Chapter 2 - Mineralogy Flashcards

1
Q

The study of minerals.

A

Mineralogy

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

The basis for the formation of rocks.

A

Minerals

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

It makes up the minerals and minerals make up rocks.

A

Matter (elements)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

A naturally occurring combination of specific elements arranged in a particular repeating three-dimensional structure or lattice.

A

Mineral

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

These determine the physical properties of minerals.

A

Chemical formula and the Crystal lattice

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

The types and proportions of the chemical elements

A

Chemical Formula

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

The geometry of how the atoms are arranged and bonded together)

A

Crystal Lattice

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Ten minerals make up most of the volume of the earth’s crust

A

Plagioclase, quartz, orthoclase, amphibole, pyroxene, olivine, calcite, biotite, garnet, and clay

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Readily observable and certainly obvious, but it is usually less reliable than other physical properties.

A

Color

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Describes the reflection of light off a mineral’s surface.

A

Luster

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

The standard names of luster

A

Metallic, glassy, pearly, silky, greasy, and dull

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

The color of a mineral’s powder. A more reliable property than color because this does not vary.

A

Streak

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

The strength with which a mineral resists its surface being scraped or punctured.

A

Hardness

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

In working with hand samples without specialized tools, mineral hardness is specified by __________.

A

Mohs hardness scale

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

The tendency of a mineral to break along certain planes to make smooth surfaces.

A

Cleavage

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

The cleavage properties of a mineral are described in terms of ________.

A

The number of cleavages and, if more than one cleavage, the angles between the cleavages

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

The possible number of cleavages a mineral may have.

A

1, 2, 3, 4, and 6

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

A break in a mineral that is not along a cleavage plane.

A

Fracture

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

The way a thick piece of glass breaks with concentric, curving ridges on the broken surfaces.

A

Conchoidal fracture

20
Q

A standard term for fractures that do not exhibit any of the qualities of the other fracture types.

A

Irregular Fracture

21
Q

Mineral glows under ultraviolet light

A

Fluorescence

22
Q

A mineral is attracted to a magnet

23
Q

Mineral gives off radiation that can be measured with a Geiger counter

A

Radioactivity

24
Q

Bubbles form when the mineral is exposed to a weak acid

A

Reactivity

25
Some minerals have a distinctive smell
Smell
26
Some minerals taste salty
Taste
27
Based on the polyatomic anion, which has a tetrahedral shape.
Silicates
28
Most minerals in the earth’s crust and mantle are ____________.
Silicate Minerals
29
The silicate tetrahedra are separated from each other and bonded completely to nonsilicate atoms.
Nesosilicates
30
The silicate tetrahedra are bonded in pairs.
Sorosilicates
31
The silicate tetrahedra are joined in rings. Beryl or emerald is an example.
Cyclosilicates
32
The tetrahedra are bonded at three corners to form flat sheets. Biotite is an example
Phyllosilicates or sheet silicates
33
The silicate tetrahedra are bonded in single chains. Pyroxenes is an example
Single-chain inosilicates
34
The silicate tetrahedra are bonded in double chains. Amphiboles is an example
Double-chain inosilicates
35
All corners of the silicate tetrahedra are bonded to corners of other silicate tetrahedra, forming a complete framework of silicate tetrahedra in all directions. Feldspar, the most common mineral in earth’s crust, and quartz are the examples
Tectosilicate
36
These are based on the sulfide ion
Sulfides
37
These are based on the carbonate ion
Carbonates
38
This tends to dissolve relatively easily in water, especially acid water, and natural rainwater is slightly acid
Carbonate Minerals
39
These are based on the oxygen anion
Oxides
40
These have a halogen element as the anion, whether it be fluoride, chloride, bromide, iodide, or astatide.
Halides
41
These have the polyatomic sulfate ion, as the anion.
Sulfates
42
These have the polyatomic phosphate ion, as the anion.
Phosphates
43
These are made of nothing but a single element.
Native Elements
44
Ways of Identifying Minerals
1. Look at it closely on all visible sides to see how it reflects light 2. Test its hardness 3. Identify its cleavage or fracture 4. Name its luster 5. Evaluate any other physical properties necessary to determine the mineral’s identity
45
Formation of Minerals
- Formation from Hot Materials - Formation from Solutions