{"id":243,"date":"2017-10-01T17:18:37","date_gmt":"2017-10-01T21:18:37","guid":{"rendered":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/6-1-what-is-a-rock\/"},"modified":"2021-08-23T14:11:13","modified_gmt":"2021-08-23T18:11:13","slug":"6-1-what-is-a-rock","status":"publish","type":"chapter","link":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/6-1-what-is-a-rock\/","title":{"raw":"6.1 What Is A Rock?","rendered":"6.1 What Is A Rock?"},"content":{"raw":"A <strong>rock<\/strong> is a solid mass of geological materials. Geological materials include individual mineral crystals, inorganic non-mineral solids like glass, pieces broken from other rocks, and even fossils. The geological materials in rocks may be inorganic, but they can also include organic materials such as the partially decomposed plant matter preserved in coal. A rock can be composed of only one type of geological material or mineral, but many are composed of several types (Figure 6.2).\r\n\r\n&nbsp;\r\n\r\n[caption id=\"attachment_1615\" align=\"aligncenter\" width=\"650\"]<a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral.png\" rel=\"attachment wp-att-1615\"><img class=\"wp-image-1615\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral.png\" alt=\"Image contains: Granite, a rock made of minerals quartz, potassium feldspar, and biotite. Quartzite, a rock made of tiny quartz crystals. A crystal of the mineral quartz, a crystal of the mineral potassium feldspar, and a rock of biotite crystals.\" width=\"650\" height=\"483\" \/><\/a> <strong>Figure 6.2<\/strong> Rocks versus minerals. Rocks in the image are made up of crystals of one or more minerals. Source: Karla Panchuk (2021), CC BY-NC-SA. Photographs by R. Weller\/ Cochise College and James St. John. <a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/6-1-what-is-a-rock\/rock-vs-mineral\/\">Click for attributions.<\/a>[\/caption]\r\n\r\n<div class=\"textbox shaded\">\r\n\r\n<strong><a id=\"165\"><\/a>Concept Check: Rock or Mineral?<\/strong>\r\n\r\n[h5p id=\"165\"]\r\n\r\n<\/div>\r\n<h1>Three Main Types of Rock<\/h1>\r\nRocks are grouped into three main categories based on how they form. <strong>Igneous rocks<\/strong> form when melted rock cools and solidifies. <strong>Sedimentary rocks<\/strong> form when fragments of other rocks are buried, compressed, and cemented together; or when minerals precipitate from solution, either directly or with the help of an organism. <strong>Metamorphic rocks<\/strong> form when heat and pressure alter a pre-existing rock. Although temperatures can be very high, metamorphism does not involve melting of the rock.\r\n\r\n&nbsp;\r\n<div class=\"textbox shaded\">\r\n\r\n<strong><a id=\"166\"><\/a>Do You Know Your Rock Types?<\/strong>\r\n\r\n[h5p id=\"166\"]\r\n\r\n<\/div>\r\n&nbsp;\r\n\r\n&nbsp;","rendered":"<p>A <strong>rock<\/strong> is a solid mass of geological materials. Geological materials include individual mineral crystals, inorganic non-mineral solids like glass, pieces broken from other rocks, and even fossils. The geological materials in rocks may be inorganic, but they can also include organic materials such as the partially decomposed plant matter preserved in coal. A rock can be composed of only one type of geological material or mineral, but many are composed of several types (Figure 6.2).<\/p>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_1615\" aria-describedby=\"caption-attachment-1615\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral.png\" rel=\"attachment wp-att-1615\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1615\" src=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral.png\" alt=\"Image contains: Granite, a rock made of minerals quartz, potassium feldspar, and biotite. Quartzite, a rock made of tiny quartz crystals. A crystal of the mineral quartz, a crystal of the mineral potassium feldspar, and a rock of biotite crystals.\" width=\"650\" height=\"483\" srcset=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral.png 1002w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral-300x223.png 300w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral-768x571.png 768w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral-65x48.png 65w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral-225x167.png 225w, https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-content\/uploads\/sites\/1304\/2017\/10\/rock-vs-mineral-350x260.png 350w\" sizes=\"auto, (max-width: 650px) 100vw, 650px\" \/><\/a><figcaption id=\"caption-attachment-1615\" class=\"wp-caption-text\"><strong>Figure 6.2<\/strong> Rocks versus minerals. Rocks in the image are made up of crystals of one or more minerals. Source: Karla Panchuk (2021), CC BY-NC-SA. Photographs by R. Weller\/ Cochise College and James St. John. <a href=\"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/6-1-what-is-a-rock\/rock-vs-mineral\/\">Click for attributions.<\/a><\/figcaption><\/figure>\n<div class=\"textbox shaded\">\n<p><strong><a id=\"165\"><\/a>Concept Check: Rock or Mineral?<\/strong><\/p>\n<div id=\"h5p-165\">\n<div class=\"h5p-iframe-wrapper\"><iframe id=\"h5p-iframe-165\" class=\"h5p-iframe\" data-content-id=\"165\" style=\"height:1px\" src=\"about:blank\" frameBorder=\"0\" scrolling=\"no\" title=\"Rock or mineral?\"><\/iframe><\/div>\n<\/div>\n<\/div>\n<h1>Three Main Types of Rock<\/h1>\n<p>Rocks are grouped into three main categories based on how they form. <strong>Igneous rocks<\/strong> form when melted rock cools and solidifies. <strong>Sedimentary rocks<\/strong> form when fragments of other rocks are buried, compressed, and cemented together; or when minerals precipitate from solution, either directly or with the help of an organism. <strong>Metamorphic rocks<\/strong> form when heat and pressure alter a pre-existing rock. Although temperatures can be very high, metamorphism does not involve melting of the rock.<\/p>\n<p>&nbsp;<\/p>\n<div class=\"textbox shaded\">\n<p><strong><a id=\"166\"><\/a>Do You Know Your Rock Types?<\/strong><\/p>\n<div id=\"h5p-166\">\n<div class=\"h5p-iframe-wrapper\"><iframe id=\"h5p-iframe-166\" class=\"h5p-iframe\" data-content-id=\"166\" style=\"height:1px\" src=\"about:blank\" frameBorder=\"0\" scrolling=\"no\" title=\"What kinds of rock are these: igneous, sedimentary, or metamorphic? Drag and drop the correct label.\"><\/iframe><\/div>\n<\/div>\n<\/div>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n","protected":false},"author":103,"menu_order":1,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-243","chapter","type-chapter","status-publish","hentry"],"part":241,"_links":{"self":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/243","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/users\/103"}],"version-history":[{"count":10,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/243\/revisions"}],"predecessor-version":[{"id":2458,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/243\/revisions\/2458"}],"part":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/parts\/241"}],"metadata":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapters\/243\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/media?parent=243"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/pressbooks\/v2\/chapter-type?post=243"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/contributor?post=243"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/wp-json\/wp\/v2\/license?post=243"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}