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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. At 32 kilometres (20 mi) in length, it is the longest river in Antarctica.[1]

Onyx River
Onyx River flowing into Lake Vanda
Onyx River Map
Location
CountryAntarctica
Physical characteristics
SourceLake Brownworth
  coordinates77°25′48″S 162°45′0″E
MouthLake Vanda
  coordinates
77°33′24″S 161°45′0″E
Length32 km (20 mi)
Discharge 
  maximum20 cubic metres per second (700 cu ft/s)

Geography


The Onyx River flows away from the ocean, an example of endorheic drainage, as the Wright Lower Glacier blocks the mouth of the Wright 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 20 cubic metres per second (700 cu ft/s).[2]


Environment


There are no fish in the Onyx River, but it supports microscopic life, and the algal blooms can be quite extensive. The environment consists mainly of cyanobacteria and other algae. A few micro-animals (nematodes, tardigrades, and rotifers) live in the river. Skuas are also occasionally present in the area.[3]


Monitoring


The Onyx River is one of the many sites studied by the United States Antarctic Program of the National Science Foundation. Discharge data has been collected at the downstream gauge near Lake Vanda since 1969 and at the upstream gauge near the Wright Lower Glacier since 1972. [4] The Antarctica New Zealand program once maintained a semi-permanent camp at Lake Vanda which has since been removed. There is a small research shelter at Lake Vanda at its eastern end. Nearby is the Comprehensive Test Ban Treaty Seismic station at Bull Pass.

Since records have been kept, the Onyx River's flow season has shifted earlier and gotten longer.[4]

Map of Wright Valley with Onyx River and Lake Vanda
Map of Wright Valley with Onyx River and Lake Vanda

See also



References


  1. Nick Middleton. Rivers: A Very Short Introduction. (page 26) ISBN 9780199588671
  2. . The Antarctic Sun. 27 September 2013. Retrieved 18 April 2015
  3. McKnight, Diane M.; Niyogi, Dev K.; Alger, Alexander S.; Bomblies, Arne; Conovitz, Peter A.; Tate, Cathy M. (December 1, 1999). "Dry Valley Streams in Antarctica: Ecosystems Waiting for Water". BioScience. 49 (12): 985–995. doi:10.2307/1313732. JSTOR 1313732.
  4. Gooseff, Michael N.; McKnight, Diane M.; Doran, Peter T.; Lyons, W. Berry (2007). "Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969". Open-File Report. USGS. doi:10.3133/ofr20071047SRP088. Retrieved 2 March 2022.



На других языках


[de] Onyx River

Der Onyx River ist mit rund 30 km der längste Fluss auf dem antarktischen Kontinent.
- [en] Onyx River

[it] Onyx (fiume)

Il fiume Onyx è un corso d'acqua dell'Antartide, originato da acqua di fusione glaciale, che scorre in direzione ovest nella valle di Wright.

[ru] Оникс (река)

Оникс — самая длинная река Антарктиды. Расположена в долине Райт[en] на Земле Виктории, в сухих долинах Мак-Мердо, характеризующихся почти круглогодичным отсутствием снега, высоким уровнем инсоляции и относительно (для Антарктиды) высокими летними температурами. Длина реки — около 30 км; она вытекает из озера Браунуорт[en] и впадает в озеро Ванда.



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