Chapter 4 Test! Flashcards
(23 cards)
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.
Silicates
The largest group. Composed of silicon bonded with
oxygen atoms. Different forms of silicates are created by having a
different number of oxygen atoms.
Native elements
Contain only one element. (Gold, Copper, Silver,
Sulfur, Diamond, Antimony, Lead, etc.)
Carbonates
Minerals formed when one carbon atom is bonded to
three oxygen atoms.
Halides
form when salt water evaporates and leaves the solid precipitate behind. Examples: Halite, Fluorite.
Oxides
Contain one or two metal elements combined with oxygen.
Examples: Magnetite and Hematite.
Phosphate
Composed of phosphorus bonded with oxygen atoms.
Example: Apatite.
Sulfate
Contain sulfur atoms bonded to four oxygen atoms. The
also form when salt water evaporates. Examples: Gypsum, Barite.
Sulfides
Form when metallic elements combine with sulfur atoms
in the absence of oxygen atoms. Examples: Pyrite, Galena, Stibnite,
Chalopyrite.