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MINERALS:
BUILDING BLOCKS OF ROCKS
Elements naturally combine
with other elements to
produce MINERALS
n 
n 
Over 100 known
elements
3700 known
minerals
(dozens discovered
every year)
Minerals combine to form
crystals
Sometimes we
can see the
crystal
formation,
sometimes we
need a
microscope.
Geologists ( geo means
Earth) study rocks and
minerals.
Properties geologists use to
classify rocks
Colour
Streak
Lustre
Hardness
Crystal Structure
Cleavage
Magnetism
Reaction to Chemicals
COLOUR
~ Minerals occur in many
different colours
STREAK
n 
n 
The powdery
mark minerals
make when
scratched on a
hard surface
More reliable
than colour
LUSTRE
n 
Degree of
shininess
n 
n 
n 
Metallic
Glossy
Dull
Hardness
(strength of the bond)
n 
Mohs
hardness
scale
n 
n 
Scratch one
mineral
against
another to
see how
hard it is
Scale 1
(softest) –
10 (hardest)
n 
Crystal Structure
Crystal size
explains the
speed a
mineral
cooled
n 
n 
Large
crystal =
slowly
cooled
Small
crystal =
rapidly
cooled
CLEAVAGE
n 
How minerals break
or fracture
n 
n 
Rough, uneven,
parallel, thin flat
sheets, cubes, 90˚,
etc.
Maximum of 6
directions
MAGNETISM
n 
n 
Ability to
attract to
a magnet
Will only
attract if
IRON is
present
REACTION TO CHEMICALS
n 
Minerals with carbonate materials react
with acidic solutions (vinegar)
n 
Fizzing and bubbling (carbon dioxide gas)
EARTH S CRUST
Rocks
Lustre
Streak
Reaction
Crystals
Geology
Magnetism
Minerals
Cleavage
Colour
Hardness