the size of leiths genitles
Clastic refers to sedimentary rocks with rock particles of various sizes cemented together in a finer matrix.
The amount of uniformity in the size of rock or sediment particles is called "sorting." Sorting can range from well-sorted (similar-sized particles) to poorly sorted (a wide range of particle sizes).
Different sized particles in sedimentary rock are a result of the varying energy levels during deposition. For example, fast-moving water can carry larger particles, while slower-moving water can only transport smaller particles. As the sediment settles, the larger particles will settle out first, followed by the smaller particles, leading to layers of different sizes in the rock.
Rock particles.
Particles of rock that have been eroded and can settle from water are called sediment. This includes various sizes of particles, such as silt, sand, gravel, and clay, which are transported by water and eventually deposited as sedimentary layers. The settling process occurs when the energy of the transporting water decreases, allowing these particles to accumulate in riverbeds, lakes, or ocean floors. Over time, these sediments can lithify into sedimentary rock.
Particles of soil and rock that are carried along in water are called sediment. They can include a range of sizes, from tiny clay particles to larger pebbles and boulders. Sediment transport is an important process in shaping the landscape and can contribute to erosion and deposition in rivers and other water bodies.
Rocks have grains because they are made up of different mineral particles that have been compacted or cemented together over time. These mineral particles can vary in size, shape, and composition, creating the overall texture and appearance of the rock.
An unsorted mixture of small particles to large boulders is called a conglomerate. It is a type of sedimentary rock characterized by its diverse range of grain sizes and is typically formed through the deposition and cementation of various rock fragments.
The rock described would be a clastic sedimentary rock.
The particles would have been compacted by pressure from the weight of sediments above.
You can see rock grains on a rock by examining its surface closely. Grains may appear as small, distinct particles of various colors and sizes. The use of a hand lens or magnifying glass can help to enhance the visibility of individual grains.
Till is a mixture of sediment and rock that is deposited directly by a glacier, while outwash is the material carried away from a glacier by meltwater and deposited in a different location. Till tends to be unsorted and can have a range of sizes of particles, while outwash is typically well-sorted and composed of smaller particles.