{"id":497,"date":"2015-09-22T22:21:55","date_gmt":"2015-09-22T22:21:55","guid":{"rendered":"https:\/\/courses.candelalearning.com\/geophysical\/?post_type=chapter&#038;p=497"},"modified":"2017-04-19T22:06:03","modified_gmt":"2017-04-19T22:06:03","slug":"causes-of-earthquakes","status":"publish","type":"chapter","link":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/chapter\/causes-of-earthquakes\/","title":{"raw":"Causes of Earthquakes","rendered":"Causes of Earthquakes"},"content":{"raw":"An <strong>earthquake<\/strong> is sudden ground movement caused by the sudden release of energy stored in rocks, called the <strong><a title=\"\" href=\"http:\/\/earthquake.usgs.gov\/learn\/animations\/animation.php?flash_title=Elastic+Rebound&amp;flash_file=elasticrebound&amp;flash_width=300&amp;flash_height=350\" target=\"_blank\">elastic rebound theory<\/a><\/strong>. Earthquakes happen when so much stress builds up in the rocks that the rocks rupture. The energy is transmitted by seismic waves. Each year there are more than 150,000 earthquakes strong enough to be felt by people and 900,000 recorded by seismometers!\r\n\r\nIn an earthquake, the initial point where the rocks rupture in the crust is called the <strong>focus\u00a0<\/strong>(sometimes called the <strong>hypocenter<\/strong>). The <strong>epicenter<\/strong> is the point on the land surface that is directly above the focus. In about 75% of earthquakes, the focus is in the top 10 to 15 kilometers (6 to 9 miles) of the crust. <strong>Shallow earthquakes<\/strong> cause the most damage because the focus is near where people live. However, it is the epicenter of an earthquake that is reported by scientists and the media.\r\n\r\nhttps:\/\/youtu.be\/VSgB1IWr6O4\r\n\r\nhttps:\/\/youtu.be\/cavq2HFBa-U","rendered":"<p>An <strong>earthquake<\/strong> is sudden ground movement caused by the sudden release of energy stored in rocks, called the <strong><a title=\"\" href=\"http:\/\/earthquake.usgs.gov\/learn\/animations\/animation.php?flash_title=Elastic+Rebound&amp;flash_file=elasticrebound&amp;flash_width=300&amp;flash_height=350\" target=\"_blank\">elastic rebound theory<\/a><\/strong>. Earthquakes happen when so much stress builds up in the rocks that the rocks rupture. The energy is transmitted by seismic waves. Each year there are more than 150,000 earthquakes strong enough to be felt by people and 900,000 recorded by seismometers!<\/p>\n<p>In an earthquake, the initial point where the rocks rupture in the crust is called the <strong>focus\u00a0<\/strong>(sometimes called the <strong>hypocenter<\/strong>). The <strong>epicenter<\/strong> is the point on the land surface that is directly above the focus. In about 75% of earthquakes, the focus is in the top 10 to 15 kilometers (6 to 9 miles) of the crust. <strong>Shallow earthquakes<\/strong> cause the most damage because the focus is near where people live. However, it is the epicenter of an earthquake that is reported by scientists and the media.<\/p>\n<p><iframe loading=\"lazy\" id=\"oembed-1\" title=\"Earthquakes 101 | National Geographic\" width=\"500\" height=\"375\" src=\"https:\/\/www.youtube.com\/embed\/VSgB1IWr6O4?feature=oembed&#38;rel=0\" frameborder=\"0\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/p>\n<p><iframe loading=\"lazy\" id=\"oembed-2\" title=\"Understanding Earthquakes | National Geographic\" width=\"500\" height=\"281\" src=\"https:\/\/www.youtube.com\/embed\/cavq2HFBa-U?feature=oembed&#38;rel=0\" frameborder=\"0\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/p>\n\n\t\t\t <section class=\"citations-section\" role=\"contentinfo\">\n\t\t\t <h3>Candela Citations<\/h3>\n\t\t\t\t\t <div>\n\t\t\t\t\t\t <div id=\"citation-list-497\">\n\t\t\t\t\t\t\t <div class=\"licensing\"><div class=\"license-attribution-dropdown-subheading\">CC licensed content, Shared previously<\/div><ul class=\"citation-list\"><li>Dynamic Earth: Introduction to Physical Geography. <strong>Authored by<\/strong>: R. Adam Dastrup. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"http:\/\/www.opengeography.org\/physical-geography.html\">http:\/\/www.opengeography.org\/physical-geography.html<\/a>. <strong>Project<\/strong>: Open Geography Education. <strong>License<\/strong>: <em><a target=\"_blank\" rel=\"license\" href=\"https:\/\/creativecommons.org\/licenses\/by-sa\/4.0\/\">CC BY-SA: Attribution-ShareAlike<\/a><\/em><\/li><\/ul><div class=\"license-attribution-dropdown-subheading\">All rights reserved content<\/div><ul class=\"citation-list\"><li>Earthquakes 101. <strong>Authored by<\/strong>: National Geographic. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"https:\/\/youtu.be\/VSgB1IWr6O4\">https:\/\/youtu.be\/VSgB1IWr6O4<\/a>. <strong>License<\/strong>: <em>All Rights Reserved<\/em>. <strong>License Terms<\/strong>: Standard YouTube License<\/li><li>Understanding Earthquakes. <strong>Authored by<\/strong>: National Geographic . <strong>Located at<\/strong>: <a target=\"_blank\" href=\"https:\/\/youtu.be\/cavq2HFBa-U\">https:\/\/youtu.be\/cavq2HFBa-U<\/a>. <strong>License<\/strong>: <em>All Rights Reserved<\/em>. <strong>License Terms<\/strong>: Standard YouTube License<\/li><\/ul><\/div>\n\t\t\t\t\t\t <\/div>\n\t\t\t\t\t <\/div>\n\t\t\t <\/section>","protected":false},"author":78,"menu_order":4,"template":"","meta":{"_candela_citation":"[{\"type\":\"cc\",\"description\":\"Dynamic Earth: Introduction to Physical Geography\",\"author\":\"R. Adam Dastrup\",\"organization\":\"\",\"url\":\"http:\/\/www.opengeography.org\/physical-geography.html\",\"project\":\"Open Geography Education\",\"license\":\"cc-by-sa\",\"license_terms\":\"\"},{\"type\":\"copyrighted_video\",\"description\":\"Earthquakes 101\",\"author\":\"National Geographic\",\"organization\":\"\",\"url\":\"https:\/\/youtu.be\/VSgB1IWr6O4\",\"project\":\"\",\"license\":\"arr\",\"license_terms\":\"Standard YouTube License\"},{\"type\":\"copyrighted_video\",\"description\":\"Understanding Earthquakes\",\"author\":\"National Geographic \",\"organization\":\"\",\"url\":\"https:\/\/youtu.be\/cavq2HFBa-U\",\"project\":\"\",\"license\":\"arr\",\"license_terms\":\"Standard YouTube License\"}]","CANDELA_OUTCOMES_GUID":"","pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-497","chapter","type-chapter","status-publish","hentry"],"part":486,"_links":{"self":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/497","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/users\/78"}],"version-history":[{"count":1,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/497\/revisions"}],"predecessor-version":[{"id":498,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/497\/revisions\/498"}],"part":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/parts\/486"}],"metadata":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/497\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/media?parent=497"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapter-type?post=497"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/contributor?post=497"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/license?post=497"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}