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cementation
The process by which dissolved minerals crystallize and glue particles of sediment together into one mass.
cleavage
A mineral's ability to split easily along flat surfaces.
compaction
the process by which sediments are pressed together under their own weight
crystallization
The process by which atoms are arranged to form a material with a crystal structure
deposition
Process in which sediment is laid down in new locations.
extrusive rock
Igneous rock that forms from lava on Earth's surface
fracture
The way a mineral looks when it breaks apart in an irregular way
granite
A usually light colored igneous rock that is found in continental crust
igneous rock
a type of rock that forms from the cooling of molten rock at or below the surface
inorganic
Not formed from living things or the remains of living things
intrusive rock
Igneous rock that forms when magma hardens beneath Earth's surface.
luster
The way a mineral reflects light
metamorphic rock
A type of rock that forms from an existing rock that is changed by heat, pressure, or chemical reactions.
rock cycle
A series of processes on the surface and inside Earth that slowly changes rocks from one kind to another
weathering
The chemical and physical processes that break down rock and other substances.
crystal
solid in which the atoms are arranged in
an orderly, repeating pattern.
hardness
measure of how easily a mineral can be scratched.
mineral
a non-living material found naturally on earth, with definite chemical composition and a crystalline structure.
streak
color of a mineral when it is in powdered form.
erosion
the process in which sediment is carried away or moved from one place to another by water, wind, ice, or gravity.
Lava
molten rock that has erupted onto Earth's surface.
Magma
molten rock below Earth's surface.
Metamorphic rock
rock that is formed or changed when existing rocks are exposed to intense heat and pressure
Sediment
parts of rocks, shells, and dead organisms that have been worn down into small pieces
Sedimentary rock
rock that is formed when layers of sediment are deposited, compacted, and cemented over long periods of time
crystalline structure
atoms arranged in a repeating pattern which gives each mineral a specific and different internal structure
rocks
naturally formed solids that are made from one or more types of minerals
Mohs Hardness Scale
a scale from 1-10 that measures the hardness of minerals