{"id":366,"date":"2014-03-10T13:44:22","date_gmt":"2014-03-10T13:44:22","guid":{"rendered":"http:\/\/www.geol.umd.edu\/facilities\/seismology\/?p=366"},"modified":"2014-03-10T13:47:34","modified_gmt":"2014-03-10T13:47:34","slug":"lithospheric-structure-of-the-western-united-states","status":"publish","type":"post","link":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/lithospheric-structure-of-the-western-united-states\/","title":{"rendered":"Lithospheric Structure of the Western United States"},"content":{"rendered":"<p>Using data from the EarthScope Transportable Array, we observed and modeled conversions of S waves to P waves across velocity contrasts within the lithosphere across the Western United States. You can read more about our findings in Lekic and Fischer, 2013 and Hopper et al. 2014, but this cartoon provides a nice summary:<\/p>\n<p><a href=\"http:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2014\/03\/WesternUS_Lithosphere.png\"><img loading=\"lazy\" decoding=\"async\" class=\"alignleft size-full wp-image-370\" alt=\"WesternUS_Lithosphere\" src=\"http:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2014\/03\/WesternUS_Lithosphere.png\" width=\"1283\" height=\"373\" srcset=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2014\/03\/WesternUS_Lithosphere.png 1283w, https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2014\/03\/WesternUS_Lithosphere-300x87.png 300w, https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2014\/03\/WesternUS_Lithosphere-1024x297.png 1024w\" sizes=\"auto, (max-width: 1283px) 100vw, 1283px\" \/><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Using data from the EarthScope Transportable Array, we observed and modeled conversions of S waves to P waves across velocity contrasts within the lithosphere across the Western United States. You can read more about our findings in Lekic and Fischer, 2013 and Hopper et al. 2014, but this cartoon provides a nice summary:<\/p>\n","protected":false},"author":2,"featured_media":370,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[5],"tags":[],"class_list":["post-366","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research"],"_links":{"self":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/posts\/366","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/comments?post=366"}],"version-history":[{"count":3,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/posts\/366\/revisions"}],"predecessor-version":[{"id":369,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/posts\/366\/revisions\/369"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/media\/370"}],"wp:attachment":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/media?parent=366"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/categories?post=366"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/tags?post=366"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}