Rocks Flashcards
What is a concept used to explain how the three basic rock types are related and how Earth processes, over geologic time, change a rock from one type into another.
ROCK CYCLE
What is an aggregate of minerals ?
ROCK
What are the three types of rocks?
Igneous
Sedimentary
Metamorphic
is any crystalline or glassy rock that forms from cooling of a magma.
Igneous rocks
Crystallized below the surface of the earth
texture: coarse-grained
Plutonic rocks
Granite
Igneous - plutonic
Diorite
Igneous - plutonic
Crystallized on the surface of the earth
texture: fine-grained
Vulcanic
Rhyolite
IGNEOUS - Vulcanic
Andesite
Igneous - vulcanic
Basalt
Igneous - Vulcanic
rocks that form near the surface of the earth through chemical precipitation from water or by cementation of loose fragments
Sedimentary
Breaking down of rocks to sediments
WEATHERING
Compaction and cementation of sediments to rocks
LITHIFICATION
causes the disintegration of rock to smaller fragments
Weathering
disintegration of rocks and minerals by a physical or mechanical process.
Physical Weathering
decomposition of rocks and minerals.
Chemical weathering
Classified on particle size
The presence of variable grain sizes is indicative of sedimentary differentiation which is actually a function of processes happening in different sedimentary environment.
CLASTICS
Conglomerate
Sedimentary - clastic
Breccia
Sedimentary - Clastic
Sandstone
Sedimentary - clastics
High quartz percent in composition
Arenities
Composed mainly clay minerals
Argillities
Formed through evaporation and precipitation
Non clastics
Evaporites (halite, gypsum dolostone)
Sedimentary - Non clastics
Precipates (limestone
Sedimentary - Non clastics
Bioclastic (coal)
Sedimentary - non clastics
form as a result of increasing the pressure and/or temperature on a previously existing rock to form a new rock.
Metamorphic rocks
Refers to the changes in mineral assemblage and texture.
Methamorphism
What are the agents of methamorphism
Heat, pressure and chemically active fluids
Heat and chemically-active fluid as agents
Creates non-foliated metamorphic rocks
Contact methamorphism
Hornfeels
Methamorphic - Contact methamorphism
Marble
Methamorphic - contact methamorphism
There are no alignment or layering of minerals.
Non- foliated rocks
Pressure as agent
Creates foliated metamorphic rocks
Occurs at regional scale
Regional metamorphism
There are visible alignment or layering of minerals.
Foliated rocks
Shale
Methamorphic - foliated rocks
Slate
Methamorphic - foliated
Phyllite
Metamorphic - foliated
Schist
Methamorphic - foliated
Gnesis
Methamorphic - foliated
Cooling and crystallization of magma
Igneous
Lithification of sediments
Sedimentary
Application of heat, pressure & fluids
Methamorphic