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• This term is used in several different ways.
• Health and fitness – extol the benefits of it
  together with vitamins.
• Mining Industry – for anything taken out
  of the ground (such as coal, iron core or
  sand and gravel).
• Geologist – any naturally occuring
  inorganic solid that possesses an orderly
  crystalline structure and a well defined
  chemical composition.
• Naturally occurring – It means that a
  mineral should be formed by natural
  geologic processes.
  – This is why synthetic diamonds and rubies,
    as well as variety of other usefuk materials
    produced by chemist are not considered
    as minerals
• Solid – In order for something to be
  considered as mineral, it should be
  solid at temperatures normally
  experienced at Earth’s surface.
  – Thus, Ice (Frozen water) is considered as
    mineral whereas liquid water is not.
• Orderly Crystalline Structure – Minerals
  are crystalline substances which
  means their atoms are arranged in an
  orderly, repetitive manner.
• This orderly packing of atoms is
  reflected in the regularly shaped
  objects we call crystals.
• Some Naturally occurring solids, such
  as volcanic glass (obsidian), lack a
  repetitive atomic structure and are
  referred to as amorphous (without
  form) and are CONSIDERED AS
  MINERALS.
• Well-defined Chemical Composition – Most
  minerals are chemical compounds made up
  of two/more elements. A few (such as Gold
  and Silver) consist of only a single element.
• The common mineral quartz consist of 2
  oxygen (O) atoms for every Silicon (Si) atoms,
  giving it a chemical composition expressed by
  the formula SiO2. Thus, no matter what the
  environment is, whenever atoms of Oxygen
  and Silicon joined together in the rato of 2 to
  1, the product is always quartz.
• Generally Inorganic
      Inorganic – Substances such as stone and
  metal that do not come from living things.
• Minerals are generally inorganic. Inorganic
  crystalline solids, as exemplified by ordinary
  table salt (Halite) that are found naturally are
  considered minerals.
• Organic Compounds on the other hand, are
  generally not.
• Ex. Sugar – (Crystalline like salt) comes from
  sugarcane or sugar beets and is common
  example of such an organic compound.
• Minerals and other earth materials are
  composed of chemical elements.
•    Elements – Fundamental
  component of matter that cannot be
  broken into a simpler particles by
  ordinary chemical processess. (Most
  common minerals consist of a small
  number – usually 2 to 5 of different
  chemical elements).
•   Oxygen
•   Silicon
•   Aluminum
•   Iron
•   Calcium
•   Sodium
•   Potassium
•   Magnesium
• In nature, most chemical elements
  have either a positive (+) or
  negative (-) charge.
  – ION- atom with either positive/negative
    charge
  – CATION – Positively charged atom
  – ANION – Negatively charged atom
• Most minerals are made up of 2-5
  essential elements. Ex. Formula of
  quartz is SiO2. One atom of Silicon for
  every 2 atoms of oxygen.
• The mineral has a crystalline structure,
  and therefore every mineral is a
  crystal.

  – Crystal – any solid element/compound
    whose atoms are arranged in a regular,
    periodically repeated manner
Ex. Mineral halite (common table salt)
• NaCl
  – One sodium for every one chlorine
                                  (You can see here
                                  that the sodium &
                                  chlorine ions
                                  alternate in orderly
                                  rows & columns
                                  intersecting at right
                                  angles. Figure 1.1 is
                                  the crystalline
                                  structure of halite).


                     Figure 1.1
• Crystalline Structure - orderly, repetitive
  arrangement of atoms in a crystal.
As evaporation
continues, more
and more
sodium
& chlorine ions
would
precipitate onto
the faces of
the growing
crystal.
• Crystal Face – flat surface that
  develops if a crystal grows freely in an
  uncrowded environment. Under
  perfect conditions, the crystal that
  forms will be symmetrical.
  – Symmetrical – has a corresponding similar
    parts: in other words, one side is the same
    as the other.
• This properties allow geologists to identify a
  mineral in the field.
  – Chemical composition
  – Crystal structure

• But if you pick a crystal of a mineral( for
  example, halite), you cannot see the atoms.
  You should measure its chemical composition
  and crystal structure by laboratory
  procedures, but such analyses are expensive
  & time consuming.
• Geologists commonly use properties to
  identify minerals.
• Crystal Habit – characteristic shape of
  an individual crystal & the manner in
  w/c aggregates of crystals grow.
                       Geologists can
                       identify that this
                       mineral is a
                       prismatic quartz
                       because of its
                       elongated
                       shape.
• Cleavage – tendency of some
  minerals to break along that surface,
  which are planes of weak bonds in the
  crystal. When a mineral has excellent
  cleavage, sheet after sheet can be
  peeled from the crystal, like peeling
  layers from an onion.
• Fracture – a manner n which minerals
  break other than along planes of
  cleavage.



The type of
fracture shown
in this picture is
concoid.
• Hardness – resistance of a mineral to
  scratching & is one of the most
  commonly used properties for
  identifying a mineral.
• Mohs Hardness Scale – after Friedrich
  Mohs, he developed this scale in the
  early 19th century.
This scale
was used to
measure the
hardness of
a mineral
more
accurately.
Mineral Hardness scale 1-10:

• Toronto Girls Can Flirt And Only Quit To Chase Dwarves .
• Terrible Giants Can Find Alligators Or Quaint Trolls Conveniently
           Digestible
• Tall Girls Can Flirt And Other Queer Things Can Do!
• The Girls Can Flirt And Other Queer Things Castrate Donkeys!
• Color – most obvious property of a
  mineral is often used in identification.
  But color can be unreliable because
  small amount of chemical impurities
  can dramatically alter color.
• Streak – refers to the color of the fine
  powder of a mineral. It is observed by
  rubbing the mineral across a piece of
  unglazed porcelain known as the
  “streak plate”.
• Streak   • Streak Plate
• Luster – manner in which a mineral
  reflects light. A mineral with a metallic
  look irrespective of color has a metallic
  luster. As a result, it looks like gold & is
  commonly called “fool’s gold”.
Pyrite
Mineral
•Metallic - Minerals with a metallic
luster are opaque and reflective,
like metal. The metallic elements,
most sulfides, and
some oxides belong in this
category.

•Opaque-
• chalcopyrite500
• Pearly - Describes a luster similar to the
  inside of a mollusk shell or shirt button.
• Earthy- This luster defines minerals with
  poor reflective qualities, much like
  unglazed porcelain. Most minerals with
  a dull luster have a rough
  or porous surface.

• Porous- Containing rounded, tiny holes
  throughout. Porous minerals are
  lightweight and easily dyed.
• Resinous - This is the luster of many yellow,
  dark orange, or brown minerals with
  moderately high refractive indices -
  honey like, but not necessarily the same
  color.


• Refractive indices- The amount
  of refraction that takes place in a
  particular substance, which is a direct
  connection to the speed of light in that
  substance.
• Reaction to acid

• Magnetism

• Radioactivity
• Fluorescence - FluorescenceProperty
  exhibited in certain minerals in which
  they display a glowing effect when
  having ample illumination
  with ultraviolet light.
• Phosphorescence- Phosphorescence
• The ability of some fluorescent minerals
  to keep on glowing for several
  seconds after the fluorescent lamp has
  been removed.

• these properties can be characteristics
  of specific minerals
• Geologists classify according to their
  chemical elements.
• Silicates, together w/ oxygen make up
  about 42% of earth’s crust. They are
  abundant for 2 reasons. First, silicon &
  oxygen are the two most plentiful
  elements in the crust. Secondly, silicon
  & oxygen combine readily.
• Carbonate minerals are much less
  common than silicates n earth’s crust,
  but they are important rock-forming
  minerals because they form
  sedimentary rocks that cover large
  regions of every continent. The shells &
  other hard parts of the most marine
  organisms such as clams, oysters &
  corals are made of carbonate
  materials.
• Commercially Important Minerals are
  minerals from which metals / other
  elements can be profitably recovered.

• Industrial minerals - rocks/ minerals that
  have economic value exclusive of
  metal ones, fuels & gems.
• Gem – mineral that is priced primarily
  for its rarity and beauty although some
  gems such as diamonds are also used
  industrially.
• Precious Gems- Any of several gems,
  including the diamond, emerald, ruby,
  and sapphire, that have high
  economic value because of their rarity
  or appearance.
Minerals
Minerals

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Minerals

  • 1.
  • 2. • This term is used in several different ways. • Health and fitness – extol the benefits of it together with vitamins. • Mining Industry – for anything taken out of the ground (such as coal, iron core or sand and gravel). • Geologist – any naturally occuring inorganic solid that possesses an orderly crystalline structure and a well defined chemical composition.
  • 3. • Naturally occurring – It means that a mineral should be formed by natural geologic processes. – This is why synthetic diamonds and rubies, as well as variety of other usefuk materials produced by chemist are not considered as minerals
  • 4. • Solid – In order for something to be considered as mineral, it should be solid at temperatures normally experienced at Earth’s surface. – Thus, Ice (Frozen water) is considered as mineral whereas liquid water is not.
  • 5. • Orderly Crystalline Structure – Minerals are crystalline substances which means their atoms are arranged in an orderly, repetitive manner.
  • 6.
  • 7. • This orderly packing of atoms is reflected in the regularly shaped objects we call crystals. • Some Naturally occurring solids, such as volcanic glass (obsidian), lack a repetitive atomic structure and are referred to as amorphous (without form) and are CONSIDERED AS MINERALS.
  • 8. • Well-defined Chemical Composition – Most minerals are chemical compounds made up of two/more elements. A few (such as Gold and Silver) consist of only a single element. • The common mineral quartz consist of 2 oxygen (O) atoms for every Silicon (Si) atoms, giving it a chemical composition expressed by the formula SiO2. Thus, no matter what the environment is, whenever atoms of Oxygen and Silicon joined together in the rato of 2 to 1, the product is always quartz.
  • 9. • Generally Inorganic Inorganic – Substances such as stone and metal that do not come from living things. • Minerals are generally inorganic. Inorganic crystalline solids, as exemplified by ordinary table salt (Halite) that are found naturally are considered minerals. • Organic Compounds on the other hand, are generally not. • Ex. Sugar – (Crystalline like salt) comes from sugarcane or sugar beets and is common example of such an organic compound.
  • 10. • Minerals and other earth materials are composed of chemical elements. • Elements – Fundamental component of matter that cannot be broken into a simpler particles by ordinary chemical processess. (Most common minerals consist of a small number – usually 2 to 5 of different chemical elements).
  • 11. Oxygen • Silicon • Aluminum • Iron • Calcium • Sodium • Potassium • Magnesium
  • 12. • In nature, most chemical elements have either a positive (+) or negative (-) charge. – ION- atom with either positive/negative charge – CATION – Positively charged atom – ANION – Negatively charged atom
  • 13. • Most minerals are made up of 2-5 essential elements. Ex. Formula of quartz is SiO2. One atom of Silicon for every 2 atoms of oxygen.
  • 14. • The mineral has a crystalline structure, and therefore every mineral is a crystal. – Crystal – any solid element/compound whose atoms are arranged in a regular, periodically repeated manner
  • 15. Ex. Mineral halite (common table salt)
  • 16. • NaCl – One sodium for every one chlorine (You can see here that the sodium & chlorine ions alternate in orderly rows & columns intersecting at right angles. Figure 1.1 is the crystalline structure of halite). Figure 1.1
  • 17. • Crystalline Structure - orderly, repetitive arrangement of atoms in a crystal.
  • 18. As evaporation continues, more and more sodium & chlorine ions would precipitate onto the faces of the growing crystal.
  • 19. • Crystal Face – flat surface that develops if a crystal grows freely in an uncrowded environment. Under perfect conditions, the crystal that forms will be symmetrical. – Symmetrical – has a corresponding similar parts: in other words, one side is the same as the other.
  • 20. • This properties allow geologists to identify a mineral in the field. – Chemical composition – Crystal structure • But if you pick a crystal of a mineral( for example, halite), you cannot see the atoms. You should measure its chemical composition and crystal structure by laboratory procedures, but such analyses are expensive & time consuming. • Geologists commonly use properties to identify minerals.
  • 21. • Crystal Habit – characteristic shape of an individual crystal & the manner in w/c aggregates of crystals grow. Geologists can identify that this mineral is a prismatic quartz because of its elongated shape.
  • 22. • Cleavage – tendency of some minerals to break along that surface, which are planes of weak bonds in the crystal. When a mineral has excellent cleavage, sheet after sheet can be peeled from the crystal, like peeling layers from an onion.
  • 23.
  • 24. • Fracture – a manner n which minerals break other than along planes of cleavage. The type of fracture shown in this picture is concoid.
  • 25. • Hardness – resistance of a mineral to scratching & is one of the most commonly used properties for identifying a mineral.
  • 26. • Mohs Hardness Scale – after Friedrich Mohs, he developed this scale in the early 19th century.
  • 27. This scale was used to measure the hardness of a mineral more accurately.
  • 28. Mineral Hardness scale 1-10: • Toronto Girls Can Flirt And Only Quit To Chase Dwarves . • Terrible Giants Can Find Alligators Or Quaint Trolls Conveniently Digestible • Tall Girls Can Flirt And Other Queer Things Can Do! • The Girls Can Flirt And Other Queer Things Castrate Donkeys!
  • 29. • Color – most obvious property of a mineral is often used in identification. But color can be unreliable because small amount of chemical impurities can dramatically alter color.
  • 30. • Streak – refers to the color of the fine powder of a mineral. It is observed by rubbing the mineral across a piece of unglazed porcelain known as the “streak plate”.
  • 31. • Streak • Streak Plate
  • 32. • Luster – manner in which a mineral reflects light. A mineral with a metallic look irrespective of color has a metallic luster. As a result, it looks like gold & is commonly called “fool’s gold”.
  • 34. •Metallic - Minerals with a metallic luster are opaque and reflective, like metal. The metallic elements, most sulfides, and some oxides belong in this category. •Opaque-
  • 36. • Pearly - Describes a luster similar to the inside of a mollusk shell or shirt button.
  • 37. • Earthy- This luster defines minerals with poor reflective qualities, much like unglazed porcelain. Most minerals with a dull luster have a rough or porous surface. • Porous- Containing rounded, tiny holes throughout. Porous minerals are lightweight and easily dyed.
  • 38.
  • 39. • Resinous - This is the luster of many yellow, dark orange, or brown minerals with moderately high refractive indices - honey like, but not necessarily the same color. • Refractive indices- The amount of refraction that takes place in a particular substance, which is a direct connection to the speed of light in that substance.
  • 40.
  • 41. • Reaction to acid • Magnetism • Radioactivity
  • 42. • Fluorescence - FluorescenceProperty exhibited in certain minerals in which they display a glowing effect when having ample illumination with ultraviolet light.
  • 43. • Phosphorescence- Phosphorescence • The ability of some fluorescent minerals to keep on glowing for several seconds after the fluorescent lamp has been removed. • these properties can be characteristics of specific minerals
  • 44. • Geologists classify according to their chemical elements. • Silicates, together w/ oxygen make up about 42% of earth’s crust. They are abundant for 2 reasons. First, silicon & oxygen are the two most plentiful elements in the crust. Secondly, silicon & oxygen combine readily.
  • 45. • Carbonate minerals are much less common than silicates n earth’s crust, but they are important rock-forming minerals because they form sedimentary rocks that cover large regions of every continent. The shells & other hard parts of the most marine organisms such as clams, oysters & corals are made of carbonate materials.
  • 46. • Commercially Important Minerals are minerals from which metals / other elements can be profitably recovered. • Industrial minerals - rocks/ minerals that have economic value exclusive of metal ones, fuels & gems.
  • 47. • Gem – mineral that is priced primarily for its rarity and beauty although some gems such as diamonds are also used industrially. • Precious Gems- Any of several gems, including the diamond, emerald, ruby, and sapphire, that have high economic value because of their rarity or appearance.