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a terminus for streams near the Alvord Desert: Aneroid Lake: in the Eagle Cap Wilderness: Antelope Flat Reservoir: in central Oregon, an impoundment of Bear Creek Antelope Reservoir: near Jordan Valley: Anthony Lakes: also known as North Powder Lakes, in the Elkhorn Mountains: Applegate Lake: a flood-control reservoir on the Applegate River ...
There are a number of water quality issues within the basins. In an average water basin, between 5 and 58 tons per square mile per year (t/mi 2 /yr) of fine-grained sediment are removed from the surrounding land in surface runoff but the Yadkin–Pee Dee River Basin sees 300 t/mi 2 /yr in runoff due to rapid population growth and agricultural ...
There are three basic types of freshwater ecosystems: Lentic (slow moving water, including pools, ponds, and lakes), lotic (faster moving water, for example streams and rivers) and wetlands (areas where the soil is saturated or inundated for at least part of the time). Limnology (and its branch freshwater biology) is a study about freshwater ...
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A stone near Crissolo, Italy, is inscribed, "Here is born the Po".. 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 known as the source stream".
The amount of water in a stream is measured as discharge (volume per unit time). As water flows downstream, streams and rivers most often gain water volume, so at base flow (i.e., no storm input), smaller headwater streams have very low discharge, while larger rivers have much higher discharge. The "flow regime" of a river or stream includes ...
A wide variety of river and stream channel types exist in limnology, the study of inland waters.All these can be divided into two groups by using the water-flow gradient as either low gradient channels for streams or rivers with less than two percent (2%) flow gradient, or high gradient channels for those with greater than a 2% gradient.
Rocky stream in Italy Frozen stream in Enäjärvi, Pori, Finland Stream near Montriond in south-eastern France Aubach (Wiehl) in North Rhine-Westphalia, Germany. A stream is a continuous body of surface water [1] flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a ...
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