Silicates SiO n silicon oxide 1/3 of all minerals are silicates about 95% of the Earth’s crust is composed of silicates
Earth’s Crust Chemical Composition ELEMENTWEIGHT% O (oxygen) 47 Si (silicon) 28 Aluminum 8 Fe (iron) 5 Ca (calcium) 4 Na (sodium) 3 K (potassium)3 Mg (magnesium) 2 Total 98.5%
Average Mineral Crustal Composition Mineral Weight% feldspar * 66 * quartz * 10 * magnetite/hematite 6 Ferromagnesium minerals * (olivine, pyroxene, amphibole, biotite) 15 * Total 97 *silicate
Other important minerals muscovite (mica) gypsum clays halite calcite dolomite
MINERAL IDENTIFICATION Primarily based on physical properties.
The properties of each mineral are determined by: chemical elements present arrangement of elements in the mineral structure
Streak (scratchability) Color of powdered mineral
Specific gravity Au gold PbS galena Density - mass/volume Specific gravity - mass of sample / mass of equal volume of water
Cleavage planar surfaces caused by breaks along planes of weakness in atomic structure. Number of directions and angle important.
Cleavage
cleavage
Cleavage
Fracture Irregular surfaces caused by breaks
Crystal form External morphology due to atomic structure. Quartz and corundum have 6 crystal faces.
Luster The way in which light is reflected, e.g., metallic, glassy
Color Poor except for metallics and silicate varieties
Hardness Mohs Hardness Scale 1. Talc 2. Gypsum 2.5finger nail 3.5penny 3. Calcite 4. Fluorite 5. Apatite 5.0 nail glass and knife blade
6. Orthoclase (feldspar) 7. Quartz 8. Topaz 9. Corundun 10. Diamond
Striations odor magnetic Double Refraction
Mineral Resources Ore -- mineral that can be mined for a profit Gangue--worthless minerals in an ore body
examples of ores Ag silver Au gold Copper sulfides (covellite) Feoxides (hematite) PbS lead sulfide (galena) The U.S.A imports about 80% of the most used 16 metals!