Minerals, Igneous, Sedimentary, Metamorphic Rocks Flashcards
Crystal form (habit)
the general shape or character of a crystal or cluster of crystals that have grown in nature unimpeded.
Cleavage
breakage of a mineral along a flat plane of weakness
Excellent Cleavage
easily identifiable; minerals that when broken produce pieces shaped as cubes, rhombohedrons, columns, pyramids or planes
Good Cleavage
minerals that when broken retain a distinctive shape with flat sides, but have distortion around parts of the mineral (ex: rounded edges)
Poor/Absent
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Mineral Hardness
measure of the resistance of a mineral to abrasion or scratching
Color
Not always diagnostic because of impurities
Streak
Color of the fine powder of a mineral obtained by rubbing the mineral across a piece of unglazed porcelain
Reaction to Hydrochloric Acid
determines whether a mineral is a member of the Carbonate family (CO3)
Rocks
aggregates of minerals in which the minerals retain their individual properties
Igneous Rocks Compositional Features
- Dominated by dark colored silicate minerals
- ~50% dark to ~50% light colored silicate minerals
- Dominated by light colored silicate minerals
Igneous Rocks Grain Size
Usually have visible crystal. Fine grain = extrusive rock. Coarse grain = intrusive rock
Felsic
Igneous rock composed mainly of light-colored minerals like quartz and feldspar
Intermediate
Igneous rock composed of a mixture of light and dark-colored minerals like quartz, feldspar, amphibole, and biotite
Mafic
Dark-colored minerals like olivine, pyroxene, and amphibole account for 45%-85% of the rock. Plagioclase feldspar makes up most of the rest of the rock.