Regional Metamorphism: This type occurs over a large area and is associated with tectonic processes such as mountain building and plate collisions. It results in the formation of foliated rocks like slate, schist, and gneiss.
Contact Metamorphism: This type occurs when rocks are in contact with magma, leading to localized changes in the rock due to the high temperatures. It often results in the formation of non-foliated rocks like marble and quartzite.
Factors Affecting Metamorphism
The process of metamorphism is influenced by several factors:
Chemical Fluids: The presence of fluids such as water and dissolved ions can aid in the exchange of elements between minerals, leading to the formation of new minerals.
Time: The longer the rocks are subjected to metamorphic conditions, the more pronounced the changes will be.
The student demonstrates an understanding of geochemical cycles by describing that most smaller rocks come from the breaking and weathering of larger rocks as part of the rock cycle.
The student demonstrates an understanding of geochemical cycles by recognizing the physical properties of water as they relate to the rock cycle.