Metamorphism
Metamorphism is the process by which rocks undergo a change in mineralogical composition, texture, or both, as a result of changes in temperature, pressure, or stress, or as a result of the action of chemical agents. This process occurs within the Earth's crust and mantle, typically at depths greater than 10 kilometers.
Types of Metamorphism
- Contact Metamorphism: This occurs when rocks are subjected to high temperatures and low pressures due to proximity to a heat source, such as a magma intrusion. The surrounding rocks are altered by the heat, but not by the pressure.
- Regional Metamorphism: This occurs over a large area and is associated with the intense deformation and high pressures that result from tectonic forces. It is commonly associated with mountain-building processes.
- Dynamic Metamorphism: This type of metamorphism occurs along fault zones and is the result of high pressure and shear stress. It often produces fault breccias and cataclasites.
- Hydrothermal Metamorphism: This occurs when hot, chemically active fluids alter the mineralogy and texture of rocks. It is commonly associated with volcanic activity and ore deposition.
Factors Affecting Metamorphism
The degree and type of metamorphism a rock undergoes are determined by several factors:
- Temperature: Higher temperatures generally lead to more extensive metamorphism. The presence of a heat source, such as magma, can cause localized metamorphism.
- Pressure: Increased pressure, typically associated with depth in the Earth's crust, can lead to the recrystallization of minerals and the development of new mineral assemblages.
- Fluids: The presence of chemically active fluids can enhance the rate of mineral reactions and the transport of ions, leading to alteration of the rock.
- Time: The longer a rock is subjected to metamorphic conditions, the more extensive the changes it will undergo.
Metamorphic Rocks
Metamorphic rocks are classified based on their texture and mineral composition. Common metamorphic rocks include:
- Slate: Formed from the metamorphism of shale, and has a fine-grained, foliated texture.
- Phyllite: Exhibits a glossy sheen and is often wavy or wrinkled in appearance due to the presence of mica minerals.
- Schist: Characterized by its medium to coarse-grained texture and often contains aligned mica minerals, giving it a shiny appearance.
- Gneiss: Exhibits a banded appearance due to the segregation of light and dark minerals, often forming distinct layers.
- Marble: Forms from the metamorphism of limestone or dolostone and typically has a crystalline texture with interlocking calcite or dolomite crystals.
- Quartzite: Derived from the metamorphism of quartz sandstone and is characterized by its granular texture and high quartz content.
Study Guide
To effectively study the topic of metamorphism, consider the following key points:
- Understand the processes and conditions that lead to metamorphism, including temperature, pressure, and chemical reactions.
- Learn to recognize and differentiate between the various types of metamorphism, such as contact, regional, dynamic, and hydrothermal.
- Be able to identify common metamorphic rocks and understand their characteristics, textures, and origins.
- Explore the geological settings in which metamorphism occurs, such as subduction zones, mountain ranges, and fault zones.
- Study the economic significance of metamorphic processes, particularly in relation to the formation of valuable mineral deposits.
By mastering these concepts and key points, you will develop a comprehensive understanding of the fascinating processes and outcomes of metamorphism.
[Metamorphism] Related Worksheets and Study Guides:
.◂Physics Worksheets and Study Guides High School. Heat
The resources above cover the following skills:
PHYSICAL SCIENCE (NGSS)
Energy
Students who demonstrate understanding can:
Create a computational model to calculate the change in the energy of one component in a system when the change in energy of the other component(s) and energy flows in and out of the system are known.
Develop and use models to illustrate that energy at the macroscopic scale can be accounted for as either motions of particles or energy stored in fields.