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Rocks

AB
Chemical Sedimentary RockSedimentary rocks that are created from the dissolved substances and they precipitate back into the soil.
Coarse-grained textureHas crystals that are large and easy to see, most crystals are roughly the same size. These are usually formed underneath the Earth’s surface.
Contact MetamorphismResults when rocks form near large plums of magma that increases the heat applied to each rock.
CrystallizationThe process where magma cools and solidifies, either below or at a volcanic eruption at the surface.
Detrital Sedimentary RocksSedimentary rocks that are formed for the weathering of different rocks and then reformed.
Disseminated DepositA deposit of metallic ions that are distributed in minute masses throughout an entire rock mass.
Evaporate DepositFormed from the evaporation of water leaving minerals that solidify into different minerals.
Extrusive (volcanic)Igneous rocks that are formed because of a volcanic explosion.
Fine-grained TextureHas crystals that cannot be seen with out the unaided eye usually cooled quickly.
Foliated TextureMetamorphic rock that contains rock layers that are banded.
Glassy TextureThe result of very rapid cooling of magma.
Hydrothermal SolutionCreated when hot, metal rich fluids containing metallic ions settle near the top of a magma chamber.
Igneous RockResult from the crystallization of magma beneath the earths surface or in volcanic eruptions.
Intrusive (plutonic)Igneous rocks that are formed below the Earth’s surface and are can be seen as overlying layers are striped away.
LavaMagma that has reached the surface and lost its gaseous components.
LithificationTerm meaning “conversion into rock.”
MagmaMolten material that forms inside Earth.
Metamorphic RockRocks that created after being buried deep into the Earth’s surface and have intense heats and pressures applied.
Non-FoliatedMetamorphic rocks that contain all of one mineral and are essentially a single crystal.
Porphyritic TextureHave some crystals which are much larger while other are much smaller and fine grain.
Regional MetamorphismUsually the result of mountain building where there are high scale deformations and high heat applied.
Rock CycleAllow s us to view many of the interrelationships among different parts of the Earth’s system.
SedimentThe deposition of rock materials that are weathered in either ocean, swamps, floodplains, or rivers.
Sedimentary RockCreated when sediment layers are compacted because of weight above and minerals fill in the pores spaces between with minerals.
Strata (beds)Different layers of sediment that are laid down on top of one another.
TextureDescribes the overall appearance of an igneous rock, based on the size and arrangement of its interlocking crystals.
Vein DepositsWhere fluids of rocks move between small cracks and leave behind metallic ions.
WeatheringThe day to day forces that decompose rocks into their constituent parts.


Middle School Science Teacher
Clinton/Graceville/Beardsley Middle School
Beardsley, MN

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