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Metamorphic Rocks
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Published on Mar 30, 2017
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1.
Metamorphic Rocks
meta - many and morph - to change
Photo by
Ron Schott
2.
Kinda like these guys...
Power rangers...morph!
Link to Video:
https://youtu.be/WqfUa1EYTuM
Play Video
3.
How and where are they formed?
DEEP in earth's crust
Formed by extreme heat and pressure
Photo by
Adventures of Pam & Frank
4.
Characteristics
Were once a SR, IR or even another MR
Still remain somewhat of a solid
Two types: foliated and non-foliated
Photo by
jimmypk218
5.
Two types of MR
foliated - bands of minerals line up (kinda like striping)
Non-foliated - minerals not arranged in lines
Photo by
jimmypk218
6.
Foliated rock
check out the mineral bands
Photo by
James St. John
7.
Non-foliated rock
No bands
Photo by
James St. John
8.
Due to slow cooling deep in earth's crust, metamorphic rocks will often have large crystals
Photo by
Ruth and Dave
9.
Why are metamorphic rocks
formed near plate boundaries?
Photo by
Jesse Varner
10.
They get buried to depths in the earth where there are high temps and lots of tectonic plate pressure so they soften and get SQUEEZED!
Photo by
jimmypk218
11.
Metamorphic Rock Examples
Marble
Gneiss
Schist
Slate
Photo by
Luke Peterson
12.
The Parent Rock
The trail that leads to each rock
Photo by
archer10 (Dennis)
13.
Gneiss
shale (SR)
slate (MR)
phyllite (MR)
schist (MR)
Photo by
Rubem Jr
14.
Slate
shale (SR)
Photo by
Mitchell Luo
15.
Schist
shale (SR)
slate (MR)
phyllite (MR)
Photo by
brewbooks
16.
Marble
limestone (SR)
Photo by
kiwanee2001
Tammy Hershey
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