INTRO: ROCKS & MINERALS Flashcards

1
Q

Name two types of isotopes

A

Radioactive and Stable (Non-Radio Active)

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2
Q

A stable configuration occurs when a valence shell contains…

A

Eight Electrons

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3
Q

There are three main types of chemical bonds:

A

Ionic, Covalent, Metallic

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4
Q

Ionic Bonds:

A

transfer electrons between atoms

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5
Q

Covalent Bonds:

A

share electrons between atoms

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6
Q

Metallic Bonds:

A

valence electrons move freely among atoms

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7
Q

Diamond consists…

A

entirely of carbon atoms united by covalent bonds in a tetrahedral
structure with a repeating pattern of 8 atoms

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8
Q

Crystal lattice:

A

The 3-D molecular structure of a mineral;

its configuration reflects relative sizes and
numbers of ions that make up the mineral

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9
Q

To form a stable compound, the ions must have:

A

1) their ionic charges be in balance, and
2) right size to allow them to fit together

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10
Q

Cation Substitution:

A

Cations of similar size and charges tend to substitute for one
another in the crystal lattice and can form compounds having the same crystal
structure but different chemical composition

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11
Q

Definition of a mineral:

A

In geology, a mineral is a naturally occurring, inorganic solid, with a crystalline structure
and definite chemical composition formed by geological processes

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12
Q

Characteristics of a Mineral:

A
  1. naturally occurring
  2. inorganic
  3. solid
  4. characteristic crystalline structure
  5. definite chemical composition
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13
Q

Crystalline solid

A

Minerals exhibit an ordered internal structure in which in which the atoms are
arranged in a regular, repeating pattern

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14
Q

Chemical composition of a mineral and the way in which atoms are bonded
determines:

A
  1. Mineral shape and appearance
  2. Mineral hardness
  3. The way in which a mineral breaks, also known as cleavage or fracture
  4. The specific gravity or weight of a mineral
  5. Optical properties such as color, luster, or diaphaneity
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15
Q

There are three types of diaphaneity:

A

*Transparent minerals transmit light freely
*Translucent minerals transmit light although it maybe hard to see through them
*Opaque minerals do not transmit light at all and appear solid

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16
Q

Three Main Types of Lustre:

A
  1. Metallic luster: appearance of polished metal
  2. Non-metallic luster: does not look like metal
  3. Sub-metallic luster: somewhat metallic without a polished sheen
17
Q

Moh’s scale of hardness:

A

Relative scale of hardness
Softest (1) talc – hardest (10) diamond

18
Q

Cleavage is described by:

A
  • Number of planes
  • Angles between adjacent planes
  • Constant for a particular mineral
19
Q

Fracture:

A
  • Some minerals break unevenly (fracture) and do not exhibit cleavage
    – Smooth, curved surfaces when minerals break in a glass-like manner:
    conchoidal fracture
    – Others include fibrous and rough fracture (asbestos)
20
Q

Silicates

A
  • Silicates are the most abundant group of minerals in the crust and mantle;
  • They contain silicon bonded to an oxygen
    in a unit structure known as the
    silica tetrahedron;

– 4 oxygen atoms (-8) surround a much smaller silicon atom (+4)

  • Most silicate minerals form at high temperatures
21
Q

How tetrahedra may be linked:

A
  • independent tetrahedra (olivine, garnet)
  • single chains (pyroxene group)
  • double chains (amphibole group)
  • Sheets (mica group)
  • Framework (feldspars and quartz)
22
Q

Feldspar groups:

A
  1. Alkali feldspars

(potassium or K-spar)
* Orthoclase, sanidine, microcline, anorthoclase

  1. Plagioclase feldspars

(solid solutions between Na and Ca)
* Albite (Na) to Anorthite (Ca)

23
Q

Non-Silicates:

A

– Carbonates
– Sulfates
– Sulfides
– Halides
– Oxides
– Native elements

24
Q

Carbonate Minerals

A

Unlike silicates, most carbonates form at low temperatures near the Earth’s
surface – precipitated from solution in shallow seas or from groundwater

Prominent carbonate rocks include limestone and dolostone

25
Q

Sulfate Minerals

A

Formed at low temperatures near the earth’s surface mainly through
evaporation of groundwater, lake, or ocean waters

26
Q

Types of Sulfate Minerals:

A

Gypsum is a common sulfate mineral:
– Does not react with HCl
– Hardness of 2 (Moh’s Scale) easily scratched with fingernail

Alabaster:
fine-grained, massive gypsum

Plaster of Paris:
powdered form of calcium sulfate. When
water is added it forms a gypsum cement

Sulfide minerals are major ores of lead, zinc, copper, and molybdenum

27
Q

Iron Oxides

A

Iron oxides form a small percentage of rocks

They are important ore bodies:

– magnetite (black streak and magnetic)
– hematite (rusty streak and not magnetic)

28
Q

Halide Minerals

A

Halides have anions of the halogen elements (fluorine, chlorine, bromine, iodine).
– Halides are made of ionic bonds
– Form as mineral-rich waters evaporated
– Halite (sodium chloride - NaCl) is salt
– Sylvite (potassium chloride - KCl) is a potassium salt (potash)

29
Q

Native Elements

A
  • Minerals of a single element
    – Gold, Silver, Copper, Sulphur
30
Q

Rock:

A

Consolidated solid material comprised of aggregates of one or more
minerals or solidified organic material.

Most rocks consist of more than one mineral, for example granite = quartz,
feldspar, mica, and hornblende.

Some rocks are composed of only one mineral, for example limestone formed
from coral reefs (calcite).

31
Q

Three
fundamental rock types that reflect their origin and processes of formation:

A
  1. Igneous,
  2. Sedimentary
  3. Metamorphic
32
Q

Igneous rocks:

A

are derived from the cooling and crystallization of molten rock

33
Q

Intrusive (Plutonic)

A

magma emplaced at depth

34
Q

Extrusive (Volcanic)

A

lava extruded at surface

35
Q

Sedimentary rocks:

A

are formed from the weathered remnants of pre-existing
rock (sediment) that has been compacted or cemented (i.e., process of
lithification)
or from minerals precipitated from water by chemical or biological
processes

36
Q

Metamorphic rocks:

A

are formed by the transformation of pre-existing rock by:

  • high temperature,
  • high pressure, and
  • chemically active fluids.