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Rocks

Terms

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magma
molten rock located below the surface of earth (heat, pressure released, fluids will enter into rock)
organic sedimentary rock
when sea shells, skeletal remains are cemented togeather
metamorphic rock
undergo a change in their structure
deposition
sediments building up into thick layers
regional metamorphosis
weight over lying rock layers cause increase in pressure and heat
chemical weathering
caused by oxygenation hydrolysis and carbonation
intermediate
mixture of felsic and mafic (dirite)
contact metamorphosis
rock comes in contact with magma, does not melt but heat and pressure cause the rock to change
batholiths
huge pools of magma in crust of earth
ultramafic
low in silica (basalt)
laccoloths
dome shaped intrusive formations that form like sills does but the center of it bulges upward
igneous rock
form when magma or lava cools and hardens
plutons
balloon shaped, dome like igneous formations
fast cooling
small grains
lava
molten rock spilling on the surface of the earth
Rock
solid mixture of crystals compsoed of one or more minerals
compaction or cementation
sediments are squeezed and solidified into sedimentary rock
dykes
vertical, wall like intrusive formations form when magma fills vertical cracks, cools, and hardens
causes of erosion
gravity, running water, wind, ocean weaves, glaciers
felsic
high in silica, light in color (rhyolite)
sills
large ,flat intrusive formations form when magma fills between rock formations
volcanic neck
remnants of magma left behind after the cone of the volcano has been eroded away
mechanical weathering
caused by wedging root pry and temperature
slow cooling
large grains
mafic
high in maagnesium and iron, low in silica, dark in color (obsidian)
non foliated
have no layers in texture
chemical sedimentary rock
when sediments are cemented togeather by chemicals dissolved in water
Factors of weathering
climate(hot fast, cold slow), surface area of rock (large fast, small slow) chemical compositions, pollution
foliated
have layers in texture
erosion
transportation of sediments
weathering
rocks broken down into smaller pieces
clastic sedimentary rock
form when different size sediments are compacted togeather

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