gt;&lt;B&gt;Jupiter&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/saturn.htm"&gt;&lt;B&gt;Saturn&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/uranus.htm"&gt;&lt;B&gt;Uranus&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/neptune.htm"&gt;&lt;B&gt;Neptune&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/dwarfpla.htm"&gt;&lt;B&gt;Dwarf Planets&lt;/B&gt;&lt;/A&gt;  |  
&lt;A  href="http://www.solstation.com/stars/oort.htm#sol-b"&gt;&lt;B&gt;Sol b?&lt;/B&gt;&lt;/A&gt;  | 
&lt;/FONT&gt;&lt;/TD&gt;&lt;/tr&gt;&lt;/table&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br&gt;&lt;div style="margin-bottom: 40px;"&gt;Tags: &lt;a href="http://clipmarks.com/tags/gravity/" rel="tag"&gt;gravity&lt;/a&gt;&lt;/div&gt;</description><clipSource>http://www.solstation.com/stars/earth.htm</clipSource><pubDate>Wed, 18 Jul 2007 21:58:37 GMT</pubDate></item></channel></rss>