Mineralogy
Definition of mineral, mineralogy, Importance of study of minerals: rock forming and ore forming minerals. Different methods of study of minerals. Study of minerals by physical identification method and their physical properties.Forms and Habits, Colour, Streak, Lustre, Fracture, Cleavage, Hardness, Specific Gravity, Degree of Transparency, Special Properties Determination of Physical properties of following minerals: Feldspar, Quartz, Flint, Jasper, Olivine, Augite, Hornblende, Muscovite, Biotite, Asbestos, Chlorite, Kyanite, Garnet, Talc, Calcite. Study of ore forming minerals such as Pyrite, Hematite, Magnetite, Amethyst, Galena, Pyrolusite, Graphite, Magnetite, and Bauxite, Coral reefs.
Importance of Mineral, Chemical Composition of Earth Crust, Structure of Silicates
Mineralogy
Definition of mineral, mineralogy, Importance of study of minerals: rock forming and ore forming minerals. Different methods of study of minerals. Study of minerals by physical identification method and their physical properties.Forms and Habits, Colour, Streak, Lustre, Fracture, Cleavage, Hardness, Specific Gravity, Degree of Transparency, Special Properties Determination of Physical properties of following minerals: Feldspar, Quartz, Flint, Jasper, Olivine, Augite, Hornblende, Muscovite, Biotite, Asbestos, Chlorite, Kyanite, Garnet, Talc, Calcite. Study of ore forming minerals such as Pyrite, Hematite, Magnetite, Amethyst, Galena, Pyrolusite, Graphite, Magnetite, and Bauxite, Coral reefs.
Importance of Mineral, Chemical Composition of Earth Crust, Structure of Silicates
Mineral is a naturally occurring substance, representable by a chemical formula, that is usually solid and inorganic, and has a crystal structure. It is different from a rock, which can be an aggregate of minerals or non-minerals and does not have a specific chemical composition.
The presentation contains basic terms of Physical Geology which is related to Geology. It is a gross presentation including images and animated gif's for better understanding.
What is mining?; Why do we need mines?; What is a mineral ?; What is an Ore Deposit? ; Concentrations of Metals; Metals enrichment factors ; Types of Ore Deposit ; GEOLOGIC CONDITIONS AND CHARACTERISTIC OF ORE DEPOSITS; Shape of ore deposits; Dip ore deposits ;Thickness ore deposits; Depth of ore deposits; Structure of ore deposits; Ore value and profitability of mining; Stability of ore rocks; Chemical and mineral characteristics of ores ; Lessening of ore deposit; Degree of breakability; Life Cycle of a Metal Resource; Mineral Supply and Demand; Conservation; Economic Impact on Mineral Supplies
Mineral is a naturally occurring substance, representable by a chemical formula, that is usually solid and inorganic, and has a crystal structure. It is different from a rock, which can be an aggregate of minerals or non-minerals and does not have a specific chemical composition.
The presentation contains basic terms of Physical Geology which is related to Geology. It is a gross presentation including images and animated gif's for better understanding.
What is mining?; Why do we need mines?; What is a mineral ?; What is an Ore Deposit? ; Concentrations of Metals; Metals enrichment factors ; Types of Ore Deposit ; GEOLOGIC CONDITIONS AND CHARACTERISTIC OF ORE DEPOSITS; Shape of ore deposits; Dip ore deposits ;Thickness ore deposits; Depth of ore deposits; Structure of ore deposits; Ore value and profitability of mining; Stability of ore rocks; Chemical and mineral characteristics of ores ; Lessening of ore deposit; Degree of breakability; Life Cycle of a Metal Resource; Mineral Supply and Demand; Conservation; Economic Impact on Mineral Supplies
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1. Identification of Minerals
• What if you have two minerals that look exactly alike?
• How will you be able to tell one from the other?
• STUDY THEIR CHARACTERISTICS
• Which is GOLD?
2. Identification of Minerals
• There are a number of different properties
or characteristics that can give you clues to
recognize different materials.
1. Color
3. Streak
5. Cleavage
2. Luster
4. Hardnes
6. Fracture
• And Other Tests
3.
4. Color
• Although color is an obvious feature of a mineral, it is often
unreliable for identification.
• Slight impurities can contaminate the mineral changing its
color.
• Example: Quartz can be white, pink, or even purple.
7. Streak
• If you were to scratch a mineral against a hard
surface, like a porcelain tile it would leave
behind a streak of colored powder.
• Streak is the color of a mineral in powder form.
• Scientist use a streak plate to do the streak test.
8. Streak
• While a mineral’s color may change, the color
of its streak usually does not. Streak is often a
much more helpful way to use color to
identify a mineral.
• Where do you use streak
in your everyday life?
• Writing with a pencil on
paper.
• Which mineral do you
use to leave the streak?
• Graphite
9.
10. Hardness
• The measure of how easily a mineral can be scratched is
known as its hardness.
• Hardness of a mineral has nothing to do with whether it
breaks easily or not.
• Hardness is measured by using THE MOH’S HARDNESS
SCALE, which is a scale that ranks ten common minerals
hardness.
11. Hardness
• The Moh’s Hardness Scale is ranked from 1 – 10.
• Talc is the softest mineral (1).
• Diamond is the hardest mineral (10).
15. Luster
• Luster is the way a mineral reflects
light.
• It is often described as either metallic or
nonmetallic.
16. Metallic Luster
• Opaque and shiny in appearance, the look of
polished or dull metal.
Metallic Examples: Gold,
Copper, Pyrite,
Sphalerite, Cinnabar
Submetallic Luster are
ones that resemble a
metal, but weathering
and corrosion made
them look dull or less
reflective.
17. Non-Metallic Luster
• Does not look like metals.
• Types of non-metallic luster:
• Adamantine: Remarkable shine and
brilliance
• Transparent / Translucent
• Diamonds, Cubic Zirconia
• Earthy, Dull: Poor Reflectivity
• Coarse and Porous
• Kaolinite, montmorillonite
• Vitreous: Luster similar to that of glass
• Transparent / Translucent
• Quartz, Calcite
• Greasy: Look as if it is coated with
oil/grease
• Resemble fat, feel greasy/waxy
• Opal, Halite
18.
19. Cleavage
• The way a mineral breaks apart is another way
that is helpful in identifying it.
• Sometimes when you break a
mineral, it will break along flat
smooth surfaces.
• This results in a nice clean cut.
20. Cleavage
• This is called
cleavage.
• Think of the way a
sharp meat cleaver
cuts meat. Nice,
clean cuts.
21. Fracture
• Sometimes, minerals do not break in nice clean, flat
cuts.
• Minerals that DO NOT break along flat, smooth
surfaces are said to fracture.
• The way a mineral break depends on the strength
and arrangements of atomic bonds within the
mineral.
22. Cleavage and Fracture
• Minerals with Cleavage
• Mica
• Calcite
• Halite
• Fluorite
• Minerals that Fracture
• Quartz
• Olivine
• All minerals fracture to some extent…even those with
cleavage do not break perfectly all the time.
23.
24. Specific Gravity
• Minerals can be identified by comparing the weights
of equal samples.
• The specific gravity of a mineral is the ratio of its
weight compared to the weight of an equal volume
of water.
• SG = WEIGHT OF MINERAL
Weight in equal volume of water.
25. Specific Gravity
• Gold has a specific gravity of 19
• Pyrite has a specific gravity of 5
That means the gold is
19 times heavier than
water and pyrite is 5
times heavier.
If gold and pyrite look
the same, you can tell
them apart by finding
their specific gravity.
If you were to lift two different
minerals, the one with the
higher specific gravity would
feel heavier.
30. Double Refraction
• Light enters the mineral as one beam of
light, but then it separates into 2 beams
• You then will see 2 objects
• Example: Calcite
31. Fluorescence
• Some minerals glow brightly under a black
light.
• Minerals glow because they have impurities
in them called activators