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Minerals & Igneous

Key words on minerals and igneous rocks

TermDefinition
Minerals basic components of rocks; formed by cooling/crystallization from a saturated solution (why it crystallizes)
Mineral Requirements -naturally occurring - inorganic (does derive from living matter) - homogenous internal structure (think ice) - definite chemical composition
Silicates any mineral that has SiO2 (silicone dioxide); 95% of earth's minerals have silicates
Silicone Dioxide - SiO2 - Quartz=purest silicate
Non-silicates minerals that do not contain silicone dioxide (usually stand-alone elements) i.e: aluminum , iron
Luster Natural reflection of light off mineral's surface - (earthy, dull; shiny, metallic= gold/silver)
Cleavage 0 dir'n- irregular 1 dir'n- flat, sheet-like (i.e muscovite) 2 dir'n- stairstep (i.e feldspar) 3 dir'n- cubic (i.e halite)
Impurities (Physical Apperance) pink in color
3 Major Rock Groups Igneous, metamorphic, sedimentary
Igneous Formation solidification of magma
Bowen Reaction Series determines sequence in a colling magma (crystallization of minerals depends on temperature)
Felsic silica-rich; more than 50% light in color (white/pink)
Mafic silica-poor; less than 50% dark in color (black, dark green, red)
Phaneritic coarse-grained; cools slowly and intrusive
Intrusive forms beneath earth's surface *describes igneous only*
Extrusive forms above earth's surface *describes igneous only*
Aphanitic fine-grained; extrusive
Glassy think obsidian's appearance :)
Extrusive Traits - glassy - aphanitic - ex: besalt, rhyolite and volcanoes
Intrusive Traits - phaneritic
Pyroclastic Flow volcanic ash mixed with water
Viscosity *think movement of honey* high flow of movement = high viscosity and vice versa
Viscosity of Hawaiian Volcanoes low viscosity because magma flows slowly and is mafic
Created by: tyty17
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