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Geology
F1 Minerals
Physical Properties of Minerals
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Created by
Meredith Thomas
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Cards (18)
Colour
Determined by the
chemical composition
of the mineral
Not a good diagnostic property.
Lustre
The way in which a mineral reflects light
Controlled by the
atomic structure
Vitreous Lustre
Glass-like
Transparent
,
Translucent
or
Opague
Metallic Lustre
Reflect light by
metal
Pearly Lustre
Mother of pear
like -> rainbow colours shown when catching the light
Silky
Lustre
Silk-like; occurs in minerals with a
fiborous
structure
Dull
Lustre
Doesn’t
reflect
light
Adamantite
Lustre
Lustre of a diamond
Streak
Colour of a minerals powder
Obtained by rubbing on white
porcelain
tile
Useful for identifying
metallic ore minerals
Any minerals harder than
6
will scratch the tile
Hardness
Measure of Mohs Scale - from 1 -> 10
Steel Nail = 5.5
Copper Coin = 3.5
Fingernail = 2.5
Cleavage
The way a mineral breaks
Controlled by lines of weakness
Can have
1
,
2
,
3
or
4
planes of cleavage
Can be perfect,good or poor
Fracture
Way a mineral breaks when struck by a hammer
Bonds between atoms are strong so no
cleavage
Not controlled by weakness in the atomic structure
Conchoidal Fracture
The same as that shown by window glass
Diagnostic Feature = Quartz
Acid Reaction
Use dilute
HCL
to test for carbonates -
Calcite
givers of CO2
Taste
Halite
tastes salty -> Diagnostic Property
Form/Habit
Common appearance of the mineral
Only noted if it helps identify
Acicular
= Needle-like crystals
Tabular
= Thin cuboid-like crystals
Bladed
= Like tabular but comes to a point
Diagnostic Properties
Properties that allow any minerals to be identified
Most minerals have at least 1
Hardness
,
Cleavage
&
Streak
are most useful
Colour
and
Lustre
are least useful
Specific Gravity
or
Relative Density
Ratio
of density of a mineral compared to the density of an equal volume of water