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naturally occuring inorganic solid specific composition (chemical formula) crystalline specific physical properties |
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cations & anions oxides silicates alumino silicates carbonates sulfides sulfates chlorides |
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precipitation from a saturated solution - add seed to saturated solution - acts as template for particles to arrange on to - CONCENTRIC GROWTH (growth in every direction in layers, making rings) |
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cools too quickly for any crystalline structure to form (cooling from hot liquid magma) |
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formed by crystallization of a liquid, produces interlocking grains and zoning |
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- form from COOLING MAGMA - crystal size vs. cooling rates: - SLOW COOLING: large grains - coarse - FAST COOLING: small grains - fine - VERY FAST COOLING: quenched, glass - orderless, non-crystalline |
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subsurface, magma squeezes its way between other rocks to form igneous rocks very slowly |
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surface, lava - pouring out of ground to form igneous rocks quickly, or ash solidifying in sky forming igneous glass |
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hardening of sediment in 3 ways: - compaction (burial) - dewatering - cementation (chemical precipitation in pore spaces) |
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sedimentary rocks composed of SOLID PARTICLES (clasts) ERODED from other rocks - NON-INTERLOCKING GRAINS |
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sedimentary rocks composed of chemically and/or organically precipitated or accumulated sediment - LIMESTONE: organic remains - calcite from shells, coral etc. - COAL: plant remains - SALT: chemical precipitation in lake or ocean |
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the process by which HEAD, PRESSURE, and CHEMICAL REACTIONS deep within the Earth altar the MINERAL CONTENT and/or STRUCTURE of preexisting rock WITHOUT MELTING IT
- ANY type of rock can be metamorphosed (igneous, sedimentary, metamorphic) |
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(slate, schist, gneiss)
rocks altered by HEAT and PRESSURE
metamorphic grade - level of metamorphism
becoming stable again: - recrystallization - baking - deformation (stretch, fold)
if GRADE TOO HIGH - melting, starting with minerals with the lowest melting temperature - IF REALLY TOO HIGH - magma |
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1. formation of rock unit (deposition, extrusion, intrusion) 2. metamorphism 3. folding, tilting 4. faulting & fracturing 5. formation of an unconformity |
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a surface that: 1. represents significant missing time 2. and had a sedimentary unit, ash, or lava flow laid down on top of it
OR is the current eroded Earth's surface (implies: erosion or period of non-deposition) - river valley that got eroded and now has a new layer of rock on top |
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past events always obeyed the laws of math, chemistry and physics like processes today
things happened in the past just like they do today, same rules apply |
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Fundamental principles of layers |
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Superposition, horizontality, continuity, intrusion, crosscutting, derivation, inclusions |
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sediment is always deposited ON TOP of some other sediment or rock that is older - younger ON TOP of older |
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sediments are deposited (almost always) as horizontal layers, beds, or strata
if the layers appear inclined it happened after they formed |
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strata found truncated (narrowing down towards the surface) originally extended in all directions until they thinned to nothing or reached the edges of their depositional basin |
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an intrusive igneous rock unit must be younger than the rock it intrudes |
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a fault, erosion surface, or intrusive igneous rock unit is younger than the rock that is cut |
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If part of a rock unit is derived from another rock unit, it must be younger than the original rock |
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parts of an older rock unit enclosed in an igneous rock body are inclusions |
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parts of an older rock unit enclosed in an igneous rock body are inclusions |
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Geologic Time Scale Hierarchy |
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- eons - eras - periods - epochs - stages (ages) |
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