Geology Midterm 1 Flashcards
Rock
Aggregate of one or more minerals
Mineral
- Inorganic
- Naturally occurring
- Crystalline solid
- Narrowly defined chemical composition
- Orderly atomic structure
- Characteristic physical properties
Ionic, Covalent, Metallic, and Van Der Waals Bonding
Ionic: transfer of ions w/ opposite electrical charges attracting one another.
Covalent: Atoms share electrons.
Metallic: Extreme electron sharing, explains why metals are good conductors of heat and electricity.
Van Der Waals: Extremely weak without available electrons to form attraction (ex. Graphite)
Cleavage-Mineral Properties
Breakage along planes of weakness. Alignment of bonds create these planes of weakness, not all minerals exhibit cleavage.
- Cleavage in one direction (basal cleavage): ex. micas- biotite, muscovite.
- Cleavage in 2 directions @ 90 degrees: ex. Feldspars- potassium feldspar and plagioclase feldspar.
- Cleavage in 2 directions NOT at 90 degrees: ex. amphibole
- Cleavage in 3 directions @ 90 degrees (cubic cleavage): ex. galena
- Cleavage in 3 directions NOT at 90 degrees (rhombohedral cleavage): ex. dolomite, calcite.
- Cleavage in 4 directions (octahedral cleavage): ex. fluorite.
- Cleavage in 6 directions (dodecahedral cleavage): ex. sphalerite
Fracture-Mineral Properties
A mineral breakage along an irregular surface. Any mineral will fracture if enough force is applied. You may have uneven or conchoidal fractures.
Hardness-Mineral Properties
Resistance to scratching or abrasion.
Moh's Hardness Scale 10-Diamond 9-Corundum 8-Topaz 7-Quartz 6-Orthoclase 5-Apatite 4-Flourite 3-Calcite 2-Gypsum 1-Talc
Luster-Mineral Properties
How a mineral reflects light (metallic or non metallic).
Non Metallic: can be light or dark coloured, shiny or dull.
Metallic: Metallic luster
Crystal Form-Mineral Properties
The shape a mineral will grow in (only if the mineral grows in unrestricted space-not common)
Broken Minerals DO NOT EQUAL crystals
- look to see if there is any internal weakness
- look to see if there are any fractured surfaces
Reaction to HCl-Mineral Properties
Some minerals will react with dilute HCl (effervesce)
Streak-Mineral Properties
The colour of the powdered form of a mineral (rub sample on porcelain)
Color-Mineral Properties
Can vary in the same mineral.
Many minerals such as quartz can take on a variety of colors
Silicates-Mineral Classes
The building block for silicate minerals is the silica tetrahedron.
Silica Tetrahedron: Net charge of 4, needs to bond w/ cations to balance the negative charge or O-2 ions can bond with other O-2 ions of nearby silica tetrahedron sharing the electrons
Nonferromagnesian Silicate: Si and O
Ferromagnesian Silicate: Contain Fe and sometimes MG
Native Elements-Mineral Classes
Copper, Gold, Lead, Graphite
These minerals DO NOT need to bond.
Oxides-Mineral Classes
Ice, hematite, corundum, magnetite.
These minerals contain O-2.
Sulphides-Mineral Classes
Galena, pyrite, chalcopyrite, sphalerite
These minerals contain S-2
Sulphates-Mineral Classes
Barite, gypsum, anhydrite
These minerals contain SO4
Halides-Mineral Classes
Flourite, halite
These contain either Cl or F
Carbonates- Mineral Classes
Calcite, Dolomite
These minerals contain CO3