Term
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Definition
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any rock formed by the cooling and hardening of
hot liquid rock
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Term
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Definition
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hot liquid rock beneath the earth’s surface
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Term
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Definition
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magma that reaches the earth’s surface
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Term
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Definition
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igneous rock that forms deep within the earth
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Term
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Definition
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igneous rock that forms from lava at the earth’s
surface
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Term
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Definition
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igneous rock that has very small or no
visible crystals and indicates that the rock cooled very
fast
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Term
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Definition
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igneous rock that has large crystal
faces, which indicates that the rock cooled very slowly
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Term
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Definition
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what the rock is made from
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Term
| light colored or granitic |
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Definition
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indicates the rock contains
minerals like quartz and feldspars which are high in silica and low in iron
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Term
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Definition
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indicates that the rock contains
minerals such as olivine and pyroxene which are high in iron, calcium or magnesium
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Term
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Definition
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igneous rock that has changed and thus
has two or more different sized mineral crystals
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Term
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Definition
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irregular formation of intrusive rock formed by magma beneath the surface of the earth as it slips into the
cracks and crevices of other rock
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Term
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Definition
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huge, irregularly shaped intrusion that extends deep
into the earth’s crust. Generally has an exposed area larger that 100 square km
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Term
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Definition
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domelike intrusion that pushes the overlying rocks(the rocks above it) into an arch and has a flat floor
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Term
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Definition
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sheetlike mass of igneous rock that lays horizontally
between rock layers
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Term
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Definition
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narrow, flat formation of igneous rock formed in the
vertical cracks in the existing rocks
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Term
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Definition
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layers of lava that build up on a flat area on the Earth’s surface. These are directly related to lava flows
and fissures
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Term
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Definition
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large cracks in the Earth’s surface where lava can ooze
out onto the ground
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Term
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Definition
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any flow of lava on the surface of the Earth due to fissures or volcanoes
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Term
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Definition
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formed when magma hardens inside of the vent of
a volcano. The rock that makes up the “neck” is harder than
the surrounding volcanic cone material. Over time, the cone material is eroded away leaving only the “neck” remaining.
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