Yes
Magma that has fallen out a volcano to make sediments through metamorphism.
everything from called to crystals is your predicate.
Foliated metamorphic rocks exhibit a layering affect with parallel layers of mineral crystals one on top of the other. A good example of this is gneiss, which has alternating layers of light and dark minerals. Foliation takes place when pressure is applied to crystals and they recrystallize or align themselves at right angles to the direction of the applied directional stress.
The minerals in the rock have been realigned into parallel bands in response to pressures exerted on the rock from a particular direction. The banding forms perpendicularly to the direction of the force.
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.
Magma that has fallen out a volcano to make sediments through metamorphism.
The metamorphic rock you are referring to is called foliated rock. Foliated rocks have mineral crystals aligned in parallel layers or bands, resulting from the re-alignment of minerals due to pressure and heat during metamorphism. Examples of foliated rocks include slate, schist, and gneiss.
Regional metamorphism
"are filled with layers of crystals"
Foliated rock has parallel layers.
everything from called to crystals is your predicate.
Foliated metamorphic rocks exhibit a layering affect with parallel layers of mineral crystals one on top of the other. A good example of this is gneiss, which has alternating layers of light and dark minerals. Foliation takes place when pressure is applied to crystals and they recrystallize or align themselves at right angles to the direction of the applied directional stress.
the rock layers were eroded at the interface between the igneous intrusion and the sedimentary rocks.
The minerals in the rock have been realigned into parallel bands in response to pressures exerted on the rock from a particular direction. The banding forms perpendicularly to the direction of the force.
A sill is formed when magma is forced into layers parallel to the surrounding rock layers. Sills are characterized by their tabular shape and are often found intruding between rock layers.
When rock layers form parallel to each other, it is called stratification. This process occurs when sediments settle and accumulate in horizontal layers over time, resulting in distinct bands or layers of rock.
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.