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Headwaters

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Headwaters

"Headwater" redirects here. For the musical group, see Headwater (band).
This article is about the heads of rivers. For the insurance company, see RiverSource.

The source or headwaters of a river or stream is the furthest place in that river or stream from its estuary or confluence with another river, as measured along the course of the river.

Definition

There is no universally agreed upon definition for determining a stream's source. The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly identified as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri - lower Mississippi length figure in lists of lengths of rivers around the world.[1]

This most common definition of a river source specifically utilizes the most distant point (along watercourses from the river mouth) in the drainage basin from which water runs year-around (perennially), or, alternatively, as the furthest point from which water could possibly flow (ephemerally).[2] The latter definition includes sometimes-dry channels and removes any possible definitions that would have the river source "move around" from month to month depending on precipitation or ground water levels. This definition, from geographer Andrew Johnston of the Smithsonian Institution, is also used by the National Geographic Society when pinpointing the source of rivers such as the Amazon or Nile. A definition given by the state of Montana agrees, stating that a river source is never a confluence but is "in a location that is the farthest, along water miles, from where that river ends."[3] Under this definition neither a lake (excepting lakes with no inflows) nor a confluence of tributaries can be a true river source, though both often provide the starting point for the portion of a river carrying a single name. For example, National Geographic and virtually every other geographic authority and atlas define the source of the Nile River not as Lake Victoria's outlet where the name "Nile" first appears, which would reduce the Nile's length by over 900 km (dropping it to fourth or fifth on the list of world's rivers), but instead use the source of the largest river flowing into the lake, the Kagera River. Likewise, the source of the Amazon River has been determined this way, even though the river changes names numerous times along its course.[4]

When not listing river lengths, however, alternate definitions may be used. The Missouri River's source is named by some USGS and other federal and state agency sources, following Lewis and Clark's naming convention, as the confluence of the Madison and Jefferson rivers, rather than the source of its longest tributary (the Jefferson).[3] This is contradicted by an US Army Corps of Engineers official on a USGS site[5] who states the most common definition: "Geographers generally follow the longest tributary to identify the source of rivers and streams. In the case of the Missouri River, Lewis and Clark would have had to travel to the east...to reach the source"...He states that the Missouri River source is well upstream from Lewis and Clark's confluence, "following the Jefferson River to the Beaverhead River to Red Rock River, then Red Rock Creek to Hell Roaring Creek."

Characteristics of sources

Sometimes the source of the most remote tributary, may be in an area that is more marsh-like, in which the "uppermost" or most remote section of the marsh would be the true source. For example, the source of the River Tees is marshland.

The furthest stream is also often called the headstream. Headwaters are usually small streams that are often cool waters, because of shade and recently melted ice or snow. They may also be glacial headwaters, waters formed by the melting of glacial ice.

The source is the farthest point of the river stream from its estuary, mouth, or its confluence with another river or stream, regardless of what name that watercourse may carry on local maps and in local usage. Most rivers have numerous tributaries and change names often; it is customary to regard the longest tributary as its source.

Headwaters are the most extreme upstream areas of a watershed, as opposed to the outflow or discharge of a watershed. The river source is often but not always on or quite near the edge of the watershed, or watershed divide. For example, the source of the Colorado River is at the Continental Divide separating the Atlantic Ocean and Pacific Ocean watersheds of North America.

Example

A river is considered a linear geographic feature, with only one mouth and one source. For an example, note how the Mississippi River and Missouri River sources are officially defined:

    • Related usages

      The verb "rise" can be used to express the general region of a river's source, and is often qualified with an adverbial expression of place. For example:

      • The River Thames rises in Gloucestershire.
      • The White Nile rises in the Great Lakes region of central Africa.

      The word "source", when applied to lakes rather than rivers or streams, refers to the lake's inflow.[6][7]

      See also

      References

      pt:Nascente (hidrografia)
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