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Metamorphic Rocks Metamorphic means “change in form”. Metamorphic rocks form from the chemical and physical alterations of pre-existing igneous or sedimentary rocks. This is done by subjecting these rocks to conditions of great heat and pressure and chemical activity. Main effects upon rocks • The heat, pressure and chemical activity will effect the metamorphic rock’s: 1. Mineralogy – a new mineralogy will form 2. Texture – the rock texture will alter. Classification of Metamorphic rocks • There are two classes of metamorphic rocks. • Contact (thermal) – these form when an igneous intrusions are injected into the crust. Heat from the magma metamorphoses (changes) the surrounding rock forming a new metamorphic rock • Regional Metamorphic Rocks – these rocks form over millions of years and many thousands of meters of sediments accumulated in the ocean basins. The overlying weight causes the sediments to lithify and eventually metamorphose. • Example shale metamorphoses into slate Agents of Metamorphism •The agents of change for metamorphic rocks are: •Heat, pressure and chemical activity Identification clue These rocks are difficult to identify because remember they used to be another kind of rock but because of high heat and pressure they look bent, twisted, tortured and or cooked. They tend to be dense and very hard. They some times show banding like when a granite metamorphoses to gneiss. Identification clue • Sometimes the flat minerals like mica all line up parallel to each other due to extreme pressure. This is called schistosity and the rock is called a schist. Identification Clue • Metamorphic Rocks are: •“Fubars” • That is they are: fouled up beyond all recognition