The depth of a water stream can vary greatly depending on factors such as location, rainfall, and topography. In general, shallow streams may only be a few inches deep, while larger rivers can reach depths of several meters. Some rivers, like the Congo River, can exceed depths of 220 meters (720 feet) in certain areas. Ultimately, the depth of a water stream is influenced by both natural and human-made conditions.
In the water
Not very deep
an old stream is a deep wide and curvy river stream
Stream like movements of water that occur near the surface of the ocean are called surface currents. Stream like movements of ocean water far below the surface are known as a deep current.
A deep gully or ditch carved by running water is called a ravine. It is typically formed by the erosive forces of flowing water over a long period of time, creating a narrow and steep-sided channel in the landscape.
A deep valley with high steep slopes that often has a stream running through it is called a canyon. Canyons are typically formed by the erosion of water over time, creating a distinctive geological feature.
When the elevation of the water table is below the stream, the stream is considered to be gaining water from the surrounding groundwater, a process known as gaining or effluent stream. In this situation, the stream acts as a discharge point for groundwater, contributing to its flow. Conversely, if the water table is above the stream, the stream may lose water to the groundwater, referred to as a losing or influent stream.
The Gulf Stream carries many juvenile tropical fish up the East Coast to the northern states. The Gulf Stream is a warm water current therefore, making the journey north not as cold as you would think.
deep water in a community near a river or stream thunderstorms the main features of a flood is the huge amount of water that covers an area and ruins crops and destroys homes
Deep wells are often in flowing aquifers. (imagine an underground stream) this can carry soil or sediment and it occasionally gets pumped to the surface. Also, when a well is chlorinated or shocked, the deposits will make the water dirty for a few days.
· The stream will erode down through its bed to achieve the base level of erosion throughout its course. If this base level is low, then the stream will rapidly cut through underlying strata and have a steep gradient, and if the base level is relatively high, then the stream will form a flood plain and meander. http://en.wikipedia.org/wiki/Stream
The mouth of a stream is where it meets a larger body of water, such as a lake, ocean, or another stream. It is where the stream's water flows out and mixes with the water of the larger body.