Geology Midterm 1 Flashcards

1
Q

Rock

A

Aggregate of one or more minerals

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2
Q

Mineral

A
  • Inorganic
  • Naturally occurring
  • Crystalline solid
  • Narrowly defined chemical composition
  • Orderly atomic structure
  • Characteristic physical properties
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3
Q

Ionic, Covalent, Metallic, and Van Der Waals Bonding

A

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)

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4
Q

Cleavage-Mineral Properties

A

Breakage along planes of weakness. Alignment of bonds create these planes of weakness, not all minerals exhibit cleavage.

  1. Cleavage in one direction (basal cleavage): ex. micas- biotite, muscovite.
  2. Cleavage in 2 directions @ 90 degrees: ex. Feldspars- potassium feldspar and plagioclase feldspar.
  3. Cleavage in 2 directions NOT at 90 degrees: ex. amphibole
  4. Cleavage in 3 directions @ 90 degrees (cubic cleavage): ex. galena
  5. Cleavage in 3 directions NOT at 90 degrees (rhombohedral cleavage): ex. dolomite, calcite.
  6. Cleavage in 4 directions (octahedral cleavage): ex. fluorite.
  7. Cleavage in 6 directions (dodecahedral cleavage): ex. sphalerite
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5
Q

Fracture-Mineral Properties

A

A mineral breakage along an irregular surface. Any mineral will fracture if enough force is applied. You may have uneven or conchoidal fractures.

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6
Q

Hardness-Mineral Properties

A

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
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7
Q

Luster-Mineral Properties

A

How a mineral reflects light (metallic or non metallic).

Non Metallic: can be light or dark coloured, shiny or dull.

Metallic: Metallic luster

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8
Q

Crystal Form-Mineral Properties

A

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
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9
Q

Reaction to HCl-Mineral Properties

A

Some minerals will react with dilute HCl (effervesce)

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10
Q

Streak-Mineral Properties

A

The colour of the powdered form of a mineral (rub sample on porcelain)

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11
Q

Color-Mineral Properties

A

Can vary in the same mineral.

Many minerals such as quartz can take on a variety of colors

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12
Q

Silicates-Mineral Classes

A

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

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13
Q

Native Elements-Mineral Classes

A

Copper, Gold, Lead, Graphite

These minerals DO NOT need to bond.

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14
Q

Oxides-Mineral Classes

A

Ice, hematite, corundum, magnetite.

These minerals contain O-2.

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15
Q

Sulphides-Mineral Classes

A

Galena, pyrite, chalcopyrite, sphalerite

These minerals contain S-2

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16
Q

Sulphates-Mineral Classes

A

Barite, gypsum, anhydrite

These minerals contain SO4

17
Q

Halides-Mineral Classes

A

Flourite, halite

These contain either Cl or F

18
Q

Carbonates- Mineral Classes

A

Calcite, Dolomite

These minerals contain CO3