Chapter 5 - Minerals Flashcards

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0
Q

Crystal lattice

A

The imaginary framework representing Ye arrangement of atoms

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1
Q

To be a mineral it must be

A

Naturally occurring, solid, formed by geologic processes, definable chemical composition, orderly arrangement of atoms. Pg 148 in organic

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2
Q

Crystalline solid

A

A material in which atoms are fixed in an orderly pattern

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3
Q

A glass

A

Atoms, ions or molecules are arranged in a semi chaotic way. Pg 124

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4
Q

What is a crystal?

A

A single, continuous piece of a crystalline solid blinded by flat surfaces called Crystal faces that grew naturally as the Mineral formed.

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5
Q

Nicholas Steno

A

The angle between two adjacent Crystal faces is identical to the angle of Crystal faces next to that angle. All angles Ina Quartz is 120 degrees. Pg 124

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6
Q

Crystal structure

A

The way in which atoms are packed

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7
Q

Anions

A

Atoms add elections and become negatively charged

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8
Q

Cations

A

Lose electrons to become positively charged

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9
Q

Halite

A

Rock salt- ironically bonded mineral, consists of oppositely charged ions that stick together Cuz opposites attract. Cl- and Na+.

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10
Q

Diamond

A

Made entirely of carbon. Atoms are in a tetrahedron. Covalent bonds are very strong in turn a diamond is very hard.

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11
Q

Graphite

A

Also made of all carbon it is opposite in look and hardness of a diamond. This is because of the shape the atoms are in they are in sheets and are bonded weakly in van see Waals bonds.

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12
Q

Polymorphs

A

Diamond and graphite.

Two different minerals have same compilation but have different Crystal structures

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13
Q

Five ways which a mineral can form:

A
  1. Solidification of a melt or freezing liquid.
  2. Can form by evaporation of liquid. Salt crystals
  3. Solid- state diffusion
  4. Bio Mineralization (fossils)
  5. Vapor. Pg 154
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14
Q

Geode

A

A mineral lined cavity in rock

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15
Q

Physical properties

A

Visual and material characteristics that distinguishes one mineral from another.

16
Q

Most commonly used physical properties

A

Color, streak, luster, hardness, specific Gravity, Crystal habit

17
Q

MOHs hardness scale

A

Helps in mineral identification. Helps compare hardness of a mineral with a common items. Such as fingernails and a penny

18
Q

Silicates:

A

Silicon- oxygen tetrahedron. Most minerals in the earth crust. A silicon atom surrounded by four oxygens arranged Ina form of a tetrahedron. Examples: olivine and Quartz
95% of the continental crust.

19
Q

Oxides

A

Consist of metal cations bonded to oxygen anions. Ex: magnetite and hematite

20
Q

Sulfides

A

Metal cation bonded to a sulfide anion. Ex Helena and pyrite

21
Q

Sulfates

A

Metal cation bonded to the SO2-4 a ionic group. Many font by perspiration out of water at or near the earths surface ex: gypsum

22
Q

Halides

A

Anion in a halide is a halogen ion. Ex: halite and fluorite

23
Q

Carbonates

A

CO 2-3 anionic group ex: calcite and dolomite

24
Q

Native metals

A

Pure masses of a single metal. Metallic bonds. Copper and gold

25
Q

Silicate - independent tetrahedra:

A

Independent and do not share oxygen atoms. Pg 161 ex: olivine and garnet

26
Q

Silicate- single chain

A

Tetrahedra link to form a chain by sharing two oxygen atoms each.

27
Q

Silicate double chains

A

Tetrahedra link to form double chain by sharing two or three oxygens. Black or dark brown elongate crystals with two cleavage directions

28
Q

Sheet silicates

A

Tetrahedra in this group all share three oxygen atoms and therefore link to form two dimensional sheets. Ex: muscovite and biotite

29
Q

Framework silicates

A

Each tetrahedron shares all four oxygen atoms with its neighbors forms 3-D structure. ex- feldspar and Quartz

30
Q

Gemstone

A

Is a mineral that has special value because it is rare and people consider it beautiful.

31
Q

Gem

A

Is cut and finished stone ready to be used in jewelry