Week 2 Flashcards

1
Q

defining characteristics of a mineral

A

1) naturally occurring
2) solid
3) inorganic (non-living)
4) definite chemical composition
5) ordered internal structure (crystalline)

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2
Q

Aggregate

A

implies that minerals are joined in such a way that the properties of each minerals are retained

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3
Q

how many elements are there

A

118, and 90 naturally occuring

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4
Q

Atom

A

the smallest part of matter that cannot chemically be split, an extremely small chemical that does the combining

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5
Q

why are atoms neutral

A

number of electrons = number of protons

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6
Q

covalent bonding

A

the sharing of an electron pair between two atoms

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7
Q

ionic bonding

A

the electrostatic force of attraction between a positively charged metal ion and a negatively charged non-metal ion

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8
Q

metallic bonding

A

Occurs in metals in pure, native form (e.g copper, gold, and silver)… Nuclei of metal atoms “float” in a sea of electrons. This free migration of electrons accounts for strong ability of metals to conduct electricity and the ease with which metals are shaped

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9
Q

intermolecular bonding

A

these bonds are very weak, produced by slight charge imbalances (“van der Waals” forces)

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10
Q

Crystal Form/Habit

A

Arrangement patterns of atoms within minerals are displayed in their external crystal form. The packing arrangement of atoms within any given mineral result in a characteristic geometry of crystal faces.

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11
Q

Cleavage

A

When a mineral breaks along well-defined planes. A mineral will preferentially break along planes of weaker bonding within the crystal structure

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12
Q

Fracture

A

Some minerals do not have a distinct cleavage due to more uniform bond strengths throughout the crystal structure (no distinct planes of weakness).
For example, broken surfaces of quartz are scoop-shaped. The curved surfaces look like the interior of a seashell, so is called conchoidal fracture.

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13
Q

Hardness

A

Measure of the resistance of minerals to being scratched. The hardness of a mineral reflects the overall strength of bonding within its crystal structure. Hardness is measured in units of Mohs scale of hardness.

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14
Q

Specific Gravity

A

A number representing the ratio of the weight of a mineral to the weight of an equal volume of water

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15
Q

Diaphaneity

A

Ability to transmit life. Can be transparent, translucent or opaque

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16
Q

Lusture

A

the appearance or quality of light reflected from the surface of a mineral

17
Q

Metallic Lusture

A

the appearance of metal
EX. gold and pyrite

18
Q

Non-metallic Lusture

A

not having the appearance of metal
EX. fluorite, calcite and tourmaline

19
Q

Colour

A

primarily manifests the chemical content of a mineral. Also relates to the charges among ions within the mineral

20
Q

Amethyst Quartz Colour

A

This “yellow” range of wavelengths of white light is absorbed. So we see wavelengths of purple, which is the complimentary colour on the colour wheel

21
Q

Streak

A

Another way of identifying some minerals is to powder them. We do this by rubbing the mineral specimen against an unglazed porcelain plate called a streak plate
EX. Hematite (iron oxide) is redish brown

22
Q

Gemstone beauty

A

Beauty of a gem is usually based on: colour, lustre, transparency, or unusual optical properties

23
Q

The four C’s of gemstones quality

A

carat weight, colour, clarity and cut

24
Q

Durability

A

the resistance of the gemstone damage and dependent upon physical properties, such as hardness and tenacity.

25
Q

Tenacity

A

the resistance to bending and breaking

26
Q

Stability

A

Usually refers to the gem’s resistance to destruction by chemical factors. Can also refer to how well a gemstone retains its colour

27
Q

Weight

A

The carat (ct) is the standard unit of weight used in the pricing of gemstones. Due to differences in the density/specific gravity of different gems, carat weight can be misleading:
EX. a one carat sapphire is much smaller than a one carat opal, and a one carat diamond is smaller than a one carat sapphire

28
Q

Rarity

A

reflects the uniqueness of natural geological processes that form them

29
Q

Demand

A

Value of certain gemstones fluctuate with trends in fashion

30
Q

Corundum

A

Usually dull in colour, Ruby and sapphire are just unusually beautiful forms of it.
Specimens of corundum with exceptional clarity and colour are used as gemstones

31
Q

Asterism

A

Star pattern of light in some sapphires and rubies, resulting from the presence of inclusions of the rutile (TiO2). Play of light usually forms a six-sided star

32
Q

Three basic cuts used

A

1) Cabochon
2) Brilliant
3) Step

33
Q

Cabochon Cut

A

Simple round- to oval-shaped dome, used principally in translucent and opaque gemstones with bold colours and intermediate hardness.
EX. turquoise and opal

34
Q

Brilliant Cut

A

Accentuates a gemstone’s ability to transmit, reflect and disperse light. Principally developed for diamonds.
Can have up to 59 facets that are carefully angled to highlight a stone’s brilliance and light disperson

35
Q

Step Cut

A

broad table-like facet with smaller and longer rectangular facets around its edges. This type of cut emphasizes the colour of stones with a low degree of light dispersion

36
Q

Varient of Step Cut: Emerald Cut

A

Developed to reduce edge damage of emeralds and other brittle gems