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        |         The two most abundant elements on earth |  | Definition 
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        |           Any naturally occuring inorganic solid chemical compound with a more or less fixed ratio composition. Homogenous and has a regular arrangement of atoms.   |  | 
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        |           Has all of the properties of a minearl except a regular arrangement of atoms.   |  | 
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        |         Smallest particle in nature that still contains all of the characteristics of a mineral.     |  | 
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        |           Composed of proton, electron and nuetron. |  | 
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        |         the number of protons and electons  |  | 
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        |         Atoms with the same atomic number but diffrent mass numbers.   |  | 
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        |           If electrically nuetral there are:   |  | Definition 
 
        |         An atom has an equal number of protons and electrons  |  | 
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        |           Electrons are configured around the nucleus in:  |  | Definition 
 
        |         Energy level shells: with # of electrons 2 4  |  | 
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        |       Involves the transfer electrons from one atom to another or in some cases the sharing of electrons  |  | 
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        |           The diffrent type of bonds are:   |  | Definition 
 
        |    Ionic: when one atom transfers an electron to another.  Covalent: when electrons from diffrent atoms are paired up Metallic: in metals, atoms are tightly packed that electrons can be shared among several atoms.  Van der Walls: a weak attractions can occur between the electrically nuetral models that have an assymmetrical charge distribution  |  | 
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        |         When an atom losses one or more electrons, leaving a positive charge.   |  | 
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        |         When an atom has gained one or more electrons, leaving a ngative charge.   |  | 
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        |          Four oxygen atoms an a silicate ion   |  | 
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        |         The diffrent silicate super groups are:   |  | Definition 
 
        |       Single Tetrahedron: olivine  Heaxagonal Ring: beryl Single chain: pyroxene group Double chain:amphibole group Sheet: mica Three dimensional lattice: quartz  |  | 
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        |         Igneous rocks are classified through:   |  | Definition 
 
        |        The cooling and crystalization of magma: the rate of cooling: how large the indiv. grains grow texture of the rock: effected by the grain size composition: mineral assemblage      |  | 
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        |       in Volcanic rocks  Fine Grained texture:grains can only be seen through magnification Extremely small mineral grains that form in solidifying magma.   |  | 
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        |       in Plutonic rocks  Course grained texture: grains can be seen by the unaided eye.  Large mineral grains typically form in the last stages of crystalization, when gases build up in teh reaining magma.   |  | 
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        |         an igneous rock formed from lava  |  | 
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        |         an ingeous rock formed undegrounf grom magma  |  | 
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        |           Mafic chemical composition  |  | Definition 
 
        |         dark colored minerals rich in magnesium and iron  |  | 
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        |         Sialic chemical composition |  | Definition 
 
        |       light colored igneous rock, rich in silicon and aluminum  |  | 
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        |         light colored and contain a lrge amount of silica  |  | 
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        | Diffrent igneous rocks:   Rhyolite:  Granite: Andesite:  Diorite:  Basalt:  Gabbro:  |  | Definition 
 
        |     Rhyolite: felsic, high silica content and consists largely of quartz and feldspars Granite: the plutonic equivalent of rhyolite, larger grain size Andesite: intermediate silica rock with lots of feldspar mixed in with darker mafic minerals. Diorite: plutonic equivalent of andesite, an intermediate silica rock Basalt: a mafic rock, is dominant in ocean crust and the most common igneous rock on earth.  Gabbro: a plutonic equivalent of basalt, a low silica rock  |  | 
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        |       the degree to which a substance resists flow; a less viscous liquid is runny and a more viscous liquid is thick  |  | 
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        |       How viscosity related to magma:  composition  tempreture  |  | Definition 
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        |         How viscocity realtes to eruption style  |  | Definition 
 
        |     If the magma is runny, the dissolved gas will escape easily- the volcano will not explode, just bubble and fountain.  If the magma is thick, it is harder for gas bubbles to escape, explosive  |  | 
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        |     broad, flat volcanoes with very gently sloping sides  Hawaiian eruptions:  very runy lava
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        |         when lava rises to the surface through long fissures that produce vast, flat lava plains  |  | 
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        |         more explosive then Hawaiian, creates cinder cones  |  | 
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        |          explosive, produce  pyroclastic flows (tend to build up strato volcanoes)  |  | 
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        |         most violent, produce ash columnsand create pyroclastic flows tend to build up (strato volcanoes)  |  | 
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        |       a volcano composed of solidified lava flows interlaced with pyroclastic material tend to erupt explosively  |  | 
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        |         hot volcanic fragments (tephra) that are buoyed by heat and volcanic gases and flow very rapidly.   |  | 
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        |         Mudflow that is created when volcanic ash mixes in with snow or rain at the summit   |  | 
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