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EXAMPLES OF MINERALS There are over 4900 known mineral species over 4,660 of these have been approved by the (IMA). Silicate minerals compose over 90% of the Earths crust. Halite, pyrite, hematite, calcite, gold, silver, quartz, feldspar, mica, gypsum, lepidolite, ruby, diamond, topaz, graphite, corundum, fluorite, apatite, clinoclase, stibnite, stillbite, azurite, malachite, copper, garnet, talc, vanadinite, sulfur, kyanite
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MINERALS
CH 5- Miss Kelley
MINERALOccur naturally
Consistent chemical composition
Solid• Orderly structured= crystalline form
Inorganic chemical composition- lacks C & H• (all living things are made up of carbon)• Inorganic compounds are traditionally
viewed as being synthesized by the agency of geological systems
EXAMPLES OF MINERALS
• There are over 4900 known mineral species• over 4,660 of these have been approved by the (IMA).
• Silicate minerals compose over 90% of the Earths crust.
Halite, pyrite, hematite, calcite, gold, silver, quartz, feldspar, mica, gypsum, lepidolite, ruby, diamond, topaz, graphite, corundum, fluorite, apatite, clinoclase, stibnite, stillbite, azurite, malachite, copper, garnet, talc, vanadinite, sulfur, kyanite
Classified as silicates and non silicates
Minerals are mainly oxides & sulfides • strictly inorganic• although they may be of biological origin.
In fact, most of the earth is inorganic
SILICATESSi & O
Classified based on structure• Is due to different ratios of Si & O • Nesosilicates • sorosilicates • cyclosilicates • inosilicates • phyllosilicates • tectosilicates
NON SILICATES
4% of earth’s crust
Don’t contain Si & O• Carbonates• Halides• Native elements• Oxides• Sulfates• sulfides
CRYSTALLINE STRUCTURE
Atoms are arranged is a repeating geometric pattern
Silicon-oxygen tetrahedral- basic unit of a structured crystalline solid
• (pyramid like)• Arranged about
The center Si
OTHER ARRANGEMENTS
6 other kinds
Isolated tetrahedral
Ring silicates
Single chain silicates
Double chain silicates
Sheet silicates
Framework silicates
ISOLATED TETRAHEDRAL
Doesn’t link with other Si or O
Uses basic silicon-oxygen of the tetrahedron bonds to another atom of a different element
RING SILICATES
O bonds with other O atoms creating a circle of tetrahedrons
SINGLE CHAIN SILICATES
Each tetrahedron is bonded with two others tetradedras
This bond forms between 2 O atoms
DOUBLE CHAIN
Two single chains combine
2 bonds with O atoms
SHEET SILICATES
Each tetrahedron shares 3 Oxygen atoms from another tetrahedron
3 bonds between oxygen atoms
FRAME WORK
Each tetrahedron is bonded with 4 tetrahedrons
4 bonds between oxygen atoms
NON MINERALS
Same structure
Without Si