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Onyx River : ウィキペディア英語版
Onyx River

The Onyx River is an Antarctic meltwater stream which flows westward through the Wright Valley from Wright Lower Glacier and Lake Brownworth at the foot of the glacier to Lake Vanda, during the few months of the Antarctic summer. Despite being only in length it is the longest river in Antarctica.〔Nick Middleton. Rivers: A Very Short Introduction. (page 26) ISBN 9780199588671〕
==Geography==
The Onyx river flows away from the ocean, an example of endorheic drainage, as the Wright Glacier blocks the entrance to the valley. It has several tributaries, and there are multiple meteorological stations along the length of the river. Flow levels are highly variable, both during the day and between summers, with the river failing to reach the lake some years. In contrast, it can cause significant erosion in flood years, and was rafted in 1984 by New Zealand researchers. At one time, the river's discharge reached 〔(). The Antarctic Sun. 27 September 2013. Retrieved 18 April 2015〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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