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6.4 Metamorphic Rock Formation of Metamorphic Rocks • Metamorphism~ process by which heat, pressure, or chemical processes change one type of rock to another • Formed from existing rock • Type of rock that forms can indicate the conditions that were in place at the time of change • Two types: 1. Contact 2. Regional Contact Metamorphism • ~Change in the texture, structure, or chemical composition of rock due to contact with magma Regional Metamorphism • ~change in rock due to changes in temperature and pressure over a large area, generally as a result of tectonic forces Classification of Metamorphic Rocks • Classified by chemical composition and texture (foliated or nonfoliated) Foliated Rocks • ~texture in which mineral grains are arranged in planes or bands • Forms in two ways: 1. Extreme pressure may cause minerals to realign or regrow to form parallel bands 2. Occurs as minerals that have different compositions separate to produce a series of alternating dark and light bands • Example: shale to slate, slate to schist, gabbro to gneiss (parent rock listed first, metamorphic second) Nonfoliated Rocks • ~mineral grains are not arranged in planes or bands • Share one of two characteristics: 1. Original rock may contain grains of only one mineral 2. Original rock may contain grains that are round or square • Examples: sandstone to quartzite, limestone to marble