★ Key Takeaways
For Example, in a Stream on a Particular Day, Water Flow May Only Be Strong Enough to Transport Grains That Are Finer Than Medium-Grained Sand. So All Clasts on the Surface of the Stream Bed That Are Equal to or Larger Than Medium Sand Will Be Left Behind. the Sediment, Therefore, Becomes Sorted.
Interested in Where Do Rivers and Streams Deposit Sediment, this article provides essential context worth reading.
For Example, in a Stream on a Particular Day, Water Flow May Only Be Strong Enough to Transport Grains That Are Finer Than Medium-Grained Sand. So All Clasts on the Surface of the Stream Bed That Are Equal to or Larger Than Medium Sand Will Be Left Behind. the Sediment, Therefore, Becomes Sorted.
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