Jump to content

Onyx River

Coordinates: 77°33′24″S 161°45′0″E / 77.55667°S 161.75000°E / -77.55667; 161.75000
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by JCW-CleanerBot (talk | contribs) at 16:45, 9 July 2020 (→‎Environment: task, replaced: Bioscience → BioScience). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

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 / 77.43000°S 162.75000°E / -77.43000; 162.75000
MouthLake Vanda
 • coordinates
77°33′24″S 161°45′0″E / 77.55667°S 161.75000°E / -77.55667; 161.75000
Length32 km (20 mi)

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]

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 700 cubic feet per second (20 m3/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 small animals (nematodes, tardigrades, and rotifers) live in the river. Gulls 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. 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.

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. ^ [1]. 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. Retrieved March 11, 2018.

External links

  • "Antarctica’s longest river", p 16, and "What the flood revealed", pp 15–21, Antarctic Sun, January 26, 2003