Chapter 5 and 6 rocks

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RacheleLaurenMiller  on April 7, 2012

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Earth Science

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Chapter 5 and 6 rocks

3 types of rocks
igneous, sedimentary, metamorphic
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3 types of rocks igneous, sedimentary, metamorphic
extrusive (igneous) fine grained due to rapid cooling examples pumice and obsidian
intrusive (igneous) coarse grained due to slow cooling below the surface example: granite
magma mix of molten rock,gases,mineral cyrstals most common elements in earths crust are also included in this (SiO2) heated to 800-1200 degrees celcius
rhyolitic magma 70% SiO2 lightest in color thick and viscous exploes only after pressure build up
andesitic magma 60% SiO2 moderate in color
basaltic magma 50% SiO2 darkest in color very fluid flow from volcanoes
partial melting the process by which different minerals in rock melt at different temperatures
felsic rocks rhyolitic magma, high in silica, light in color, high in quartz and feldspar
intermediate rocks andesitic magma, moderate silica, moderate color
mafic rocks basaltic magma, low in silica, dark in color, contains iron magnessium pyroxene and olivene
porphyritic texture fine and coarse due to it being in differnet parts of the earth leading to different sizes of grains
obsidian black glass no cyrstals extrusive rock
pumice 50% holes due to trapped gas rhyolitic magma floats
uses buliding materials
weathering The breaking down of rocks and other materials on the Earth's surface.
physical or mechanical weathering Physical weathering (also known as mechanical weathering) breaks rocks down into smaller pieces without changing their chemical composition.
chemical weathering the process by which rocks break down as a result of chemical reactions
erosion The process by which wind, water, ice, or gravity transports soil and sediment from one location to another
deposition the natural process of laying down a deposit of something
burial covered by other sediments
lithification The process that converts sediments into solid rock by compaction or cementation.
compaction The process by which sediments are pressed together under their own weight.
cementation The process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock.
layers of rocks oldest on bottom newest on top
fossils often in rocks and show about past
clastic rocks formed from particles of rock produced by weathering and erosion of previously existing rock [from compaction or cementation] classified by coarse medium or fine grained
organic rocks sedimentary rocks formed from the remains of plants and animals settle to bottom in ocean and mix with other remains
chemical rocks form when minerals are precipitated from a solution or left behind when a solution evaporates
ripple marks the recorded motion of wind or water in sedimentary rock same marks on both side mean ocean or lake on one side is river or stream
metamorphic rocks formed from preexisting rock subjected to heat and pressure (rock is solid, but minerals break down, form, change shape)
foliated Term used to describe metamorphic rocks whose grains are arranged in parallel layers or bands.
non-foliated the metamorphic rock texture in which mineral grains are not arranged in planes or bands.
rock cycle continual remaking of rocks and change into different rocks at anytime

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