Chapter 03B: Rocks Flashcards
Rocks
Aggregate of one or more minerals
Rock types
Igneous
Sedimentary
Metamorphic
Igneous rocks
Minerals with the highest melting point crystalize first
Made from magma and lava/extremely high heat and pressure
Magma
Subsurface melted rock
Lava
Surface melted rock
Intrusive
Forming of a rock below the surface
Associated with slow cooling and coarse grain, crystals
Extrusive
Forming of rock above the surface
Associated with rapid cooling and fine grain, lack of visible crystals
Aphanitic
Fine-grained texture of igneous rocks formed extrusively (rapid cooling)
Phaneritic
Coarse-grained texture of igneous rocks formed intrusively (slow cooling)
Porphyritic
Coarse-grained texture within a fine-grained matrix of igneous rocks formed both intrusively and extrusively (slow and rapid cooling)
Vesicular
Igneous rocks with cavities (vesicles) formed from escaping gas bubbles formed extrusively (rapid cooling)
Glassy
Very fine-grained texture of igneous rocks formed extrusively (very rapid cooling) – few or no crystals (microscopic)
Pegmatitic
Very coarse-grained texture of igneous rocks formed intrusively (very slow cooling)
Pyroclastic (fragmental)
Igneous rocks formed from compaction of volcanic ash and explosive debris.
Mafic
Igneous rock color with mostly dark colored minerals
Intermediate
Igneous rock with mixture of light and dark minerals
Felsic
Igneous rock with mostly light colored minerals
Sedimentary rocks
Rocks formed from pre-existing rocks that were weathered and eroded down to sediments, transported, deposited, and lithified into sedimentary rocks
Often contain void spaces that hold/transport water and petroleum
Raw materials for glass, concrete, sheetrock
Physical weathering
The breaking apart of rocks without changing their chemica composition
E.g. frost wedging, plant roots
Chemical weathering
Breaking down of rocks by chemical means and changing its chemical composition
E.g. dissolution, hydrolysis, redox
Lithification
The compaction and cementation of sediment
Detrital/Clastic rocks
Sedimentary rocks formed from mechanical weathering debris.
Chemical rocks
Sedimentary rocks that are made chemically or biochemically, i.e. through a means like dissolution or excretion (by organisms)
E.g. limestone, rock salt
Metamorphic rocks
Rocks created from pre-existing rocks that are altered with heat and pressure, but no melting
Contact metamorphism
Heat, low pressure
Nonfoliated texture (eg. marble, quartzite)
Regional metamorphism
Heat, high pressure
Foliated texture (e.g. slate, gneiss)
Cementation glues (sedimentary rocks) (3)
Silica
Iron oxide
Calcite