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Ch 3 Geology: Rocks and the Rock Cycle

Matching, flash cards, and concentration for the vocaulary associated with Rocks and the Rock Cycle

AB
Classify RocksRocks are classified by their color, texture, and mineral composition
ColorDark (mafic) or Light (Felsic)
Texturethe size, shape, and pattern of a mineral's grains
Grainsthe particles of minerals or other rocks that make up a rock
fine-grainedgrains can be seen with magnification
coarse-grainedeasily discernable grains
No visible grainNo grain because the rock formed so quickly or formed from sediment particles too small to be seen
Rounded GrainConglomerate, often made up of weathered rockparticle, often from stream beds, held together by a finer grained groundmass
Jagged GrainBreccia, made up of unweathered rock particles, such as those from glacial abrasion
FoliatedBanded, like layers that have been compressed
Non-foliatednon banded, like a homogenous layer
Originhow a rock was formed: Igneous, Metamorphic, and Sedimentary
Igneous rockformed from the cooling of molten material
Sedimentary RockFormed when particles of other rocks and/or the remains of plants and animals are pressed and cemented together in layers below the surface
Metamorphic Rockformed when existing rock is changed by heat, pressure, or chemical reactions.
Classifying Igneous RockOrigin, texture, and mineral composition
Extrusive Igneous RockIgneous rock that formed on or near the Earth's surface. Fine or no grained, Basalt
Intrusive Igneous RockIgneous rock that formed deep below Earth's surface. Large or medium grained, Granite
Texture of Igneous rockdetermined by the size and shape of the mineral crystals in igneous rock
aphaneticfine grained
phanereticcoarse grained
porphyritica misture of fine and coarse gained (like the pores on your face)
silicathe mineral part of igneous rock that determines the viscosity of the molten material
High silicaHigh Viscosity (resistance to flow)
Low SilicaLow Viscosity (runny)
Sedimentsmall and solid pieces of material that has been weathered, eroded, and deposited. (can be mineral or organic)
ErosionDestructive forces that constantly break up and wear away Earth's surface
Depositionthe process by which sediment settles out of the fluid that carries it
compactionthe process that presses sediments tightly together
cementationthe process in which dissolved minerals crystallize and glue particles of sediment together
Groups of sedimentary rockclastic, organic, and chemical
clastic sedimentary rockformed when rock particles are squeezed together, shale, sandstone, conglomerate, and breccia
Organic Sedimentary Rockformed from the deposited remains of plants and animals, coal, limestone
Chemical Sedimentary Rockformed when minerals in a solution crystallize or when the solution evaporates, leaving behind the mineral
coral reefformed by millions of tiny coral animals in warm and shallow marine waters that live, die, and rebuild on the tiny skeletons of their ancestors
Limestone from coralcan be found in very high plateaus all over the world. This tells us that the area had long ago been under water
Classifying Metamorphic Rocksby the arrangement of the grains that make up the rock (foliated or non-foliated)
Rock CycleThe ever evolving process or rock being changed from one type to another

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