4: Earth Materials Flashcards

1
Q

What is the definition of a “natural mineral”?

A
  1. They occur naturally
  2. They are inorganic
  3. Has a specific chemical composition
  4. Solid at room temperature
  5. The atoms are arranged in a repeating pattern.
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2
Q

What materials make up 75% of the earth’s crust?

A

Oxygen and silicon.

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3
Q

What percentage of oxygen is in the crust?

A

46.6%

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4
Q

What percentage of silicon is in the crust?

A

27.7%

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5
Q

What percentage of aluminum is in the crust?

A

8.1%

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6
Q

What percentage of iron is in the crust?

A

5.0%

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7
Q

What percentage of calcium is in the crust?

A

3.6%

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8
Q

What percentage of sodium is in the crust?

A

2.8%

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9
Q

What percentage of potassium is in the crust?

A

2.6%

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10
Q

What percentage of magnesium is in the crust?

A

2.3%

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11
Q

What percentage of other materials are in the crust?

A

1.5%

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12
Q

How are crystals formed?

A

When heat is lost, the atoms come closer together forming bonds. Crystals form in different solutions - it often forms in a liquid and then precipitates.

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13
Q

What structure is a diamond in?

A

Carbon Tetrahedral

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14
Q

What structure is graphite in?

A

A sheet of carbon atoms

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15
Q

What are the names of the 6 mineral structures?

A

Cubic, Tetragonal, Orthorhombic, Monoclinic, Triclinic, Hexagonal?

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16
Q

What does the cubic mineral structure look like?

A

The 3 axises are the same length and they join together at a 90º.

17
Q

What is an example of a cubic mineral structure?

18
Q

What does the tetragonal mineral structure look like?

A

All 3 axes intersect at a perpendicular angle - two of which are the same length.

19
Q

What is an example of a tetragonal mineral structure?

20
Q

What does the orthorhombic mineral structure look like?

A

All 3 axes intersect at a perpendicular angle to one another, but are differing in lengths.

21
Q

What is an example of the orthorhombic mineral structure?

22
Q

What does the monoclinic mineral structure look like?

A

All 3 of the axes are different lengths, 2 of which intersect at a 90º angle and the last intersecting at an oblique angle (not 90º).

23
Q

What is an example of the monoclinic mineral structure?

24
Q

What does the triclinic mineral structure look like?

A

All 3 axes are different in length and join together at oblique angles.

25
What is an example of triclinic mineral structure?
Kyanite
26
What does the hexagonal mineral structure look like?
All 3 axes are the same length meeting together at 60º. The 4th axis can be vertical and is often different in length.
27
What is an example of the triclinic mineral structure?
Quartz
28
What are the 6 categories we can separate the mineral identification in?
Silicates, Carbonate, Oxides, Sulphides, Sulphates, Halides, Phosphates, Natural Elements
29
What percentage of minerals are in the silicate family on earth?
90%
30
What are 2 types of silicate minerals?
Non-Ferromagnesium and Ferromagnesium
31
What is Non-Ferromagnesium?
Minerals that contain silicon and oxygen (quartz)
32
What is Ferromagnesium?
Minerals that contain silicon, oxygen, magnesium/iron.
33
What are carbonates in terms of mineral identification?
Negatively charged carbonate ion + positively charged metal ion.
34
What are oxides in terms of mineral identification?
Minerals that are combined with oxygen.
35
What are sulphides in terms of mineral identification?
Minerals that are combined with sulphurs.
36
What are halides in terms of the mineral identification?
Minerals that contain a halite (fluorine or chlorine) with a positively charged metal ion.
37
What are phosphates in terms of mineral identification?
Minerals that contain a phosphate ion and a positively charged metal ion.
38
What are native elements in terms of mineral identification?
Elements that occur naturally according to the 5 characteristics.