Fascinating World of Minerals

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Minerals
 
What is a mineral?
 
Naturally occurring
inorganic (no living thing or remains)
Solid
Definite 
shape
  ( arranged in an orderly
pattern)
definite chemical composition
Is it inorganic?
 
Coal?
No,  it is not a mineral- How is it made?
magnetite
Yes, a mineral
pearl
No, not a mineral- How is it made?
Does it occur naturally?
 
Quartz
yes, a mineral- one of the last minerals to
form from a magma chamber.
Silver
yes, a mineral
steel
no, not a mineral- How is it made?
Solid in crystalline form?
 
Petroleum
no, not a mineral- What is its natural form?
mercury
no, not a mineral- What is its natural form?
glass
not a mineral- What is its form?
amorphous
Definite chemical composition?
 
Calcium
yes, Ca  a mineral
Graphite
yes, C
Concrete
no, not a mineral- Why?
Rock forming minerals
 
Over 3000 minerals
only 20 are common, these are rock forming
minerals
two main groups- silicates and nonsilicates
Silicates
 
96% 
of the crust
contain silicon (Si) and Oxygen (O)
Feldspars 
are the most common silicate
minerals, contain Ca, K, and Na
Examples- Orthoclase and plagioclase
Ferromagnesium- contain Fe and Mg
Nonsilicates
 
4% of the crust
No 
silica
Six major groups
carbonates-ex. Calcite
halides- ex halite
native elements- Made of one element ex.
copper and silver
oxides- hematite and corundum
sulfates- gypsum
sulfides- galena, pyrite
 
Crystal Structure
 
Specific geometric arrangement of atoms or
ions
Crystal = natural solid with a definite shape
Can be seen under microscope or with the
aid of x rays
Identifying Minerals
 
Characteristics of Minerals
Each mineral has 
specific
 properties that
provide useful clues for identifying
minerals
.
Optical properties- 
properties will be
identified by looking at the mineral.
Tests
- tools are used to run tests on the
mineral.
Optical Properties
Color
 
Most easily observed
ex. Sulfur is bright yellow, azurite is deep
blue
least
 reliable characteristic
quartz consists of many colors
weathering may hide true color
Luster
 
Light reflected from the surface of a mineral
metallic luster- 
like polished metal like
silver
All others are non metallic
vitreous luster- reflects like 
glass
pearly luster
adamantine- brilliant luster ex. 
Diamond 
or gems
other lusters include: waxy, greasy, dull, earthy
Crystal Shape
 
Regularly shaped particles, or pattern.
Most crystal shapes are hard to identify.
six crystal systems
cubic
 ex. Halite, Pyrite
orthorhombic ex. Sulfur
tetragonal ex. Chalcopyrite
hexagonal ex. Plagioclase, Orthoclase
monoclinic ex. Micas
triclinic ex. Kyanite
Cleavage
 
The tendency to split along certain flat
surfaces and is related to types of bonds
ex. Mica (general name) splits easily in one
direction, it has one
 perfect 
cleavage ( splits
in parallel sheets)
Example- biotite and muscovite
Fracture
 
Some minerals do not break along cleavage
planes
instead they fracture or break 
unevenly
 into
curved or irregular pieces
splintery or fibrous fracture- looks like
pieces of broken wood
conchoidal- curved surfaces like the inside
of a shell
Simple Tests
Streak Test
 
The color of a mineral in powdered form
observed by rubbing the mineral against a
piece of unglazed ceramic tile called a
streak plate
the streak is not always the same color as
the mineral
mineral that  have a hardness 
higher
 than
the streak plate can not be tested
Hardness
 Test
 
The ability to resist scratching
hardness does not mean resistance to
cleavage or fracture
the hardness of an unknown mineral may be
determined by using Moh’s Hardness Scale
-this scale lists 10 minerals in order of
increasing hardness
-Softest is talc with a hardness of 1
The hardest is diamond with a hardness of
10
 
Moh’s Hardness Scale
 
Mineral
 
  hardness
 
  common test
talc
 
   
 
   
 
1
      
easily
 scratched
 
by fingernail
gypsum
 
     2  
 
  can be scratched by fingernail
calcite
 
     3       can not scratch  a copper penny
fluorite             4       can easily scratch a penny
Apatite
 
     5       can barely scratch glass
Feldspar           6        can scratch glass
quartz               7       very easily/deeply scratches steel and glass
topaz
 
      8       scratches quartz
corundum         9       no simple tests
diamond          10      scratches everything
Specific Gravity
 
The ratio of the weight of the mineral to the
weight of an equal volume of water.
Each mineral has its own specific gravity
Can be used to identify a mineral
 
Acid Test
 
Used to easily identify 
calcite
    A drop of HCl dropped onto Calcite will
cause it to effervesces.   The bubbles are
CO
2
 gas.
Dolomite also responds to the acid test but
not as violently and 
only in powdered
form.
Special Properties
 
Magnetism-  Can attach a magnet
Fluorescence- the ability to 
glow
 under
UV light ex. Calcite appears red under
UV
Phosphorescence- minerals that
continue to glow after a UV light is
removed
.ex sphalerite
Special Properties con’t
 
Double 
refraction-
crystals that bend light
in such a way that they
produce a double image
of any object viewed.
 
Radioactivity
- certain
atoms have unstable
electron or neutron
arrangements. These
minerals activate a
Geiger counter.
 
End of Minerals
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Discover what minerals are, their characteristics, and how they form naturally. Learn about the distinction between minerals like quartz and silver versus substances like coal or glass. Explore the diverse categories of rock-forming minerals, including silicates and nonsilicates, and delve into their crystal structures.

  • Minerals
  • Characteristics
  • Formation
  • Rock-forming
  • Silicates

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  1. Minerals

  2. What is a mineral? Naturally occurring inorganic (no living thing or remains) Solid Definite shape ( arranged in an orderly pattern) definite chemical composition

  3. Is it inorganic? Coal? No, it is not a mineral- How is it made? magnetite Yes, a mineral pearl No, not a mineral- How is it made?

  4. Does it occur naturally? Quartz yes, a mineral- one of the last minerals to form from a magma chamber. Silver yes, a mineral steel no, not a mineral- How is it made?

  5. Solid in crystalline form? Petroleum no, not a mineral- What is its natural form? mercury no, not a mineral- What is its natural form? glass not a mineral- What is its form? amorphous

  6. Definite chemical composition? Calcium yes, Ca a mineral Graphite yes, C Concrete no, not a mineral- Why?

  7. Rock forming minerals Over 3000 minerals only 20 are common, these are rock forming minerals two main groups- silicates and nonsilicates

  8. Silicates 96% of the crust contain silicon (Si) and Oxygen (O) Feldspars are the most common silicate minerals, contain Ca, K, and Na Examples- Orthoclase and plagioclase Ferromagnesium- contain Fe and Mg

  9. Nonsilicates 4% of the crust No silica Six major groups carbonates-ex. Calcite halides- ex halite native elements- Made of one element ex. copper and silver oxides- hematite and corundum sulfates- gypsum sulfides- galena, pyrite

  10. Crystal Structure Specific geometric arrangement of atoms or ions Crystal = natural solid with a definite shape Can be seen under microscope or with the aid of x rays

  11. Identifying Minerals Characteristics of Minerals Each mineral has specific properties that provide useful clues for identifying minerals. Optical properties- properties will be identified by looking at the mineral. Tests- tools are used to run tests on the mineral.

  12. Optical Properties Color Most easily observed ex. Sulfur is bright yellow, azurite is deep blue least reliable characteristic quartz consists of many colors weathering may hide true color

  13. Luster Light reflected from the surface of a mineral metallic luster- like polished metal like silver All others are non metallic vitreous luster- reflects like glass pearly luster adamantine- brilliant luster ex. Diamond or gems other lusters include: waxy, greasy, dull, earthy

  14. Crystal Shape Regularly shaped particles, or pattern. Most crystal shapes are hard to identify. six crystal systems cubic ex. Halite, Pyrite orthorhombic ex. Sulfur tetragonal ex. Chalcopyrite hexagonal ex. Plagioclase, Orthoclase monoclinic ex. Micas triclinic ex. Kyanite

  15. Cleavage The tendency to split along certain flat surfaces and is related to types of bonds ex. Mica (general name) splits easily in one direction, it has one perfect cleavage ( splits in parallel sheets) Example- biotite and muscovite

  16. Fracture Some minerals do not break along cleavage planes instead they fracture or break unevenly into curved or irregular pieces splintery or fibrous fracture- looks like pieces of broken wood conchoidal- curved surfaces like the inside of a shell

  17. Simple Tests Streak Test The color of a mineral in powdered form observed by rubbing the mineral against a piece of unglazed ceramic tile called a streak plate the streak is not always the same color as the mineral mineral that have a hardness higher than the streak plate can not be tested

  18. Hardness Test The ability to resist scratching hardness does not mean resistance to cleavage or fracture the hardness of an unknown mineral may be determined by using Moh s Hardness Scale -this scale lists 10 minerals in order of increasing hardness -Softest is talc with a hardness of 1 The hardest is diamond with a hardness of 10

  19. Mohs Hardness Scale hardness common test easily scratched by fingernail 2 can be scratched by fingernail 3 can not scratch a copper penny fluorite 4 can easily scratch a penny Apatite 5 can barely scratch glass Feldspar 6 can scratch glass quartz 7 very easily/deeply scratches steel and glass topaz 8 scratches quartz corundum 9 no simple tests diamond 10 scratches everything Mineral talc gypsum calcite 1

  20. Specific Gravity The ratio of the weight of the mineral to the weight of an equal volume of water. Each mineral has its own specific gravity Can be used to identify a mineral

  21. Acid Test Used to easily identify calcite A drop of HCl dropped onto Calcite will cause it to effervesces. The bubbles are CO2gas. Dolomite also responds to the acid test but not as violently and only in powdered form.

  22. Special Properties Magnetism- Can attach a magnet Fluorescence- the ability to glow under UV light ex. Calcite appears red under UV Phosphorescence- minerals that continue to glow after a UV light is removed.ex sphalerite

  23. Special Properties cont Double refraction- crystals that bend light in such a way that they produce a double image of any object viewed. Radioactivity- certain atoms have unstable electron or neutron arrangements. These minerals activate a Geiger counter.

  24. End of Minerals

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