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Opening Day, Statewide - April 3, one opening day in Find waters by using one or more of our interactive maps :. You may be trying to access this site from a secured browser on the server.

Please enable scripts and reload this page. An Official Pennsylvania Government Website. The general pattern is that the first order streams contain particulate matter decaying leaves from the surrounding forests which is processed there by shredders like Plecoptera larvae.

The products of these shredders are used by collectors, such as Hydropsychidae , and further downstream algae that create the primary production become the main food source of the organisms. All changes are gradual and the distribution of each species can be described as a normal curve , with the highest density where the conditions are optimal.

In rivers succession is virtually absent and the composition of Boat And Stream Questions In Malayalam Night the ecosystem stays fixed. The chemistry of rivers is complex and depends on inputs from the atmosphere, the geology through which it travels and the inputs from man's activities. The chemical composition of the water has a large impact on the ecology of that water for both plants and animals and it also affects the uses that may be made of the river water.

Understanding and characterising river water chemistry requires a well designed and managed sampling and analysis. Brackish waster occurs in most rivers where they meet the sea. The extent of brackish water may extend a significant distance upstream, especially in areas with high tidal ranges. Flooding is a natural part of a river's cycle. The majority of the erosion of river channels and the erosion and deposition on the associated floodplains occur during the flood stage.

In many developed areas, human activity has changed the form of river channels, altering magnitudes and frequencies of flooding. Some examples of this are the building of levees , the straightening of channels, and the draining of natural wetlands.

In many cases human activities in rivers and floodplains have dramatically increased the risk of flooding. Straightening rivers allows water to flow more rapidly downstream, increasing the risk of flooding places further downstream.

Building on flood plains removes flood storage, which again exacerbates downstream flooding. The building of levees only protects the area behind the levees and not those further downstream. Levees and flood-banks can also increase flooding upstream because of the back-water pressure as the river flow is impeded by the narrow channel banks. Detention basins finally also reduce the risk of flooding significantly by being able to take up some of the flood water.

Studying the flows of rivers is one aspect of hydrology. Rivers flow downhill with their power derived from gravity. The direction can involve all directions of the compass and can be a complex meandering path. Rivers flowing downhill, from river source to river mouth, do not necessarily take the shortest path. For alluvial streams, straight and braided rivers have very low sinuosity and flow directly down hill, while meandering rivers flow from side to side across a valley.

Bedrock rivers typically flow in either a fractal pattern, or a pattern that is determined by weaknesses in the bedrock, such as faults , fractures , or more erodible layers.

Volumetric flow rate , also known as discharge, volume flow rate, and rate of water flow, is the volume of water which passes through a given cross-section of the river channel per unit time.

Volumetric flow rate can be thought of as the mean velocity of the flow through a given cross-section, times that cross-sectional area. Mean velocity can be approximated through the use of the Law of the Wall. In general, velocity increases with the depth or hydraulic radius and slope of the river channel, while the cross-sectional area scales with the depth and the width: the double-counting of depth shows the importance of this variable in determining the discharge through the channel. In its youthful stage the river causes erosion in the water-course, deepening the valley.

Hydraulic action loosens and dislodges the rock which further erodes the banks and the river bed. Over time, this deepens the river bed and creates steeper sides which are then weathered. The steepened nature of the banks causes the sides of the valley to move downslope causing the valley to become V-shaped. Waterfalls also form in the youthful river valley where a band of hard rock overlays a layer of soft rock.

Differential erosion occurs as the river erodes the soft rock more readily than the hard rock, this leaves the hard rock more elevated and stands out from the river below. A plunge pool forms at the bottom and deepens as a result of hydraulic action and abrasion. Sediment yield is the total quantity of particulate matter suspended or bedload reaching the outlet of a drainage basin over a fixed time frame.

Yield is usually expressed as kilograms per square kilometre per year. The theoretical concept of the 'sediment delivery ratio' ratio between yield and total amount of sediment eroded captures the fact that not all of the sediment is eroded within a certain catchment that reaches out to the outlet due to, for example, deposition on floodplains.

Such storage opportunities are typically increased in catchments of larger size, thus leading to a lower yield and sediment delivery ratio. Rivers are often managed or controlled to make them more useful or less disruptive to human activity.

River management is a continuous activity as rivers tend to 'undo' the modifications made by people. Dredged channels silt up, sluice mechanisms deteriorate with age, levees and dams may suffer seepage or catastrophic failure. The benefits sought through managing rivers may often be offset by the social and economic costs of mitigating the bad effects of such management.

As an example, in parts of the developed world, rivers have been confined within channels to free up flat flood-plain land for development. Floods can inundate such development at high financial cost and often with loss of life. Rivers are increasingly managed for habitat conservation , as they are critical for many aquatic and riparian plants, resident and migratory fishes , waterfowl , birds of prey , migrating birds , and many mammals.

From Wikipedia, the free encyclopedia. Natural flowing watercourse. For other uses, see River disambiguation. For other uses, see Rivers disambiguation. For riverine warfare, see Brown-water navy.

Main article: Intermittent river. Main article: River ecosystem. Main article: River chemistry. Further information: Brackish water. Main article: Flood. Main article: Streamflow. Main article: River engineering. Rivers portal Environment portal Ecology portal. See also: geography , water cycle , and drainage basin. Bridge Ferry Boat And Stream Questions In Malayalam Zip Code Ford crossing Tunnel. Lists of rivers List of international border rivers List of rivers by continent List of rivers by discharge List of rivers by length List of waterways.

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