Answer:
There are two fundamental sorts of transformative rocks. Foliated changeable shakes, for example, gneiss, phyllite, schist, and record have a layered or united appearance that is created by presentation to warm and coordinated weight.
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Transformative rocks have been changed after some time by extraordinary weight and warmth.
Changeable rocks can be framed by pressure profound under the World's surface, from the outrageous warmth brought about by magma or by the extraordinary impacts and erosion of structural plates.
Inspire and disintegration help carry changeable shake to the World's surface. Instances of changeable rocks incorporate anthracite, quartzite, marble record, granulite, gneiss and schist. Anthracite is a sort of coal with a high carbon tally, barely any debasements and with a high radiance (which means it looks sparkling). Marble is a changeable shake that is framed from the sedimentary shake limestone. Quartzite is a changeable shake that is framed from the sedimentary shake sandstone. Record is a changeable shake that is shaped from the sedimentary shake mudstone. Granulite is a changeable shake that is shaped from the volcanic shake basalt.
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