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The two most abundant elements on earth |
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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: |
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An atom has an equal number of protons and electrons |
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Electrons are configured around the nucleus in: |
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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: |
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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: |
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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: |
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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 |
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dark colored minerals rich in magnesium and iron |
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Sialic chemical composition |
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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: |
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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 |
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How viscocity realtes to eruption style |
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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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