Clastic sedimentary rock is formed from the accumulation of fragments or clasts of pre-existing rocks. These fragments, which can range in size from tiny grains to large boulders, are transported and then deposited by various agents such as water, wind, or ice. Over time, the sediments become compacted and cemented together to form solid rock.
Clastic sedimentary rock is a type of sedimentary rock composed of fragments or clasts of pre-existing rocks. These rock fragments are transported by fluids like water or wind and are then deposited and compacted over time to form the rock. The clasts in clastic sedimentary rock can vary in size and composition, ranging from fine grains like clay to larger particles like sand or gravel.
Clastic sedimentary rocks are a type of rock formed from fragments of pre-existing rocks called clasts. These fragments are produced by weathering and erosion processes, such as the breaking down of rocks by water, wind, or ice. The clasts are then transported and deposited, eventually becoming cemented together to form clastic sedimentary rock.
