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LO.6 Geology G10

          

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 We have in LO.6 Geology G10

First: the Concepts

A) Changes in temperature, pressure, or composition in Earth's subsurface can change the texture
and mineral composition of pre-existing rocks, creating metamorphic rocks.

 B) Deformation during metamorphism produces foliated textures and may destroy original textures.

 C) Deformation (change in shape) and stresses (distribution of forces) are related, but maximum
deformation and maximum stress are not always parallel.

 D) The metamorphic texture and mineralogy observed in metamorphic rocks are most commonly
related to the conditions when the rock experienced its maximum temperature.

Second: the References

Earth comm: Ch.3 sec.4
      
Third: the Videos links



Fourth: Skills

A) Identifying and differentiating slate, phyllite, schist, gneiss, hornfels, marble, and quartzite in
hand specimens and outcrops according to texture and mineral composition.

 B) Using microscopic scale features to interpret and classify different types of metamorphic rocks.

 C) Using metamorphic rock texture to infer the presence or absence of deformation at the time of
metamorphism

 D) Interpreting geological maps that describe the geology of Egypt.

Fifth: the materials as PPT., DOCX., and PDF
 
In the Drive from this link

To go the first site, just click the back bottom in your phone


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