{"id":606,"date":"2008-07-08T05:26:00","date_gmt":"2008-07-08T05:26:00","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/2008\/07\/08\/rockfalls-from-the-eiger\/"},"modified":"2010-10-21T13:55:13","modified_gmt":"2010-10-21T17:55:13","slug":"rockfalls-from-the-eiger","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2008\/07\/08\/rockfalls-from-the-eiger\/","title":{"rendered":"Rockfalls from the Eiger"},"content":{"rendered":"<p>In 2006 Hans Rudolf <span class=\"blsp-spelling-error\">Keusen<\/span> of <a href=\"http:\/\/www.geotest.ch\/index.cfm\/fuseaction\/show\/path\/1-285.htm\"><span class=\"blsp-spelling-error\">Geotest<\/span><\/a> raised concerns that a large pillar on the <span class=\"blsp-spelling-error\">Eiger<\/span> mountain in Switzerland had become unstable.  Over the next few weeks the pillar did indeed progressively fail, providing some amazing images of a large rockfall in action (Fig 1):<\/p>\n<div style=\"text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_07-eiger-1.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_07-eiger-1.jpg\" alt=\"\" border=\"0\" \/><\/a><span style=\"font-size:85%\"><span style=\"font-family:verdana\"><a href=\"http:\/\/media.npr.org\/programs\/morning\/features\/2007\/aug\/rocks\/rockfall400.jpg\"><span style=\"font-weight: bold\">Figure 1:<\/span> AP image<\/a> entitled: On July 13, 2006, masses of rock fell down from <span class=\"blsp-spelling-error\">Eiger<\/span>, near <span class=\"blsp-spelling-error\">Grindelwald<\/span>. The event came after days of warnings from scientists regarding rock loosened by melting glacial ice.<\/span><\/span><\/div>\n<p class=\"caption\">\n<p>    Yesterday, Hans Rudolf <span class=\"blsp-spelling-error\">Keusen<\/span> again warned of the dangers of summer rockfalls on the <span class=\"blsp-spelling-error\">Eiger<\/span>.  Once again, rockfalls have been occurring on the northwest side of the mountain, associated with the melting of the Lower <span class=\"blsp-spelling-error\">Grindelwald<\/span> glacier, which has left the flank of the mountain unsupported.  The concern this time is that a rockfall could fall into a small lake at the toe of the slope, displacing &#8220;up to 900,000 cubic metres of water&#8230;in the space of several hours&#8221; (see <a href=\"http:\/\/www.swissinfo.ch\/eng\/news_digest\/Crumbling_Eiger_rock_prompts_new_concern.html?siteSect=104&amp;sid=9306588&amp;cKey=1215457445000&amp;ty=nd\">here<\/a>).  Fortunately, monitoring systems are in place to detect any sudden rises in lake level, so a warning should be available.<\/p>\n<p>The <a href=\"http:\/\/glaciology.ethz.ch\/messnetz\/index.html\">Swiss Glacier Monitoring Network<\/a> has a rather nice image of the glacier in question (Fig. 2):<\/p>\n<div style=\"text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_07-eiger-2.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_07-eiger-2.jpg\" alt=\"\" border=\"0\" \/><\/a><span style=\"font-size:85%\"><span style=\"font-family:verdana\"><span style=\"font-weight: bold\">Fig 2. <\/span><a href=\"http:\/\/glaciology.ethz.ch\/messnetz\/index.html\">Swiss Glacier Monitoring Network<\/a> image of the Lower <span class=\"blsp-spelling-error\">Grindelwald<\/span> glacier, showing the <span class=\"blsp-spelling-error\">debuttressed<\/span> slopes above the moraines deposited by the glacier as it retreated.<\/span><\/span><\/div>\n<p>The magnitude of the problem is well-illustrated by annual <span class=\"blsp-spelling-corrected\">monitoring<\/span> data that they have collected on the length of the glacier (Fig. 3).  This shows the dramatic retreat of the glacier over a century, in which more than a kilometre has been lost.  Unfortunately the data only extends to 1983, but the current average retreat rate is about 20 m per year.<\/p>\n<div style=\"text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_07-Eiger-3.png\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_07-Eiger-3.png\" alt=\"\" border=\"0\" \/><\/a><span style=\"font-size:85%\"><span style=\"font-family:verdana\"><span style=\"font-weight: bold\">Fig 3. <\/span><a href=\"http:\/\/glaciology.ethz.ch\/messnetz\/glaciers\/untgrindelwald.html?locale=en\">Swiss Glacier Monitoring Network graph<\/a> of the length of the Lower <span class=\"blsp-spelling-error\">Grindelwald<\/span> glacier in the period 1879 to 1983.<\/span><\/span><\/div>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>In 2006 Hans Rudolf Keusen of Geotest raised concerns that a large pillar on the Eiger mountain in Switzerland had become unstable. Over the next few weeks the pillar did indeed progressively fail, providing some amazing images of a large rockfall in action (Fig 1): Figure 1: AP image entitled: On July 13, 2006, masses of rock fell down from Eiger, near Grindelwald. The event came after days of warnings &hellip;<!-- AddThis Advanced Settings generic via filter on wp_trim_excerpt --><!-- AddThis Share Buttons generic via filter on wp_trim_excerpt --><\/p>\n","protected":false},"author":22,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":"","_members_access_role":[],"_members_access_error":""},"categories":[1],"tags":[333,447,446,56],"class_list":["post-606","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-333","tag-alps","tag-eiger","tag-rockfall"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/606","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/users\/22"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/comments?post=606"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/606\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=606"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=606"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=606"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}