Streams are formed from water runoff from precipitation, such as rain or melting snow. As the water flows downhill, it collects in small channels, which gradually develop into larger streams.
The flow of a stream is influenced by factors such as the gradient of the land, the volume of water, and the shape of the stream channel. Faster-flowing streams tend to have a steeper gradient and carry a larger volume of water.
Streams can be classified based on their flow patterns. There are three main types of streams: perennial streams, which flow all year round; intermittent streams, which flow only at certain times of the year; and ephemeral streams, which flow only in response to precipitation.
Streams have the ability to erode and transport sediment, shaping the landscape over time. Erosion occurs as the force of the flowing water wears away the land, while deposition happens when the water loses energy and drops the sediment it was carrying.
Streams support diverse ecosystems, hosting a variety of plants and animals. The health of stream ecosystems is influenced by factors such as water quality, temperature, and the availability of food and shelter for organisms.