Mineralogy Flashcards

1
Q

8 elements of Earth;s crust

A

Oxygen Silicon Aluminum<br></br>Iron Calcium Sodium<br></br>Potassium Magnesium

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2
Q

Physical Properties for Mineral Identification

A
  1. Color<br></br>2. Luster<br></br>3. Hardness; fracture<br></br>4. Streak<br></br>5. Specific gravity<br></br>6. Cleavage<br></br>7. Crystal form
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3
Q

Least reliable trait for mineral identification

A

Color

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4
Q

Physical appearance
of the unweathered
surface. The Way it reflects sunlight

A

luster

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5
Q

Measure of the strength of the structure of the mineral relative to the
strength of its chemical bonds

A

Hardness

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6
Q

Is the resistance of a mineral’s smooth surface (face) to
being scratched by a point or an edge

A

Hardness

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7
Q

Mohs Scale of Hardness

A

Talc<br></br>Gypsum<br></br>Calcite<br></br>Fluorite<br></br>Apatite<br></br>Orthoclase<br></br>Quartz<br></br>Topaz<br></br>Corundum<br></br>Diamond

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8
Q

Hardness of fingernail

A

2.5

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9
Q

hardness of penny

A

3

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10
Q

hardness of knife blade

A

5.5

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11
Q

Color of a mineral in its ground or
powdered form

A

streak

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12
Q

ratio of a mineral’s mass to the mass of an equal volume of water

A

specific gravity

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13
Q

a break along a smooth, flat
plane producing smooth flat surfaces
called faces

A

cleavage

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14
Q

a break that is not smooth but
produces irregular surfaces

A

fracture

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15
Q

a description of the way a mineral tends to break

A

fracture

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16
Q

smooth curved fracture that is similar to a broken glass

A

conchoidal

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17
Q

similar to conchoidal, just not as curved but still smooth

A

subconchoidal

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18
Q

has sharp points or edges that catch on a finger that’s
rubbed across the surface.

A

jagged

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19
Q

a fracture type that occurs in fibrous or finely acicular
minerals

A

splintery

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20
Q

a fracture that produces a texture similar to broken children’s clay

A

earthy

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21
Q

result from the internal atomic arrangement of
a mineral

A

crystal form

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22
Q

repetition of crystal forms which produce the visible shape of the mineral

A

crystal system

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23
Q

minerals that have the same chemical composition, but different crystal formation

A

polymorphs

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24
Q

imaginary straight lines that pass through the center of the
crystal faces at right angles to these faces and intersect at the center
of a perfect crystal

A

axes

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25
• 3 equal exes intersecting at right angles to each other
• Same measure
• 6 faces
• Each face is a square
• Angle between two adjacent sides is 90 deg.
• Ex. Galena, halite, pyrite
Isometric or Cubic
26
Four axes
• 3 of the 4 intersect at 60oangles to others in the same plane
• 4 th axis intersects the other 3 at a 90oangle
• Each of the similar 6 faces join each other at 60o
• 2 more identical faces are different form the other 6
• 2 identical faces form 90owith the other 6
• Ex. Calcite, quartz and apatite
Hexagonal
27
Two equal, horizontal, mutually perpendicular axes (a1, a2)
• Vertical axis (c) is perpendicular to the horizontal axes and is of a different length.
• All 3 axis intersect at 90 deg
• 2 of the 3 axis are of equal length
• Four identical often rectangular faces and two square faces
• All adjacent faces hit at 90 deg
• Ex. Chalcopyrite, zircon
Tetragonal
28
• 3 axis intersect at 90 deg
• None of the axis are equal length
• Four of the faces form similar rectangles
• 2 of the other faces are similar rectangles but different from the first 4
• All adjacent sides meet at 90 deg
• Ex. Olivine, sulfur, topaz
Orthorhombic
29
• 3 axes none of equal length
• Only 2 axes intersect at 90 deg
• 4 identical or similar faces
• 2 identical faces unlike the first 4
• 6 sided prism
• Faces meet at 90 deg and other angles
• Ex. Mica, gypsum, orthoclase, hornblende
Monoclinic
30
• 3 unequal axes • None of the axes intersect at 90 deg • Four similar or identical polygons and 2 larger similar or identical polygons different form the first 4 • None of the faces intersect at 90 deg • Ex. feldspars
Triclinic
31
The phenomenon wherein a mineral takes the external shape of some other mineral or object
pseudomorphism
32
process that cause pseudomorphism wherein removal of the atoms of the original object and replacement with atoms of the other mineral
substitution
33
process that cause pseudomorphism where one mineral encrusts or coats another. Then the encrusted mineral may dissolve away leaving behind the encrusting mineral as a pseudomorph
encrustation
34
process that cause pseudomorphism wherein conversion of one mineral to another by chemical reaction usually involving the addition of water
alteration
35
process that cause pseudomorphism wherein after a polymorphic change, the external shape of the previous polymorph may be retained
polymorphic transformations
36
subclasses of the silicate group
• Nesosilicates(single tetrahedrons)
• Sorosilicates(double tetrahedrons)
• Inosilicates(single and double chains)
• Cyclosilicates(rings)
• Phyllosilicates(sheets)
• Tectosilicates(frameworks)
37
•Structure possessing isolated silicate tetrahedra
nesosilicate
38
Structure possessing double island silicate tetrahedra
sorosilicate
39
Structure possessing parallel single chains of silicate tetrahedra
inosilicate
40
Structure possessing isolated rings of silicate tetrahedra
cyclosilicate
41
Structure possessing parallel sheets of silicate tetrahedra
phyllosilicate
42
Structure possessing a three-dimensional framework of silicate tetrahedra
tectosilicate
43
Common rock forming mineral
dark mineral and most common is hornblende
crystals are generally long and thin
amphibole
44
other common, light-coloured rock-forming mineral.
generally dull to opaque with a porcelain-like appearance
feldspar
45
red pink and white feldspar
orthoclase
46
green, grey and white feldspar
plagioclase
47
distinguished by its characteristic of peeling into many thin flat smooth sheets or flakes.
the cleavage planes are in only one direction and no right angle face joins occur
Mica
48
white and pearly mica
muscovite
49
dark and shiny mica
biotite
50
peridote in the jewellery trade
• yellow-green, translucent and glassy looking.
• Crystals are not uncommon
• usually occurs as rounded grains in igneous rocks or as granular masses
olivine
51
generally dark green to black in color
 • forms short, stubby crystals
pyroxene
52
glassy looking, transparent or translucent mineral
 • varies in color from white and grey to smoky.
 • individual crystals are generally clear, while in larger masses quartz looks more milky white.
 • it can easily scratch a steel knife blade
quartz
53
common rock forming minerals
amphibole
feldspar
mica
olivine
pyroxene
quartz
54
mineral resources
aluminum
chrysotile
coal
copper
gold
potash
salt
zinc
55
relatively soft, silvery white metal with a dull luster
use are transportation, building and construction, containers and packaging, electrical, machinery and equipment
aluminum
56
a fibrous mineral with more than 2000 different uses.
• Qualities such as fire resistance, spinnability and tensile strength makes it an excellent material for brake linings in cars and aircraft to pipes for water and sewer systems.
chrysotile
57
second only to oil in meeting the world's energy needs and critical input in the manufacture of steel
coal
58
• In nature, is usually associated with other metals such as zinc, nickel, and gold. • may occur in massive sulphide deposits or as porphyries. • applications are in electrical transmissions, water tube, castings and heat exchangers.
copper
59
valued for its extreme ductility, high resistance to corrosion, lustrous beauty, and for its scarcity.
 • The most familiar use of gold is the manufacture of jewelry, coins and other ornamentation.
also used in electronics, dentistry and the aerospace industry. The remainder is purchased by investors.
gold
60
one of the three most important nutrients to plants, which are nitrogen, phosphorus and potassium.
About 4% of total production goes into the manufacture of soaps and detergents, glass and ceramic products, and de-icing.
potash
61
Sodium chloride (NaCl), as it is known to the industry, is used in the manufacture of chlorine, caustic soda and soda ash, three of the most important products in the heavy chemical industry.
salt
62
usually occurs in association with copper or lead or both.
The greatest use is as a coating for iron and steel products to make them resistant to rust and corrosion
zinc
63
A symmetrical intergrowth of two or more crystals of the same mineral
twinning
64
type of twins - single planar surface connecting twins
contact twins
65
type of twins - contact surface is irregular; two twins are interpenetrating
penetration twins
66
type of twinned crystal in which two crystals of the same mineral grow together with a 180° rotation about the crystallographic c-axis. This results in a mirror image relationship between the two halves of the twin.
carlsbad twin
67
type of twins - multiple twin planes are not parallel; radiating
cyclic twins
68
type of twins - multiple planes are parallel
polysynthetic twins
69
origin of twinning - accident of growth
growth twins
70
origin of twinning - caused by external stress inducing twinning as deformation
deformation twinning
71
origin of twinning - due to polymorphic change
transformation twinning