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THE MINERALS / THEIR
UTILIZATION MANAGEMENT
Prepared by MJ Salvaña
MINERALS
 Mineral - a naturally occurring
substance composed of
specific chemical elements or
compounds, with characteristic
crystal structure, and certain
fixed or slightly variable
physical properties
Minerals are considered as
archetypal and are the core of
non-renewable resources.
-are extracted from the earths
crust.
The deposits are formed on geological
time scales of a totally different order
from that of the human scales of
their use
Classification of Minerals
 a) metallic minerals;
 b) non-metallic or industrial minerals; and
 c) fuel minerals
Four types of Mineral
Resources
 Metals ( e.g. Iron, Copper, Aluminum)
 Industrial Minerals (e.g. Lime, Potash)
 Construction Materials
(e.g. sand, stone, gravel)
 Energy Minerals
(e.g. Uranium)
Mineral ClassificationMineral Classification
 There are 7 MajorMineral Groups:There are 7 MajorMineral Groups:
 SilicatesSilicates
 Native ElementsNative Elements
 HalidesHalides
 CarbonatesCarbonates
 OxidesOxides
 SulfatesSulfates
 SulfidesSulfides
 Minerals are classified by theirchemical composition and internal crystal structure.
Mineral ClassificationMineral Classification
 Silicates are composed of silicon-Silicates are composed of silicon-
oxygen tetrahedrons, anoxygen tetrahedrons, an
arrangement which contains fourarrangement which contains four
oxygen atoms surrounding aoxygen atoms surrounding a
silicon atom (SiOsilicon atom (SiO44
-4-4
).).
1. Silicates1. Silicates
QuartzQuartz
Copyright©Stonetrust, Inc.
Silicates comprise the majority ofSilicates comprise the majority of
minerals in the Earth’s crust and upperminerals in the Earth’s crust and upper
mantle. Over 25% of all minerals aremantle. Over 25% of all minerals are
included in this group, with over 40% ofincluded in this group, with over 40% of
those accounting for the most commonthose accounting for the most common
and abundant minerals.and abundant minerals.
Feldspar, Quartz, Biotite, andFeldspar, Quartz, Biotite, and
Amphibole are the most commonAmphibole are the most common
silicatessilicates
2.Native Elements2.Native Elements
 Native elements are minerals that are composed of a singleNative elements are minerals that are composed of a single
element.element.
 Some examples are: Gold (Au), Silver (Ag), Copper (Cu), Iron (Fe),Some examples are: Gold (Au), Silver (Ag), Copper (Cu), Iron (Fe),
Diamonds (C), Graphite (C), and Platinum (Pt)Diamonds (C), Graphite (C), and Platinum (Pt)
Image Courtesy of the USGS
GoldGold SilverSilver
Image Courtesy of the USGS
3. Halides3. Halides
 Halides consist of halogen elements, chlorine (Cl), bromine (Br),Halides consist of halogen elements, chlorine (Cl), bromine (Br),
fluorine (F), and iodine (I) forming strong ionic bonds with alkali andfluorine (F), and iodine (I) forming strong ionic bonds with alkali and
alkali earth elements sodium (Na), calcium (Ca) and potassium (K)alkali earth elements sodium (Na), calcium (Ca) and potassium (K)
 Some examples include Halite (NaCl) and Flourite (CaFSome examples include Halite (NaCl) and Flourite (CaF22).).
HaliteHalite
Copyright©Stonetrust, Inc.
FluoriteFluorite
Image courtesy of USGS
4.Carbonates4.Carbonates
 Carbonates are anionic groups of carbon and oxygen. Carbonate minerals result fromCarbonates are anionic groups of carbon and oxygen. Carbonate minerals result from
bonds between these complexes and alkali earth and some transitional metalsbonds between these complexes and alkali earth and some transitional metals
 Common carbonate minerals include calcite CaCOCommon carbonate minerals include calcite CaCO33 , calcium carbonate, and dolomite, calcium carbonate, and dolomite
CaMg(COCaMg(CO33))22 , calcium/magnesium carbonate, calcium/magnesium carbonate
 Carbonate minerals react when exposed to hydrochloric acid. Geologist will oftenCarbonate minerals react when exposed to hydrochloric acid. Geologist will often
carry dilute hydrochloric acid in the field to test if a mineral contains calciumcarry dilute hydrochloric acid in the field to test if a mineral contains calcium
carbonate. If the mineral fizzes when it comes in contact with the hydrochloric acid itcarbonate. If the mineral fizzes when it comes in contact with the hydrochloric acid it
contains calcium carbonate. Some cola soft drinks can also be used for this testcontains calcium carbonate. Some cola soft drinks can also be used for this test
because it contains enough hydrochloric acid to react with calcium carbonate.because it contains enough hydrochloric acid to react with calcium carbonate.
DolomiteDolomite
CalciteCalcite
Copyright©Stonetrust, Inc.
5.Oxides5.Oxides
 Oxides are minerals that include one or more metal cations bondedOxides are minerals that include one or more metal cations bonded
to oxygen or hydroxyl anions.to oxygen or hydroxyl anions.
 Examples of oxide minerals include: Hematite (FeExamples of oxide minerals include: Hematite (Fe22OO33), Magnetite), Magnetite
(Fe(Fe33OO44), Corundum (Al), Corundum (Al22OO33), and Ice (H), and Ice (H22O)O)
HematiteHematite
SulfatesSulfates
 Sulfates are minerals that include SOSulfates are minerals that include SO44 anionic groupsanionic groups
combined with alkali earth and metal cations.combined with alkali earth and metal cations.
 Anhydrous (no water) and hydrous (water) are the twoAnhydrous (no water) and hydrous (water) are the two
major groups of Sulfates.major groups of Sulfates.
 Barite (BaSOBarite (BaSO44) is an example of a anhydrous sulfate and) is an example of a anhydrous sulfate and
Gypsum (CaSOGypsum (CaSO4·4· 2H2H22O) is an example of a sulfate.O) is an example of a sulfate.
GypsumGypsum
Image Courtesy of the USGS
BariteBarite
Image Courtesy of the USGS
6. SulfidesSulfides
 Sulfides are minerals composed of one or more metal cationsSulfides are minerals composed of one or more metal cations
combined with sulfur. Many sulfides are economically importantcombined with sulfur. Many sulfides are economically important
ores.ores.
 Pyrite (FeSPyrite (FeS22) or “fool’s gold”, Galena (PbS), Cinnabar (HgS) an) or “fool’s gold”, Galena (PbS), Cinnabar (HgS) an
Molybdenite (MoSMolybdenite (MoS22) are a few commonly occurring sulfide minerals) are a few commonly occurring sulfide minerals
Pyrite “Fool’s Gold”Pyrite “Fool’s Gold”
Copyright©Dr. Richard Busch
CinnabarCinnabar
Minerals have distinctive physical properties thatMinerals have distinctive physical properties that
geologists use to identify and describe themgeologists use to identify and describe them..
 .. Crystal FormCrystal Form
 2. Hardness2. Hardness
 3. Luster3. Luster
 4. Color4. Color
 5. Streak5. Streak
 6. Cleavage6. Cleavage
 7. Specific Gravity7. Specific Gravity
A variety of different minerals.A variety of different minerals.
Copyright©Dr. Richard BuschCopyright©Dr. Richard Busch
.. Crystal FormCrystal Form
 Crystal form is the external expression of the internally orderedCrystal form is the external expression of the internally ordered
arrangement of atoms.arrangement of atoms.
 During mineral formation, individual crystals develop well-formedDuring mineral formation, individual crystals develop well-formed
crystal faces that are specific to that mineral.crystal faces that are specific to that mineral.
six major crystal forms:
1.1. Isometric (Cubic)Isometric (Cubic)
2.2. TetragonalTetragonal
3.3. OrthorhombicOrthorhombic
4.4. HexagonalHexagonal
5.5. MonoclinicMonoclinic
6.6. TriclinicTriclinic
Crystal Form, cont.Crystal Form, cont.
 Isometric:
Isometric crystals are blockshaped with relatively
similar and symmetrical faces. The crystal form has
three axes all at 90° angles and all the same length.
Mineral Example: Pyrite
Tetragonal:
Tetragonal crystals are shaped like four-sided
pyramids or prisms. The crystal formhas three axes
that are all perpendicularto one another. Two axis
have the same length, and one is different. The axes
that are the same length lie on a horizontal plane,
with the third axis at a right angle to the othertwo.
Mineral Example: Zircon
Orthorhombic:
Orthorhombic crystals are shaped like a rectangular
prismwith a rectangularbase. The crystal has three
axes of different lengths and intersect at 90° angles.
Mineral Example: Topaz
Copyright© Dr. Richard Busch
Isometric: PyriteIsometric: Pyrite
Tetragonal: ZirconTetragonal: Zircon
Copyright© Dr. Richard Busch
Axes Length Relationships: A = B= C
Angles: α = β = γ = 90°
AA
CC
BB
AA BB
CC
Axes Length Relationships: A= B≠ C
Angles: α = β = γ = 90°
CC
BBAA
Axes Length Relationships: A ≠ B≠ C
Angles: α = β = γ = 90°
Orthorhombic: TopazOrthorhombic: Topaz
Photo Courtesy USGSPhoto Courtesy USGS
15
Table of Contents
Standard 3-3.1
Standard 3-3.2
CC
BBAA
αβ
γ
Crystal Form, cont.Crystal Form, cont.
Hexagonal:
Hexagonal crystals have three symmetrical axes that occurin
the same plane and are all the same length. The fourth axis
may be either longeror shorter, and it intersects the other
three axis at 90° angles. The sides intersect at 120 ° angles.
Mineral Example: Amethyst
Monoclinic:
Monoclinic crystals are short and stubby with tilted faces.
Each crystal has three axes that are unequal. Two of the axes
lie in the same plane at right angles to each other, the third
axis is inclined. Mineral Example: Gypsum
Triclinic:
Triclinic crystals have three axis which are all different lengths
and all three axis intersect at angles other than 90°.
Mineral Example: Kyanite
Monoclinic: GypsumMonoclinic: Gypsum
Copyright © Stonetrust ,Inc.
AA
BB
DD
CC
AA
BB
CC
AA
BB
CC
Axes length Relationships: A = B= C ≠ D
Angles: α = β = 90° and γ = 120°
Axes Length Relationships: A ≠ B≠ C
Angles: α ≠ β ≠ γ
Axes Length Relationships: A ≠ B≠ C
Angles: α ≠ γ = β = 90°
Hexagonal: AmethystHexagonal: Amethyst
Copyright © Stonetrust ,Inc.
Triclinic: KyaniteTriclinic: Kyanite
Copyright © Stonetrust ,Inc.
16
Table of Contents
Standard 3-3.1
Standard 3-3.2
CC
BBAA
αβ
γ
HardnessHardness
 Hardness is the ability of a mineral to resist abrasion or scratchingHardness is the ability of a mineral to resist abrasion or scratching
on its surface.on its surface.
 One way geologists measure hardness is using a relative scaleOne way geologists measure hardness is using a relative scale
referred to as Moh’s scale of mineral hardness which ranks 10referred to as Moh’s scale of mineral hardness which ranks 10
common minerals along a scale from 1-10 (1 refers to the softestcommon minerals along a scale from 1-10 (1 refers to the softest
minerals while 10 refers to the hardest mineral).minerals while 10 refers to the hardest mineral).
TalcTalc
Copyright©Dr. Richard Busch
Talc is a soft mineral that you can scratchTalc is a soft mineral that you can scratch
with your fingernail, and has a hardness ofwith your fingernail, and has a hardness of
“1” measured by Moh’s relative scale of“1” measured by Moh’s relative scale of
mineral hardness.mineral hardness.
Moh’s Scale of Mineral HardnessMoh’s Scale of Mineral Hardness
 1-Talc1-Talc
 2-Gypsum2-Gypsum
 3-Calcite3-Calcite
 4-Fluorite4-Fluorite
 5-Apatite5-Apatite
 6-Orthoclase6-Orthoclase
 7-Quartz7-Quartz
 8-Topaz8-Topaz
 9-Corundum9-Corundum
 10-Diamond10-Diamond
........your fingernail has ayour fingernail has a
hardness of 2.5hardness of 2.5
....a penny has a hardness....a penny has a hardness
of about 3.5of about 3.5
....glass and a steel nail....glass and a steel nail
have nearly equalhave nearly equal
hardness of 5.5hardness of 5.5
....a streak plate has a....a streak plate has a
hardness of 6.5hardness of 6.5
Hardness of Common Minerals:Hardness of Common Minerals: Common Scratching Tools:Common Scratching Tools:
SoftestSoftest
HardestHardest
------------------------------------------------------------------------
18
Table of Contents
Standard 3-3.1
Standard 3-3.2
ColorColor
 Mineral color is determined by how the crystals absorb and reflect light.Mineral color is determined by how the crystals absorb and reflect light. Although color isAlthough color is
easy to recognize, it is often misleading.easy to recognize, it is often misleading.
 Minerals, such as quartz, fluorite, halite, and calcite occur in a wide variety of colors, andMinerals, such as quartz, fluorite, halite, and calcite occur in a wide variety of colors, and
other minerals, such as olivine, malachite, and amphibole have fairly distinctive colors.other minerals, such as olivine, malachite, and amphibole have fairly distinctive colors.
 Variations in a mineral’s color may be the result of impurities in the atomic structure of theVariations in a mineral’s color may be the result of impurities in the atomic structure of the
crystal or the presence of a particular chemical when the crystal formed.crystal or the presence of a particular chemical when the crystal formed.
 Because some minerals can occur in several colors, color is generally not a goodBecause some minerals can occur in several colors, color is generally not a good
characteristic for describing and identifying minerals.characteristic for describing and identifying minerals.
Different Colors of Calcite
Image courtesy of the USGSImage courtesy of the USGS
copyright@Stonetrust, Inccopyright@Stonetrust, Inc
Different Colors of Fluorite
copyright@Stonetrustcopyright@Stonetrust, Inc, Inc
Image courtesy of the USGSImage courtesy of the USGS Image courtesy of theImage courtesy of the
Albert Copley OklahomaAlbert Copley Oklahoma
University ArchivesUniversity Archives
Different Colors of Quartz
copyright@Stonetrustcopyright@Stonetrust, Inc, Inc
19
Table of Contents
Standard 3-3.1
Standard 3-3.2
StreakStreak
 Streak refers to the color of a mineral’s powdered form left behind afterStreak refers to the color of a mineral’s powdered form left behind after
it is scraped or rubbed across a porcelain streak plate.it is scraped or rubbed across a porcelain streak plate.
 A mineral may appear one color and then produce a streak with aA mineral may appear one color and then produce a streak with a
different color.different color.
 A mineral’s streak color is a more reliable identification characteristicA mineral’s streak color is a more reliable identification characteristic
than the minerals perceived surface color.than the minerals perceived surface color.
20
Table of Contents
Even though the mineral pyrite isEven though the mineral pyrite is
gold in color, it leaves a greygold in color, it leaves a grey
“pencil lead” streak on the“pencil lead” streak on the
porcelain streak plate.porcelain streak plate.
Standard 3-3.1
Standard 3-3.2
Photo: SCGS
CleavageCleavage
 Cleavage refers to the tendency of aCleavage refers to the tendency of a
mineral to break along planes ofmineral to break along planes of
weakness in the chemical bonds, or alongweakness in the chemical bonds, or along
planes where bond strength is the least.planes where bond strength is the least.
Cleavage, cont.Cleavage, cont.
 One direction of cleavage (one plane)One direction of cleavage (one plane)
 Mineral Example: Micas (muscovite)Mineral Example: Micas (muscovite)
 Two directions of cleavage (two planes)Two directions of cleavage (two planes)
 Mineral Example: FeldsparMineral Example: Feldspar
 Three directions of cleavage (three planes)Three directions of cleavage (three planes)
 Cubic : Mineral Example: GalenaCubic : Mineral Example: Galena
 Rhombohedral: Mineral Example: CalciteRhombohedral: Mineral Example: Calcite
 Fourdirections of cleavage (fourplanes)Fourdirections of cleavage (fourplanes)
 Mineral Example: FlouriteMineral Example: Flourite
Courtesy United States Geological SurveyCourtesy United States Geological Survey
plane one:plane one:
plane two:plane two:
Feldspar: Two Cleavage PlanesFeldspar: Two Cleavage Planes
Galena: Three Cleavage PlanesGalena: Three Cleavage Planes
Plane one:Plane one:
Plane two:Plane two:
Plane three:Plane three:
Copyright©Dr.Richard BuschCopyright©Dr.Richard Busch
Calcite: Three Cleavage PlanesCalcite: Three Cleavage Planes
Plane one:Plane one:
Plane two:Plane two:
Plane three:Plane three: Copyright©Stonetrust, IncCopyright©Stonetrust, Inc
22
Table of Contents
Standard 3-3.1
Standard 3-3.2
Specific GravitySpecific Gravity
 Specific gravity refers to the weight or heaviness of a mineral, andSpecific gravity refers to the weight or heaviness of a mineral, and
it is expressed as the ratio of the mineral’s weight to an equalit is expressed as the ratio of the mineral’s weight to an equal
volume of water.volume of water.
23
Table of Contents
Standard 3-3.1
Standard 3-3.2
But how can we get these
minerals from the earth surface???
Mining
 Mining is the process of extracting minerals
from the earth, and it follows a cycle of
operations of rock breakage and materials
handling.
The Mining Process
 Surface Mining
 Surface mining areas are developed by means of:
a) area mining (on flat terrain);
 b) contour mining and
 c) open-pit mining.
Mining process
 Underground Mining
 Underground mining areas are developed as follows:
a) drift mine (horizontal tunneling);
 b) slope mine (downward, slanted tunneling); and
 c) shaft mine (vertical tunneling).
Scales of mining operations
a.) Small-Scale;
b.) Medium- Scale; and
c.) Large-Scale
 small-scale mining operations rely heavily on
manual labor using simple implements and
methods and do not use explosives or heavy
mining equipment.
 Large-scale mining, involves the mobilization
of substantial capital, heavy equipment, high
technology and a much bigger workforce.
Impacts of mining
 Extracting minerals from the earth and
processing them produces enormous
environmental damage.
 Mining produces ¾ of all waste (Colins)
 Waste
 In 1991 990 million tons of ore were mind to produce
only 9 million tons of copper!-this wastage will
increase as poorer deposits are mind.
 This waste pilled into slagheaps which are difficult to
re-vegetate.
 Mining produces as much soil erosion as all
rivers combined.
 Air pollution from the mineral industry has
made tens of thousands of hectares of land
uninhabitable and
 causes thousands of birth deformities and
illness each year.
 Pollution
 Tailings and slag often toxic materials which can
be leached out into surroundings soil and can
pollute waterways.
 Such toxins include sulfuric acid, arsenic,
mercury, cyanides etc.
 Soil erosion
 Caused principally because dirt roads are built to
reach mines
 Landscape also often dotted with “Borrow Pits”
left after small deposits are dug out of surface
 Such pits often fill with water and are dangerous
and unsightly.
Mineral Use
 Production
Mineral use
Mineral Management
Three alternatives to diminishing
supplies:
 Recycling
 Conservation
 Substitution
Recycling
conservation
substitution

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Minerals

  • 1. THE MINERALS / THEIR UTILIZATION MANAGEMENT Prepared by MJ Salvaña
  • 2. MINERALS  Mineral - a naturally occurring substance composed of specific chemical elements or compounds, with characteristic crystal structure, and certain fixed or slightly variable physical properties Minerals are considered as archetypal and are the core of non-renewable resources. -are extracted from the earths crust. The deposits are formed on geological time scales of a totally different order from that of the human scales of their use
  • 3. Classification of Minerals  a) metallic minerals;  b) non-metallic or industrial minerals; and  c) fuel minerals
  • 4. Four types of Mineral Resources  Metals ( e.g. Iron, Copper, Aluminum)  Industrial Minerals (e.g. Lime, Potash)  Construction Materials (e.g. sand, stone, gravel)  Energy Minerals (e.g. Uranium)
  • 5. Mineral ClassificationMineral Classification  There are 7 MajorMineral Groups:There are 7 MajorMineral Groups:  SilicatesSilicates  Native ElementsNative Elements  HalidesHalides  CarbonatesCarbonates  OxidesOxides  SulfatesSulfates  SulfidesSulfides  Minerals are classified by theirchemical composition and internal crystal structure.
  • 6. Mineral ClassificationMineral Classification  Silicates are composed of silicon-Silicates are composed of silicon- oxygen tetrahedrons, anoxygen tetrahedrons, an arrangement which contains fourarrangement which contains four oxygen atoms surrounding aoxygen atoms surrounding a silicon atom (SiOsilicon atom (SiO44 -4-4 ).). 1. Silicates1. Silicates QuartzQuartz Copyright©Stonetrust, Inc. Silicates comprise the majority ofSilicates comprise the majority of minerals in the Earth’s crust and upperminerals in the Earth’s crust and upper mantle. Over 25% of all minerals aremantle. Over 25% of all minerals are included in this group, with over 40% ofincluded in this group, with over 40% of those accounting for the most commonthose accounting for the most common and abundant minerals.and abundant minerals. Feldspar, Quartz, Biotite, andFeldspar, Quartz, Biotite, and Amphibole are the most commonAmphibole are the most common silicatessilicates
  • 7. 2.Native Elements2.Native Elements  Native elements are minerals that are composed of a singleNative elements are minerals that are composed of a single element.element.  Some examples are: Gold (Au), Silver (Ag), Copper (Cu), Iron (Fe),Some examples are: Gold (Au), Silver (Ag), Copper (Cu), Iron (Fe), Diamonds (C), Graphite (C), and Platinum (Pt)Diamonds (C), Graphite (C), and Platinum (Pt) Image Courtesy of the USGS GoldGold SilverSilver Image Courtesy of the USGS
  • 8. 3. Halides3. Halides  Halides consist of halogen elements, chlorine (Cl), bromine (Br),Halides consist of halogen elements, chlorine (Cl), bromine (Br), fluorine (F), and iodine (I) forming strong ionic bonds with alkali andfluorine (F), and iodine (I) forming strong ionic bonds with alkali and alkali earth elements sodium (Na), calcium (Ca) and potassium (K)alkali earth elements sodium (Na), calcium (Ca) and potassium (K)  Some examples include Halite (NaCl) and Flourite (CaFSome examples include Halite (NaCl) and Flourite (CaF22).). HaliteHalite Copyright©Stonetrust, Inc. FluoriteFluorite Image courtesy of USGS
  • 9. 4.Carbonates4.Carbonates  Carbonates are anionic groups of carbon and oxygen. Carbonate minerals result fromCarbonates are anionic groups of carbon and oxygen. Carbonate minerals result from bonds between these complexes and alkali earth and some transitional metalsbonds between these complexes and alkali earth and some transitional metals  Common carbonate minerals include calcite CaCOCommon carbonate minerals include calcite CaCO33 , calcium carbonate, and dolomite, calcium carbonate, and dolomite CaMg(COCaMg(CO33))22 , calcium/magnesium carbonate, calcium/magnesium carbonate  Carbonate minerals react when exposed to hydrochloric acid. Geologist will oftenCarbonate minerals react when exposed to hydrochloric acid. Geologist will often carry dilute hydrochloric acid in the field to test if a mineral contains calciumcarry dilute hydrochloric acid in the field to test if a mineral contains calcium carbonate. If the mineral fizzes when it comes in contact with the hydrochloric acid itcarbonate. If the mineral fizzes when it comes in contact with the hydrochloric acid it contains calcium carbonate. Some cola soft drinks can also be used for this testcontains calcium carbonate. Some cola soft drinks can also be used for this test because it contains enough hydrochloric acid to react with calcium carbonate.because it contains enough hydrochloric acid to react with calcium carbonate. DolomiteDolomite CalciteCalcite Copyright©Stonetrust, Inc.
  • 10. 5.Oxides5.Oxides  Oxides are minerals that include one or more metal cations bondedOxides are minerals that include one or more metal cations bonded to oxygen or hydroxyl anions.to oxygen or hydroxyl anions.  Examples of oxide minerals include: Hematite (FeExamples of oxide minerals include: Hematite (Fe22OO33), Magnetite), Magnetite (Fe(Fe33OO44), Corundum (Al), Corundum (Al22OO33), and Ice (H), and Ice (H22O)O) HematiteHematite
  • 11. SulfatesSulfates  Sulfates are minerals that include SOSulfates are minerals that include SO44 anionic groupsanionic groups combined with alkali earth and metal cations.combined with alkali earth and metal cations.  Anhydrous (no water) and hydrous (water) are the twoAnhydrous (no water) and hydrous (water) are the two major groups of Sulfates.major groups of Sulfates.  Barite (BaSOBarite (BaSO44) is an example of a anhydrous sulfate and) is an example of a anhydrous sulfate and Gypsum (CaSOGypsum (CaSO4·4· 2H2H22O) is an example of a sulfate.O) is an example of a sulfate. GypsumGypsum Image Courtesy of the USGS BariteBarite Image Courtesy of the USGS
  • 12. 6. SulfidesSulfides  Sulfides are minerals composed of one or more metal cationsSulfides are minerals composed of one or more metal cations combined with sulfur. Many sulfides are economically importantcombined with sulfur. Many sulfides are economically important ores.ores.  Pyrite (FeSPyrite (FeS22) or “fool’s gold”, Galena (PbS), Cinnabar (HgS) an) or “fool’s gold”, Galena (PbS), Cinnabar (HgS) an Molybdenite (MoSMolybdenite (MoS22) are a few commonly occurring sulfide minerals) are a few commonly occurring sulfide minerals Pyrite “Fool’s Gold”Pyrite “Fool’s Gold” Copyright©Dr. Richard Busch CinnabarCinnabar
  • 13. Minerals have distinctive physical properties thatMinerals have distinctive physical properties that geologists use to identify and describe themgeologists use to identify and describe them..  .. Crystal FormCrystal Form  2. Hardness2. Hardness  3. Luster3. Luster  4. Color4. Color  5. Streak5. Streak  6. Cleavage6. Cleavage  7. Specific Gravity7. Specific Gravity A variety of different minerals.A variety of different minerals. Copyright©Dr. Richard BuschCopyright©Dr. Richard Busch
  • 14. .. Crystal FormCrystal Form  Crystal form is the external expression of the internally orderedCrystal form is the external expression of the internally ordered arrangement of atoms.arrangement of atoms.  During mineral formation, individual crystals develop well-formedDuring mineral formation, individual crystals develop well-formed crystal faces that are specific to that mineral.crystal faces that are specific to that mineral. six major crystal forms: 1.1. Isometric (Cubic)Isometric (Cubic) 2.2. TetragonalTetragonal 3.3. OrthorhombicOrthorhombic 4.4. HexagonalHexagonal 5.5. MonoclinicMonoclinic 6.6. TriclinicTriclinic
  • 15. Crystal Form, cont.Crystal Form, cont.  Isometric: Isometric crystals are blockshaped with relatively similar and symmetrical faces. The crystal form has three axes all at 90° angles and all the same length. Mineral Example: Pyrite Tetragonal: Tetragonal crystals are shaped like four-sided pyramids or prisms. The crystal formhas three axes that are all perpendicularto one another. Two axis have the same length, and one is different. The axes that are the same length lie on a horizontal plane, with the third axis at a right angle to the othertwo. Mineral Example: Zircon Orthorhombic: Orthorhombic crystals are shaped like a rectangular prismwith a rectangularbase. The crystal has three axes of different lengths and intersect at 90° angles. Mineral Example: Topaz Copyright© Dr. Richard Busch Isometric: PyriteIsometric: Pyrite Tetragonal: ZirconTetragonal: Zircon Copyright© Dr. Richard Busch Axes Length Relationships: A = B= C Angles: α = β = γ = 90° AA CC BB AA BB CC Axes Length Relationships: A= B≠ C Angles: α = β = γ = 90° CC BBAA Axes Length Relationships: A ≠ B≠ C Angles: α = β = γ = 90° Orthorhombic: TopazOrthorhombic: Topaz Photo Courtesy USGSPhoto Courtesy USGS 15 Table of Contents Standard 3-3.1 Standard 3-3.2 CC BBAA αβ γ
  • 16. Crystal Form, cont.Crystal Form, cont. Hexagonal: Hexagonal crystals have three symmetrical axes that occurin the same plane and are all the same length. The fourth axis may be either longeror shorter, and it intersects the other three axis at 90° angles. The sides intersect at 120 ° angles. Mineral Example: Amethyst Monoclinic: Monoclinic crystals are short and stubby with tilted faces. Each crystal has three axes that are unequal. Two of the axes lie in the same plane at right angles to each other, the third axis is inclined. Mineral Example: Gypsum Triclinic: Triclinic crystals have three axis which are all different lengths and all three axis intersect at angles other than 90°. Mineral Example: Kyanite Monoclinic: GypsumMonoclinic: Gypsum Copyright © Stonetrust ,Inc. AA BB DD CC AA BB CC AA BB CC Axes length Relationships: A = B= C ≠ D Angles: α = β = 90° and γ = 120° Axes Length Relationships: A ≠ B≠ C Angles: α ≠ β ≠ γ Axes Length Relationships: A ≠ B≠ C Angles: α ≠ γ = β = 90° Hexagonal: AmethystHexagonal: Amethyst Copyright © Stonetrust ,Inc. Triclinic: KyaniteTriclinic: Kyanite Copyright © Stonetrust ,Inc. 16 Table of Contents Standard 3-3.1 Standard 3-3.2 CC BBAA αβ γ
  • 17. HardnessHardness  Hardness is the ability of a mineral to resist abrasion or scratchingHardness is the ability of a mineral to resist abrasion or scratching on its surface.on its surface.  One way geologists measure hardness is using a relative scaleOne way geologists measure hardness is using a relative scale referred to as Moh’s scale of mineral hardness which ranks 10referred to as Moh’s scale of mineral hardness which ranks 10 common minerals along a scale from 1-10 (1 refers to the softestcommon minerals along a scale from 1-10 (1 refers to the softest minerals while 10 refers to the hardest mineral).minerals while 10 refers to the hardest mineral). TalcTalc Copyright©Dr. Richard Busch Talc is a soft mineral that you can scratchTalc is a soft mineral that you can scratch with your fingernail, and has a hardness ofwith your fingernail, and has a hardness of “1” measured by Moh’s relative scale of“1” measured by Moh’s relative scale of mineral hardness.mineral hardness.
  • 18. Moh’s Scale of Mineral HardnessMoh’s Scale of Mineral Hardness  1-Talc1-Talc  2-Gypsum2-Gypsum  3-Calcite3-Calcite  4-Fluorite4-Fluorite  5-Apatite5-Apatite  6-Orthoclase6-Orthoclase  7-Quartz7-Quartz  8-Topaz8-Topaz  9-Corundum9-Corundum  10-Diamond10-Diamond ........your fingernail has ayour fingernail has a hardness of 2.5hardness of 2.5 ....a penny has a hardness....a penny has a hardness of about 3.5of about 3.5 ....glass and a steel nail....glass and a steel nail have nearly equalhave nearly equal hardness of 5.5hardness of 5.5 ....a streak plate has a....a streak plate has a hardness of 6.5hardness of 6.5 Hardness of Common Minerals:Hardness of Common Minerals: Common Scratching Tools:Common Scratching Tools: SoftestSoftest HardestHardest ------------------------------------------------------------------------ 18 Table of Contents Standard 3-3.1 Standard 3-3.2
  • 19. ColorColor  Mineral color is determined by how the crystals absorb and reflect light.Mineral color is determined by how the crystals absorb and reflect light. Although color isAlthough color is easy to recognize, it is often misleading.easy to recognize, it is often misleading.  Minerals, such as quartz, fluorite, halite, and calcite occur in a wide variety of colors, andMinerals, such as quartz, fluorite, halite, and calcite occur in a wide variety of colors, and other minerals, such as olivine, malachite, and amphibole have fairly distinctive colors.other minerals, such as olivine, malachite, and amphibole have fairly distinctive colors.  Variations in a mineral’s color may be the result of impurities in the atomic structure of theVariations in a mineral’s color may be the result of impurities in the atomic structure of the crystal or the presence of a particular chemical when the crystal formed.crystal or the presence of a particular chemical when the crystal formed.  Because some minerals can occur in several colors, color is generally not a goodBecause some minerals can occur in several colors, color is generally not a good characteristic for describing and identifying minerals.characteristic for describing and identifying minerals. Different Colors of Calcite Image courtesy of the USGSImage courtesy of the USGS copyright@Stonetrust, Inccopyright@Stonetrust, Inc Different Colors of Fluorite copyright@Stonetrustcopyright@Stonetrust, Inc, Inc Image courtesy of the USGSImage courtesy of the USGS Image courtesy of theImage courtesy of the Albert Copley OklahomaAlbert Copley Oklahoma University ArchivesUniversity Archives Different Colors of Quartz copyright@Stonetrustcopyright@Stonetrust, Inc, Inc 19 Table of Contents Standard 3-3.1 Standard 3-3.2
  • 20. StreakStreak  Streak refers to the color of a mineral’s powdered form left behind afterStreak refers to the color of a mineral’s powdered form left behind after it is scraped or rubbed across a porcelain streak plate.it is scraped or rubbed across a porcelain streak plate.  A mineral may appear one color and then produce a streak with aA mineral may appear one color and then produce a streak with a different color.different color.  A mineral’s streak color is a more reliable identification characteristicA mineral’s streak color is a more reliable identification characteristic than the minerals perceived surface color.than the minerals perceived surface color. 20 Table of Contents Even though the mineral pyrite isEven though the mineral pyrite is gold in color, it leaves a greygold in color, it leaves a grey “pencil lead” streak on the“pencil lead” streak on the porcelain streak plate.porcelain streak plate. Standard 3-3.1 Standard 3-3.2 Photo: SCGS
  • 21. CleavageCleavage  Cleavage refers to the tendency of aCleavage refers to the tendency of a mineral to break along planes ofmineral to break along planes of weakness in the chemical bonds, or alongweakness in the chemical bonds, or along planes where bond strength is the least.planes where bond strength is the least.
  • 22. Cleavage, cont.Cleavage, cont.  One direction of cleavage (one plane)One direction of cleavage (one plane)  Mineral Example: Micas (muscovite)Mineral Example: Micas (muscovite)  Two directions of cleavage (two planes)Two directions of cleavage (two planes)  Mineral Example: FeldsparMineral Example: Feldspar  Three directions of cleavage (three planes)Three directions of cleavage (three planes)  Cubic : Mineral Example: GalenaCubic : Mineral Example: Galena  Rhombohedral: Mineral Example: CalciteRhombohedral: Mineral Example: Calcite  Fourdirections of cleavage (fourplanes)Fourdirections of cleavage (fourplanes)  Mineral Example: FlouriteMineral Example: Flourite Courtesy United States Geological SurveyCourtesy United States Geological Survey plane one:plane one: plane two:plane two: Feldspar: Two Cleavage PlanesFeldspar: Two Cleavage Planes Galena: Three Cleavage PlanesGalena: Three Cleavage Planes Plane one:Plane one: Plane two:Plane two: Plane three:Plane three: Copyright©Dr.Richard BuschCopyright©Dr.Richard Busch Calcite: Three Cleavage PlanesCalcite: Three Cleavage Planes Plane one:Plane one: Plane two:Plane two: Plane three:Plane three: Copyright©Stonetrust, IncCopyright©Stonetrust, Inc 22 Table of Contents Standard 3-3.1 Standard 3-3.2
  • 23. Specific GravitySpecific Gravity  Specific gravity refers to the weight or heaviness of a mineral, andSpecific gravity refers to the weight or heaviness of a mineral, and it is expressed as the ratio of the mineral’s weight to an equalit is expressed as the ratio of the mineral’s weight to an equal volume of water.volume of water. 23 Table of Contents Standard 3-3.1 Standard 3-3.2
  • 24. But how can we get these minerals from the earth surface???
  • 25. Mining  Mining is the process of extracting minerals from the earth, and it follows a cycle of operations of rock breakage and materials handling.
  • 26. The Mining Process  Surface Mining  Surface mining areas are developed by means of: a) area mining (on flat terrain);  b) contour mining and  c) open-pit mining.
  • 27. Mining process  Underground Mining  Underground mining areas are developed as follows: a) drift mine (horizontal tunneling);  b) slope mine (downward, slanted tunneling); and  c) shaft mine (vertical tunneling).
  • 28. Scales of mining operations a.) Small-Scale; b.) Medium- Scale; and c.) Large-Scale  small-scale mining operations rely heavily on manual labor using simple implements and methods and do not use explosives or heavy mining equipment.  Large-scale mining, involves the mobilization of substantial capital, heavy equipment, high technology and a much bigger workforce.
  • 29. Impacts of mining  Extracting minerals from the earth and processing them produces enormous environmental damage.  Mining produces ¾ of all waste (Colins)  Waste  In 1991 990 million tons of ore were mind to produce only 9 million tons of copper!-this wastage will increase as poorer deposits are mind.  This waste pilled into slagheaps which are difficult to re-vegetate.
  • 30.  Mining produces as much soil erosion as all rivers combined.  Air pollution from the mineral industry has made tens of thousands of hectares of land uninhabitable and  causes thousands of birth deformities and illness each year.
  • 31.  Pollution  Tailings and slag often toxic materials which can be leached out into surroundings soil and can pollute waterways.  Such toxins include sulfuric acid, arsenic, mercury, cyanides etc.
  • 32.  Soil erosion  Caused principally because dirt roads are built to reach mines  Landscape also often dotted with “Borrow Pits” left after small deposits are dug out of surface  Such pits often fill with water and are dangerous and unsightly.
  • 36. Three alternatives to diminishing supplies:  Recycling  Conservation  Substitution

Editor's Notes

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