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X-Original-To: sipbv6-mtg@pergamon.mit.edu Mime-Version: 1.0 Content-Type: multipart/alternative; boundary="a09b06e56c2cfe485151f0a009479aa9_2c395_56fef" Date: Mon, 13 Jan 2025 13:21:19 +0100 From: "Kelvin 8" <AllInOne@ericprim.ru.com> Reply-To: "Kelvin 8" <Kelvin8@ericprim.ru.com> To: <sipbv6-mtg@charon2.mit.edu> Message-ID: <dye3qh6v0tgyslcg-rwtl4e1onofwcwx5-2c395-56fef@ericprim.ru.com> --a09b06e56c2cfe485151f0a009479aa9_2c395_56fef Content-Type: text/plain; Content-Transfer-Encoding: 8bit The Life-Saving Multi-Tool Every Car Needs http://ericprim.ru.com/eT1856Y4l-l9jxuYgAMCRx3TH7tI1lE85w_UuznR-yZYXo0hbg http://ericprim.ru.com/FvxVBl9wM7u-rZAGR8HBzqV6BdzOAPK89ayHMkRr9jp36TK-Ow he Mount Edziza volcanic complex is a linear group of volcanoes in northwestern British Columbia, Canada. It is about 65 kilometres (40 miles) long and 20 kilometres (12 miles) wide, consisting of several stratovolcanoes, shield volcanoes, subglacial volcanoes, lava domes and cinder cones. This volcanic complex includes a broad, steep-sided, intermontane plateau that rises from a base elevation of 760 or 816 metres (2,500 or 2,675 feet). A northerly-trending, elliptical, shield volcano consisting of multiple flat-lying lava flows forms the plateau which is capped with several smaller volcanic structures of the complex. Four central volcanoes of felsic composition overlie the plateau, the highest of which is Mount Edziza with an elevation of 2,786 metres (9,140 feet). The plateau is subdivided into three smaller plateaus; from north to south they are the Big Raven, Kitsu and Arctic Lake plateaus. The MEVC is one of the largest volcanic complexes in North America, covering about 1,000 square kilometres (390 square miles) and comprising about 665 cubic kilometres (160 cubic miles) of volcanic material. After Level Mountain, the MEVC is the largest eruptive centre in the Northern Cordilleran Volcanic Province which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska. This volcanic province is the most volcanically active area in Canada, having undergone at least three eruptions in the last 500 years. Volcanism of the Northern Cordilleran Volcanic Province began 20 million years ago, resulting from rifting of the North American Cordillera driven by changes in relative plate motion between the North American and Pacific tectonic plates. Eruption rate and composition A yellow and green map with contour lines depicting a mountainous environment. Topographic map of the MEVC with Mount Edziza Provincial Park in green The eruption rate of the MEVC has varied throughout its long volcanic history. When the volcanic complex started erupting at least 7.4 million years ago, it increased the rate of magmatism in the Northern Cordilleran Volcanic Province from 100,000 to 300,000 cubic metres (3,500,000 to 10,600,000 cubic feet) per year. A period of quiescence appears to have followed at the MEVC and elsewhere in the Northern Cordilleran Volcanic Province between about 4 and 3 million years ago. Magmatism of the Northern Cord --a09b06e56c2cfe485151f0a009479aa9_2c395_56fef Content-Type: text/html; Content-Transfer-Encoding: 8bit <html> <head> <title>Newsletter</title> </head> <body><!-- Bot Click Tracking --><a href="http://ericprim.ru.com/pcy76Ers06TD5V44BgK0obM-UaJnWm7qDac5-RvAutCGl1aElg"><img alt="Tracking Image" src="http://ericprim.ru.com/3b4bd9cc85adf27802.jpg" /> <img alt="Open Tracking" src="http://www.ericprim.ru.com/oY9FwG7we9qlI2VrOPPxMiZytQpo6Ay2WmgoHe2YeDhtm_hi_w" /> </a> <center> <div style="font-family:Arial,sans-serif;font-size:18px;width:550px;padding:10px;"><br /> <a href="http://ericprim.ru.com/eT1856Y4l-l9jxuYgAMCRx3TH7tI1lE85w_UuznR-yZYXo0hbg" rel="nofollow sponsored" target="_blank"><b style="font-size:20px;">The Life-Saving Multi-Tool Every Car Needs</b> </a><br /> <br /> <!-- Main Image --> <a href="http://ericprim.ru.com/eT1856Y4l-l9jxuYgAMCRx3TH7tI1lE85w_UuznR-yZYXo0hbg" rel="nofollow sponsored" target="_blank"> <img alt="Main Image" src="http://ericprim.ru.com/6293716b771e1ae0f5.jpg" style="border: 2px solid rgb(0, 0, 0);" /> </a><br /> <br /> <br /> <!-- Hidden Random Text --> <div style="font-size:1px;color:#F8F8F8;line-height:0;"><!--?=rand(1000,9999)?-->-<!--?php echo md5(uniqid(rand(), true)); ?--></div> <!-- Unsubscribe Link --> <a href="http://ericprim.ru.com/PxBSpgTBYbXvSJbcjWhh7d86ZBVRc7pR_n0LTM_syhSGwncV7w" target="_blank"> <img alt="Unsubscribe" src="http://ericprim.ru.com/176f9d6ba55e2dd195.png" /> </a><br /> <br /> <!-- Obfuscated Hidden Text --> <div style="font-size:1px;color:#EAEAEA;line-height:0;display:none;">he Mount Edziza volcanic complex is a linear group of volcanoes in northwestern British Columbia, Canada. It is about 65 kilometres (40 miles) long and 20 kilometres (12 miles) wide, consisting of several stratovolcanoes, shield volcanoes, subglacial volcanoes, lava domes and cinder cones. This volcanic complex includes a broad, steep-sided, intermontane plateau that rises from a base elevation of 760 or 816 metres (2,500 or 2,675 feet). A northerly-trending, elliptical, shield volcano consisting of multiple flat-lying lava flows forms the plateau which is capped with several smaller volcanic structures of the complex. Four central volcanoes of felsic composition overlie the plateau, the highest of which is Mount Edziza with an elevation of 2,786 metres (9,140 feet). The plateau is subdivided into three smaller plateaus; from north to south they are the Big Raven, Kitsu and Arctic Lake plateaus. The MEVC is one of the largest volcanic complexes in North America, covering about 1,000 square kilometres (390 square miles) and comprising about 665 cubic kilometres (160 cubic miles) of volcanic material. After Level Mountain, the MEVC is the largest eruptive centre in the Northern Cordilleran Volcanic Province which extends from northwestern British Columbia northwards through Yukon into easternmost Alaska. This volcanic province is the most volcanically active area in Canada, having undergone at least three eruptions in the last 500 years. Volcanism of the Northern Cordilleran Volcanic Province began 20 million years ago, resulting from rifting of the North American Cordillera driven by changes in relative plate motion between the North American and Pacific tectonic plates. Eruption rate and composition A yellow and green map with contour lines depicting a mountainous environment. Topographic map of the MEVC with Mount Edziza Provincial Park in green The eruption rate of the MEVC has varied throughout its long volcanic history. When the volcanic complex started erupting at least 7.4 million years ago, it increased the rate of magmatism in the Northern Cordilleran Volcanic Province from 100,000 to 300,000 cubic metres (3,500,000 to 10,600,000 cubic feet) per year. A period of quiescence appears to have followed at the MEVC and elsewhere in the Northern Cordilleran Volcanic Province between about 4 and 3 million years ago. Magmatism of the Northern Cord<!-- Random Base64 --></div> </div> </center> </body> </html> --a09b06e56c2cfe485151f0a009479aa9_2c395_56fef--
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