Composed of silicon-oxygen tetrahedrons (SiO4) the fundamental building block of silicate minerals<|>90% of rock-forming minerals belong here
Silicate minerals
feldspar
mica
quartz
pyroxene
olivine
Oxides
Minerals containing Oxygen anion (02-) combined with one or more metal ions
Oxide minerals
magnetite (Fe304)
Hematite (Fe2O3)
Sulfates
Contain Sulfur and Oxygen anion (SO4)- combined with other ions (metal cation)<|>Usually precipitate out of water near Earth's surface
Sulfides
Contain sulfur anion (S2-) combined with one or more ions<|>Economically important metals
Sulfide minerals
copper
lead
zinc
galena (lead sulfite)
covellite (copper sulfide)
wurtzite (zinc iron sulfide)
Carbonates
Carbonate anion (CO3)2- combined with other elements<|>Characterized by the presence of carbonic acid (H2CO3) which bonds elements such as calcium or magnesium to form calcite or dolomite
Halides
Contain Halogen elements combined with one or more elements<|>Chlorine or fluorine form Halite or Rock Salt (NaCl) and Fluorite (CaF2)
Native Elements
Metals
Inter-metals
Semi-metals
Non-metals
Metals
High thermal and electrical conductivity, typically with metallic luster, low hardness (gold, lead)
Semi-metals
More fragile than metals and have low conductivity (arsenic, bismuth)
Non-metals
Nonconductive (sulfur, diamond)
Silicate minerals make up 90% of the Earth's crust
Most silicate minerals also contain other elements like aluminum, iron, or magnesium
Types of rocks
Igneous
Sedimentary
Metamorphic
Earth is a solid rock to a depth of 2,900 kilometers where mantle meets the liquid outer core
Rock
Naturally occurring solid aggregate of one or more minerals<|>The aggregate minerals forming the rocks are held together by chemical bonds<|>Grains can be different in color, texture, and sizes
Petrology
The scientific study of rocks. Rocks are combined aggregation of minerals. Petrologist