Lesson 2.1 Minerals
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naturally-occurring, inorganic solid, with a definite chemical composition and an ordered internal source
Mineral
General Characteristics of a Mineral
Naturally-occurring Inorganic Solid Definite Chemical Composition Ordered internal structure
the appearance of light reflected from a mineral surface.
Luster
measurement of the strength of the chemical bonds in its structure
Hardness
not a reliable feature for identifying minerals because it can be altered by chemical impurities within its structure
Color and Streak
composed primarily of silicon-oxygen tetrahedrons
Silicates
the tendency of a mineral to break along planes of weakness is known as cleavage.
Cleavage and Fracture
consists of a single metal such as copper and gold
Native metals
composed of a halogen ion such as chlorine or fluorine which forms halite or rock salt
Halides
Specific gravity is the measure of the density of a mineral
Density
characterized by the presence of carbonic ion
Carbonates
consists of metal cations bonded to oxygen anions
Oxides
consists of metal cation bonded to sulfide
Sulfides
substances that fulfill all the requirements but do not have an ordered internal structure
Mineraloids
consists of a metal cation bonded to the SO2 anionic group. They usually precipitate out of water near Earth’s surface
Sulfate
outward appearance of the mineral’s crystal form
Habit
a definite structure which crystallizes
Crystal Form
dependent on the chemical composition of the mineral
Crystal Structure