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41 Cards in this Set
- Front
- Back
rocks
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aggregates of one or more kind of minerals.
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minerals
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inorganic, naturally occurring substances that have a charactersitic chemical composition, distinctive physical properties, and crystalline structure.
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Crystalline structure
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orderly three-dimensional arrangement of atoms or molecules
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Not true minerals
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Limonite and opal
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clarity
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transparent, translucent, or opaque.
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crystal forms
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cubes, pyramids, or prisms
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cryptocrystalline
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too small to see with th enaked eye
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luster
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how light reflects from the surface of an object, such as a mineral. Either metallic or nonmetallic
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Metallic luster
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reflect light just like the metal objects in the house
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nonmetallic luster
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a luster unlike that of metal objects
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streak
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color of a substance after is has been ground to a find powder
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hardness
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measure of resistance to straching
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fracture
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any break in a mineral that does not occur along a cleavage plane
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cleavage
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tendency of some minerals to break along flat, parallel surfaces.
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tenactiy
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manner in which a substance resist breakage.
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magma
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rock exists in isolated bodies below earth's surface
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intrusion
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a body of magma that pushes its way into the earth's crust
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instrusive igneous rock
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rock that was magma and forced out of the earth's crust and then cooled with visible crystals
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lava
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comes from the earths surface
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extrusive igneous rock
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is made when lava cools
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Texture
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ignoues rocks description of it's constituent parts and their sizes, shapes, and arrangement.
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aphanitic texture
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to small to see without a hand lens
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phaneritic texture
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coarse grained
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pegmatitic texture
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very coarse grained
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porphyritic texture
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two distinct sizes of crystals, phenocrysts which are the large crystals and matrix which are the smaller onces.
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vesicular texture
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vesicles. igneous rocks like scoria
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felsic minerals
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quartz, plagioclase feldspar, potassium feldspar. light colored.
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mafic minerals
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miotite mica, amphibole, pyroxene olivine. dark colored
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color index
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percentage of the mafic mineral crystals in the rock.
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felsic igneous rocks
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0-15% mafic minerals crystals
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Intermediate igneous rocks
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16-45% mafic mineral crystals
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Mafic Igneous rocks
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46-85% mafic mineral crystals
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Ultramafic igneous rocks
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86-100% mafic mineral crystals
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chemical weathering
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decomposition or dissoultion of earth materials
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sediments
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loose grains and chemical residues of earth materials
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physical/mechanical weathering
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corcking, scrathcing, crushing, abrasion, or other physical distintergration of earth materials
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grain size
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gravel, sand, silt, and clay
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crystalline teture
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clearly visbile crystals
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bioclastic sediments
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comprised mostly of the reamins of organism, such as shells
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Chemical
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sedmients and rocks are comprised mostly of intergrown mineral crystals
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Detrital
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compsed mostly of detrital grains
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