silt because there is a specific oder these substances go in order by. This goes from greatest mass to least mass: sand, silt , clay
Generally, clay particles are smaller and lighter than silt particles, so they tend to stay suspended in water longer. Silt particles are larger and heavier, causing them to settle faster in comparison to clay particles.
Silt is larger in particle size than clay and feels gritty when dry, while clay is finer in particle size and feels sticky when wet. Silt is more fertile than clay and drains better, while clay holds more water and nutrients.
Clay particles are smaller than silt particles. Clay particles are smaller than 0.002 mm in diameter, while silt particles range from 0.002 to 0.05 mm.
Clay is the most dense soil type, followed by silt and then sand. Clay particles are finer and more closely packed, which gives clay a higher density compared to silt and sand.
Clay holds more water than sand and silt. Clay particles are smaller and create a denser structure that can hold water more effectively than the larger particles of sand and silt.
Generally, clay particles are smaller and lighter than silt particles, so they tend to stay suspended in water longer. Silt particles are larger and heavier, causing them to settle faster in comparison to clay particles.
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.
It is more accurate to say it is formed from clay and silt.
clay
gravel,coarse,fine sand,silt and clay
Silt is larger in particle size than clay and feels gritty when dry, while clay is finer in particle size and feels sticky when wet. Silt is more fertile than clay and drains better, while clay holds more water and nutrients.
Clay particles are smaller than silt particles. Clay particles are smaller than 0.002 mm in diameter, while silt particles range from 0.002 to 0.05 mm.
Clay is the most dense soil type, followed by silt and then sand. Clay particles are finer and more closely packed, which gives clay a higher density compared to silt and sand.
Clay holds more water than sand and silt. Clay particles are smaller and create a denser structure that can hold water more effectively than the larger particles of sand and silt.
suspensions
silt
A good example of sand, silt, and clay carried by a tornado falling to the ground would be the aftermath of the tornado where you can see different layers of sediment deposited on the ground. This layering effect occurs because of the varying sizes and weights of the particles in the tornado's air current, with heavier particles such as sand falling first followed by finer particles like silt and clay settling on top.