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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.
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.
A parallel alignment of minerals that have been subjected to stress is called foliation. It creates distinctive layering or banding in rocks, such as in metamorphic rocks like schist or gneiss, where the minerals align parallel to the direction of stress.
Metamorphic rocks with grains arranged randomly are said to be non-foliated. This means they do not have a layered or banded structure like foliated metamorphic rocks. Examples include marble and quartzite.
The material that forms a crystal is called a crystalline solid. It has a regular, repeating arrangement of atoms or molecules that give it a distinct crystalline structure.
The parallel arrangement of mineral grains in a rock that gives it a striped appearance is called foliation. This typically occurs in metamorphic rocks due to the alignment of minerals under pressure and heat, resulting in distinct bands or stripes. Foliation can provide clues about the rock's history and the direction of metamorphic forces.
A crystal has a definite arrangement of particles in a repeating pattern called a crystal lattice. The order in their arrangement gives crystals their characteristic shape and structure.
Crystal
a crystal.
A regular repeating arrangement of atoms within a rock is called a crystal lattice. This lattice gives crystals their characteristic shape and internal structure, which can be seen under a microscope or macroscopically.
The total three-dimensional array of points that describes the arrangement of particles in a crystal is called a lattice. It consists of regularly repeating points in space that represent the positions of atoms, ions, or molecules in the crystal structure. The lattice provides a framework for understanding the symmetry and properties of the crystal.
A regular repeating arrangement of atoms, ions and molecules is called a crystal. This structure has its plane faces in a symmetrical order.
An orderly three-dimensional arrangement formed by ions is called a crystal lattice. In a crystal lattice, ions are arranged in a repeating pattern that maximizes the attraction forces between them, resulting in a stable structure. This arrangement gives crystals their characteristic shape and properties.
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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.
Yes, a crystal is a regular repeating arrangement of particles in a three-dimensional pattern. The particles, which can be atoms, ions, or molecules, are arranged in a specific geometric pattern called a crystal lattice. This regular arrangement gives crystals their characteristic shape and structure.
The pattern of ions that form a crystal is called the crystal lattice. It refers to the repeating arrangement of ions in three-dimensional space that gives a crystal its structure and properties. The crystal lattice dictates the shape and symmetry of the crystal.