Chapter 4 Test! Flashcards

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0
Q

Formation from Magma

A

Minerals form from the cooling of magma and/or lava.

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1
Q

Minerals

A
  • Solid
  • natural
  • inorganic
  • Definite chemical composition
  • crystal structure due to internal arrangement of atoms.
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2
Q

Formation from solutions

A

As water evaporates from solutions, it leaves behind mineral particles. Mineral deposits that form between cracks of rocks are called veins.

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3
Q

Formation from pressure

A

Minerals can change form or change completely because of the temperature and pressure.

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4
Q

Common minerals found in rocks

A
  • quarts
  • olivine
  • feldspar
  • Amphibole
  • Muscovite
  • magnetite
  • biotite
  • pyrite
  • calcite
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5
Q

Identification properties

A
  • hardness
  • luster
  • crystal shape(form)
  • color
  • streak
  • cleavage/fracture
  • density
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6
Q

Hardness

A
  • ability to scratch another mineral.

- MOHs scale from 1(talc) to 10(diamond).

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7
Q

Crystal shape

A
  • external structure due to internal arrangement of atoms.

- six basic groups of shapes with about three dozen variations.

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8
Q

Luster

A
  • describes how light reflects off the surface.

- main actor forties are metallic and non metallic.

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9
Q

Color

A

-results from ability to absorb some wavelengths and reflect others.

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10
Q

Streak

A

Color of the powder when rubbed on a streak plate.

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11
Q

Cleavage/fracture

A
  • 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.
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12
Q

Density

A
  • All minerals have density(mass/volume)

- specific gravity is the density of the material compared with the density of water.

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13
Q

Special characteristics

A

Some minerals will glow when placed under short wave or long wave ultraviolet rays.

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14
Q

Special characteristics

A

Salty taste— DO NOT TASTE.

Halite is the exception, it will taste salty.

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15
Q

Silicates

A

The largest group. Composed of silicon bonded with
oxygen atoms. Different forms of silicates are created by having a
different number of oxygen atoms.

16
Q

Native elements

A

Contain only one element. (Gold, Copper, Silver,

Sulfur, Diamond, Antimony, Lead, etc.)

17
Q

Carbonates

A

Minerals formed when one carbon atom is bonded to

three oxygen atoms.

18
Q

Halides

A

form when salt water evaporates and leaves the solid precipitate behind. Examples: Halite, Fluorite.

19
Q

Oxides

A

Contain one or two metal elements combined with oxygen.

Examples: Magnetite and Hematite.

20
Q

Phosphate

A

Composed of phosphorus bonded with oxygen atoms.

Example: Apatite.

21
Q

Sulfate

A

Contain sulfur atoms bonded to four oxygen atoms. The

also form when salt water evaporates. Examples: Gypsum, Barite.

22
Q

Sulfides

A

Form when metallic elements combine with sulfur atoms
in the absence of oxygen atoms. Examples: Pyrite, Galena, Stibnite,
Chalopyrite.