Naturally-occurring, inorganic, homogeneous solid, with a definite chemical composition, and ordered internal structure
Mnemonic for mineral properties: N-I-H-D-O
Inorganic
Must not be composed of the complex hydrocarbon molecules that are the basis of life-forms
Naturally-occurring
A mineral must form through natural geologic processes
Crystalline solid
The atoms that make up the mineral are arranged in an orderly, repeating, three-dimensional pattern
Definite chemical composition
Definite chemical formula
Physical properties of minerals
Color
Streak
Luster
Hardness
Cleavage
Fracture
Odor
Taste
Magnetism
Hardness
The ability of a mineral to resist scratching or abrasion
Cleavage
The ability to break, when struck/split, along preferred planal directions
Fracture
The rough and irregular breakage of a mineral
Ore minerals
Metallic and some nonmetallic minerals which contain useful substances that can be mined for a profit
Minerals
Naturally-occurring, inorganic, crystalline solid that has a specific chemical composition
Rocks
Naturally-formed aggregates of minerals or mineral-like substances
Types of rocks
Igneous
Sedimentary
Metamorphic
Igneous rocks
Formed when magma or lava cools and solidifies
The study of igneous rocks provides us with an insight into the composition of Earth's mantle and the processes that cause it to melt
Types of igneous rocks
Extrusive
Intrusive
Extrusive igneous rocks
Formed when magma solidifies at the surface
Intrusive igneous rocks
Formed when magma solidifies beneath the surface
Igneous rock classification
Intrusive/Plutonic
Extrusive/Volcanic
Pyroclastic
Intrusive/Plutonic igneous rocks
Coarse-grained igneous rocks formed when magma solidifies far below the surface so that the cooling was slow enough to enable the large crystals to grow
Extrusive/Volcanic igneous rocks
Fine-grained igneous rocks formed when magma solidifies at or near the surface so that the cooling is rather rapid; there is little time for crystals to form, so extrusive igneous rocks have tiny crystals
Pyroclastic igneous rocks
Rocks formed from pieces of other rocks, animal/plant remains, or minerals
Pyroclastic igneous rock examples
Scoria
Pumice
Tuff
Obsidian
Conditions for magma formation
Increase in temperature
Decrease in pressure
Addition of volatiles
Sedimentary rocks
Rocks that were formed from weathered and eroded remains of preexisting rocks, precipitation from solutions, or animal/plant remains
Lithification
General term for the processes that convert loose sediments into sedimentary rocks, including compaction, cementation, and crystallization
Types of sedimentary rocks
Detrital
Chemical
Organic
Detrital sedimentary rocks
Formed from weathered and eroded remains of preexisting rocks
Chemical sedimentary rocks
Deposited by precipitation of minerals from a solution
Organic sedimentary rocks
Composed of organic molecules (Carbon)
Metamorphic rocks
Rocks that were formed from exposure to extreme heat and pressure in the crust
Types of metamorphism
Contact
Regional
Contact metamorphism
Involves existing rocks coming into contact with intense heat
Regional metamorphism
Occurs when rocks are buried deep in the crust, commonly associated with convergent plate boundaries and the formation of mountain ranges
Classification of metamorphic rocks
Foliated
Non-foliated
Foliated metamorphic rocks
Have a layered or banded appearance due to exposure to heat and direct pressure
Non-foliated metamorphic rocks
Do not possess a layered or banded appearance, and minerals are not preferentially-aligned
Rock cycle
Shows the interrelationship between igneous, sedimentary, and metamorphic rocks, and how rocks move from deep to shallow, and from high to low temperatures and pressures, in response to tectonic forces and isostasy
Weathering
The process that changes the physical and chemical character of a rock at or near the surface