

{"id":1350,"date":"2016-01-08T21:21:25","date_gmt":"2016-01-08T21:21:25","guid":{"rendered":"http:\/\/www.scsn.org\/?page_id=1350"},"modified":"2021-10-07T16:33:57","modified_gmt":"2021-10-07T16:33:57","slug":"nevada-nuclear-testing","status":"publish","type":"page","link":"https:\/\/www.scsn.org\/index.php\/education-outreach-2\/understanding-waveforms\/nevada-nuclear-testing\/","title":{"rendered":"Nevada Nuclear Testing"},"content":{"rendered":"<p>From 1951 to 1992 the Nevada Test Site was the primary location for nuclear blast testing in the United States.* During this time, due to proximity and station sensitivity, the SCSN was\u00a0able to locate and catalog the seismic waves generated at the Nevada Test Site, just as if an actual large magnitude earthquake had occurred in Southern Nevada.<\/p>\n<p>Because of\u00a0the uniformly compressional nature of the radiating blast energy associated with nuclear bombs\u00a0(the first motion of the waves as they arrive at stations is away from the blast, which is upwards on a vertical sensor) these tests were very useful to the growing seismic\u00a0network. Since the waveforms were guaranteed to point up first, the blasts were used to properly calibrate the polarity of stations within the network and spot problems with analog station installation. Over the years this observed feature of nuclear testing helped to improve the accuracy and quality of the SCSN&#8217;s earthquake analysis and reporting.<\/p>\n<p>*Note:\u00a0The United States no longer utilizes the Nevada Test Site for nuclear testing.<\/p>\n<p>Below is a sample of 400 out of the &gt;600 nuclear tests that were recorded\u00a0by the SCSN from 1951 to 1992. Their magnitudes range from 1.9 to 5.8.<\/p>\n<div id=\"dashb_canvas\" class=\"google-visualization-controls-theme-plus\">\n<h5>Nuclear Blasts at the Nevada Test Site<\/h5>\n<p>Use the slider to investigate how the number and distribution of nuclear arms tests has has changed through time (map shows all tests prior to slider date). Clicking on the mushroom clouds shows you the name and equivalent earthquake magnitude of the blast during each test. (for simplicity tests have been grouped where they were performed on the same day).<br \/>\n<!--\n\n<div id=\"date_canvas\"><\/div>\n\n--><br \/>\n<!--\n\n<div id=\"nuke_canvas\"><\/div>\n\n--><\/p>\n<div id=\"nukeslider\"><\/div>\n<div id=\"map_nuke\"><\/div>\n<\/div>\n<p>Below is a multi waveform view from Bomb &#8220;Montello&#8221; on April 1991, which generated a blast with the equivalent seismic energy of a M5.06 earthquake felt by the network. Click the image for a larger comprehensive view.<\/p>\n<div id=\"attachment_1362\" style=\"width: 1510px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/www.scsn.org\/wp-content\/uploads\/nukelist.jpg\"><img decoding=\"async\" aria-describedby=\"caption-attachment-1362\" class=\"wp-image-1362 size-full\" src=\"http:\/\/www.scsn.org\/wp-content\/uploads\/nukelist.jpg\" alt=\"blast\" width=\"100%\" height=\"700\" \/><\/a><p id=\"caption-attachment-1362\" class=\"wp-caption-text\">Note that this window\u00a0is representing roughly 1 minute of time but the waveform is energetic enough that it was felt by the network for many minutes, which can be seen in the comprehensive view Below.<\/p><\/div>\n<p><script type=\"text\/javascript\">initmap(\"nukes\")<\/script><script type=\"text\/javascript\">initnukeslider()<\/script><br \/>\n<script type=\"text\/javascript\">movenukeslider()<\/script><\/p>\n","protected":false},"excerpt":{"rendered":"<p>From 1951 to 1992 the Nevada Test Site was the primary location for nuclear blast testing in the United States.* During this time, due to proximity and station sensitivity, the SCSN was\u00a0able to locate and catalog the seismic waves generated<span class=\"ellipsis\">&hellip;<\/span><\/p>\n<div class=\"read-more\"><a href=\"https:\/\/www.scsn.org\/index.php\/education-outreach-2\/understanding-waveforms\/nevada-nuclear-testing\/\">Read more &#8250;<\/a><\/div>\n<p><!-- end of .read-more --><\/p>\n","protected":false},"author":2,"featured_media":0,"parent":1938,"menu_order":6,"comment_status":"closed","ping_status":"closed","template":"responsive\/sidebar-content-page.php","meta":{"footnotes":""},"class_list":["post-1350","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/pages\/1350","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/comments?post=1350"}],"version-history":[{"count":37,"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/pages\/1350\/revisions"}],"predecessor-version":[{"id":4089,"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/pages\/1350\/revisions\/4089"}],"up":[{"embeddable":true,"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/pages\/1938"}],"wp:attachment":[{"href":"https:\/\/www.scsn.org\/index.php\/wp-json\/wp\/v2\/media?parent=1350"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}