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This runoff starts as a thin film called sheet wash, combined with a network of tiny rills, together constituting sheet runoff; when this water is concentrated in a channel, a stream has its birth.
Some creeks may start from ponds or lakes. To qualify as a stream, a body of water must be either recurring or perennial. Recurring intermittent streams have water in the channel for at least part of the year.
A stream of the first order is a stream which does not have any other recurring or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream.
When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream.
Thus, if a first-order stream joins a second-order stream, it remains a second-order stream. It is not until a second-order stream combines with another second-order stream that it becomes a third-order stream.
The gradient of a stream is a critical factor in determining its character and is entirely determined by its base level of erosion.
The base level of erosion is the point at which the stream either enters the ocean, a lake or pond, or enters a stretch in which it has a much lower gradient, and may be specifically applied to any particular stretch of a stream.
In geological terms, 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.
Meanders are looping changes of direction of a stream caused by the erosion and deposition of bank materials. These are typically serpentine in form.
Typically, over time the meanders gradually migrate downstream. If some resistant material slows or stops the downstream movement of a meander, a stream may erode through the neck between two legs of a meander to become temporarily straighter, leaving behind an arc-shaped body of water termed an oxbow lake or bayou.
A flood may also cause a meander to be cut through in this way. Typically, streams are said to have a particular profile , beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders.
The initial stage is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream.
However, a stream may meander for some distance before falling into a "young" stream condition. Streams can carry sediment, or alluvium.
The amount of load it can carry capacity as well as the largest object it can carry competence are both dependent on the velocity of the stream.
A perennial stream is one which flows continuously all year. Blue-line streams are perennial streams and are marked on topographic maps with a solid blue line.
Generally, streams that flow only during and immediately after precipitation are termed ephemeral. There is no clear demarcation between surface runoff and an ephemeral stream,  : 58 and some ephemeral streams can be classed as intermittent—flow all but disappearing in the normal course of seasons but ample flow backups restoring stream presence—such circumstances are documented when stream beds have opened up a path into mines or other underground chambers.
In the United States, an intermittent or seasonal stream is one that only flows for part of the year and is marked on topographic maps with a line of blue dashes and dots.
Washes can fill up quickly during rains, and there may be a sudden torrent of water after a thunderstorm begins upstream, such as during monsoonal conditions.
These flash floods often catch travelers by surprise. An intermittent stream can also be called an arroyo in Latin America , a winterbourne in Britain, or a wadi in the Arabic -speaking world.
In Italy , an intermittent stream is termed a torrent Italian torrente. In full flood the stream may or may not be "torrential" in the dramatic sense of the word, but there will be one or more seasons in which the flow is reduced to a trickle or less.
Typically torrents have Apennine rather than Alpine sources, and in the summer they are fed by little precipitation and no melting snow.
In this case the maximum discharge will be during the spring and autumn. However, there are also glacial torrents with a different seasonal regime.
In Australia, an intermittent stream is usually called a creek and marked on topographic maps with a solid blue line.
The extent of land basin drained by a stream is termed its drainage basin also known in North America as the watershed and, in British English, as a catchment.
This delineation is termed the Eastern Continental Divide. Similarly, the Gulf of Mexico basin may be divided into the Mississippi River basin and several smaller basins, such as the Tombigbee River basin.
Continuing in this vein, a component of the Mississippi River basin is the Ohio River basin, which in turn includes the Kentucky River basin, and so forth.
Stream crossings are where streams are crossed by roads , pipelines , railways , or any other thing which might restrict the flow of the stream in ordinary or flood conditions.
Any structure over or in a stream which results in limitations on the movement of fish or other ecological elements may be an issue.
From Wikipedia, the free encyclopedia. A body of surface water flowing down a channel. For other uses, see Stream disambiguation.
For the moth, see Rivulet moth. This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources.
Unsourced material may be challenged and removed. Play media. See also: Intermittent river. Manual of Hydrology: Part 1.
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