at convergent plate boundries
The most common type of metamorphism is regional metamorphism, which occurs over large areas typically associated with tectonic plate boundaries. This type of metamorphism involves high pressure and temperature conditions, leading to the formation of minerals like mica, quartz, and feldspar in rocks.
Contact metamorphism: The temperature of the intruding magma is most important as it affects the minerals in the surrounding rock. Regional metamorphism: Pressure from tectonic forces is most important as it influences the recrystallization of minerals over a large area. Hydrothermal metamorphism: The presence of hot, aqueous fluids is most important as it facilitates mineral alteration through chemical reactions.
Metamorphic rocks are formed by the process of extreme heat, pressure and other chemicals. Two types of metamorphism are dynamic which makes the pressure and extreme heat and thermal which is caused by the heat of magma from a volcanic eruption.
The most widely distributed metamorphic rock is schist. Schist forms from the metamorphism of rocks such as shale or slate, and it is characterized by its foliated texture composed of platy minerals like mica. Schist is found in many regions worldwide, occurring in areas where regional metamorphism has taken place.
Convergent plate boundary, because it is associated with plutonism. It is the result of the temperature increase from the intrusion into the surrounding country rock. More info: http://geology.csupomona.edu/alert/metamorphic/contact.htm http://en.wikipedia.org/wiki/Metamorphism http://geology.csupomona.edu/alert/metamorphic/contact.htm
regional metamorphism
Dynamic Metamorphism >.<
The most common type of metamorphism is regional metamorphism, which occurs over large areas typically associated with tectonic plate boundaries. This type of metamorphism involves high pressure and temperature conditions, leading to the formation of minerals like mica, quartz, and feldspar in rocks.
The two processes resulting from sedimentary into metamorphic rock are known as contact metamorphism and regional metamorphism. Regional metamorphism most notably involves two tectonic plates colliding, while contact metamorphism occurs due to the intrusion of magma.
Regional metamorphism occurs deep within the Earth's crust where high temperatures and pressures cause changes to the mineral composition and texture of rocks over large areas. This process is typically associated with the formation of mountain ranges and convergent plate boundaries.
Metamorphic rocks can occur in both small patches and wide regions, depending on the geological processes involved. Regional metamorphism typically occurs over wide regions as a result of large-scale tectonic forces, while contact metamorphism tends to occur in smaller, localized areas near igneous intrusions.
eight kilometers below the earth's surface
Contact metamorphism: The temperature of the intruding magma is most important as it affects the minerals in the surrounding rock. Regional metamorphism: Pressure from tectonic forces is most important as it influences the recrystallization of minerals over a large area. Hydrothermal metamorphism: The presence of hot, aqueous fluids is most important as it facilitates mineral alteration through chemical reactions.
Convergent boundary
Shale is the most likely sedimentary rock to be changed into slate during regional metamorphism. Shale is a fine-grained sedimentary rock composed of clay minerals, which are easily recrystallized under heat and pressure to form the dense, foliated texture characteristic of slate.
Metamorphic rocks are formed by the process of extreme heat, pressure and other chemicals. Two types of metamorphism are dynamic which makes the pressure and extreme heat and thermal which is caused by the heat of magma from a volcanic eruption.
in your house