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Description
MINERALS
Chemical composition of the Crust
Oxygen most abundant- 46.6% Followed by silicon and aluminum Iron, Calcium, Sodium, Potassium, Magnesium The most common minerals will be composed mostly of these elements Silica & silicates
MINERAL vs. ROCK
ROCK An
aggregate of one or more MINERALS (usually- coal, organic)
MINERAL Solid Crystalline-
orderly arrangement of atoms Naturally occurring Inorganic Definite chemical composition e.g.
SiO2 for quartz; KAlSi3O8 for feldspar
Atom & Elements
Atoms Neutral Nucleus Proton,
Electron
Ions Electrical
neutron
Charge
Molecule- e.g. water molecule
Chemical activity
Stable atoms want positive
& negative charges balanced electron shells full
Ions- positive (Cations) and negative (Anions) Bonding Ionic Covalent Metallic Van
der Waal’s
Element
Atomic number Number
of PROTONS
Isotope Differing
number of NEUTRONS
Atomic weight Mass
of PROTONS and NEUTRONS
Crystallinity
3 dimensional orderliness of atoms Silicon-oxygen tetrahedron Silicate structures Single-
e.g. olivine
Chain Single
chain- pyroxene Double chain- amphibole Sheet-
e.g. mica, clay Framework- e.g. quartz, feldspar
MINERALS
Crystalline solids Natural and Inorganic Substances Definite chemical composition Can
be written as a chemical formula Solid solution (within a range)
Important Minerals
Quartz (most abundant) FELDSPAR Group Potassium
Feldspar - Orthoclase Plagioclase Feldspar Sodium
(Na) Albite Calcium (Ca) Anorthosite
Important Minerals
PYROXENE Group- Augite most common AMPHIBOLE Group- Hornblende most common MICA Group- Si + O in sheets Biotite Muscovite
CALCITE- CaCO3
Properties of Minerals
Color Not
always reliable (Olivine, green; Flourite, yellow, purple, green…) Ferromagnesian minerals green or black
Streak- powdered form Luster- reflectance of light Metallic Nonmetallic Vitreous Earthy
or Glassy
Properties of Minerals
Hardness- resistance to scratching Moh’s Hardness Scale Fingernail
= 2.5 Penny = 3.5 Knife/Glass = 5.5 Streak Plate= 6.5
Cleavage
Properties of Minerals
Quality
(poor, good, perfect) Number of directions One-
e.g. Mica Two at right angles- e.g. Feldspar, Pyroxene Two not at right angles- e.g. Amphibole Three at right angles (cubic)- e.g. Halite Three not at right angles (rhombohedral)- e.g. calcite Four (Flourite) or six (Sphalerite)- not common
Properties of Minerals
Fracture Absence
of cleavage Irregular fracture Conchoidal fracture- Quartz
Density Specific
Gravity
Some unusual properties Striations,
refraction
Magnetism, Taste, Odor, Double
Chemical tests
Reaction with HCl Calcite
effervesces
Mineral Groups
Silicates Carbonates Oxides Sulfides Sulfates Native Elements Halides
Silicates
Quartz Feldspar Plagioclase Orthoclase Micas Muscovite Biotite Amphibole (Hornblende) Pyroxene (Augite) Olivine
Carbonates
Calcite (calcium carbonate) Dolomite (calcium-magnesium carbonate) Both are used as Portland Cement
Oxides
Hematite (iron oxide) Iron
Magnetite Iron
ore, pigment ore
Corundum (aluminum oxide) Sapphire, Abrasive
ruby (gemstone)
Sulfides
Galena (Lead sulfide) Lead
Sphalerite Zinc sulfide) Zinc
ore
ore
Pyrite (Iron sulfide) Sulfuric
acid
Chalcopyrite (Copper Iron sulfide) Copper
ore
Sulfates
Gypsum Anhydrite Both use in plaster
Native Elements
Gold- trade, instruments Silver- photography, conductors Copper- electrical Platinum- catalysts Sulfur- chemicals, pharmaceuticals Diamond- carbon Gemstone, abrasive Graphite- carbon Lubricant, pencils
Minerals as Resources
Reserves: Minerals that can be extracted at a profit under current economic and technological conditions Ores: metallic minerals Industrial Rocks or Minerals: non metallic minerals (phosphate) Aggregates: crushed rock
ROCK CYCLE
Equilibrium Interrelationships between igneous
rocks sediment sedimentary rocks metamorphic rocks weathering and erosion
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