{"id":241,"date":"2017-05-10T16:33:12","date_gmt":"2017-05-10T20:33:12","guid":{"rendered":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/part\/chapter-6-the-rock-cycle\/"},"modified":"2021-08-18T12:35:02","modified_gmt":"2021-08-18T16:35:02","slug":"chapter-6-the-rock-cycle","status":"publish","type":"part","link":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/part\/chapter-6-the-rock-cycle\/","title":{"raw":"Chapter 6. The Rock Cycle","rendered":"Chapter 6. The Rock Cycle"},"content":{"raw":"[caption id=\"attachment_1609\" align=\"aligncenter\" width=\"998\"]<a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples.png\" rel=\"attachment wp-att-1609\"><img class=\"wp-image-1609 size-full\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples.png\" alt=\"\" width=\"998\" height=\"565\" \/><\/a> <strong>Figure 6.1<\/strong> A petrified beach near Rock Springs, Wisconsin, U. S. A. The wrinkled face of this vertical cliff displays ripples from an ancient beach. Flowing water moved sand grains to form ripples, and over time the sand was transformed into a solid sedimentary rock. The petrified beach was buried deeper and deeper, and the higher pressures and temperatures caused the sand grains to lose their individual boundaries and merge together. Thus, the sedimentary rock was transformed into a different type of rock, called a metamorphic rock. Source: Karla Panchuk (2021), CC BY-SA 4.0. <a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/part\/chapter-6-the-rock-cycle\/wisconsin-quartzite-ripples\/\">Click for more attributions<\/a>.[\/caption]\r\n<h1>Chapter Goals<\/h1>\r\nComplete this chapter so you can:\r\n<ul>\r\n \t<li>Explain what a rock is.<\/li>\r\n \t<li>Summarize the main characteristics of igneous, sedimentary, and metamorphic rocks.<\/li>\r\n \t<li>Describe the rock cycle and the types of processes that lead to the formation of igneous, sedimentary, and metamorphic rocks.<\/li>\r\n \t<li>Explain why there is an active rock cycle on Earth.<\/li>\r\n<\/ul>","rendered":"<figure id=\"attachment_1609\" aria-describedby=\"caption-attachment-1609\" style=\"width: 998px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples.png\" rel=\"attachment wp-att-1609\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1609 size-full\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples.png\" alt=\"\" width=\"998\" height=\"565\" srcset=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples.png 998w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples-300x170.png 300w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples-768x435.png 768w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples-65x37.png 65w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples-225x127.png 225w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/05\/Wisconsin-quartzite-ripples-350x198.png 350w\" sizes=\"auto, (max-width: 998px) 100vw, 998px\" \/><\/a><figcaption id=\"caption-attachment-1609\" class=\"wp-caption-text\"><strong>Figure 6.1<\/strong> A petrified beach near Rock Springs, Wisconsin, U. S. A. The wrinkled face of this vertical cliff displays ripples from an ancient beach. Flowing water moved sand grains to form ripples, and over time the sand was transformed into a solid sedimentary rock. The petrified beach was buried deeper and deeper, and the higher pressures and temperatures caused the sand grains to lose their individual boundaries and merge together. Thus, the sedimentary rock was transformed into a different type of rock, called a metamorphic rock. Source: Karla Panchuk (2021), CC BY-SA 4.0. <a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/part\/chapter-6-the-rock-cycle\/wisconsin-quartzite-ripples\/\">Click for more attributions<\/a>.<\/figcaption><\/figure>\n<h1>Chapter Goals<\/h1>\n<p>Complete this chapter so you can:<\/p>\n<ul>\n<li>Explain what a rock is.<\/li>\n<li>Summarize the main characteristics of igneous, sedimentary, and metamorphic rocks.<\/li>\n<li>Describe the rock cycle and the types of processes that lead to the formation of igneous, sedimentary, and metamorphic rocks.<\/li>\n<li>Explain why there is an active rock cycle on Earth.<\/li>\n<\/ul>\n","protected":false},"parent":0,"menu_order":6,"template":"","meta":{"pb_part_invisible":false,"pb_part_invisible_string":""},"contributor":[],"license":[],"class_list":["post-241","part","type-part","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/parts\/241","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/parts"}],"about":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/types\/part"}],"version-history":[{"count":5,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/parts\/241\/revisions"}],"predecessor-version":[{"id":2440,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/parts\/241\/revisions\/2440"}],"wp:attachment":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/media?parent=241"}],"wp:term":[{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/contributor?post=241"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/license?post=241"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}