Composite Volcano

Also called Stratovolcanoes, composite volcanoes usually have very steep sides (Topinka, 2003).  These volcanoes are usually built by its own eruptive material including, tephras, lava and pyroclastic flows (VHP WWW Team, 2000).   Because they are built this way, they take hundreds of thousands of years. 

Most composite volcanoes have a crater at the top that contains a central or a cluster of vents (Topinka, 2003).  Lava flows through the cracks in the crater or flows through cracks on the side of the mountain (Topinka, 2003). 

The rocks typically found around these volcanoes are basalt, dacite, andesite, and rhyolite ( VHP WWW Team, 2000).  All of these rock types minus basalt will create violent eruptions ( VHP WWW Team, 2000). 

Some of the more famous composite volcanoes are:

Mount Fuji

http://www.traveladdicts.connectfree.co.uk/Japan/Images/Mount_Fuji_Postcard.jpg
Mount Shasta

, http://www.peakware.com/photos.html?pk=233
Mount Cotopaxi

http://www.grant-margison.com/journeys/images/SA-052Cotopaxi.jpg
Mount Saint Helens

http://vulcan.wr.usgs.gov/Volcanoes/MSH/description_msh.html
Mount Pinatubo

http://epod.usra.edu/archive/images/wisland3c.jpg
 

 

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