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crystal habit/ shape
angle of intersection of equivalent crystal faces are identical on all samples of a particular material
Nicholas Steno
“first law of crystallogrophy“
can be unhelpful when minerals grow in masses
amorphous metals
rigid substance BUT no ordered arrangement of atoms (NOT mineral)
glass or obsidian
luster
quality and intensity of light reflected from a mineral
can be subjective
metallic OR non-metallic
non metallic luster categories
glassy/ vitreous
dull or earthy
greasy
brilliant
colour of minerals
results from the way they absorb/ transmit light
can be very variable
most unreliable characteristic
ferromagnesium silicates are always…
DARK (black, brown, green)
minerals with metallic luster have a more ….
consistent colour
streak test
colour of thin powder layer on a streak plate
not used with silicates (most leave white)
useful with oxides and sulfides
mohs hardness scale
scale of ten minerals used to compare hardness between the rest
diamond = 10 (hardest)
talc = 1 (softest)
cleavage
breakage or splitting of mineral crystals along a smooth plane
# of planes determined by crystal structure
can distinguish between minerals that otherwise look the same
can further categorize by QUALITY of cleavage
basal cleavage
1 plane
prismatic cleavage
2 planes at a right angle
non-prismatic cleavage
2 planes NOT at right angle
cubic cleavage
3 planes at right angles
rombohedral cleavage
3 planes NOT at right angles
octohedral cleavage
4 planes of breakage
fracture
irregular breakage of mineral
3 kinds of fracture
irregular
splintery
conchoidal (curved, as in broken glass)
a material that fractures could be
a mineral with poorly defined cleavage (ex. olivine)
a material with irregular distribution of atoms (ex. glass, obsidian)
density/ specific gravity
mass per unit volume
ratio of weight of a mineral divided by weight of an equal vol of water @ 4 degrees C
optical properties
opacity
translucent/ not
if double refraction occurs, the mineral is always…
calcite!!