EVERYDAY SCIENCE

Detailed explanation-1: -Metamorphic rocks are often squished, smeared out, and folded. Despite these uncomfortable conditions, metamorphic rocks do not get hot enough to melt, or they would become igneous rocks! Common Metamorphic Rocks: Common metamorphic rocks include phyllite, schist, gneiss, quartzite and marble.

Detailed explanation-2: -Foliated metamorphic rocks such as gneiss, phyllite, schist and slate have a layered or banded appearance that is produced by exposure to heat and directed pressure. Non-foliated metamorphic rocks such as hornfels, marble, quartzite and novaculite do not have a layered or banded appearance.

Detailed explanation-3: -The various types of foliated metamorphic rocks, listed in order of the grade or intensity of metamorphism and the type of foliation are slate, phyllite, schist, and gneiss (Figure 7.8).

Detailed explanation-4: -The best known and most commonly seen metamorphic rocks are those produced by Barrovian (also called regional) metamorphism. Beginning with a shale parent, Barrovian metamorphism produces a sequence of metamorphic rocks that goes through slate, and then through phyllite, schist, and gneiss.

Detailed explanation-5: -Some examples of metamorphic rocks are gneiss, slate, marble, schist, and quartzite.