Grains in igneous rocks determine the rock's classification. They can be classified as:
no texture
The texture of a rock consists of it's grain or mineral crystal size, the arrangement of the grains or crystals, and the degree of uniformity of the grains or crystals. Examples of rock texture would be: * Coarse grained--visible crystals or grains as in granite. * Fine grained--small grains, invisible to the unaided eye as in shale. * Porphyritic--large visible crystals in a fine grained matrix as in granite porphyry. * Schistose--layers of flattened micaceous minerals such as in mica schist. * Foliated--a metamorphic rock texture of parallel mineral banding as in gneiss. * Homogenous--same grain apperance in all directions as in basalt.
A)fossils B)small grains C)vesicular texture D) porphyrtic texture Its one of these answers i chose D. because its more likely to have it. Idk if its the right answer.
Yes. The grain texture also matters. For example, basalt and gabbro have the same mineral composition, but basalt, which forms on the surface, has microscopic grains while gabbro, which forms underground, has larger mineral grains.
When all the grains in a rock are large and easy to see, the rock is described as "coarse-grained." This texture indicates that the rock has undergone a slower cooling process, allowing larger crystals to form. Coarse-grained rocks are often associated with igneous rocks, such as granite, where the individual mineral grains can be distinctly identified.
The word that describes the shapes and sizes of grains in a rock is "texture." Texture refers to the arrangement and size of mineral grains in a rock, whether they are fine-grained, coarse-grained, or other specific characteristics.
no texture
It has a foliated texture.
texture
A schistose texture.
The texture of soil depends on its particle size: clay-fine grains, very little space for water. sand- coarse grains, loose, water drains quicklysilt-medium grains, retains water.
The sizes,shapes,and positions of the grains that make up a rock.
Texture.
Yes m that it true, other than glasses all rocks have grains.
The sizes, shapes, and positions of the grains in a rock determine its texture. Texture influences properties such as hardness, strength, and permeability in rocks. It also provides clues about the rock's history and how it formed.
The grains of constituent compounds and their grain size.
Its true.