Chapter 4 Test! Flashcards
Formation from Magma
Minerals form from the cooling of magma and/or lava.
Minerals
- Solid
- natural
- inorganic
- Definite chemical composition
- crystal structure due to internal arrangement of atoms.
Formation from solutions
As water evaporates from solutions, it leaves behind mineral particles. Mineral deposits that form between cracks of rocks are called veins.
Formation from pressure
Minerals can change form or change completely because of the temperature and pressure.
Common minerals found in rocks
- quarts
- olivine
- feldspar
- Amphibole
- Muscovite
- magnetite
- biotite
- pyrite
- calcite
Identification properties
- hardness
- luster
- crystal shape(form)
- color
- streak
- cleavage/fracture
- density
Hardness
- ability to scratch another mineral.
- MOHs scale from 1(talc) to 10(diamond).
Crystal shape
- external structure due to internal arrangement of atoms.
- six basic groups of shapes with about three dozen variations.
Luster
- describes how light reflects off the surface.
- main actor forties are metallic and non metallic.
Color
-results from ability to absorb some wavelengths and reflect others.
Streak
Color of the powder when rubbed on a streak plate.
Cleavage/fracture
- some minerals split along flat surfaces when struck hard —-this is called cleavage.
- other minerals break unevenly along rough or curved surfaces—this is called fracture.
Density
- All minerals have density(mass/volume)
- specific gravity is the density of the material compared with the density of water.
Special characteristics
Some minerals will glow when placed under short wave or long wave ultraviolet rays.
Special characteristics
Salty taste— DO NOT TASTE.
Halite is the exception, it will taste salty.