What type of stream is characterized as losing?

A stream characterized as losing has water that seeps into the groundwater. This phenomenon occurs when the stream's water level is higher than the water table, allowing water to flow from the streambed into the adjacent, saturated ground. As a result, the stream loses water along its course rather than gaining from groundwater contributions.

This type of stream is often found in arid or semi-arid regions where the surrounding soil or rock formations are more permeable. The process helps to recharge the groundwater supply while reducing the flow of water in the stream itself. Understanding this concept is crucial, as losing streams play an important role in the hydrology of an area, influencing both surface water and groundwater interactions.