Formation: Streams are typically formed from the runoff of rainwater or meltingsnow. They may also originate from springs or seepage from underground aquifers.
Channels: Streams flow in channels, which can range from small, narrow rivulets to large, meandering rivers. The shape and size of the channel can affect the behavior of the stream.
Gradient: The steepness of the land over which a stream flows is known as its gradient. A steep gradient results in a faster flow, while a gentle gradient leads to a slower flow.
Velocity: The speed of the water in a stream is referred to as its velocity. It can vary based on factors such as the slope of the channel, the volume of water, and the presence of obstacles.
Stream Patterns: Streams can exhibit different patterns, including dendritic (tree-like), radial (spokes of a wheel), rectangular, and trellis patterns, depending on the geological structure of the area.
The student demonstrates an understanding of the structure, function, behavior, development, life cycles, and diversity of living organisms by describing the structure-function relationship