Texture In Rocks
The texture of a rock is the size shape and arrangement of the grains for sedimentary rocks or crystals for igneous and metamorphic rocks.
Texture in rocks. The texture of a rock refers to the details of its visible character. The texture of igneous rocks can be analyzed to understand how the rock became solid or crystallized from liquid melted rock. Texture or rock microstructure in geology refers to the relationship between the materials of which a rock is composed. Texture of a rock is the appearance of the rock and how one feels touching it.
Also of importance are the rock s extent of homogeneity i e uniformity of composition throughout and the degree of. Below we define a few of the terms geologists use to describe these textures. Rock stone texture seamless 12699. Rock stone texture seamless 12698.
Grains or clasts do not interlock but rather are piled together and cemented. This includes the size and quality and interrelations of its grains and the fabric they form. The texture of a rock provides a clue whether the magma cooled fast or slowly and where the rock was formed. The broadest textural classes are crystalline in which the components are intergrown and interlocking crystals fragmental in which there is an accumulation of fragments by some physical process aphanitic in which crystals are not visible to the unaided eye and.
Click each image to see a larger version plus information about the rock s texture. Larger scale features such as fractures and layering are considered rock structures in comparison. The sedimentary rock textures chart on the following illustrates the major sedimentary rock textures. Rocks with wire mesh texture seamless 17476.