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See also:AMUR (known also as the See also:Sakhalin-ula) , a See also:river of eastern See also:Asia, formed by the confluence of the Argun and the Shilka, at Ust-Stryelka, in 530 19' N. See also:lat. and 120° 30' E. See also:long . Both these See also:rivers come from the See also:south-See also:west: the Argun, or Kerulen as it is called above See also:Lake Kulun (Dalai-nor), through which it flows about See also:half way between its source and Ust-Stryelka, rises in 49° N. lat. and 109° E. long.; the Shilka is formed by the See also:union of the Onon and the Ingoda, both of which have their See also:sources a little farther See also:north-See also:east than the Kerulen (Argun) . The See also:Amur proper flows at first in a south-easterly direction for about 800 m., as far as long . 132' E., separating See also:Manchuria from the Amur See also:government; it then turns to the north-east, cuts its way through the Little See also:Khingan mountains in a See also:gorge 2000 ft. wide and 140 M. long, and after a See also:total course of over 1700 M. discharges into the See also:Sea of See also:Okhotsk, opposite to the See also:island of See also:Sakhalin . It is estimated to drain an See also:area of 772,000 sq. m. its See also:principal tributaries from the south are the Sungari, which the See also:Chinese consider to be the true See also:head-river of the Amur, and the Usuri; from the north it receives the Oldoi, Zeya, Bureya, Kur, Gorin and Amgun . As the mouth is choked with sandbanks, goods are disembarked at See also:Mariinsk and carried by See also:train (9 m.) to See also:Alexandrovsk at the head of the Gulf of Tartary . See also:Navigation on the river is open from See also:April to See also:early in See also:November . See T . W . See also:Atkinson, Travels in the Region of the Amoor (186o); See also:Collins, Exploration of the Amoor (ed . 1864) and Voyage down the Amoor (1866) ; See also:Andree, See also:Des Amurgebiet (ed . 1876) ; and Grum-Grshimaylo, See also:Account of the Amur (See also:Russian, 1894) .
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