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Metamorphic Rocks

 


Metamorphic Rocks

    The metamorphic rocks are formed by the alteration of the pre-existing rocks, which had undergone a change due to high temperature or pressure or the action of chemical agents give rise to metamorphic rock. The petrological section in the Geology Gallery housed in the main hall includes metamorphic rock case.

    The important features of metamorphic rocks are

-- Generally they have hard interlocking grains.

-- Fossils are rarely preserved in rocks of sedimentary origin.

-- Andalusite, kyanite, sillimanite and garnet are the common minerals.

The important metamorphic rocks such as  mica schist, amphibolite, slate, chlorite schist and marble are on display.

   

 

 

Mica Schist

    It is comprised of finely granular and colourless quartz and muscovite. This specimen was collected from Wyanad.

 

Mica Schist

Amphibolite

 

Amphibolite

    It is a dark grey, medium grained granular rock. It is comprised of pale yellowish green plagioclase and dark glistening grains of hornblende.

 

Slate

    It is a dark grey compact rock displaying fine slaty cleavage. It has a concoidal fracture and gives an earthy odour on breathing upon it.

Slate

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