answersLogoWhite

0

foliation

User Avatar

Wiki User

12y ago

What else can I help you with?

Continue Learning about Earth Science

What is the parallel alignment of platy grains in a rock called?

The parallel alignment of platy grains in a rock is called foliation. Foliation is commonly seen in metamorphic rocks where minerals align in a preferred orientation due to pressure and temperature changes during deformation.


What is a metamorphic rock that has parallel alignment of mineral grains?

Schist is a metamorphic rock that exhibits parallel alignment of mineral grains, giving it a foliated appearance. This alignment is typically a result of regional metamorphism where intense pressure and temperature conditions cause the minerals to recrystallize in a preferred orientation.


Is it true when magnitic minerals grains in a rock form they become magnetized in the direction parallel to earth existing magnetic field?

Yes, when magnetic mineral grains in a rock form, they can become magnetized in the direction parallel to Earth's existing magnetic field. This is due to the alignment of the mineral grains with the magnetic field at the time of formation, resulting in the retention of this magnetization in the rock.


What is the parallel crystal arrangement of layers in metamorphic rock called?

The parallel crystal arrangement of layers in metamorphic rock is called foliation. Foliation is a common feature in rocks that have undergone intense heat and pressure, resulting in the alignment of mineral grains into distinct layers.


What aligns in parallel bands do to added pressure on a rock during metamorphism?

The parallel bands in a rock, also known as foliation, can rotate or deform in response to added pressure during metamorphism. This can lead to the alignment of minerals or elongation of grains in the direction of pressure, ultimately resulting in a reorientation of the rock's structure.

Related Questions

Parallel alignment of platy grains.?

foliation


What is the parallel alignment of platy grains in a rock called?

The parallel alignment of platy grains in a rock is called foliation. Foliation is commonly seen in metamorphic rocks where minerals align in a preferred orientation due to pressure and temperature changes during deformation.


What is it when platy materials have a parallel alignment?

foliated


When platy materials have a parallel alignment a rock is .?

foliated


When platy materials have a parallel alignment a rock is a?

foliated


When platy materials have a paralled alignment a rock is what?

When platy materials have a parallel alignment, the rock is considered foliated. Foliated rocks have a layered or banded appearance due to the parallel alignment of minerals like mica or chlorite. This alignment typically occurs through pressure and temperature changes during rock formation.


What platy parallel mineral grains are the most visual aspect of foliated metamorphic rocks?

Mica.


What is a metamorphic rock that has parallel alignment of mineral grains?

Schist is a metamorphic rock that exhibits parallel alignment of mineral grains, giving it a foliated appearance. This alignment is typically a result of regional metamorphism where intense pressure and temperature conditions cause the minerals to recrystallize in a preferred orientation.


What platy mineral grains are the most visual aspect of foliated metamorphic rocks?

Mica.


Parallel alignment of minerals that have been subjected to stress?

parallel alignment of minerals that have been subjected to stress


Is it true when magnitic minerals grains in a rock form they become magnetized in the direction parallel to earth existing magnetic field?

Yes, when magnetic mineral grains in a rock form, they can become magnetized in the direction parallel to Earth's existing magnetic field. This is due to the alignment of the mineral grains with the magnetic field at the time of formation, resulting in the retention of this magnetization in the rock.


What is salt's cleavage?

The rocks tend to spilt along parallel planes defined by distribution and parallel arrangment of platy mineral crystals.