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Transcript
Definition of a Mineral
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Naturally occurring
Solid substance
Orderly crystalline structure
Definite chemical composition
Generally considered inorganic
There are roughly around 2500 known
minerals!
How Minerals Form
• Crystalization from
magma
• Precipitation
• Pressure and
temperature
• Hydrothermal
solutions
How Minerals Form
• Note the slower a
substance cools,
generally the larger
the crystals that will
form.
• This is how precious
gems are made deep
in the Earth!
Minerals are identified by their key
characteristics
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Hardness
Crystal shape
Luster
Color
Streak
Cleavage/Fracture
Density
Mineral Hardness
• Ability to scratch
another mineral
• Mohs scale from 1
(talc) to 10
(diamond)
• Quartz (most
common mineral
and most dust
particles) is 7
Mineral Hardness
Crystal Shape (Form)
• External structure due
to internal
arrangement of the
atoms
• Six basic groups of
shapes, with about
three dozen variations
Crystal Shape (Form)
Luster
• Describes how light
reflects off the
surface
• Main categories are
“metallic” and “nonmetallic”
• Non-metallic
includes “dull,”
glassy,” waxy,”
“pearly,” and others
Color
• Results from ability
to absorb some
wavelengths and
reflect others
• Some minerals have
characteristics
colors
• Others vary due to
chemical differences
or impurities (atoms
mixed inside the
main elements)
Non-metallic mineral
Metallic mineral
Streak
• Color of the powder
when rubbed on a
“streak plate”
(unglazed porcelain)
• May be same as
hand-specimen or
different
• Some paint is based
on powdered
minerals (streaks).
Mineral cleavage/fracture
• Some minerals split along flat surfaces when struck hard-this is called mineral cleavage
• Other minerals break unevenly along rough or curved
surfaces--this is called fracture
• A few minerals have both cleavage and fracture
Density (Specific Gravity)
• All minerals have
density (mass /
volume), but some are
very dense
• Examples include
galena, magnetite,
and gold
• Specific Gravity is the
density of the mineral
compared with density
of water