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Hello Fleming College
We have a rock and mineral ID test coming up
We got ah 40 rocks and minerals on there
21 minerals and 19 rocks
So let's get down to business
Start off with our minerals
Quartz
Quartz has a hardness of 7 and is the hardest mineral in this set
The luster is glassy
Non-metallic
But be careful because quartz can be almost any colour
It has concoidal fracture
No cleavage but is sometimes in crystal form
It has sharp edges and is a common rock forming mineral
Calcite
Has a hardness of 3 and can be scratched with a knife
It's lustre is vitreous to earthy and non metallic
It has good cleavage and is rhombic
It can be many different colours
and effervesces with a dilute ten percent HCL
Plagioclase
Has a hardness of 6 and a non metallic lustre
It streaks white and has good cleavage at right angles
And twinning striations
It's usually light in colour white or grey
Orthoclase
A hardness of 6
It's lustre is non metallic vitreous
It streaks white it has good cleavage at 90 degrees
Colour is most often light to medium red but
can be white grey or green
Biotite and Muscovite
With a hardness of 2.5 to 3 it's very soft
It's lustre is non metallic
Perfect basal cleavage
Splits off easily into thin sheets that are
elastic or plastic
The colour is opaque to translucent
Biotite is always black
Muscovite is brown light green or beige
Hornblende
With a hardness of 5.5 it's as hard as a knife
It's lustre is vitreous non metallic
It has a bright black splintery appearance
It's cleavage not always easy to see
Angles fifty six degrees and one hundred twenty four degrees
The colour is black to dark green or brown
Pyroxene
Hardness of 5.5 same hardness as a knife blade
The lustre is vitreous to glassy and non metallic
The colour is light to medium grey or green
has visible cleavage plains at approximately ninety degrees
Talc
With a hardness of 1 it's very soft
and can be scratched with a fingernail
The cleavage is perfect basal
The streak is white the lustre is pearly to greasy
non metallic silky appearance slippery to the touch
Colour is pale green white yellow or translucent
Pyrite
Hardness of 6 to 6.5 it's harder than a knife blade
The lustre is metallic it has no cleavage
And is massive
The streak is greenish or brownish black
The colour is opaque pale brass yellow
Sometimes called fools gold
And is harder than chalcopyrite
Chalcopyrite
It's hardness is 3.5 to 4 softer than a knife blade
It has no cleavage and is massive
The lustre is metallic
The streak is greenish black
Softer than pyrite
The colour is brassy to greenish yellow
Graphite
The hardness of 1 to 2
It's lustre is metallic to dull
The cleavage is perfect basal
The streak is black and it marks paper
Has a greasy appearance and feel
The colour is black to steel grey
Hematite
A hardness of 5.5 to 6.5
The lustre is mostly non metallic
Found in compact red earthy masses but can
also be metallic dull silver
The streak is always red
Red powder will come off in your hands
The colours are red reddish brown black or metallic steel grey
Magnetite
With a hardness of 6 it can't be scratched with a knife
It's lustre is sub metallic dull metal appearance
There is no cleavage and it is massive
The streak is black
It is magnetic and will affect a compass
The colour is iron black
Gypsum
With a hardness of 2 it scratches easily with a fingernail
Lustre is non metallic
Clear crystalline form called celonite
Compact variety called alabaster most often in massive form
Colour usually white also grey reddish or brown
Serpentine
With a hardness of 2.5 to 4
Cleavage is not prominent concoidal fractures
lustre is non metallic greasy to waxy
Texture often has greasy or slippery feel
And the colour is most often green
Barite
A hardness or 2.5 to 3.5
The lustre is non metallic vitreous often transparent or translucent
The streak is white
The cleavage is perfect basal and prismatic or
Could be massive with fractures
Specific gravity 4.3 to 4.6
Occurs in tabular crystals in granular form
or in compact masses resembling marble
Colour it's colourless to white yellow brown red green or black
Chrysotile
Hardness of 2.5 to 4
The texture it has flexible fibres which are easily separated
The lustre is non metallic and silky
Colours can be green white yellow or brown
Galena
Hardness of 2.5
Lustre is metallic
The specific gravity of 7.6
The streak is medium grey and colours are
medium to dark grey
The cleavage is parallel to crystal cube faces
Pyrrhotite
With a hardness of 3.5 to 4.5
The streak is greyish black
It has no cleavage and a specific gravity of 4.6
It may be yellow to bronze in colour
and tarnishes to iridescent colours
and may be magnetic and the lustre is metallic
Sphalerite
With a hardness of 3.5 to 4
The lustre can be black variety metallic or
other common colours that are non metallic
It has cleavage with a specific gravity to 3.9 to 4
The streak is brown
Colours can be yellow brown red or black
if iron is present
All right that will do the minerals
now let's get into the rocks
We're gonna start off with granite
It's texture is panoritic medium to coarse grained
The structure is massive
The colour is white to grey mostly pink
The hardness is greater than 5.5
It's composition is made up of quartz
orthoclase plagioclase biotite and hornblende
Basalt
Texture is affinitic fine grained
Structure is massive vesicular amygdaloidal
flow pillows ropey blocky or columnar
The colour is dark grey to black
The hardness is greater than 5 to 6
It's composition consists of
plagioclase pyroxene olivine and some hornblende and biotite
Limestone
Texture is calcareous coarse grained
The structure is characteristically thick bedded to
massive may contain fossils
particularly in the cement
The colour is variable
The hardness is between 3 and 4
Composition it must consist of fifty percent
or more of calcite
Shale
Texture is fine grained
Structure is laminated splits into thin plates
may contain fossils
Colours are light to dark grey
iron oxides may give brown and red colours which are dull
The hardness is soft easily scratched and weathered
may disintegrate in humid climates
It's composition consists of
silt and clay size particles and clay minerals
Gneiss
Texture is uneven granular
medium to coarse grained crystalline
Structure
Gneissic banding parallel mineral orientation
alternating light and dark bands
Colour is light granular layers and
dark foliated bands
The hardness
Granular layers 6 to 7
foliated layers 2.5 to 3
It's composition consists of
orthioclase quartz biotite hornblende
and it is named for parent rock
Marble
Texture is even granular
fine to medium grained calcite crystals
Structure is massive
Colour is white but accessory minerals will colour the rock
The hardness is 3 is easily scratched
and easily eroded
It consists of calcite or dolomite
Rhyolite
Texture is aphanitic may be porphyritic
medium to coarse grained
Structure is massive
Colour is light grey yellow and red
The hardness is 6 to 6.5
The composition consists of
Quartz sanidine feldspar biotite and hornblende
Andesite
Texture is aphanitic may be
porphyritic fine grained
The structure is massive
Colour is brown green and dark grey
Hardness is 5 to 6
and it's composition consists of
plagioclase hornblende pyroxene and biotite
Diorite
Texture is phaneritic
coarse grained structure is massive
Colour is light to dark grey
Hardness is 5.5 to 6
The composition consists of
greater than ten percent of quartz
with orthioclase plagioclase hornblende and biotite
Gabbro
Texture is phaneritic coarse grained
The structure is massive
The colour is dark grey or greenish black
The hardness is greater than 5.5
and the composition consists of
plagioclase pyroxene hornblende and olivine
Porphyry
The texture is porphyritic
it has coarse crystals it's a light colour matrix
The background is fine grained and dark colour
ahh the colour varies
The hardness is greater than 5.5
usually picked from the individual mineral
the composition varies
Nepheline Syenite
Texture is phaneritic and coarse grained
Structure it has poor cleavage
is translucent with greasy to glassy lustre
The colours can be white yellow grey green
or even reddish or pink
The hardness is around 5.5 to 6
The composition consists of
sodalite apatite pyroxene sphene and feldspar
Limestone
Texture calcareous rock fine grained
Composed mainly of the mineral calcite
The structure stratification usually indistinct
sometimes fossils present on surface of rock
colour is variable
The hardness is ahh 3 to 4
dense variety's break with a concoidal fracture
It must consist of fifty percent or more
of calcite
Dolomite
Texture is coarse to fine grained
Structure is massive
Colour is white colourless buff brown pink or grey
Hardness is 3 to 4
effervesces very slowly in cold hydrochloric acid
Sandstone
Texture
even granular sand size
Structure is massive bedded cross bedding
and ripple marks
Colour varies depending on cement
white tan brown red or green
Hardness varies depending on cementing materials
quartz grains
The composition consists of quartz grains
if feldspar grains called arcos silica carbonates clay
or iron oxides as cementing agents
Talc Schist
Texture is medium to coarse grained
talc feel and flakeyness
Structure
Schistose foliation parallel alignment of
flaky minerals make more than fifty percent
Colour is silvery white grey yellow to brown
tones from iron oxides
Hardness and ease of splitting depends on
micaceous minerals present
usually soft 1 to 3
Composition consists of name for foliation
producing minerals which are present
micas muscovites
chlorite talc and hornblende
Slate
Texture is dense and fine grained
Structure is slatey foliation
thinner layers parallel alignment of mica
flakes no fossils
Colour is usually medium to dark grey
or black green purple red brown
and shiney lustre
The hardness is easily scratched with a knife
and is brittle
It's parent rocks are shale or mudstone
Quartzite
Texture is even granular
fine to medium grained sugary
Structure
massive thick bedded outlined of
original grains imperceptible
Colour is white when pure
light to dark grey or brownish to pink
from accessory minerals
Hardness is 7 tough but brittle
with splintery fractures
The parent rock is quartz rich sandstones
grains and cement
Muscovite Schist
The texture is medium to coarse grained
with a talc like feel and flakeyness
The structure is schistose foliation
parallel alignment of flaky minerals
make up fifty percent
The colour is silvery white grey yellow with brown
tones from iron oxides
Hardness and ease of splitting depend
on micaceous minerals present
which are soft
from 1 to 3
The composition named according to the
most conspicuous foliating producing
mineral in the rock