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	<title>Toba Lake</title>
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		<title>Toba Lake</title>
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		<title>Toba Lake</title>
		<link>http://tobalake.wordpress.com/2008/06/16/toba-lake/</link>
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		<pubDate>Mon, 16 Jun 2008 19:46:21 +0000</pubDate>
		<dc:creator>suriirawadi</dc:creator>
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		<description><![CDATA[Lake Toba (Indonesian: Danau Toba) is a lake, 100 km long and 30 km wide, and 505 m. (1,666 ft.) at its deepest point, in the middle of the northern part of the Indonesian island of Sumatra with a surface elevation of about 900 m (3,000 feet), stretching from 2.88° N 98.52° E to 2.35° [...]<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=tobalake.wordpress.com&amp;blog=3995184&amp;post=3&amp;subd=tobalake&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p><strong>Lake Toba</strong> (<a title="Indonesian language" href="http://en.wikipedia.org/wiki/Indonesian_language">Indonesian</a>: <em><strong>Danau Toba</strong></em>) is a <a title="Lake" href="http://en.wikipedia.org/wiki/Lake">lake</a>, 100 km long and 30 km wide, and 505 m. (1,666 ft.) at its deepest point, in the middle of the northern part of the <a title="Indonesia" href="http://en.wikipedia.org/wiki/Indonesia">Indonesian</a> <a title="Island" href="http://en.wikipedia.org/wiki/Island">island</a> of <a title="Sumatra" href="http://en.wikipedia.org/wiki/Sumatra">Sumatra</a> with a surface elevation of about 900 m (3,000 feet), stretching from <span class="plainlinksneverexpand"><img style="cursor:pointer;padding:0 3px 0 0;" src="http://upload.wikimedia.org/wikipedia/commons/thumb/9/9a/Erioll_world.svg/18px-Erioll_world.svg.png" alt="" /><a class="external text" title="http://toolserver.org/~magnus/geo/geohack.php?pagename=Lake_Toba&amp;params=2.88_N_98.52_E_" rel="nofollow" href="http://toolserver.org/~magnus/geo/geohack.php?pagename=Lake_Toba&amp;params=2.88_N_98.52_E_"><span title="Maps, aerial photos, and other data for this location">2.88° N 98.52° E</span></a></span> to <span class="plainlinksneverexpand"><img style="cursor:pointer;padding:0 3px 0 0;" src="http://upload.wikimedia.org/wikipedia/commons/thumb/9/9a/Erioll_world.svg/18px-Erioll_world.svg.png" alt="" /><a class="external text" title="http://toolserver.org/~magnus/geo/geohack.php?pagename=Lake_Toba&amp;params=2.35_N_99.1_E_" rel="nofollow" href="http://toolserver.org/~magnus/geo/geohack.php?pagename=Lake_Toba&amp;params=2.35_N_99.1_E_"><span title="Maps, aerial photos, and other data for this location">2.35° N 99.1° E</span></a></span>. It is the largest <a class="mw-redirect" title="Volcanic lake" href="http://en.wikipedia.org/wiki/Volcanic_lake">volcanic lake</a> in the world.<sup> </sup></p>
<h2><span class="mw-headline">Geology</span></h2>
<h2><span class="mw-headline">In 1949 the <a title="Netherlands" href="http://en.wikipedia.org/wiki/Netherlands">Dutch</a> <a title="Geologist" href="http://en.wikipedia.org/wiki/Geologist">geologist</a> <a class="mw-redirect" title="Rein van Bemmelen" href="http://en.wikipedia.org/wiki/Rein_van_Bemmelen">Rein van Bemmelen</a> reported that Lake Toba was surrounded by a layer of <a title="Ignimbrite" href="http://en.wikipedia.org/wiki/Ignimbrite">ignimbrite</a> rocks, and that it was a large volcanic <a title="Caldera" href="http://en.wikipedia.org/wiki/Caldera">caldera</a>. Later researchers found <a title="Rhyolite" href="http://en.wikipedia.org/wiki/Rhyolite">rhyolite</a> ash similar to that in the ignimbrite around Toba (now called Young Toba <a title="Tuff" href="http://en.wikipedia.org/wiki/Tuff">Tuff</a> to distinguish it from layers deposited in previous explosions) in <a title="Malaysia" href="http://en.wikipedia.org/wiki/Malaysia">Malaysia</a> and <a title="India" href="http://en.wikipedia.org/wiki/India">India</a>, 3,000 km away. <a title="Oceanography" href="http://en.wikipedia.org/wiki/Oceanography">Oceanographers</a> discovered Toba ash, with its characteristic chemical &#8220;fingerprint&#8221;, on the floor of the eastern <a title="Indian Ocean" href="http://en.wikipedia.org/wiki/Indian_Ocean">Indian Ocean</a> and the <a title="Bay of Bengal" href="http://en.wikipedia.org/wiki/Bay_of_Bengal">Bay of Bengal</a>.</span></h2>
<h2><span class="mw-headline"></p>
<h3><span class="mw-headline">The Eruption</span></h3>
<h3><span class="mw-headline">The <strong>Toba eruption</strong> (the <strong>Toba event</strong>) occurred at what is now Lake Toba about 67,500 to 75,500 years ago. It had an estimated <a title="Volcanic Explosivity Index" href="http://en.wikipedia.org/wiki/Volcanic_Explosivity_Index">Volcanic Explosivity Index</a> of 8 (described as &#8220;mega-colossal&#8221;), making it possibly the largest explosive <a class="mw-redirect" title="Volcanic eruption" href="http://en.wikipedia.org/wiki/Volcanic_eruption">volcanic eruption</a> within the last twenty-five million years. <a title="William I. Rose" href="http://en.wikipedia.org/wiki/William_I._Rose">Bill Rose</a> and <a class="new" title="Craig Chesner (page does not exist)" href="http://en.wikipedia.org/w/index.php?title=Craig_Chesner&amp;action=edit&amp;redlink=1">Craig Chesner</a> of <a title="Michigan Technological University" href="http://en.wikipedia.org/wiki/Michigan_Technological_University">Michigan Technological University</a> deduced that the total amount of erupted material was about 2800 cubic km (670 cubic miles) — around 2,000 km³ of <a title="Ignimbrite" href="http://en.wikipedia.org/wiki/Ignimbrite">ignimbrite</a> that flowed over the ground and around 800 km³ that fell as ash, with the wind blowing most of it to the west. By contrast, the <a title="1980 eruption of Mount St. Helens" href="http://en.wikipedia.org/wiki/1980_eruption_of_Mount_St._Helens">1980 eruption of Mount St. Helens</a> ejected around 1.2 cubic km of material, whilst the largest volcanic eruption in historic times, at <a title="Mount Tambora" href="http://en.wikipedia.org/wiki/Mount_Tambora">Mount Tambora</a> in <a title="1815" href="http://en.wikipedia.org/wiki/1815">1815</a>, emitted the equivalent of around 100 cubic kilometres of dense rock and created the &#8220;<a title="Year Without a Summer" href="http://en.wikipedia.org/wiki/Year_Without_a_Summer">Year Without a Summer</a>&#8221; as far away as North America.The Toba eruption was the latest of a series of at least three <a title="Caldera" href="http://en.wikipedia.org/wiki/Caldera">caldera</a>-forming eruptions which have occurred at the volcano. Earlier calderas were formed around 700,000 and 840,000 years ago. To give an idea of its magnitude, consider that although the eruption took place in <a title="Indonesia" href="http://en.wikipedia.org/wiki/Indonesia">Indonesia</a>, it deposited an ash layer approximately 15 cm (6 in) thick over the entire Indian subcontinent; at one site in central India, the Toba ash layer today is up to 6 m (20 feet) thick and parts of <a title="Malaysia" href="http://en.wikipedia.org/wiki/Malaysia">Malaysia</a> were covered with 9 m of ashfall. In addition it has been calculated that 10 metric tons of <a class="mw-redirect" title="Sulphuric acid" href="http://en.wikipedia.org/wiki/Sulphuric_acid">sulphuric acid</a> was ejected into the atmosphere by the event, causing <a title="Acid rain" href="http://en.wikipedia.org/wiki/Acid_rain">acid rain</a> fallout.  </p>
<p> </p>
<p></span></h3>
<p></span></h2>
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		<title>Hello world!</title>
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		<pubDate>Mon, 16 Jun 2008 19:25:13 +0000</pubDate>
		<dc:creator>suriirawadi</dc:creator>
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