A clastic texture refers to sedimentary rocks made up of fragments of pre-existing rocks that have been broken down, transported, and then deposited. These fragments, called clasts, can vary in size and are typically held together by a cementing material such as silica, calcite, or clay minerals. Clastic textures are commonly found in sandstone, conglomerate, and shale rocks.
None of the above. These terms describe sedimentary rocks. Granite is igneous.
Igneous rocks formed from large masses of magma solidifying far below Earth's surface typically have a coarse-grained texture. This is because the slower cooling process allows larger mineral crystals to form within the rock.
Clastic sediments are sediments that have particles or pieces of rock (clasts) in them. The clasts can be of igneous, metamorphic or sedimentary rock. Non-clastic sediments are made up of dissolved minerals or organic matter.
Shale, sandstone, and conglomerate are examples of clastic sedimentary rock.
Conglomerate is a clastic rock. They are coarse-grained sedimentary rocks.
composition
Clastic rocks are composed of broken pieces of older rocks that have been broken up by the process of weathering and are therefore sedimentary in nature. The "clasts" (bits of older rock) may vary in size.
Different clastic sediments have different textures based on the size, shape, and sorting of the grains they are composed of. The composition of a clastic sedimentary rock will vary depending on the mineralogy of the grains present in the rock. Factors such as the source rock, transportation distance, and depositional environment can all contribute to the differences in texture and composition between clastic sedimentary rocks.
Sandstone will have a gritty clastic texture, created by the cemented particles of sand sized particles of rock. You should be able to see the individual sand grains.
The texture that refers to rocks composed mainly of mineral and volcanic fragments is known as "clastic texture". This texture is characterized by the presence of distinct particles or fragments that are cemented together to form the rock.
You probably mean clastic. In that case: Sandstone.
Clastic sedimentary rock texture is also influenced by factors such as mineral composition, sorting (uniformity of particle size), rounding (degree of edges and corners), and grain angularity (shape of grains). These factors can provide information about the energy of the environment where the rock was formed.
Chalk is non-clastic, as it is primarily composed of the mineral calcite (calcium carbonate) formed from the remains of microscopic marine organisms such as plankton. These organisms contribute to the fine-grained texture of chalk through chemical precipitation rather than mechanical weathering or erosion.
Clastic rocks are sedimentary rocks consisting of bits and pieces of other rocks created by physical/mechanical weathering. Non-clastic are also sedimentary rocks; however are absent bits and pieces of other rocks and are formed through chemical processes (e.g. hydrolysis, evaporation, precipitation, oxidation) or form out of organic material (e.g. coal, chalk).
clastic
It is clastic
Sandstone is an example of a medium-grained clastic sedimentary rock. It is composed of sand-sized particles that are typically visible to the naked eye, giving it a medium-grained texture. Sandstone forms from the accumulation and cementation of sand grains.