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Earth Science Unit 2 Chap. 4 Lecture Notes B. Rife page 1 / 4 Unit 2 Chapter 4 Minerals HOMEWORK: HW 1 Extra Credit HW 2 Topic Questions: PG. 52, 57 Review, Interpret & Apply, Crit. Thinking pg 60-61 Unit 1 Identifying Minerals Topic 1 Rock-Forming Minerals Matter consists of protons, neutrons, and electrons. Matter made up of one kind of atom is an element. Elements may be combined to form chemical compounds. Single elements (gold) and chemical compounds (quartz) occur as minerals. Most frequently as compounds. Minerals and mixtures of minerals occur as rocks. Common minerals that make up most of the rocks in Earth’s crust are called rockforming minerals. The study of minerals and their properties is called mineralogy. A mineral is a naturally occurring, inorganic, crystalline solid, with a definite chemical composition. A mineral is inorganic. (consist of matter that is not plant or animal) A mineral is natural. (can’t be man made) A mineral is solid. (solids that have a geometric crystal system - cubic, hexagonal) A mineral has an exact chemical composition. (If the chemical composition changes, the mineral changes) Minerals are either elements or compounds, and thus can be identified using chemical symbols and formulas. The formula for quartz, a compound, is SiO2 Topic 2 Identification by Inspection Minerals are identified by their physical properties. Color is a mineral’s most conspicuous characteristic and is largely dependent on chemical composition and the arrangement of atoms. Some minerals possess colors that are constant, such as green in malachite, blue in azurite and metallic yellow in pyrite and gold. Earth Science Unit 2 Chap. 4 Lecture Notes B. Rife page 2 / 4 Color can be altered by small amounts of impurities. Rubies and sapphires are variations in composition due to impurities. Luster refers to the way light is reflected from a mineral’s surface. Metallic luster - If a mineral looks like a metal, regardless of color. (pyrite, galena) Nonmetallic luster - is described as dull, pearly (pearl), silky, glassy or vitreous (quartz), and brilliant or adamantine (diamond). A crystal is a solid bounded by plane surfaces that has a definite shape due to its internal atomic arrangement. Crystal System Isometric or Cubic Hexagonal Tetragonal Orthorhombic Monoclinic Triclinic Examples Halite, Galena Quartz, Calcite Zircon Sulfur, Topaz Hornblend, Orthoclase (white feldspar), Muscovite (mica) Albite, Plagioclase (pink feldspar), Turquoise Topic 3 Identification by Simple Tests Streak is the color of the powdered mineral. As a rule, the streak of a metallic mineral is at least as dark as the hand specimen. The streak of a nonmetallic mineral is usually colorless or white. Minerals of a hardness of greater than five do not streak. (gold streak is yellow, pyrite is dark) Cleavage of a mineral is its tendency to split or break along smooth flat planes. (Muscovite mica) Fracture is breakage along an irregular surface. The surface may be rough (quartz) or conchoidal (obsidian) Hardness - is a mineral’s resistance to being scratched. a mineral’s hardness depends largely on the strength of bonds between the atoms. Friedrich Mohs, a German mineralogist, worked out a relative scale of hardness of ten common minerals used for mineral identification. Earth Science Unit 2 Chap. 4 Lecture Notes B. Rife page 3 / 4 Moh’s Scale of Hardness Field Scale of Hardness 1 2 3 4 5 6 7 8 9 10 1 soft, greasy, flakes on fingers 2 scratched by fingernail 3 scratched by penny (copper) 4 scratched easily by knife (soft steel) 5 scratched by knife with difficulty 6 scratched by glass 7 scratched by steel file (nail) 8 scratches quartz No approximations above 8 Talc Gypsum Calcite Fluorite Apatite Orthoclase (white feldspar) Quartz Topaz Corundum Diamond Topic 4 Specific Gravity Specific gravity is the ratio of the weight of a mineral to the weight of an equal volume of water. Specific gravity is the ratio of the density of the mineral to the density of water. It is a dimensionless quantity, that is it has no units. Specific gravity is useful in recognizing heavy minerals and some gem stones. Gold has a specific gravity (SG) of 19.3 while the SG of pyrite is 5.0 Topic 5 The Acid Test Calcite is the principal mineral in limestone (sedimentary) and marble (metamorphic) rocks. Calcite is CaCO3. It reacts with hydrochloric acid (HCl) by forming CO2 bubbles. Topic 6 Special Properties of Minerals Halite (rock salt) tastes salty Lodestone is a magnet. Magnetite can be picked up by a magnet. Fluorite and calcite fluorescence (glows) under ultraviolet (“black”) lights. Carnotite and uraninite (uranium ores) are radioactive. Sulfur has a specific odor. Calcite creates double refraction. Unit II Descriptions of Rock-Forming Minerals Topic 7 Silicates: From Silica Tetrahedrons Earth Science Unit 2 Chap. 4 Lecture Notes B. Rife page 4 / 4 Silicates are mineral compounds of silicon oxygen combined with other metals and nonmetals. They make up the largest group of minerals. a. Quartz is only silicon and oxygen (SiO2). Quartz is the second most abundant mineral in Earth’s crust. b. Feldspar are the most abundant family of minerals Othoclase is a potassium aluminum silicate and usually has a whitish appearance. Plagioclase is a sodium calcium silicate and usually has a pinkish appearance. c. Micas are soft silicates with a hardness of about 2.5 Muscovite is known as white mica and has a silvery appearance. Biotite is known as black mica The above three are principal components of granites (intrusive igneous rocks). d. Talc is the softest mineral (hardness of 1) Amphibloes, pyroxenes, olivine, garnets, and kaolin are other silicates. Topic 8 Carbonates Minerals: Calcite and Colomite Carbonates are the next largest group of minerals. They contain carbonate (CO3) and some other element. Calcite CaCO3 found in limestone and marble. Dolomite is calcium magnesium carbonate. Malachite is a copper carbonate with a distinctive green color. Azurite is a copper carbonate with a distinctive blue color. Topic 9 Iron Oxides and Sulfides Oxides are combinations of oxygen and some other element.\ Hematite Fe2O3 is iron ore. Often has a red appearance. Magnetite is a black magnetic iron oxide. Pyrite is an iron sulfide with a gold metallic luster, thus called “fool’s gold” Pyrite can react with water and form sulfuric acid responsible for “acid mine drainage”