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Dynamic Earth Chapter 4-Highlights Rocks and Minerals A. Highlights for Section 1 pages 79-87 Natural occurring, inorganic solid that has a definite chemical composition and crystal shape is called a mineral. o Must be inorganic—not formed from living things o Quartz is a mineral o Atoms are arranged in a definite, repeated pattern— crystal Minerals have certain physical properties o Color—easily observed o Luster—way mineral reflects light from its surface…either metallic or dull luster o Hardness—ability of a mineral to resist being scratched – Mohs Hardness Scale If unknown mineral is scratched by a known mineral, it is softer than the known mineral If unknown mineral scratches the known mineral, it is harder than that mineral If they do not scratch each other, they have the same hardness o Streak—color powder scraped off o Density—amount of matter in a given space o Crystal shape—six basic shapes o Cleavage—mineral splits along smooth surface o Fracture—break along rough jagged surface I. Highlights for Section 2 pages 88-91 Ores are minerals from which metals and nonmetals can be removed in usable amounts Metals are elements that have shiny surfaces and are able to conduct electricity and heat o During smelting—ore is heated so that the metal can be separated o Iron used in making steel—copper for wire—aluminum for cans Nonmetals are minerals that have dull surfaces and add are poor conductors of electricity and heat o Sulfur used for matches and meds and fertilizers Some minerals are hard-durable-beautiful o Cut and polished for jewelry o Gemstones Rarest—diamonds, rubies, sapphires, emeralds are precious stones All other gemstones are semiprecious—zircons, turquoises M. Highlights for Section 3 pages 93-97 Rock is hard substance composed of one or more minerals—rocks are placed in three main groups o Igneous rocks—were originally hot, fluid magma within Earth o Sedimentary rocks—are formed from particles that have been carried along and deposited by wind and water Sediments include bits of rock in the form of mud, sand, pebbles---later pressed together to form rocks o Metamorphic rocks—are formed when chemical reactions, tremendous heat, or great pressure change existing rocks into new kids of rocks. Rocks that form the Earth’s surface are subject to change o Continuous changing of rocks from one kind to another over long periods of time---rock cycle Has no definite sequence R. Highlights for Section 4 pages 97-100 Igneous rocks are classified according to their composition and texture o Composition Way magma cools and where it cools determines the size of mineral crystals The longer it takes magma to cool, the larger the crystals that form. o Texture Glassy and fine grained rocks from lava on the Earth’s surface Course grained rocks from magma within the Earth Rocks formed from lava are called extrusive or volcanic rocks. Igneous rocks formed from deep within the Earth are called intrusive rocks. W. Highlights for Section 5 pages 101-104 Sedimentary rocks are placed into 3 main categories according to origin of materials from which they are made o Clastic rocks—sedimentary rocks made from fragments of previously existing rocks Further classified according to size and shape of fragments in them Example---sandstone o Organic rocks—come from organisms—formed directly or indirectly from material that once was living Example---limestone o Chemical rocks—when a sea or lake dries up— leaving large amounts of minerals that were dissolved in water Example---rock salt EE. Highlights for Section 6 pages 105-107 Already existing rocks are buried within the Earth, tremendous heat, great pressure, and chemical reactions may cause them to change into different rocks with different textures and structures--changing of one type of rock into another is called metamorphism o Pressure within Earth tends to squeeze mineral crystals of rock together—forming denser materials o Slate formed from shale o Gneiss formed from granite