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| | Vic Camp - scoria cones |
 | | Scoria cones, also known as cinder cones, are the most common type of volcano. |
 | | Unlike the other two main volcano types, scoria cones have straight sides and very large summit craters, with respect to their relatively small edifices. |
 | | They are often symmetric, although many are asymmetric due to (1) the build up of tephra on the downwind flank of the edifice, (2) elongation of the volcano above an eruptive fissure, or (3) partial rafting of an outer wall of the volcano due to basalt lava oozing outward from beneath the volcano edifice. |
| www.geology.sdsu.edu /how_volcanoes_work/scoriacone_page.html (295 words) |
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