By exposure to heat and/or pressure through depth of burial, directed pressure, or proximity to a magma source. Existing minerals can recrystallize, non-hydrous minerals can replace hydrous minerals, new minerals can be formed from the introduction of new ions from heated solutions, and minerals can become flattened and aligned in parallel layers.
foliated
The alignment of minerals into bands (foliation) is caused by the massive force of pressure and high temperature which results from mountain building processes caused by plate collisions. The heat and pressure combine to realign the existing minerals from a random orientation to one of parallel orientation, thus creating the visible lines or platy cleavages found in foliated metamorphic rocks. The lines of foliation are created perpendicularly to the force being applied.
A fossil is the prehistoric remains of a plant or animal. After an animal or plant dies, it may be buried under many layers of mud, sand, or rock, and under intense pressure a replica of that animal or plant is formed from minerals.
Yes, and it looks very gneiss.
Gneiss is a foliated metamorphic rock, meaning it has visible layers or bands of different minerals. These layers are formed due to the intense pressure and temperature conditions that gneiss undergoes during the metamorphic process.
i think they all are in the earth and are all layers and have minerals and are hot and have pressure
i think they all are in the earth and are all layers and have minerals and are hot and have pressure
The condition that produces distinct layers of flat and elongated minerals in foliated metamorphic rocks is directed pressure, which causes the minerals to align perpendicular to the direction of pressure. This pressure helps give the rock its characteristic layered structure, known as foliation.
The segregation of light and dark colored minerals into thin layers or bands is known as foliation. This occurs during the process of metamorphism, where the minerals align in parallel layers due to the deformation and recrystallization of the rock under intense pressure and temperature conditions. Foliation gives the rock a banded appearance and can indicate the direction of pressure during its formation.
The direction of stress applied can affect the alignment of minerals in a metamorphic rock. When stress is applied in a particular direction, minerals tend to align perpendicular to the direction of stress, resulting in foliation if the rock undergoes sufficient pressure. This alignment can create layers of minerals within the rock, giving it a distinct texture and cleavage.
By exposure to heat and/or pressure through depth of burial, directed pressure, or proximity to a magma source. Existing minerals can recrystallize, non-hydrous minerals can replace hydrous minerals, new minerals can be formed from the introduction of new ions from heated solutions, and minerals can become flattened and aligned in parallel layers.
By exposure to heat and/or pressure through depth of burial, directed pressure, or proximity to a magma source. Existing minerals can recrystallize, non-hydrous minerals can replace hydrous minerals, new minerals can be formed from the introduction of new ions from heated solutions, and minerals can become flattened and aligned in parallel layers.
By exposure to heat and/or pressure through depth of burial, directed pressure, or proximity to a magma source. Existing minerals can recrystallize, non-hydrous minerals can replace hydrous minerals, new minerals can be formed from the introduction of new ions from heated solutions, and minerals can become flattened and aligned in parallel layers.
Gneiss undergoes regional metamorphism, which involves high temperatures and pressures over large areas of the Earth's crust. This can result in the reorganization of minerals within the rock, forming distinct layers or bands of different minerals.
The process of layers of sediment building up is known as sedimentation. Over time, sediments such as sand, silt, and clay accumulate in bodies of water or on land, forming distinct layers. As more layers are deposited, the weight of the upper layers exerts pressure on those beneath, compacting them and causing the minerals within to bind together. This pressure can eventually lead to lithification, transforming loose sediments into solid rock formations.
Foliated is the correct answer!!!