A River Drops Its Mud and Builds Land
A river carries more than water. As it rushes along, it picks up tiny bits of soil, sand, and clay. These bits are called sediment. A fast river can carry a lot of it, which is why a river after a storm often looks brown.
When a river reaches the sea or a big lake, something changes. The water spreads out and slows down. A slow river cannot hold as much sediment, so it drops it. The heavier bits fall first, and the finest mud settles last.
Over many years, the sediment piles up and builds new land where the river meets the sea. This land is called a delta. Many deltas are shaped a little like a triangle. The river often splits into several smaller streams that wander across the delta, and the streams may shift their paths from time to time.
The soil in a delta is rich, so farmers often grow crops there. Deltas are also homes for birds, fish, and many plants that like wet ground. A delta is proof that moving water can build land as well as wear it away.