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GEOL 108 - Crises of a Planet Lab 5 - Rocks, Weathering, and Minerals. Oct. 2 - 5, 2012. Department of Earth Sciences. QUIZ 3 REVIEW. Solid Bedrock. Unconsolidated sediments.
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GEOL 108 - Crises of a PlanetLab 5- Rocks, Weathering, and Minerals • Oct. 2 - 5, 2012 Department of Earth Sciences
QUIZ 3 REVIEW Solid Bedrock Unconsolidated sediments A large earthquake occurs with the epicenter at point C. Is there likely to be more damage at point A or at point B, and why? Bonus: Name these 3 cartoon dogs (1 pt). REVIEW | 2 Department of Earth Sciences
LAB 5 - ROCKS, WEATHERING, AND MINERALS • Identify minerals • Compare clay properties • Relate weathering of rocks to clay formation ROCKS, WEATHERING, MINERALS | 3 Department of Earth Sciences
WHAT IS A MINERAL? • Definition of a Mineral: • naturally occurring • inorganic • solid • characteristic crystalline structure • definite chemical composition steel plastic sugar table salt mercury ice coal no, #1 no, #1 no, #1,2 YES! no, #3 YES! no, #2 basalt obsidian mica gold paper chalk coral no, #5 no, #4 YES! YES! no, #1,2 no, #2 no, #2 Source: www.sci.uidaho.edu/geol111/Geology%20101/minerals_II_jh.ppt • ROCKS, WEATHERING, MINERALS | 4 Department of Earth Sciences
LUSTER • Metallic • Non-metallic • Glassy (vitreous) • Waxy • Silky • Greasy • Earthy (dull and powdery) • Pearly Shiny ≠ metallic! • ROCKS, WEATHERING, MINERALS | 5 Department of Earth Sciences
COLOR • In general, color is not a diagnostic property • Impurities in the crystal can change the color • Color is less variable for minerals with metallic luster http://nature.berkeley.edu/classes/eps2//wisc/jpeg/l15s32.jpeg • ROCKS, WEATHERING, MINERALS | 6 Department of Earth Sciences
STREAK • Streak is the color of a mineral’s powder • A mineral’s streak is the same for all specimens regardless of apparent color. Example: Metallic and earthy hematite (Fe2O3) both have red-brown streaks. • ROCKS, WEATHERING, MINERALS | 7 Department of Earth Sciences
CLEAVAGE • A specific type of breakage • Occurs because bonds between atoms are weaker in some directions. • There may be up to 6, but usually 1-3 • Angles between cleavage directions 1 direction 2 directions 3 directions (90°) 3 directions (not 90°) • ROCKS, WEATHERING, MINERALS | 8 Department of Earth Sciences
CLEAVAGE • One direction of cleavage Example: Mica • ROCKS, WEATHERING, MINERALS | 9 Department of Earth Sciences
CLEAVAGE • Two directions of cleavage feldspar hornblende • ROCKS, WEATHERING, MINERALS | 10 Department of Earth Sciences
FRACTURE • No planes of weakness • leads to irregular or • conchoidalfracture • ROCKS, WEATHERING, MINERALS | 11 Department of Earth Sciences
CRYSTAL HABIT • A crystal’s habit is the shape it takes when it grows unimpeded by other grains (somewhat rare). • Commonly confused • with cleavage. Two intergrownStaurolite crystals “St. Andrew’s Cross” twinning • ROCKS, WEATHERING, MINERALS | 12 Department of Earth Sciences
HARDNESS • What can a mineral scratch and what is it scratched by? It will only be scratched by harder material. • Please don’t test samples on each other! • ROCKS, WEATHERING, MINERALS | 13 Department of Earth Sciences
OTHER PROPERTIES • Specific Gravity (density compared to water) • Magnetism • Reaction to acid (Carbonate minerals –CO3) • ROCKS, WEATHERING, MINERALS | 14 Department of Earth Sciences
THE ROCK CYCLE Clays • ROCKS, WEATHERING, MINERALS | 15 Department of Earth Sciences
CLAYS • Group of minerals, commonlyfound in sedimentaryrocks • montmorillonite • kaolinite • illite (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2·nH2O Al2O3·2SiO2·2H2O (K,H3O)(Al,Mg,Fe)2(Si,Al)4O10[(OH)2,(H2O)] • ROCKS, WEATHERING, MINERALS | 16 Department of Earth Sciences