{"id":180144,"date":"2021-02-17T00:36:59","date_gmt":"2021-02-16T21:36:59","guid":{"rendered":"https:\/\/en.buradabiliyorum.com\/slow-motion-precursors-give-earthquakes-the-fast-slip\/"},"modified":"2021-02-17T00:36:59","modified_gmt":"2021-02-16T21:36:59","slug":"slow-motion-precursors-give-earthquakes-the-fast-slip","status":"publish","type":"post","link":"https:\/\/buradabiliyorum.com\/en\/slow-motion-precursors-give-earthquakes-the-fast-slip\/","title":{"rendered":"#Slow motion precursors give earthquakes the fast slip"},"content":{"rendered":"<p>&#8220;<strong>#Slow motion precursors give earthquakes the fast slip<\/strong>&#8221;<\/p>\n<div>\n<div class=\"article-gallery lightGallery\">\n<div data-thumb=\"https:\/\/scx1.b-cdn.net\/csz\/news\/tmb\/2021\/slowmotionpr.jpg\" data-src=\"https:\/\/scx2.b-cdn.net\/gfx\/news\/2021\/slowmotionpr.jpg\" data-sub-html=\"Matthew Siegfried inspects a GPS device, powered by a solar panel at Whillans Ice Plain. Grace Barcheck\/Cornell University. Credit: Cornell University\">\n<figure class=\"article-img\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/scx1.b-cdn.net\/csz\/news\/800a\/2021\/slowmotionpr.jpg\" alt=\"Slow motion precursors give earthquakes the fast slip\" title=\"Matthew Siegfried inspects a GPS device, powered by a solar panel at Whillans Ice Plain. Grace Barcheck\/Cornell University. Credit: Cornell University\" width=\"800\" height=\"450\"\/><figcaption class=\"text-darken text-low-up text-truncate-js text-truncate mt-3\">\n                Matthew Siegfried inspects a GPS device, powered by a solar panel at Whillans Ice Plain. Grace Barcheck\/Cornell University. Credit: Cornell University<br \/>\n            <\/figcaption><\/figure>\n<\/div>\n<\/div>\n<p>At a glacier near the South Pole, earth scientists have found evidence of a quiet, slow-motion fault slip that triggers strong, fast-slip earthquakes many miles away, according to Cornell University research published in <i><a href=\"https:\/\/buradabiliyorum.com\/en\/category\/sciencee\/\" data-internallinksmanager029f6b8e52c=\"5\" title=\"Science\" target=\"_blank\" rel=\"noopener\">Science<\/a> Advances<\/i>.<\/p>\n<section class=\"article-banner first-banner ads-336x280\"><!-- \/4988204\/Phys_Story_InText_Box --><br \/>\n      <\/section>\n<p>During an earthquake, a fast slip h<a href=\"https:\/\/buradabiliyorum.com\/en\/category\/download-scripts-themes-apps\/\" data-internallinksmanager029f6b8e52c=\"9\" title=\"Download Scripts &amp; Themes &amp; Apps\" target=\"_blank\" rel=\"noopener\">app<\/a>ens when energy builds up underground and is released quickly along a fault. Blocks of earth rapidly slide against one another.<\/p>\n<p>However, at an Antarctic glacier called Whillans Ice Plain, the earth scientists show that &#8220;slow slips&#8221; precede dozens of large magnitude 7 earthquakes. &#8220;We found that there is almost always a precursory &#8216;slow slip&#8217; before an earthquake,&#8221; said lead author Grace Barcheck, research associate in Earth and Atmospheric Sciences at Cornell University.<\/p>\n<p>Barcheck said that these slow-slip precursors\u2014occurring as far as 20 miles away from the epicenter\u2014are directly involved in starting the earthquake. &#8220;These slow slips are remarkably common,&#8221; she said, &#8220;and they migrate toward where the fast earthquake slip starts.&#8221;<\/p>\n<p>Observations before several large tsunami-generating magnitude 8 and 9 earthquakes on subduction zone faults suggest a similar process may have occurred, according to Patrick Fulton, assistant professor and Croll Sesquicentennial Fellow in the Department of Earth and Atmospheric Sciences.<\/p>\n<p>As these faults are mostly offshore and deep underwater, and because it is difficult to know when or where a large earthquake will occur, the start of large earthquakes is <a href=\"https:\/\/buradabiliyorum.com\/en\/category\/general\/\" data-internallinksmanager029f6b8e52c=\"3\" title=\"General\" target=\"_blank\" rel=\"noopener\">general<\/a>ly hard to observe.<\/p>\n<p>To overcome these challenges, the scientists placed GPS sensors above an icy glacial fault at Whillans Ice Plain, where large magnitude 7 earthquakes occur nearly twice a day over a 60-mile-wide area of the glacier.<\/p>\n<p>Within a period of two months in 2014, the group captured 75 earthquakes at the bottom of the Antarctic glacier. Data from GPS stations indicated that 73\u2014or 96% &#8211; of the 75 earthquakes showed a period of precursory slow motion.<\/p>\n<p>The data from the GPS tracking stations and surface seismometers allowed the team to identify how the slow precursory slip triggers the fast earthquake slip.<\/p>\n<p>&#8220;Our group was a little surprised to see so many precursors,&#8221; Barcheck said.<\/p>\n<p>&#8220;In some cases, we can actually see the migration of the earthquake precursor towards where the earthquake begins.&#8221;<\/p>\n<p>&#8220;Before we pored over the data, I thought that if we saw any precursors before the earthquakes, they would be rare and in the same place as the earthquake epicenter,&#8221; she said. &#8220;Instead, we found many slow-slip precursors\u2014starting miles from the epicenters and migrating across the fault.&#8221;<\/p>\n<p>Field work and analysis for this research was supported by the National Science Foundation.<\/p>\n<hr\/>\n<div class=\"article-main__explore my-4 d-print-none\">\n<p>                                            Deep, slow-slip action may direct largest earthquakes and their tsunamis\n                                        <\/p><\/div>\n<hr class=\"mb-4\"\/>\n<div class=\"article-main__more p-4\">\n                                                                                                <strong>More information:<\/strong><br \/>\n                                                G. Barcheck et al, Migratory earthquake precursors are dominant on an ice stream fault, <i>Science Advances<\/i> (2021).  <a rel=\"nofollow noopener\" target=\"_blank\" data-doi=\"1\" href=\"http:\/\/dx.doi.org\/10.1126\/sciadv.abd0105\">DOI: 10.1126\/sciadv.abd0105<\/a><\/p><\/div>\n<div class=\"d-inline-block text-medium my-4\">\n                                                Provided by<br \/>\n                                                                                                    Cornell University<br \/>\n                                                                                                        <a rel=\"nofollow noopener\" target=\"_blank\" class=\"icon_open\" href=\"http:\/\/www.cornell.edu\/\"><br \/>\n                                                        <svg><use href=\"https:\/\/phys.b-cdn.net\/tmpl\/v6\/img\/svg\/sprite.svg#icon_open\" x=\"0\" y=\"0\"\/><\/svg><\/a><\/p><\/div>\n<p>                                        <!-- print only --><\/p>\n<div class=\"d-none d-print-block\">\n<p>                                                 <strong>Citation<\/strong>:<br \/>\n                                                 Slow motion precursors give earthquakes the fast slip (2021, February 16)<br \/>\n                                                 retrieved 16 February 2021<br \/>\n                                                 from https:\/\/phys.org\/<a href=\"https:\/\/buradabiliyorum.com\/en\/category\/news\/\" data-internallinksmanager029f6b8e52c=\"2\" title=\"News\" target=\"_blank\" rel=\"noopener\">news<\/a>\/2021-02-motion-precursors-earthquakes-fast.html<\/p>\n<p>                                            This document is subject to copyright. 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Grace Barcheck\/Cornell University. Credit: Cornell University At a glacier near the South Pole, earth scientists have found evidence of a quiet, slow-motion fault slip that triggers strong, fast-slip earthquakes many miles away,&#8230;<\/p>\n","protected":false},"author":1,"featured_media":180145,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"fifu_image_url":"https:\/\/scx2.b-cdn.net\/gfx\/news\/2021\/slowmotionpr.jpg","fifu_image_alt":"","footnotes":""},"categories":[16],"tags":[],"class_list":["post-180144","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-sciencee"],"_links":{"self":[{"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/posts\/180144","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/comments?post=180144"}],"version-history":[{"count":0,"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/posts\/180144\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/media\/180145"}],"wp:attachment":[{"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/media?parent=180144"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/categories?post=180144"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/buradabiliyorum.com\/en\/wp-json\/wp\/v2\/tags?post=180144"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}