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GEOLOGY TEST OUT REVIEW
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pyrite chalcopyrite
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magnetite Magnetic Heavy Metallic Black streak
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galena 3= 90 cleavage Metal heavy
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graphite writes
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quartz Most common mineral Scratches glass NMV Hexagonal crystals
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calcite Fizzes 3 ≠ 90 cleavage Double refraction Soft
Main mineral in limestone and marble
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biotite
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muscovite Flakey- 1 directional cleavage Light in color
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halite Salty 3= 90 cleavage soft
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kaolinite talc
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HEMATITE Red streak Metal Heavy
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Olivine green
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plagioclase Scratches glass White 2 directional cleavage
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K-feldspar (orthoclase)
Pink Scratches glass 2= 90 cleavage
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gypsum Soft; chalky
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garnet Deep red Hard= 8
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fluorite Soft Many colors; purple and green 4 directional cleavage
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chalcedony Microcrystalline quartz White-blue Globby looking
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AMPHIBOLE Hornblende Dark black Hardness ≈ 6
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PYROXENE Dark green to black augite
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Amphibole vs. pyroxene
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IGNEOUS ROCKS
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GRANITE Intrusive igneous Cooled slowly Felsic
Has quartz, plag., biotite, K-feld, hornblende Formed underground (dikes, sills, batholiths)
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gabbro “black granite” Intrusive Mafic
Formed underground (dikes, sills, batholiths) Granite’s mafic cousin
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rhyolite Felsic extrusive
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Rhyolite porphyry
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This rhyolite is usually on the test!!
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basalt Extrusive Mafic Shield volcanoes From runny lava flows
Pahoehoe and Aa are types of basalt
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andesite
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Andesite Porphyry Contains plag From strato volcanoes (extrusive)
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pegmatite Coarse granite
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diorite Salt and pepper No quartz
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SEDIMENTARY
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conglomerate Round pebbles
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sandstone Gritty From beach/desert clastic
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shale Fine clastic From mud
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dolostone Looks like limestone Slow fizz
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coal Bioclastic From swamps Organic lightweight
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Fossiliferous limestone
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limestone Fizzes Chemical precipitate Forms in deep ocean
From dissolved shells
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Oolitic limestone
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siltstone Like shale Not as flat
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Metamorphic
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Gneiss Banded (striped) Foliated Parent rock- granite
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Schist Foliated Highly reflective May have garnets
Amphibole- black sparkly Mica schist
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slate Metamorphosed shale foliated
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marble Can be many colors Metamorphosed limestone Not foliated
Will fizz (calcite)
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Quartzite Metamorphosed sandstone Non foliated Will scratch glass
Any color
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metaconglomerate
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OTHER STUFF
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Lava or pyroclast?
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Earth’s layers Crust- Mantle- olivine outer core- liquid iron
Continental- feldspar, quartz Oceanic- pyroxene, plag, olivine Mantle- olivine outer core- liquid iron Inner core- iron
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Ocean crust Denser Mafic Thinner Only 200 million years old
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How do plates move? Convection currents Slab pull
Where does heat come from? Radioactive decay
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Plates
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Sea floor spreading Oldest ocean crust= 200 my Polar reversals
New crust in center of ridge
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Plate boundaries
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Pangea
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Why wasn’t Wegener’s cont. drift accepted?
No seafloor data No earthquake data No mechanism to move plates Convection currents Slab pull Ridge push (thermal plumes)
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isostasy is a term used in geology to refer to the state of gravitational equilibrium between the earth's lithosphere and asthenosphere such that the tectonic plates "float" at an elevation which depends on their thickness and density
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Accretionary wedge
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Magmatic arc
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Half life problem If you begin with 80 grams of 14C after a time, 20 grams are left. How old is the sample? One half life= 14,000 years
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Magnitude scale Each step is 10x
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Passive plate margins Non- tectonic Continental shelf- slope- rise
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Rock cycle
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dissolution Usually limestone Acid rain
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unconformities
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volcanoes
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Wegner’s evidence?
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faults
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EARTH LAYERS http://crack. seismo. unr
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