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PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage1
PRACTICAL PROSPECTOR'S GUIDE TO
MINERALS
By
Prof. Dr. Hassan Z. Harraz
Geology Department
Faculty Sciences, Tanta University-Egypt
hharraz2006@yahoo.com
Outline
Topic 1:Rock-Forming Minerals
Topic 2:Ores (Metallic)
Topic 3:Ores (NON-Metallic)
Topic 4:Industrial Minerals
Topic 5:Gem Minerals
PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage2
PRACTICAL PROSPECTOR'S GUIDE TO
MINERALS
I- Rock-Forming Minerals
Quartz
 Most common mineral species
 Vitreous luster; conchoidal fracture; hexagonal, prismatic crystals are
diagnostic
 Many color varieties: amethyst, smoky, rose, citrine
 Uses: glass manufacture, abrasive, flux, optical instruments,
electronics
Feldspar Group
Potassium feldspars: microcline, orthoclase, sanidine
 blocky crystals, often show perthitic texture (especially microcline)
Plagioclase feldspars: albite – anorthite series
 range from white to black
 often show play of colors (labradorescence)
 striations on cleavage surface (albite twinning)
Mica Group
Muscovite (white mica)
Biotite (black mica)
Phlogopite (brown mica)
Sericite (brown to buff mica)
Lepidolite (purple mica)
 lithium-rich pegmatites
 micaceous cleavage, elastic nature of plates and hardness distinguish
micas from all other sheet-like minerals such as talc, gypsum and
brucite
Pyroxene Group
 Generally green to black (except spodumene, which can be white,
yellowish, pink or green).
 2 good to perfect cleavages at nearly right angles (chief distinguishing
 characteristic between pyroxenes and amphiboles).
 Pyroxenes are common in mafic to ultramafic rocks and in skarns
 Emerald-green diopside (chrome-diopside) is a diamond indicator
mineral
 Spodumene is a lithium pyroxene found in rare-element pegmatites
 Jadeite is one of the "true" jades and is a pyroxene
Amphibole Group
• Generally green to black (some, like tremolite, are white)
PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage3
 2 good to perfect cleavages at 56 and 124 degrees (chief
distinguishing
 characteristic between amphiboles and pyroxenes).
 BC jade is "nephrite", a variety actinolite, and is considered a "true"
jade.
 amphiboles are common in skarns and in fairly high-grade
metamorphic rocks.
Garnet Group
Almandine (iron – aluminum garnet)
 generally red
 found in schists
Pyrope (magnesium – aluminum garnet)
 generally red
 diamond indicator mineral (kimberlites, lamprophyres)
Spessartine (manganese – aluminum garnet)
 red to orange
 most often in rare-element pegmatites
Grossular (calcium – aluminum garnet)
 brown, green, red, yellow
 often found in skarns
 gem brown variety known as "hessonite"
Andradite (calcium – iron garnet)
 brown, green, red, yellow, black
 often found in skarns
 gem green variety could be "demantoid"
 titaniferous variety (black) is known as "melanite"
Uvarovite (calcium – chromium garnet)
 chrome green
 associated with altered ultramafic rocks.
Serpentine Group
 varied green color, greasy luster, often fibrous (or splintery)
Olivine
 vitreous luster, conchoidal fracture, green color, presence in basalt as
nodules
Carbonate Group
Calcite
 3 cleavages not at right angles
 fizzes readily with weak acid
Siderite
 typical carbonate cleavage
 light to dark brown
Dolomite
 curved, rhombohedral crystals
 white, pink, gray
PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage4
II- Ores (Metallic)
A. Gold
B. Platinum Group Elements:
 Platinum, Palladium, Iridium, Osmium
 placer deposits, ultramafic rocks
C. Native Silver
 wires in pockets, hackly fracture, tarnishes black
 often as an impurity in galena
D. Sulfosalts
 Pyrargyrite/Proustite (ruby silvers)
 Stephanite
 Tetrahedrite
E. Native Copper (100% Cu)
 often in basalt; sometimes in oxidized zone; hackly fracture,
copper color
F. Chalcopyrite (35% Cu)
 no cleavage, greenish-black streak, slightly greener yellow than
pyrite
G. Bornite (63% Cu)
 purple-blue iridescent tarnish, BRONZY on FRESH
SURFACE
H. Covellite (66% Cu)
 ELECTRIC BLUE, platy cleavage
I. Chalcocite (79% Cu)
 black, SECTILE
J. Galena
 3 perfect CLEAVAGES at right angles, DENSITY, lead-gray
color
 secondary lead minerals: anglesite, cerussite, pyromorphite
J. Molybdenite
 chief ore of molybdenum
 SOFT, slightly bluer-gray than graphite (compare it with a
pencil ‘lead’)
L. Pyrite
 often in good crystals (pyritohedra, cubes, octahedra); brittle,
black streak
M. Arsenopyrite
 no cleavage, "garlic" smell sometimes when broken
N. Pyrrhotite
 bronzy color, sometimes magnetic
O. Stibnite
 main ore of antimony.
 elongate crystals that are often ‘bent’; ONE PERFECT
CLEAVAGE and lower density distinguish it from galena.
 will easily melt in a candle flame
P. Graphite
 SOFT, black (like pencil "lead")
PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage5
III- Ores (NON-Metallic)
A. Sphalerite
 resinous to sub-metallic luster
 yellow to green to red to black
 Important ore of cadmium as well
 alters to smithsonite, hydrozincite (fluorescent)
B. Wolframite
 HEAVY, reddish to black, tabular crystals with one perfect
cleavage
C. Scheelite
 White to brown, fluoresces bluish white
D. Manganese Oxides
 psilomelane is a mixture of compact manganese oxides;
mixture of earthy manganese oxides is known as wad.
 black, soft (often show dendritic stains)
E. Iron Oxides
 mixture of iron oxides is generally known as limonite
1. Hematite: red-brown streak
2. Goethite: brown streak
F. Magnetite
 black, dense, MAGNETIC
G. Cassiterite
 black; glassy to resinous luster
H. Cinnabar
 red; bright red streak; soft
I. Cuprite
 red, often associated with malachite or other secondary copper
minerals
J. Malachite/Azurite
 both are alteration products of other copper minerals
 (MALACHITE is GREEN; AZURITE is BLUE (‘azure-blue’,
in fact)
PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage6
IV- Industrial Minerals
Diamond
 as adamantine crystals in kimberlite or lamprophyre
 placer deposits (weathered kimberlites/lamprophyres)
Sulfur
 as a native element in sedimentary rocks (often associated with
petroleum)
Barite
 one to two good cleavages, VERY heavy
 in hydrothermal veins and sedimentary exhalative deposits
Gypsum
 white to gray, softness is characteristic
 sedimentary rocks
Magnesite
 generally white
 found most commonly in sedimentary rocks, but also in
carbonatites
 hydromagnesite and epsomite are evaporites found in playa
lakes (from the alteration of volcanic rocks)
Apatite
 hexagonal crystals, many colors
 found in many environments
 distinguished from beryl by its hardness (beryl cannot be
scratched by a knife)
Zeolite Group
 generally white or off-white
 found in volcanic rocks or low grade metamorphic rocks
 economic deposits found as beds of altered volcanic ash
 "boil" when torched
Fluorite
 four directions of perfect CLEAVAGE
Corundum
 HARDNESS of 9
PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage7
V- Gem Minerals
The following are reasonable to be expected, or have already been found in British
Columbia.
Corundum
 Ruby: red corundum coloured by chromium
 Sapphire: BLUE, green, pink, yellow, colourless corundum coloured
by iron and/or titanium
Diamond
Beryl
 hexagonal cross-section; prismatic to tabular crystals; generally in
pegmatites
Varieties of Beryl:
 Aquamarine: blue to green beryl coloured by iron
 Emerald: green beryl coloured by chromium or vanadium
 Goschenite: colourless beryl (originally cesium-bearing beryl)
 Heliodor: yellow beryl coloured by iron
Tourmaline
 diamond-shape cross-section; perfect basal cleavage (perpendicular to
the length of the crystal)
Varieties of Gemmy Tourmaline:
 Schorl: black tourmaline found in simple pegmatites, hydrothermal
veins and metamorphic rocks
 Elbaite: lithium-bearing tourmaline found almost exclusively in
pegmatites;
 Rubellite (pink), Verdelite (green), Indicolite (blue), Achroite
(colourless)
 Liddicoatite: another lithium-bearing tourmaline, again in pegmatites
Topaz
 diamond-shape cross-section; perfect basal cleavage (perpendicular to
the length of the crystal)
Garnet
 metamorphic rocks; pegmatites
Varieties of Gemmy Garnet:
 Grossular: gem brown variety is hessonite
 Andradite: gem green variety is demantoid
 Spessartine: bright orange is best quality
Quartz
Varieties of Quartz:
 Amethyst: purple quartz coloured by iron (Fe4+)
 Citrine: yellow/orange quartz coloured by iron
 Smoky Quartz: brown to black quartz affected by radiation
 Rose Quartz: pink quartz coloured by manganese
PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012
HZH, Tanta UnivPage8
 Chalcedony: cryptocrystalline quartz; gray, greasy to silky luster;
found in volcanic rocks and some sedimentary rocks
 Agate: concentrically banded chalcedony; variously coloured
 Onyx: flat, layered chalcedony; usually black/white or red/white<
 Carnelian: chalcedony coloured red by iron
 Chrysoprase: chalcedony coloured green by nickel
 Jasper: chalcedony coloured red, green, yellow or black by iron oxide
Opal
 in volcanic and sedimentary rocks
 common versus precious opal

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Practical prospector's guide to minerals

  • 1. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage1 PRACTICAL PROSPECTOR'S GUIDE TO MINERALS By Prof. Dr. Hassan Z. Harraz Geology Department Faculty Sciences, Tanta University-Egypt hharraz2006@yahoo.com Outline Topic 1:Rock-Forming Minerals Topic 2:Ores (Metallic) Topic 3:Ores (NON-Metallic) Topic 4:Industrial Minerals Topic 5:Gem Minerals
  • 2. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage2 PRACTICAL PROSPECTOR'S GUIDE TO MINERALS I- Rock-Forming Minerals Quartz  Most common mineral species  Vitreous luster; conchoidal fracture; hexagonal, prismatic crystals are diagnostic  Many color varieties: amethyst, smoky, rose, citrine  Uses: glass manufacture, abrasive, flux, optical instruments, electronics Feldspar Group Potassium feldspars: microcline, orthoclase, sanidine  blocky crystals, often show perthitic texture (especially microcline) Plagioclase feldspars: albite – anorthite series  range from white to black  often show play of colors (labradorescence)  striations on cleavage surface (albite twinning) Mica Group Muscovite (white mica) Biotite (black mica) Phlogopite (brown mica) Sericite (brown to buff mica) Lepidolite (purple mica)  lithium-rich pegmatites  micaceous cleavage, elastic nature of plates and hardness distinguish micas from all other sheet-like minerals such as talc, gypsum and brucite Pyroxene Group  Generally green to black (except spodumene, which can be white, yellowish, pink or green).  2 good to perfect cleavages at nearly right angles (chief distinguishing  characteristic between pyroxenes and amphiboles).  Pyroxenes are common in mafic to ultramafic rocks and in skarns  Emerald-green diopside (chrome-diopside) is a diamond indicator mineral  Spodumene is a lithium pyroxene found in rare-element pegmatites  Jadeite is one of the "true" jades and is a pyroxene Amphibole Group • Generally green to black (some, like tremolite, are white)
  • 3. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage3  2 good to perfect cleavages at 56 and 124 degrees (chief distinguishing  characteristic between amphiboles and pyroxenes).  BC jade is "nephrite", a variety actinolite, and is considered a "true" jade.  amphiboles are common in skarns and in fairly high-grade metamorphic rocks. Garnet Group Almandine (iron – aluminum garnet)  generally red  found in schists Pyrope (magnesium – aluminum garnet)  generally red  diamond indicator mineral (kimberlites, lamprophyres) Spessartine (manganese – aluminum garnet)  red to orange  most often in rare-element pegmatites Grossular (calcium – aluminum garnet)  brown, green, red, yellow  often found in skarns  gem brown variety known as "hessonite" Andradite (calcium – iron garnet)  brown, green, red, yellow, black  often found in skarns  gem green variety could be "demantoid"  titaniferous variety (black) is known as "melanite" Uvarovite (calcium – chromium garnet)  chrome green  associated with altered ultramafic rocks. Serpentine Group  varied green color, greasy luster, often fibrous (or splintery) Olivine  vitreous luster, conchoidal fracture, green color, presence in basalt as nodules Carbonate Group Calcite  3 cleavages not at right angles  fizzes readily with weak acid Siderite  typical carbonate cleavage  light to dark brown Dolomite  curved, rhombohedral crystals  white, pink, gray
  • 4. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage4 II- Ores (Metallic) A. Gold B. Platinum Group Elements:  Platinum, Palladium, Iridium, Osmium  placer deposits, ultramafic rocks C. Native Silver  wires in pockets, hackly fracture, tarnishes black  often as an impurity in galena D. Sulfosalts  Pyrargyrite/Proustite (ruby silvers)  Stephanite  Tetrahedrite E. Native Copper (100% Cu)  often in basalt; sometimes in oxidized zone; hackly fracture, copper color F. Chalcopyrite (35% Cu)  no cleavage, greenish-black streak, slightly greener yellow than pyrite G. Bornite (63% Cu)  purple-blue iridescent tarnish, BRONZY on FRESH SURFACE H. Covellite (66% Cu)  ELECTRIC BLUE, platy cleavage I. Chalcocite (79% Cu)  black, SECTILE J. Galena  3 perfect CLEAVAGES at right angles, DENSITY, lead-gray color  secondary lead minerals: anglesite, cerussite, pyromorphite J. Molybdenite  chief ore of molybdenum  SOFT, slightly bluer-gray than graphite (compare it with a pencil ‘lead’) L. Pyrite  often in good crystals (pyritohedra, cubes, octahedra); brittle, black streak M. Arsenopyrite  no cleavage, "garlic" smell sometimes when broken N. Pyrrhotite  bronzy color, sometimes magnetic O. Stibnite  main ore of antimony.  elongate crystals that are often ‘bent’; ONE PERFECT CLEAVAGE and lower density distinguish it from galena.  will easily melt in a candle flame P. Graphite  SOFT, black (like pencil "lead")
  • 5. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage5 III- Ores (NON-Metallic) A. Sphalerite  resinous to sub-metallic luster  yellow to green to red to black  Important ore of cadmium as well  alters to smithsonite, hydrozincite (fluorescent) B. Wolframite  HEAVY, reddish to black, tabular crystals with one perfect cleavage C. Scheelite  White to brown, fluoresces bluish white D. Manganese Oxides  psilomelane is a mixture of compact manganese oxides; mixture of earthy manganese oxides is known as wad.  black, soft (often show dendritic stains) E. Iron Oxides  mixture of iron oxides is generally known as limonite 1. Hematite: red-brown streak 2. Goethite: brown streak F. Magnetite  black, dense, MAGNETIC G. Cassiterite  black; glassy to resinous luster H. Cinnabar  red; bright red streak; soft I. Cuprite  red, often associated with malachite or other secondary copper minerals J. Malachite/Azurite  both are alteration products of other copper minerals  (MALACHITE is GREEN; AZURITE is BLUE (‘azure-blue’, in fact)
  • 6. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage6 IV- Industrial Minerals Diamond  as adamantine crystals in kimberlite or lamprophyre  placer deposits (weathered kimberlites/lamprophyres) Sulfur  as a native element in sedimentary rocks (often associated with petroleum) Barite  one to two good cleavages, VERY heavy  in hydrothermal veins and sedimentary exhalative deposits Gypsum  white to gray, softness is characteristic  sedimentary rocks Magnesite  generally white  found most commonly in sedimentary rocks, but also in carbonatites  hydromagnesite and epsomite are evaporites found in playa lakes (from the alteration of volcanic rocks) Apatite  hexagonal crystals, many colors  found in many environments  distinguished from beryl by its hardness (beryl cannot be scratched by a knife) Zeolite Group  generally white or off-white  found in volcanic rocks or low grade metamorphic rocks  economic deposits found as beds of altered volcanic ash  "boil" when torched Fluorite  four directions of perfect CLEAVAGE Corundum  HARDNESS of 9
  • 7. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage7 V- Gem Minerals The following are reasonable to be expected, or have already been found in British Columbia. Corundum  Ruby: red corundum coloured by chromium  Sapphire: BLUE, green, pink, yellow, colourless corundum coloured by iron and/or titanium Diamond Beryl  hexagonal cross-section; prismatic to tabular crystals; generally in pegmatites Varieties of Beryl:  Aquamarine: blue to green beryl coloured by iron  Emerald: green beryl coloured by chromium or vanadium  Goschenite: colourless beryl (originally cesium-bearing beryl)  Heliodor: yellow beryl coloured by iron Tourmaline  diamond-shape cross-section; perfect basal cleavage (perpendicular to the length of the crystal) Varieties of Gemmy Tourmaline:  Schorl: black tourmaline found in simple pegmatites, hydrothermal veins and metamorphic rocks  Elbaite: lithium-bearing tourmaline found almost exclusively in pegmatites;  Rubellite (pink), Verdelite (green), Indicolite (blue), Achroite (colourless)  Liddicoatite: another lithium-bearing tourmaline, again in pegmatites Topaz  diamond-shape cross-section; perfect basal cleavage (perpendicular to the length of the crystal) Garnet  metamorphic rocks; pegmatites Varieties of Gemmy Garnet:  Grossular: gem brown variety is hessonite  Andradite: gem green variety is demantoid  Spessartine: bright orange is best quality Quartz Varieties of Quartz:  Amethyst: purple quartz coloured by iron (Fe4+)  Citrine: yellow/orange quartz coloured by iron  Smoky Quartz: brown to black quartz affected by radiation  Rose Quartz: pink quartz coloured by manganese
  • 8. PRACTICAL PROSPECTOR'S GUIDE TO MINERALS[ ] October 3, 2012 HZH, Tanta UnivPage8  Chalcedony: cryptocrystalline quartz; gray, greasy to silky luster; found in volcanic rocks and some sedimentary rocks  Agate: concentrically banded chalcedony; variously coloured  Onyx: flat, layered chalcedony; usually black/white or red/white<  Carnelian: chalcedony coloured red by iron  Chrysoprase: chalcedony coloured green by nickel  Jasper: chalcedony coloured red, green, yellow or black by iron oxide Opal  in volcanic and sedimentary rocks  common versus precious opal