MINERALS - CLASSIFICATION AND IDENTIFYING
PROPERTIES
We will be looking at the properties of minerals and how we can
use them to identify which mineral we have.
Minerals are defined as naturally occurring inorganic crystalline
materials with distinct chemical and physical properties. So any
manmade materials even if they are otherwise identical aren't
minerals really, nor are any materials made by other living things.
Although we generally include the carbonate minerals since we only
recently discovered that in most cases they are actually made by
living things. In addition there are a number of "mineraloids" that
get lumped in - despite not fitting the exact definition above *G* .
Minerals have a crystal structure - that is the atoms they
are made of are arranged in a definite and repeating pattern. These
patterns form shapes, and these shapes can be grouped so that we can
see symmetries in them. Symmetries are repeating identical faces as
we turn the material or view it in a mirror. It turns out that all
the different shapes possible fall into 6 groups. Each group can be
identified by the number, lengths, and angles between the axis of the
crystal's faces the 6 groups are:
Hexagonal crystals: with 1 axis at 90* to the other 3 which are at
60* to each other
the 3 axis at 60* are of equal length but the 1 at 90* is of a
different length (either shorter or longer).
There is a subgroup of the hexagonals called the trigonals where the
symmetry breaks down some and may leave only 3 rotations that are
identical instead of the normal 6.
Isometric
crystals: -3 equal sized axis of rotation all set at 90 degrees
to each other (like a cube).
Tetragonal crystals: -3 axis at right angles to each other with 2
equal in length and the third different.
Orthorhombic crystals: - 3 axis of symmetry all at 90* - but all
of different lengths (like a shoe box).
Monoclinic crystals: - 3 axis of different lengths; 2 at 90* and
the third at some other angle.
Triclinc (3 angles) crystals: -3 axis of different lengths with
the angles between them different and not 90*
Well have I completely confused everyone now?
{t} fine so far.
{a} are there exceptions to this rule?
* {a} is trying to fit opals into these
a: actually no - all the different possible closed flat faced
shapes fall into one of the groups.
Opals aren't minerals - they are stacks of balls of silica and can
take any shape - more on opals and the other mineraloids at the end
<G>
{a} k
All minerals have a their own characteristic crystal shapes (yes
they can have more than one but they all will have the same type of
symmetry). The crystal shapes are one of the most important and
useful tools for identifying minerals. In many cases the the crystal
shape is enough to identify the mineral or mineral group all by its
self - like with garnets .
{W} What about sulfur? It comes in several shapes, Rhomboidal, and
prismatic!
W: - yes it comes in several shapes - but all the shapes have the
same crystal symmetry.
We also use other properties including color (not that useful in most
cases really), streak (the color of the powdered mineral) - also not
very useful in most cases, and hardness.
While there are a number of different scales that can be used, in
mineralogy we use a simple one called the Mohs scale (after the guy
that created it).
MOHS SCALE of RELATIVE HARDNESS
1 - talc
(ground up its called talcum powder)
2 - gypsum
(yes the stuff in dryboards)
3 - calcite
(better known as limestone and marble)
4) fluorite
5 - Apatite
(no its not a hungry mineral :P)
6 - feldspar
7 - quartz
8 - topaz
9 - corundum
(better known to most of us as ruby and sapphire).
10 - diamond
In addition to hardness we also use the density (or specific
gravity -essentially the same) while we do measure the actual density
for field purposes we can split them into ranges:
very light - density < 2.0
light - D 2 to 3
heavy - D 3 to 5
very heavy D 5 to 10
extremely heavy D > 10
Most minerals fall into the light or heavy range but a few
are identified by there density.
We can also use the way a mineral breaks to help ID
it
{W} Cleavage and fracture?
Yes - if it breaks with a series of smooth flat planes it is said
to cleave ( like the faces had been cut loose with a knife), if the
surface is rough or curved its is called fracture.
Glass and glass like materials generally have curving fractures
called chonchoidal. The angles between the cleavage planes is often
very useful in identifying the mineral as is the shape of the pieces
that brake off. In addition there are a number of other properties
that are very useful for selected minerals but not for most these
include:
acid dissolution - if it dissolves easily its calcite if you have
to gently heat it its dolomite.
magnetic - if it acts like its a magnet its magnetite; if a magnet
picks it up is either magnetite, hematite, pyrrhotite or a nickel
ore
radioactivity - if a Geiger counter clicks a lot its a uranium or
thorium mineral
dissolves in water - its probably salt - if it tastes salty it is
a salt if not its probably borax or gypsum.
And we can even use some optical properties
{W} Like double refractivity?
Yes
A few minerals like calcite have distinctive optical properties
like double refraction (:P) Others will fluoresce - rereadiate light
if an ultraviolet light is held over them in the dark. While the
different physical properties are used for lab and field
identification the minerals are defined on their chemical
compositions and their crystal habits.
Mineral Chemistry
All the known minerals (over 2500 types) are divided into 8 groups
with a ninth for the mineraloids (inorganic mineral like substances
that don't fit the exact definition for one reason or another), and a
tenth - organics - for those materials (clearly) created by living
things.
These groups are:
1)
Native
Elements and alloys (also carbides, nitrides, & phosphides)
Essentially pure elements or simple alloys of two metals or a
metal with carbon, nitrogen, or phosphorous.
2)
Sulfides
(and selenides, tellurides, arsenides, antimonidies, and bismuthides)
combinations with elemental sulfur, tellurium, arsenic, antimony,
selenium, or bisthmuth.
combinations of a alkaline earth or metal and a halogen gas.
Combinations with oxygen or with oxygen and water.
Combinations with nitrate (NO3), carbonate
(CO3), or borate (BO3)
6)
Sulfates
(and chromates, molybdates, and Wolframates)
combinations with sulfate (SO4) or with chromate
(CrO4), molybdate (MoO4), or vanadate
(VO4)
Combinations involving phosphate (PO4), arsenate
(AsO4), or vanadate (VO4)
8)
Silicates
(6 subtypes based on the arrangements of the silica molecules)
any combination involving the silica molecule (SiO2).
The silicates form 80% of all the minerals and so we need to look at
their subgroups a bit. Silica forms tetrahedra (four sided pyramids
(including the base as a side), the tetrahedra can be linked at their
points in several ways and these are the means of classifying the
silicate subgroups.
Cyclosilicates
- 3, 4 or 6 linked to form rings
Inosilicates
- chains there are actually 2 types
single chains where the tetrahedra flip back and
forth,
double chains where they form a chain of 6 sided rings
Phyllosilicates
- which form sheets (micas are the best examples)
Tectosilicates
- which form 3 dimensional networks
And now that I have completely confused you all into silence I'll
take questions <G>
{a} can you give samples of the others like you did with
phyllosilicates?
Nesosilicates - topaz
Sorosilicates - epidote
Cyclosilicates - beryl (emerald/Aquamarine)
Inosilicates - single chain - amphibole (hornblende); double chain
- pyroxene (augite)
Tectosilicates - Quartz
9)
Mineraloids
- including opal - inorganic materials that don't have a crystal
structure.
10)Organics:
including jet, coral, amber, and a few others - created by living
things and generally still containing the organic carbon.
We also frequently group minerals according their usefulness or
frequency in the rocks around us. When organized this way the 4 major
groups are:
Rock Forming Minerals
Accessory Rock Forming
Minerals
Economic Minerals
Gems and Decrative Minerals.
* DH checks the pulses of his students - ok not dead just asleep
<G>
* An chuckles
* P grins
* K thinks he understood most of it pretty okay, but can always
read back later :)
{P} DH, is sapphire a Beryl?
no sapphire is a corundum - aluminum oxide just like ruby
{P} OH RIGHT! DOH! :>
{An} Hmmm, what about emerald?
Emerald is beryl as is Aquamarine
Actually ruby is red gem corundum and sapphire is any other color gem
corundum
{P} I've only ever heard of it coming in blue or white... and yellow
I think...
you ladies prolly keep some corundum handy for working on your
talons - the low grade stuff is called emery. Well anytime you hear
them talking about an "oriental" <gem> its actually sapphire of
the appropriate color
* P nodnods
{P} OH! I know... I once heard someone refer to "yellow"
diamonds... is that correct or would they have meant a topaz?
Diamonds come in all colors so there are yellows.
{A} do metallic minerals all fall into the above classes (am thinking
of mercury)
Mercury is found as a native element - group one
* anna grins ... should have thought of that *grin*
Over the next few weeks we will go over minerals in groups looking at
the specific properties that allow us to identify them. So if you
check out the classroom webpage on my complex you can see the
upcoming lessons and download the previous ones *G*
{a} where on the page (have lynx and have looked but could not find)
* Sol nods.
it should be no problem for lynx users as its strictly downloadable
files or text of upcoming stuff.
http://www.ilhawaii.net/~dh/classroom.html
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