Mineral groups Flashcards
Silicates
Most common mineral group Composed of Silicon and Oxygen
Have the same fundamental building block, the silicon-oxygen tetrahedron
Negative ion (anion)
Most silicate minerals have a net negative charge
Positive ions (cations) balance the charge by bonding with the unshared oxygen ions in the tetrahedron
Light silicates
Generally light in color
Noticeably less dense than dark silicates
Contain varying amounts of aluminum, potassium, calcium, and sodium rather than iron and magnesium
Feldspar
Most common mineral in Earth’s crust
Potassium feldspar - contains K
Quartz
2nd most common mineral in Earth’s crust
Only common silicate mineral that consists entirely of silicon and oxygen
Occurs in a variety of colors due to impurities
Muscovite
Common member of the mica family
Cleavage in one direction
Historically used as window “glass”
Now used in cosmetics, electronics and automotive industries
Clay minerals
Originate as products of the chemical breakdown (chemical weathering) of other silicate minerals
Clay minerals make up a large percentage of the surface material (soil)
Dark silicates
Generally darker in color and denser than light silicates
Contain varying amounts Fe and Mg
Olivine Group
Family of high temperature silicate minerals, are black to olive green in color and have a glassy luster and conchoidal fracture
Pyroxene Group
Hornblends is the most common member
Found in igneous rocks, where it often makes up the dark portion of an otherwise light colored rock
Often forms elongated crystals. This helps distinguishes it from pyroxene group, which forms rather blocky crystals
Biotite
Dark, iron rich member of the mica family like other micas, biotite possesses a sheet structure that gives it excellent cleavage in one direction Amphibole
Non silicates
All other minerals fall into these groups
Grouped based on anion present or can occur as single elements
Non renewable resource
Process that create them are so slow that significant deposits take millions of years to accumulate
Renewable resources
Replenished over relatively short time
Ore deposit
Naturally occurring concentration of one or more metallic minerals that can be extracted economically