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Igneous
Rocks formed from cooled magmaÂ
Intrusive
Igneous rock forced into voids inside the Earth
Extrusive
Igneous rock reaching the Earth’s surface before cooling and solidifying
Sedimentary
Rock formed from cementation and compaction of previously weathered rock fragments
Cementation
New minerals stick those grains of sediment together
Compaction
Sediments under pressure have grains squeezed tightly together
Metamorphic
Rock formed from a different type of rock through heat and pressure
Soil
A mixture of weathered rock. Soil consists of rocks, sand, silt, and clay with decaying organic matter
Permeability
How easily water passes through soil
Porosity
The measure of empty space in a material
Bedding
Pattern of layered levels of rock
Weathering
the process that breaks down rock
Mechanical Weathering
Rocks are broken apart by physical process. The overall chemical makeup of the rock stays the same. Each piece of characteristics similar to the original rock.
Chemical Weathering
Changes the chemical composition
Deposition
The agents of erosion lay sediment down
Erosion
Transport of weathered rock material