{"id":1383,"date":"2015-08-03T23:02:40","date_gmt":"2015-08-03T23:02:40","guid":{"rendered":"https:\/\/courses.candelalearning.com\/earthscienceck12\/?post_type=chapter&#038;p=1383"},"modified":"2015-08-03T23:06:35","modified_gmt":"2015-08-03T23:06:35","slug":"video-violent-volcanoes","status":"publish","type":"chapter","link":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/chapter\/video-violent-volcanoes\/","title":{"raw":"Videos: Violent Volcanoes","rendered":"Videos: Violent Volcanoes"},"content":{"raw":"Prior to the Mount St. Helens eruption in 1980, the Lassen Peak eruption on May 22, 1915, was the most recent Cascades eruption. A column of ash and gas shot 30,000 feet into the air. This triggered a high-speed pyroclastic flow, which melted snow and created a volcanic mudflow known as a\u00a0<strong>lahar<\/strong>.\u00a0Lassen Peak currently has geothermal activity and could erupt explosively again. Mt. Shasta, the other active volcano in California, erupts every 600 to 800 years. An eruption would most likely create a large pyroclastic flow, and probably a lahar. Of course, Mt. Shasta could explode and collapse like Mt. Mazama in Oregon.\r\n\r\nhttps:\/\/www.youtube.com\/watch?v=s2i4XS0Esks\r\n\r\nMafic magma creates gentler\u00a0<strong>effusive eruptions<\/strong>. Although the pressure builds enough for the magma to erupt, it does not erupt with the same explosive force as felsic magma. People can usually be evacuated before an effusive eruption, so they are much less deadly. Magma pushes toward the surface through fissures and reaches the surface through volcanic vents.\u00a0<a title=\"\" href=\"http:\/\/hvo.wr.usgs.gov\/multimedia\/archive\/2009\/Nov\/OverflightFLIR_13Jan2010.mov\" target=\"_blank\">Click here<\/a>\u00a0to view a lava stream within the vent of a Hawaiian volcano using a thermal camera.\r\n\r\nhttps:\/\/www.youtube.com\/watch?v=BtH79yxBIJI\r\n\r\n&nbsp;","rendered":"<p>Prior to the Mount St. Helens eruption in 1980, the Lassen Peak eruption on May 22, 1915, was the most recent Cascades eruption. A column of ash and gas shot 30,000 feet into the air. This triggered a high-speed pyroclastic flow, which melted snow and created a volcanic mudflow known as a\u00a0<strong>lahar<\/strong>.\u00a0Lassen Peak currently has geothermal activity and could erupt explosively again. Mt. Shasta, the other active volcano in California, erupts every 600 to 800 years. An eruption would most likely create a large pyroclastic flow, and probably a lahar. Of course, Mt. Shasta could explode and collapse like Mt. Mazama in Oregon.<\/p>\n<p><iframe loading=\"lazy\" id=\"oembed-1\" title=\"Violent Volcanoes | National Geographic\" width=\"500\" height=\"375\" src=\"https:\/\/www.youtube.com\/embed\/s2i4XS0Esks?feature=oembed&#38;rel=0\" frameborder=\"0\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/p>\n<p>Mafic magma creates gentler\u00a0<strong>effusive eruptions<\/strong>. Although the pressure builds enough for the magma to erupt, it does not erupt with the same explosive force as felsic magma. People can usually be evacuated before an effusive eruption, so they are much less deadly. Magma pushes toward the surface through fissures and reaches the surface through volcanic vents.\u00a0<a title=\"\" href=\"http:\/\/hvo.wr.usgs.gov\/multimedia\/archive\/2009\/Nov\/OverflightFLIR_13Jan2010.mov\" target=\"_blank\">Click here<\/a>\u00a0to view a lava stream within the vent of a Hawaiian volcano using a thermal camera.<\/p>\n<p><iframe loading=\"lazy\" id=\"oembed-2\" title=\"Kilauea Eruption October 12\" width=\"500\" height=\"375\" src=\"https:\/\/www.youtube.com\/embed\/BtH79yxBIJI?feature=oembed&#38;rel=0\" frameborder=\"0\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/p>\n<p>&nbsp;<\/p>\n\n\t\t\t <section class=\"citations-section\" role=\"contentinfo\">\n\t\t\t <h3>Candela Citations<\/h3>\n\t\t\t\t\t <div>\n\t\t\t\t\t\t <div id=\"citation-list-1383\">\n\t\t\t\t\t\t\t <div class=\"licensing\"><div class=\"license-attribution-dropdown-subheading\">All rights reserved content<\/div><ul class=\"citation-list\"><li>Violent Volcanoes. <strong>Authored by<\/strong>: National Geographic. <strong>Provided by<\/strong>: Youtube. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"https:\/\/www.youtube.com\/watch?v=s2i4XS0Esks\">https:\/\/www.youtube.com\/watch?v=s2i4XS0Esks<\/a>. <strong>License<\/strong>: <em>All Rights Reserved<\/em>. <strong>License Terms<\/strong>: Standard Youtube License<\/li><li>Kilauea Eruption October 12. <strong>Authored by<\/strong>: WIRED. <strong>Provided by<\/strong>: Youtube. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"https:\/\/www.youtube.com\/watch?v=BtH79yxBIJI\">https:\/\/www.youtube.com\/watch?v=BtH79yxBIJI<\/a>. <strong>License<\/strong>: <em>All Rights Reserved<\/em>. <strong>License Terms<\/strong>: Standard Youtube License<\/li><\/ul><\/div>\n\t\t\t\t\t\t <\/div>\n\t\t\t\t\t <\/div>\n\t\t\t <\/section>","protected":false},"author":1367,"menu_order":4,"template":"","meta":{"_candela_citation":"[{\"type\":\"copyrighted_video\",\"description\":\"Violent Volcanoes\",\"author\":\"National Geographic\",\"organization\":\"Youtube\",\"url\":\"https:\/\/www.youtube.com\/watch?v=s2i4XS0Esks\",\"project\":\"\",\"license\":\"arr\",\"license_terms\":\"Standard Youtube License\"},{\"type\":\"copyrighted_video\",\"description\":\"Kilauea Eruption October 12\",\"author\":\"WIRED\",\"organization\":\"Youtube\",\"url\":\"https:\/\/www.youtube.com\/watch?v=BtH79yxBIJI\",\"project\":\"\",\"license\":\"arr\",\"license_terms\":\"Standard Youtube License\"}]","CANDELA_OUTCOMES_GUID":"","pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-1383","chapter","type-chapter","status-publish","hentry"],"part":1286,"_links":{"self":[{"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/pressbooks\/v2\/chapters\/1383","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/wp\/v2\/users\/1367"}],"version-history":[{"count":3,"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/pressbooks\/v2\/chapters\/1383\/revisions"}],"predecessor-version":[{"id":1386,"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/pressbooks\/v2\/chapters\/1383\/revisions\/1386"}],"part":[{"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/pressbooks\/v2\/parts\/1286"}],"metadata":[{"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/pressbooks\/v2\/chapters\/1383\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/wp\/v2\/media?parent=1383"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/pressbooks\/v2\/chapter-type?post=1383"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/wp\/v2\/contributor?post=1383"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/earthscienceck12\/wp-json\/wp\/v2\/license?post=1383"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}