Jump to content

Selwyn River

Coordinates: 43°45′S 172°26′E / 43.750°S 172.433°E / -43.750; 172.433
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Schwede66 (talk | contribs) at 20:24, 30 June 2017 (tidy up, replaced: → [[Canterbury, New Zealand|, [[New Zealand → New Zealand (2), [New Zealand State Highway network → [New Zealand state highway network using AWB). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Selwyn River
Map
Physical characteristics
Source 
 • locationSouthern Alps
Mouth 
 • location
Lake Ellesmere / Te Waihora
Length80 km (50 mi)

The Selwyn River / Waikirikiri flows through the Selwyn District of Canterbury in the South Island of New Zealand.[1]

Description

The river has its source in the foothills of the Southern Alps and flows east for 80 kilometres (50 mi) before emptying into Lake Ellesmere / Te Waihora, south of Banks Peninsula. Terrace cliffs above the river's upper reaches gave the town of Whitecliffs its name.

For much of its course the river flows through wide shingle channels. In drought years, the river can disappear beneath this bed and seem to dry up completely. This frequently occurs where State Highway 1 crosses the river at the settlement of Selwyn, about 20 kilometres (12 mi) upstream from its outflow into Lake Ellesmere.

In the foothills, the Selwyn flows year-round. On the plains, the riverbed is highly permeable, and the river overlays a deep and porous aquifer. As soon as the river reaches the plains, water begins leaking down through the bed and into the aquifer. In most months, all river-water disappears within 5 kilometres (3 mi) of leaving the foothills. The next 35 kilometres (22 mi) of the river remains dry for most of the year, apart from a small section around the confluence with the permanently flowing Hororata River. About 15 kilometres (9 mi) upstream from Lake Ellesmere shallow groundwater rises back to the surface, and the Selwyn becomes permanent again.

Disappearing river flows have significant ecological effects: when the river’s surface water disappears, so does the habitat for many aquatic plants and animals. In response to loss of surface water, aquatic invertebrates and fish must disperse, seek refuge in remnant aquatic habitats, or die. Aquatic plants, algae, and bacteria must form resting stages or die. The dry central reaches of the Selwyn River also constitute a significant barrier for dispersal of invertebrates and for fish migrating between Lake Ellesmere and the headwaters.[2]

Naming

The Selwyn River and its gorge were named in 1849 by the chief surveyor of the Canterbury Association, Joseph Thomas, for Bishop Selwyn. The name was later adopted for the township, the district, and an electorate.[3]

References

  1. ^ "Place name detail: Selwyn River/Waikirikiri". New Zealand Gazetteer. New Zealand Geographic Board. Retrieved 5 April 2008.
  2. ^ Mike Scarsbrook; Scott Larned; Graham Fenwick; Dave Kelly. "Biodiversity in a disappearing river". NIWA. Retrieved 22 March 2013.
  3. ^ Reed, A. W. (2010). Peter Dowling (ed.). Place Names of New Zealand. Rosedale, North Shore: Raupo. p. 362. ISBN 9780143204107.

43°45′S 172°26′E / 43.750°S 172.433°E / -43.750; 172.433