Rivers and sedimentary basins.
The three types of weathered rock particles found in soil are sand, silt, and clay. Sand particles are the largest, followed by silt, and clay particles are the smallest.
If the river is moving slower than ~0.01 cm/sec, then clay may be found in the river bed. If it is slower than ~0.3 cm/sec, then silt may be found. Any faster and the clay and silt would be deposited at the mouth of the river where the velocity decreases greatly.
Clay and silt are both soil particles that fall within the fine-grained category. They are smaller than sand but larger than colloids, with silt being larger than clay. Both clay and silt contribute to soil fertility but can also pose drainage and compaction issues.
Clayey silt is a soil type that contains a high proportion of fine particles, with a mixture of clay and silt. The clay content provides cohesion and plasticity to the soil, while the silt component helps with drainage and fertility. Clayey silt is commonly found in areas with moderate water retention and good agricultural potential.
Some examples of silt include fine grains of sand, mud, and clay that are deposited by water or wind and typically found near river banks, deltas, and estuaries. Silt particles are larger than clay but smaller than sand.
suspensions
Yes. Including clay and sand.
The three types of weathered rock particles found in soil are sand, silt, and clay. Sand particles are the largest, followed by silt, and clay particles are the smallest.
If the river is moving slower than ~0.01 cm/sec, then clay may be found in the river bed. If it is slower than ~0.3 cm/sec, then silt may be found. Any faster and the clay and silt would be deposited at the mouth of the river where the velocity decreases greatly.
Clay and silt are both soil particles that fall within the fine-grained category. They are smaller than sand but larger than colloids, with silt being larger than clay. Both clay and silt contribute to soil fertility but can also pose drainage and compaction issues.
It is more accurate to say it is formed from clay and silt.
They are formed when rocks are weathered. They are found in the soil
sand, silt, clay, and organic matter
The reason many rivers contain clay is because clay particles are lighter than the small rocks and pebbles beneath, so the clay particles are deposited on top of the rocks. However clay is not lighter than silt particles, in fact clay is much heavier. Normally the silt would cover the clay, but if the river is fast enough, it may continue to carry away the silt particles, and leave the clay.
clay
Clayey silt is a soil type that contains a high proportion of fine particles, with a mixture of clay and silt. The clay content provides cohesion and plasticity to the soil, while the silt component helps with drainage and fertility. Clayey silt is commonly found in areas with moderate water retention and good agricultural potential.
Some examples of silt include fine grains of sand, mud, and clay that are deposited by water or wind and typically found near river banks, deltas, and estuaries. Silt particles are larger than clay but smaller than sand.