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.
Small crystal grains form when molten rock cools quickly. In an extrusive igneous rock, it's referred to as aphanitic texture.
It has a foliated texture.
no texture
texture
texture
They are references to the rock's 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
Texture.
Yes m that it true, other than glasses all rocks have grains.
Texture.