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Metamorphic Rocks

Published on Mar 30, 2017

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PRESENTATION OUTLINE

Metamorphic Rocks

meta - many and morph - to change
Photo by Ron Schott

Kinda like these guys...

Power rangers...morph!

How and where are they formed?

  • DEEP in earth's crust
  • Formed by extreme heat and pressure

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

Two types of MR

  • foliated - bands of minerals line up (kinda like striping)
  • Non-foliated - minerals not arranged in lines
Photo by jimmypk218

Foliated rock

check out the mineral bands

Non-foliated rock

No bands 

Due to slow cooling deep in earth's crust, metamorphic rocks will often have large crystals

Photo by Ruth and Dave

Why are metamorphic rocks

formed near plate boundaries?
Photo by Jesse Varner

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

Metamorphic Rock Examples

  • Marble
  • Gneiss
  • Schist
  • Slate
Photo by Luke Peterson

The Parent Rock

The trail that leads to each rock

Gneiss

  • shale (SR)
  • slate (MR)
  • phyllite (MR)
  • schist (MR)
Photo by Rubem Jr

Slate

  • shale (SR)
Photo by Mitchell Luo

Schist

  • shale (SR)
  • slate (MR)
  • phyllite (MR)
Photo by brewbooks

Marble

  • limestone (SR)
Photo by kiwanee2001