thumb|Frozen stream in Enäjärvi, Pori
A stream is a body of water
with surface water flowing within the bed
s of a channel
. The flow of a stream is controlled by three inputs – surface water, subsurface water and groundwater. The surface and subsurface water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls.
Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called river
Streams are important as conduits in the water cycle
, instruments in groundwater recharge
, and corridors for fish
migration. The biological habitat
in the immediate vicinity of a stream is called a riparian zone
. Given the status of the ongoing Holocene extinction
, streams play an important corridor
role in connecting fragmented habitat
s and thus in conserving biodiversity
. The study of streams and waterway
s in general is known as ''surface hydrology
'' and is a core element of environmental geography
A stream smaller than a creek, especially one that is fed by a spring
. It is usually small and easily forded
. A brook is characterised by its shallowness.
A creek () or crick ():
* In Australia, Canada, New Zealand, and the United States, a (narrow) stream that is smaller than a river; a minor tributary of a river; brook. Sometimes navigable by motor craft and may be intermittent.
* In parts of Maryland
, New England
, the UK and India, a tidal inlet
, typically in a salt marsh
or mangrove swamp
, or between enclosed and drained former salt marshes or swamps (e.g. Port Creek
separating Portsea Island
from the mainland). In these cases, the stream is the tidal stream, the course of the seawater
through the creek
channel at low and high tide.
A large natural stream, which may be a waterway
The linear channel between the parallel ridges or bars
on a shoreline beach or river floodplain, or between a bar and the shore. Also called a swale
is a contributory stream, or a stream which does not reach a static body of water such as a lake or ocean, but joins another river (a parent river). Sometimes also called a branch or fork.
[Bisson, Peter and Wondzell, Steven]
"Olympic Experimental State Forest Synthesis of Riparian Research and Monitoring"
United States Forest Service, p. 15 (December 1, 2009).
There are a number of regional names for a stream.
* ''Allt'' is used in the Scottish Highlands
'' is used in Lincolnshire
in areas which were once occupied by the Danes and Norwegians.
'' or ''winterbourne
'' is used in the chalk downland
of southern England for ephemeral rivers. When permanent, they are ''chalk streams
* ''Burn'' is used in Scotland and North East England
'' or ''ghyll'' is seen in the north of England and Kent
influenced by Old Norse
. The variant "ghyll" is used in the Lake District
and appears to have been an invention of William Wordsworth
* ''Nant'' is used in Wales.
* '' Rivulet'' is a term encountered in Victorian era publications.
'' is used in lowland
Scotland and Cumbria for a seasonal stream.
* ''Branch'' is used to name streams in Maryland and Virginia.
* ''Creek'' is common throughout the United States, as well as Australia.
* ''Falls'' is also used to name streams in Maryland, for streams/rivers which have waterfalls on them, even if such falls only have a small vertical drop. Little Gunpowder Falls
and the Jones Falls
are actually rivers named in this manner, unique to Maryland.
'' in New York
, and New Jersey
comes from a Dutch language
word meaning "riverbed" or "water channel", and can also be used for the UK meaning of 'creek'.
* ''Run'' in Ohio
, New Jersey, Pennsylvania, Virginia, or West Virginia can be the name of a stream.
* ''Run'' in Florida
is the name given to streams coming out of small natural springs
. ''River'' is used for streams from larger springs like the Silver River
and Rainbow River
* ''Stream'' and ''brook'' are used in Midwestern states
, Mid-Atlantic states
, and New England
: A shoal
that develops in a stream as sediment is deposited as the current slows or is impeded by wave action at the confluence.
: A fork into two or more streams.
: A depression created by constant erosion
that carries the stream's flow.
: The point at which the two streams merge. If the two tributaries are of approximately equal size, the confluence may be called a fork.
; Drainage basin
: (also known as a ''watershed'' in the United States) The area of land where water flows into a stream. A large drainage basin such as the Amazon River
contains many smaller drainage basins.
: Lands adjacent to the stream that are subject to flood
ing when a stream overflows its banks.
; Gaging station
: A site along the route of a stream or river, used for reference marking or water monitoring.
: The part of a stream or river proximate to its source. The word is most commonly used in the plural where there is no single point source
: The point on a stream's profile where a sudden change in stream gradient
: The point at which the stream discharges, possibly via an estuary
, into a static body of water such as a lake
: A segment where the water is deeper and slower moving.
: A turbulent
, fast-flowing stretch of a stream or river.
: A segment where the flow is shallower and more turbulent
: A large natural stream, which may be a waterway
; Run: A somewhat smoothly flowing segment of the stream.
: The spring from which the stream originates, or other point of origin of a stream.
: The point at which a stream emerges from an underground course through unconsolidated sediment
s or through caves. A stream can, especially with cave
s, flow aboveground for part of its course, and underground for part of its course.
; Stream bed
: The bottom of a stream.
; Stream corridor: Stream, its floodplains, and the transitional upland fringe
: The water moving through a stream channel.
: The river's longitudinal section, or the line joining the deepest point in the channel at each stage from source to mouth.
or cascade: The fall of water where the stream goes over a sudden drop called a knickpoint
; some knickpoints are formed by erosion when water flows over an especially resistant stratum
, followed by one less so. The stream expends kinetic energy
in "trying" to eliminate the knickpoint.
; Wetted perimeter
: The line on which the stream's surface meets the channel walls.
Streams typically derive most of their water from precipitation
in the form of rain
. Most of this water re-enters the atmosphere by evaporation
from soil and water bodies, or by the evapotranspiration
of plants. Some of the water proceeds to sink into the earth by infiltration
and becomes groundwater
, much of which eventually enters streams. Some precipitated water is temporarily locked up in snow fields and glacier
s, to be released later by evaporation or melting. The rest of the water flows off the land as runoff
, the proportion of which varies according to many factors, such as wind, humidity, vegetation, rock types, and relief. 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.
s 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.
The stream load
is defined as the solid matter carried by a stream. 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.
Perennial and non-perennial
A ''perennial stream
'' is one which flows continuously all year.
[ Water Supply Paper 494.]
Some perennial streams may only have continuous flow in segments of its stream bed year round during years of normal rainfall.
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,
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.
According to official US definitions, the channels of intermittent streams are well-defined,
as opposed to ephemeral streams, which may or may not have a defined channel, and rely mainly on storm runoff, as their aquatic bed is above the water table
An ephemeral stream does not have the biological, hydrological, and physical characteristics of a continuous or intermittent stream.
[ The same non-perennial channel might change characteristics from intermittent to ephemeral over its course.] [
Intermittent or seasonal stream
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.
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.
A ''wash'' or ''desert wash'' is normally a dry streambed in the deserts of the American Southwest, which flows only after significant rainfall.
In Italy, an intermittent stream is termed a torrent . 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.
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 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).
A basin may also be composed of smaller basins. For instance, the Continental Divide in North America divides the mainly easterly-draining Atlantic Ocean and Arctic Ocean basins from the largely westerly-flowing Pacific Ocean basin. The Atlantic Ocean basin, however, may be further subdivided into the Atlantic Ocean and Gulf of Mexico drainages. (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.
* Chalk stream
* Head cut
* Playfair's Law
* River ecosystem
* Rock-cut basin
Glossary of stream-related terms
Category:Bodies of water