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.
Its texture.
granite
metamorphic
Metamorphic rocks that consist of only one mineral that forms large interlocking crystals often have a _____ texture.
They use the mineral composition, color, and texture.
rocks are idenified by texture
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
Usually have a rougher texture
Crystalline texture.
what is the texture of all inorganic land derived sedimentary rocks
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.
Obsidian
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.
hard
Texture in rocks is not the same as color or shape. Texture refers to the size, shape, and arrangement of mineral grains or crystals within a rock, while color refers to the outward appearance of the rock. Similarly, shape in rocks refers to their physical form or structure, and not the internal arrangement of mineral grains which defines texture.
Non-foliated Texture!
The texture of rocks differs based on their formation processes and mineral composition. Igneous rocks typically have a crystalline texture, with interlocking mineral grains formed from cooling magma or lava. Sedimentary rocks often exhibit a layered or granular texture due to the accumulation and compaction of sediments. Metamorphic rocks may display a foliated or non-foliated texture, resulting from the alteration of existing rocks under heat and pressure, leading to the alignment of minerals or a more homogenous appearance.