{"id":307,"date":"2015-05-13T20:07:15","date_gmt":"2015-05-13T20:07:15","guid":{"rendered":"http:\/\/blogs.tntech.edu\/hwleimer\/?page_id=307"},"modified":"2016-03-08T09:28:07","modified_gmt":"2016-03-08T14:28:07","slug":"classification-systems-materials","status":"publish","type":"page","link":"https:\/\/sites.tntech.edu\/hwleimer\/geol-1040\/geol-1040-lab\/classification-systems-materials\/","title":{"rendered":"Classification Systems Materials"},"content":{"rendered":"<p>1.\u00a0<u> Table salt,<\/u>\u00a0Morton&#8217;s standard blue container, the mineral halite having a composition of NaCl (sodium Chloride). Tastes salty. Halite grows as cubic crystals and also breaks as cubes.<\/p>\n<p>2.\u00a0 <u>Hematite<\/u>, mineral with a composition of Fe2O3 (Iron Oxide), non-metallic-earthy luster, rounded structures are called oolites.<\/p>\n<p>3.\u00a0<u> Petrified palm wood<\/u>\u00a0with tree rings. All woody material replaced by quartz with a composition of SiO2<\/p>\n<p>4.\u00a0<u> Granite, gray,<\/u>\u00a0igneous rock, phaneritic (coarse grained) composed of the minerals quartz and potash feldspar (orthoclase).<\/p>\n<p>5.\u00a0<u> Quartz stream pebbles<\/u>, rounded by action of the stream<\/p>\n<p>6.\u00a0<u> Terazzo<\/u>, sawed slab from floor of University Center<\/p>\n<p>7.\u00a0<u> Halite<\/u>\u00a0as comes from ground. Shape due to breakage<\/p>\n<p>8.\u00a0<u> Native copper<\/u>\u00a0as comes from ground.<\/p>\n<p>9.\u00a0<u> Quartz, milky,<\/u>\u00a0as comes from the ground<\/p>\n<p>10.\u00a0<u> Granite, gray,<\/u>\u00a0sawed with diamond saw<\/p>\n<p>11.\u00a0<u> Concrete<\/u>, part of sidewalk torn up just south of Kittrell Hall. Quicklime plus quartz sand plus limestone aggregate.<\/p>\n<p>12.\u00a0<u> Marble,<\/u>\u00a0metamorphic rock, non-oriented mineral grains, composed of the mineral calcite, CaCO3<\/p>\n<p>13.\u00a0<u> Obsidian,<\/u>\u00a0igneous rock, glassy texture, no minerals<\/p>\n<p>14.\u00a0<span style=\"text-decoration: underline\"> Fossiliferous limestone<\/span>, sedimentary rock, precipitated from sea water, made up of the mineral calcite.<\/p>\n<p>15.\u00a0<u> Pyrite,<\/u>\u00a0metallic mineral composed of FeS2, shape due to growth, also called Fool&#8217;s gold.<\/p>\n<p>16.\u00a0<u> Glass slag<\/u>, product of smelting iron ores near the Tennessee River during the Civil War.<\/p>\n<p>17.\u00a0<u> Graphite<\/u>, mineral composed of carbon (C), looks like a metal. Feels slippery.<\/p>\n<p>18.\u00a0<u> Calcite<\/u>, mineral composed of CaCO3, shape due to breakage.<\/p>\n<p>19.\u00a0<u> Silicon<\/u>, man-made composed of Si, looks like a metal but is not very heavy. Not to be confused with silica, silicate, or silicone.<\/p>\n<p>20.\u00a0<u> Corundum<\/u>, mineral composed of Al2O3 (aluminum oxide), six-sided shape due to growth.<\/p>\n<p>21<u>.<\/u> \u00a0<u> Galena<\/u>, mineral that looks like a metal, very heavy, grows in shape of cubes, breaks in shape of cubes.<\/p>\n<p>22. \u00a0<u> Whetstone<\/u>, a slightly metamorphosed rock composed of microcrystalline quartz, used to sharpen knives.<\/p>\n<p>23. \u00a0<u> Quartz beach sand<\/u>\u00a0from Panama City, Florida.<\/p>\n<p>24.\u00a0 <u>Obsidian beach sand<\/u>\u00a0from Hawaii.<\/p>\n<p><u><\/u>25.\u00a0 <u>Magnetite<\/u>, mineral composed of Fe3O4 (iron oxide), fairly heavy, magnetic.<\/p>\n<p>26.\u00a0<u> Hard boiled chicken egg,<\/u>\u00a0shell composed of calcium carbonate.<\/p>\n<p>27.\u00a0<u> Tiger&#8217;s eye egg<\/u>, yellow-brown variety of the mineral quartz used in jewelry.<\/p>\n<p>28.\u00a0<u> Crude oil<\/u>\u00a0from Overton Co., TN<\/p>\n<p>29.\u00a0<u> Tree<\/u>\u00a0cross section with tree rings, maple tree.<\/p>\n<p>30.\u00a0<u> Quartz crystal<\/u>, six parallel sides with point on end.<\/p>\n<p>31.-39.\u00a0 3 bolts, 3 nuts, 3 washers.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>1.\u00a0 Table salt,\u00a0Morton&#8217;s standard blue container, the mineral halite having a composition of NaCl (sodium Chloride). Tastes salty. Halite grows as cubic crystals and also breaks as cubes. 2.\u00a0 Hematite, mineral with a composition of Fe2O3 (Iron Oxide), non-metallic-earthy luster, &hellip; <a href=\"https:\/\/sites.tntech.edu\/hwleimer\/geol-1040\/geol-1040-lab\/classification-systems-materials\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":11,"featured_media":0,"parent":227,"menu_order":1,"comment_status":"closed","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-307","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/pages\/307","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/users\/11"}],"replies":[{"embeddable":true,"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/comments?post=307"}],"version-history":[{"count":5,"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/pages\/307\/revisions"}],"predecessor-version":[{"id":551,"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/pages\/307\/revisions\/551"}],"up":[{"embeddable":true,"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/pages\/227"}],"wp:attachment":[{"href":"https:\/\/sites.tntech.edu\/hwleimer\/wp-json\/wp\/v2\/media?parent=307"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}