Foliated metamorphic gneiss. Regional metamorphism—occurs when great masses of rock change over a wide area due to pressure exerted on rocks at plate boundaries. Plutonic Metamorphism 6. The three main types of metamorphism are: Regional Metamorphism. Contact Metamorphism. A rock is squeezed under directed pressure during metamorphism it is likely to be deformed, and this can result in a textural change such that the minerals are elongated in the direction perpendicular to the main stress. Hydrothermal metamorphism. Nearly all traces of the original structures (including fossils) and fabric (such as layering and ripple marks) are wiped out as the minerals migrate and recrystallize. This involves development of large-scale changes in the structural and chemical constitution of the pre-existing rocks under the combined action of pressure, temperature and fluids. What type of metamorphism would a rock at location A be subjected to? Burial Metamorphism 5. Conditions producing widespread regionally metamorphosed rocks occur during an orogenic event. Regional Regional or Barrovian metamorphism covers large areas of continental crust typically associated with mountain ranges, particularly those associated with convergent tectonic plates or the roots of previously eroded mountains. Impact Metamorphism. Regional metamorphism is associated with the major events of Earth dynamics, and the vast majority of metamorphic rocks are so produced.They are the rocks involved in the cyclic processes of erosion, sedimentation, burial, metamorphism, and mountain building (), events that are all related to major convective processes in Earth’s mantle. Foliated Metamorphic Rocks . Regional metamorphism includes any metamorphic process that occurs over a large region. Type # 1. The collision of twocontinental … Regional Metamorphism 4. This is also referred as REGIONAL METAMORPHISM and may be considered as the most important as well as prevalent type of metamorphic processes. Which type of metamorphism is most likely produced in this environment? As already noted, slate is formed from the low-grade metamorphism of shale, and has microscopic clay and mica crystals that have grown perpendicular to the stress. Contact or Thermal Metamorphism: This type of metamorphism takes place when the very hot magma moves up through the crystal rocks and brings with it high levels of heat. This type of metamorphic was created by regional metamorphism, in which a sedimentary or igneous rock has been deeply buried and subjected to high temperatures and pressures. Types of Metamorphism: Regional Associated with Mountain buildings Also known as Dynamothermal - produces both foliated and non-foliated metamorphic rocks. Regional metamorphism. Regional Metamorphism: A type of metamorphism that affects an extensive region, as opposed to local metamorphism that is effective only in a relatively restricted area. 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). It is therefore the most widespread and common type of metamorphism. This type of metamorphism occurs with rocks that are buried deep down the Earth’s crust. Regional metamorphism is a type of metamorphism where the formation of a metamorphic rock occurs in a wide area. What is Regional Metamorphism. There are two main types of metamorphism: Contact metamorphism—occurs when magma contacts a rock, changing it by extreme heat (Figure 4.14). dynamothermal or regional metamorphism. NPS photo by Tim Connors. 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