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Made of small grains of sand
Sandstone
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As the rock is exposed to () and/or () the individual mineral grains recrystallize.
Grains are much larger Quartzite
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There are 2 types of metamorphism that occur.
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() metamorphism Lava Contact Metamorphism Magma Contact Metamorphism
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Contact metamorphism Intrusive Igneous Rock Metamorphic Rock
Extrusive Igneous Rock Metamorphic Rock Intrusive Igneous Rock Metamorphic Rock
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Contact Metamorphism – () the () rocks
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What is parent rock you ask…
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Lets take a look. Side Note
All metamorphic rocks come from () in a () rock. The parent rock is the original rock the metamorphic rock came from. Lets take a look.
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Parent Rock
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Contact metamorphism Parent rock Metamorphic rock
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Parent Rock
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Contact metamorphism Parent rock Metamorphic rock
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Parent Rock It doesn’t say, but what sedimentary rock do you think is the parent rock?
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conglomerate Metaconglomerate Parent rock Metamorphic rock
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The 2nd type of metamorphism that occurs.
2. () metamorphism – heat and pressure combine to alter () over a large area. These rocks get changed when () plates collide. The () the rock is to the plate boundaries the more the rock gets changed.
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Differential stress Regional metamorphism can create mountains!!!
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Folded rock caused by plate tectonics
Regional Metamorphism (large area)
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Folded rock caused by plate tectonics
Regional Metamorphism (large area)
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What is the parent rock???
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Foliation
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Rock type and depth of burial
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() regional metamorphism (high heat and pressure) () the minerals in a rock. This flattens and () the minerals. Foliated – flattened and aligned minerals. () rocks split easily along the flattened, aligned mineral layers. Lets see what foliation looks like…
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The minerals normally line up perpendicular to the direction of the pressure.
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When the minerals are () into light and dark mineral layers it is called ()
Nice!!! oops… Gneiss!!!
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One more thing… Since metamorphic rocks are formed under such () what do think happens to their ()?
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() metamorphism – just () that changes rock
Summing it all up () metamorphism – just () that changes rock Regional ()– heat and () change rock
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Metamorphic Rock Identification
Reference tables page 7 Metamorphic Rock Identification Lets check out the properties of metamorphic rocks.
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What it looks like
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How big the mineral grains are
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What minerals are in the rock
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Is it formed by regional or contact metamorphism
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Important information
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Umm, rock names
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How the rock may be shown on a map
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Lets try to figure out a mystery metamorphic rock.
Observed properties: 1. The texture is foliated, minerals are aligned but not banded. 2. The grains are fine to medium sized. 3. Contains, mica, quartz, feldspar, amphibole, garnet and pyroxene.
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1. The minerals are aligned but not banded.
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2. The grains are fine to medium sized.
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3. Contains, mica, quartz, feldspar, amphibole, garnet and pyroxene.
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Through which rock do all the properties match?
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Our mystery rock is… Yup, it is Schist.
We can figure out information about any metamorphic rock with the E.S.R.T.
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