{"id":351,"date":"2021-04-15T12:54:57","date_gmt":"2021-04-15T18:54:57","guid":{"rendered":"https:\/\/osbge.org\/?p=351"},"modified":"2021-04-15T12:54:57","modified_gmt":"2021-04-15T18:54:57","slug":"why-are-there-relatively-few-aftershocks-for-certain-cascadia-earthquakes","status":"publish","type":"post","link":"https:\/\/osbge.org\/index.php\/2021\/04\/15\/why-are-there-relatively-few-aftershocks-for-certain-cascadia-earthquakes\/","title":{"rendered":"Why are there relatively few aftershocks for certain cascadia earthquakes?"},"content":{"rendered":"<p>In the Cascadia subduction zone, medium and large-sized &#8216;intraslab&#8217; earthquakes, which take place at greater than crustal depths within the subducting plate, will likely produce only a few detectable aftershocks, according to a new study. <\/p>\n<p>Title: Why are there relatively few aftershocks for certain cascadia earthquakes?<br \/>Sourced From: www.sciencedaily.com\/releases\/2021\/04\/210413121012.htm<br \/>Published Date: Tue, 13 Apr 2021 12:10:12 EDT<\/p>\n<p><\/p>\n<p>News&#8230;. <a href=\"https:\/\/news.wcmo.edu\/success\/alumnus-brian-boatright-appointed-chief-justice-of-colorado-supreme-court\/\">browse around here<\/a><\/p>\n<p><\/p>\n<\/p>\n<p><\/p>\n<p><p><\/p>\n<div style=\"text-align: center;\"><iframe loading=\"lazy\" src=\"https:\/\/chart.googleapis.com\/chart?chs=150x150&amp;cht=qr&amp;chl=https:\/\/twitter.com\/i\/topics\/news\/e197880795?cn=ZmxleGlibGVfcmVjcw?denver News\" style=\"border:0px #ffffff none;\" name=\"myiFrame\" scrolling=\"no\" marginheight=\"0px\" marginwidth=\"0px\" height=\"400px\" width=\"600px\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/div>\n<p>\n<a href=\"https:\/\/twitter.com\/i\/topics\/news\/e2016931374?cn=ZmxleGlibGVfcmVjcw\">check this link right here now<\/a>\n<\/p>\n<\/p>\n<p><\/p>\n<p><!-- start www.rssground.com code snippet --><br \/>\n<iframe loading=\"lazy\" src=\"\/\/www.rssground.com\/services\/rss-converter\/5fb2c53cdf142\/CCN%20NDT%20NDN\" width=\"100%\" height=\"100%\" scrolling=\"yes\" align=\"middle\" frameborder=\"0\" style=\"background: transparent\">Your browser does not support inline frames or is currently configured not to display inline frames.<\/iframe><br \/>\n<!-- end www.rssground.com code snippet --><br \/>Did you miss our previous article&#8230; <br \/><a href=\"https:\/\/osbge.org\/index.php\/2021\/04\/13\/mountain-growth-influences-greenhouse-effect\/\">https:\/\/osbge.org\/index.php\/2021\/04\/13\/mountain-growth-influences-greenhouse-effect\/<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>In the Cascadia subduction zone, medium and large-sized &#8216;intraslab&#8217; earthquakes, which take place at greater than crustal depths within the subducting plate, will likely produce only a few detectable aftershocks, according to a new study. Title: Why are there relatively few aftershocks for certain cascadia earthquakes?Sourced From: www.sciencedaily.com\/releases\/2021\/04\/210413121012.htmPublished Date: Tue, 13 Apr 2021 12:10:12 EDT <a href=\"https:\/\/osbge.org\/index.php\/2021\/04\/15\/why-are-there-relatively-few-aftershocks-for-certain-cascadia-earthquakes\/\" class=\"more-link\">&#8230;<span class=\"screen-reader-text\">  Why are there relatively few aftershocks for certain cascadia earthquakes?<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[3],"class_list":["post-351","post","type-post","status-publish","format-standard","hentry","category-news","tag-geology-news"],"jetpack_featured_media_url":"","_links":{"self":[{"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/posts\/351","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/comments?post=351"}],"version-history":[{"count":1,"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/posts\/351\/revisions"}],"predecessor-version":[{"id":352,"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/posts\/351\/revisions\/352"}],"wp:attachment":[{"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/media?parent=351"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/categories?post=351"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/osbge.org\/index.php\/wp-json\/wp\/v2\/tags?post=351"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}