upper course of a river wikipedia

In the late 1600s Czech Jesuit Father Samuel Fritz, an apostle of the Omagus established some forty mission villages. The river is significantly shortened from its natural course due to a number of canalisation projects completed in the 19th and 20th century. Between Eglisau and Basel, the High Rhine consistently forms the border. The Rhine: an eco-biography, 1815–2000. It gathers its waters from 5 degrees north latitude to 20 degrees south latitude. [18] Tulla is considered to have domesticated the Upper Rhine, domestication that served goals such as reducing stagnant bogs that fostered waterborne diseases, making regions more habitable for human settlement, and reduce high frequency of flooded water. The Upper Rhine region was changed significantly by a Rhine straightening program in the 19th Century. Coeval absolute sea-level rise and tectonic subsidence have strongly influenced delta evolution. Every year, the river rises more than 9 metres (30 ft), flooding the surrounding forests, known as várzea ("flooded forests"). They join the Rhine near Koblenz, for the right and left respectively. From an analysis of maps of the river between 1776 and 1843, it was concluded in a study that the river avulsion was more likely gradual than catastrophic and sudden, and may have been generated by bank erosion, perhaps around a large mid-channel bar, causing a diversion of the channel into the existing floodplain channel.

[23], Many indigenous tribes engaged in constant warfare. [39] Since only four percent of the Amazon's hydropower potential has been developed in countries like Brazil,[40] more damming projects are underway and hundreds more are planned. The northern flow keeps the name IJssel until it flows into Lake IJsselmeer. The Alsace on the left banks of the Upper Rhine was sold to Burgundy by Archduke Sigismund of Austria in 1469 and eventually fell to France in the Thirty Years' War. The weather is a cold and harsh climate. The dolphins use echolocation to navigate and hunt in the river's tricky depths. Scijmonsbergen (1999) contends that width changes in the Jamuna may respond to these faults and they may also cause increased sedimentation upstream of the fault. The Lahajang and the Elengjany were also important rivers. [25] In the Miocene period, the watershed of the Rhine reached south, only to the Eifel and Westerwald hills, about 450 km (280 mi) north of the Alps. The Padma and Meghna converge near Chandpur and flow out into the Bay of Bengal.

[68], The tucuxi (Sotalia fluviatilis), also a dolphin species, is found both in the rivers of the Amazon basin and in the coastal waters of South America. But then, at the so-called Rheinbrech, the Rhine water abruptly falls into the depths because of the greater density of cold water.

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