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Know : A list of the oldest rivers on Earth

The age of a river is difficult to determine. Generally, the age is estimated based upon which mountains are the source of the river, the age of any mountains it dissects, the sea or ocean to which it eventually outflows, and where it forms its delta. For instance, if a river dissects a mountain range, then this often means the river existed before the mountain range rose.
Each of these factors can make a final contribution in determining the age of a river. Below follows an incomplete list of rivers older than 1 Ma (One million years = 1,000,000 years).
Continent color key
AfricaAsiaOceaniaEuropeNorth AmericaSouth America
RiverAge (Ma)OutflowMost significant criterion for the age
1. 380North SeaPaleozoic, dissects the Ardennes during the Hercynian
2. 350-400Lake Eyre
(intermittent)
Predates the Alice Springs Orogeny; many other rivers in the Northern Territory are of a similar age
2.
(Chang Jiang)
365East China SeaCrosses Paleozoic and Mesozoic mountains
3.  
(Kanawha River)
300Kanawha RiverDissects the Appalachian Mountains
4.Susquehanna River300Chesapeake BayDissects the Appalachian Mountains
5.Nile250Mediterranean SeaMesozoic
6.Rhine240North SeaTriassic, maybe older because of the Hercynian; not the Eocene with the Alps, nor the Miocene with the Upper Rhine Graben
7.Save205Indian OceanFormed during rifting when Gondwana broke up.
8.Amazon200Atlantic OceanJurassic, but it seems to have flowed in the opposite direction as an extension of the Congo, i.e. long before the formation of Andes
9.Amur125Sea of OkhotskKnown to be at least Cretaceous in age, but crosses mountains even older
10.Macleay River80Tasman SeaPredates uplift of Great Escarpment
11.Murrumbidgee River75Murray RiverPredates uplift of Australian Alps
12.Colorado
(Western U.S.)
75Gulf of CaliforniaUplift during Laramide orogeny, see Geology of the Grand Canyon area
13.Thames58North SeaLate Palaeocene Period Thanetian Stage.
14.
(Sindhu)
45Arabian SeaSource in the Himalayas and Karakoram Mountains

Courtesy : Wikipedia 
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