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Revision as of 20:10, 8 August 2005 view sourceSade (talk | contribs)3,956 editsm revert: html is being used becuase of the "Misc. --> Auto-number headings" option in preferences← Previous edit Revision as of 20:12, 8 August 2005 view source Sade (talk | contribs)3,956 editsm Reverted edits by Oven Fresh to last version by ABCDNext edit →
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Revision as of 20:12, 8 August 2005

Welcome to Misplaced Pages, the 💕 that anyone can edit.

In this English version, started in 2001, we are currently working on 6,939,602 articles.

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Today's featured article

Big Raven Plateau, at the northern end of the Mount Edziza volcanic complexBig Raven Plateau, at the northern end of the Mount Edziza volcanic complex

Volcanism of the Mount Edziza volcanic complex in British Columbia, Canada, spans more than 7 million years. The first magmatic cycle took place between 7.5 and 6 million years ago and is represented by the Raspberry, Little Iskut and Armadillo geological formations. Volcanism has taken place during five cycles of magmatic activity, each producing less volcanic material than the previous one. During these cycles volcanism has created several types of volcanoes, including cinder cones, stratovolcanoes, subglacial volcanoes, shield volcanoes and lava domes. The roughly 1,000-square-kilometre (400-square-mile) volcanic plateau of the MEVC originated from the successive eruptions of highly mobile lava flows. Several types of volcanic rocks were deposited by multiple eruptions of the MEVC. At least 10 distinct flows of obsidian were produced by volcanism of the MEVC, some of which were exploited by indigenous peoples in prehistoric times to make tools and weapons. (Full article...)

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