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This show is Dark, Suspenseful. More Originals. Coming Soon. As terminology, the words "stream" and "branch" tend to be used rather than "river". The classic stream order , also called Hack's stream order or Gravelius' stream order , is a "bottom up" hierarchy that allocates the number "1" to the river with its mouth at the sea the main stem.
Its tributaries are given a number one greater than that of the river or stream into which they discharge. So, for example, all immediate tributaries of the main stem are given the number "2".
Tributaries emptying into a "2" are given the number "3" and so on. This type of stream order indicates the river's place in the network.
It is suitable for general cartographic purposes, but can pose problems because at each confluence, a decision must be made about which of the two branches is a continuation of the main channel, and whether the main channel has its source at the confluence of two other smaller streams.
The first order stream is the one which, at each confluence, has the greatest volumetric flow, usually reflecting the long-standing naming of rivers.
Associated with this stream order system was the quest by geographers of the 19th century to find the "true" source of a river. In the course of this work, other criteria were discussed to enable the main stream to be defined.
In addition to measuring the length of rivers the distance between the farthest source and the mouth and the size of the various catchments , geographers searched for the stream which deviated least at the actual confluence, as well as taking into account the successive names of rivers and their tributaries, such as the Rhine and the Aare or the Elbe and the Vltava.
According to the "top down" system devised by Strahler , rivers of the first order are the outermost tributaries.
If two streams of the same order merge, the resulting stream is given a number that is one higher. If two rivers with different stream orders merge, the resulting stream is given the higher of the two numbers.
The Strahler order is designed to reflect the morphology of a catchment and forms the basis of important hydrographical indicators of its structure, such as its bifurcation ratio, drainage density and frequency.
Its basis is the watershed line of the catchment. It is, however, scale-dependent. The larger the map scale , the more orders of stream may be revealed.
A general lower boundary for the definition of a "stream" may be set by defining its width at the mouth or, referencing a map, by limiting its extent.
The system itself is also applicable for other small-scale structures outside of hydrology. First- through third-order streams are also called headwater streams and constitute any waterways in the upper reaches of the watershed.
Going up in size and strength, streams that are classified as fourth- through sixth-order are medium streams, while anything larger up to 12th-order is considered a river.
For example, to compare the relative size of these different streams, the Ohio River in the United States is an eighth-order stream while the Mississippi River is a 10th-order stream.
Unlike the smaller order streams, these medium and large rivers are usually less steep and flow more slowly. They do however tend to have larger volumes of runoff and debris as it collects in them from the smaller waterways flowing into them.
If, however, two streams of different order join neither increases in order. For example, if a second-order stream joins a third-order stream, the second-order stream simply ends by flowing its contents into the third-order stream, which then maintains its place in the hierarchy.
Stream order also helps people like biogeographers and biologists in determining what types of life might be present in the waterway.
This is the idea behind the River Continuum Concept, a model used to determine the number and types of organisms present in a stream of a given size.
More types of plants, for example, can live in sediment-filled, slower flowing rivers like the lower Mississippi than can live in a fast-flowing tributary of the same river.