{"id":649,"date":"2008-05-20T22:53:00","date_gmt":"2008-05-20T22:53:00","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/2008\/05\/20\/the-problem-of-cracks-in-mountains-after-earthquakes\/"},"modified":"2010-10-21T13:55:26","modified_gmt":"2010-10-21T17:55:26","slug":"the-problem-of-cracks-in-mountains-after-earthquakes","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2008\/05\/20\/the-problem-of-cracks-in-mountains-after-earthquakes\/","title":{"rendered":"The problem of cracks in mountains after earthquakes"},"content":{"rendered":"<p><a href=\"http:\/\/news.xinhuanet.com\/english\/2008-05\/20\/content_8215687.htm\"><span class=\"blsp-spelling-error\">Xinhua<\/span><\/a> is today reporting the following:<br \/><span style=\"font-family: verdana;font-size:85%\"><br \/>Nearly 9,000 people in a quake zone were evacuated on  Tuesday for fear that huge cracks on a mountain could lead to further disasters.<\/span><span style=\"font-family: verdana;font-size:85%\">    Many crevices, measuring up to 1,500 meters long, 250  m high and 50 centimeters wide, have been spotted on the <span class=\"blsp-spelling-error\">Shiziliang<\/span> Mountain in  the <span class=\"blsp-spelling-error\">Qingchuan<\/span> County seat, <span class=\"blsp-spelling-error\">Guangyuan<\/span> City, since Sunday, threatening about  50,000 people and quake-relief soldiers.<\/span><span style=\"font-family: verdana;font-size:85%\">    Part of the mountain, distorted in the 8.0-magnitude  earthquake and many aftershocks over the past week, has sunk about 1 meter and  caused many road works to cave in.<\/span><span style=\"font-family: verdana;font-size:85%\">    A house at the foot of the mountain was damaged by a  falling boulder.<\/span><span style=\"font-family: verdana;font-size:85%\">    Any new aftershock or heavy rainfall in the area  could trigger serious landslides and cause casualties, according to the quake  relief headquarters at the site.<\/span><span style=\"font-family: verdana;font-size:85%\">    The local government on Tuesday launched an emergency  evacuation of 9,000 residents near the mountain. The area has been cordoned off  and is under round-the-clock monitoring.<\/span><\/p>\n<p>Reading this <span class=\"blsp-spelling-error\">gave<\/span> me a very strong sense of <span class=\"blsp-spelling-error\">deja<\/span> <span class=\"blsp-spelling-error\">vu<\/span>.  One of the greatest challenges in Pakistan after the 2005 earthquake was trying to interpret the meaning of similar crack networks, which we found all over the hillsides.  The following two images show what these looked like.<\/p>\n<div style=\"text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/PICT0049.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/PICT0049.jpg\" alt=\"\" border=\"0\" \/><\/a><span style=\"font-size:85%\"><span style=\"font-family: verdana\">A cracked slope near to <span class=\"blsp-spelling-error\">Muzaffarabad<\/span> in Kashmir after the 2005 earthquake (click for a bigger image).  Cracked slopes like this occurred throughout the earthquake zone.  To date very few have led to a slope failure, but we remain very concerned by them.<\/span><\/span><\/div>\n<p><\/p>\n<div style=\"text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/PICT0021.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/PICT0021.jpg\" alt=\"\" border=\"0\" \/><\/a><span style=\"font-size:85%\"><span style=\"font-family: verdana\">A further cracked slope near to <span class=\"blsp-spelling-error\">Muzaffarabad<\/span> in Kashmir after the 2005 earthquake (click for a bigger image).  Note that in this case the cracks are very close to a steep cliff.  Nonetheless, this slope has still not failed.<\/span><\/span><\/div>\n<p>In Pakistan we assumed that these were incipient landslides and worked with the authorities to move people off the worst affected areas before the monsoon.  We also put instruments to measure four of the most notable sites.  However, this was only an assumption.  As it turned out, almost none of these slopes have to date failed.  We don&#8217;t know why.  Are they in fact not landslides at all &#8211; if so, what are they?  If they are landslides, are they in fact sufficiently stable that they can only move in a large earthquake?  Or are they incipient landslides, but they have not failed yet as the rainfall associated with the two monsoons (2006 and 2007) since the earthquake has not been intense in this area (which is the case)?  I must admit that I err on the latter, and worry greatly <span class=\"blsp-spelling-error\">about<\/span> what will happen in Pakistan in the next really strong monsoon.<\/p>\n<p>In <span class=\"blsp-spelling-error\">Sichuan<\/span>, I would be willing to bet that close inspection will reveal that these cracks also occur very extensively across the landscape.  Once again the same conundrum will occur.  In the case described by <span class=\"blsp-spelling-error\">Xinhua<\/span> above the authorities are absolutely right to be cautious, especially if it is actually moving.  Evacuation and monitoring appears to be the correct approach.  I suspect that this drama will play out in many other places.  In Kashmir essentially no resource was dedicated to finding out what these cracks actually meant.  I hope very much that this is not repeated in <span class=\"blsp-spelling-error\">Sichuan<\/span>.<\/p>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>Xinhua is today reporting the following:Nearly 9,000 people in a quake zone were evacuated on Tuesday for fear that huge cracks on a mountain could lead to further disasters. Many crevices, measuring up to 1,500 meters long, 250 m high and 50 centimeters wide, have been spotted on the Shiziliang Mountain in the Qingchuan County seat, Guangyuan City, since Sunday, threatening about 50,000 people and quake-relief soldiers. Part of the &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":""},"categories":[1],"tags":[333,16,412,23,959,132],"class_list":["post-649","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-333","tag-china","tag-cracks","tag-earthquake","tag-landslide-report","tag-sichuan"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/649","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=649"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/649\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=649"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=649"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=649"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}