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Minerals meet these basic criteria: |
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Naturally occurring (not man made) Crystalline Solid (atoms and molecules have regular structure) Inorganic substance Definite chemical composition Distinctive physical properties |
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Crystallization – growth of a solid from particles in a liquid or gas |
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HOW DO WE IDENTIFY A MINERAL? |
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Color Streak Luster Crystalline Structure Hardness Cleavage |
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Color of mineral in its powdered form |
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the way crystals in the mineral form |
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igneous rocks cooler temperatures |
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igneous rocks
faster crystallization means |
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crystals visable to the naked eye |
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crytals to small for naked eye |
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composed of disaggregated igneous rocks |
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transitional b/w sedimentary snd igneous (from volcanoes) |
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fragmented material created by volcano |
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Rock formed from sediments or fragments of other older rocks |
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process where loose sediment grains are converted into a rock |
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hardening and welding of sediments by precipitation of mineral matter into spaces between sediments |
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sedimentary composition
minerals and rock fragments |
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sedimentary composition
crystals that precipitate from water |
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sedimentary composition
shells made of calcite by organisms (same as chemical, add organisms) |
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formed from physically weather sediments of other rocks, classified on basis on grain size Ex: sandstone, breccia, shale |
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formed due to decomposition of organic remains under pressure and temperature Ex: coal, lignite |
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Evaporites: formed from evaporation of sea water |
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formed from carbonate by organic sources or by chemical leaching Ex: limestone, dolomite |
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Process of determining when something formed or happened in relation to something else |
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Determining when something formed or happened in exact units of time such as days or years. |
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The order in which rocks are placed or accumulated in beds one above another. |
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principle of superposition |
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Assumption that sedimentary rocks were originally deposited horizontality |
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principal of original horizontality |
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Rock formations which contain inclusions of another rock are younger than the inclusion. |
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surfaces that represent gaps in the geologic record. |
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Where sedimentary rock lies above and was deposited on metamorphic and igneous rock |
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erosion or non deposition between parallel layers of sedimentary rocks |
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Unconformity where horizontal parallel strata of sedimentary rock are deposited on tilted and eroded layers |
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Age of rock = # of half lives that have occurred x length of half life for isotope |
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