Lake Alexandrina (New Zealand)

Lake Alexandrina

A view of Lake Alexandrina from the top of nearby Mount John
Location Mackenzie District, Canterbury Region, South Island
Coordinates 43°57′S 170°27′E / 43.950°S 170.450°E / -43.950; 170.450Coordinates: 43°57′S 170°27′E / 43.950°S 170.450°E / -43.950; 170.450
Type Mesotrophic
Basin countries New Zealand
Max. length 7.2 kilometres (4.5 mi)
Max. width 0.9 kilometres (0.56 mi)
Surface area 640 hectares (1,600 acres)
Max. depth 27 metres (89 ft)
Residence time 4 years
Surface elevation 732 metres[1]

Lake Alexandrina (Maori: Whakatukumoana) is a lake located in the Mackenzie Basin of New Zealand's South Island. It lies immediately to the west of the much larger Lake Tekapo and further to the east of Lake Pukaki, located to the north of Lake Tekapo township. It is a shallow lake with distinct indications of glacial origin and is spring fed with an outlet on its eastern shore mid-way down the lake.[2][3] The outlet feeds into a smaller lake, Lake MacGregor before feeding into Lake Tekapo described as “Opaque and milky blue” in colour.[3] In the desert terrain of the Mackenzie Plains, Lake Alexandrina is considered as an “oasis of life”. Lake Alexandrina is a nature reserve and a delight to a fisherman, well documented for its brown and rainbow trout and salmon.[4]

Geography

Landscape near the lake

Categorised as a Canterbury High County lake in the Mackenzie Basin, it lies a short distance from Lake Tekapo while also being connected to it.[5] Lake Alexandrina is approached from the State Highway 8 via the Godley Peaks Road.[4] The lake, located at an altitude of 732 metres (2,402 ft),[1] covers an area of 640 hectares (1,600 acres) with width of 0.9 kilometres (0.56 mi) and extending to a length of 7.2 kilometres (4.5 mi). Its shores are flat. The maximum water depth in the lake is reported to be 27 metres (89 ft). The lake catchment has landscape that provides for plentiful wildlife but also has extensive cultivation which brings in a lot of nutrients, enriching the lake's with phosphorus.[2]

The lake's annual balance is contributed by surface streams: 5.72 million m3 (27%), overland flows: 1.11 million m3 (5%), ground water sources: 10.1 million m3 (48%) and precipitation: 4.11 million m3 (20%). The storage in the lake lasts four years.[2]

Chemical properties

Map

The lake has been classified as mesotrophic type. Chlorophyll levels of 0.4–3.8 mg/1 have recorded during observations carried out between November 1978 and March 1979. The total phosphorus at 1 m depth was 0.009–0.015 mg/L as measured in March 1979. The reasons attributed to high nutrient content and consequent high degree of phosphorus levels are due to nutrients entering from the lake catchment, underground sources, grazing on the periphery of the lake, human habitations around the lake, aerial spray and stocking in the trout-spawning streams.[2]

Ecology

The lake catchment is biologically rich, with 45 species of birds, which include the southern crested grebe, shoveler and scaup.[3] The Australian shoveller is a common bird seen in the lake area,[6] as well as pelicans, black swans and ducks. Six species of waterbirds have been recorded in total.[7][8] Paradise shelducks flock here during the summer season, seeking sanctuary when they become flightless during their moult.[7][9] Freshwater snails Potamopyrgus antipodarum have also been analysed in the basin area.[10] For example, studies in 1994 found that there are more male snails in the lake's shallow water than females, and that snails are sicker in shallow water than deep water.[11]

Vegetation

The breeding of the Elodea canadensis species has been inhibited at Lake Alexandrina because of the steep slopes on the east and west sides of the lake, as well as turbulence caused by high winds of 10–14 m/s.[12]

Aqua fauna

The lake has plentiful stocks of brown trout, rainbow trout and salmon, which are well known to fishing enthusiasts. The trout are not found in abundance because of overfishing and inadequate spawning duration. However, the fish do grow to a large size, especially the trout,[13] each weighing as much as 2.5 kilograms (5.5 lb) on an average. Some of prize catch could be of 4.5 kilograms (9.9 lb) weight for rainbows and 6.3 kilograms (14 lb) for brown variety trout (which generally are found along the shores of the lake where flies and insects abound).[4]

Conservation

Lake Alexandrina is one of New Zealand's Scenic Reserves, a valid Crown Protected Area.[14]

Threats

The threats to the lake waters that were identified in the 1980s were the regular occurrence of algal (Anabaena) blooms, which were a result of high nutrient levels of phosphorus, survival of wildlife, and recreational fishery. It was assessed by measurements that nearly 50% of the phosphorus was contributed by groundwater, with 32% from surface water inflows and only 3–9% from hut settlements. This resulted in poor quality of the lake waters and subsequently, measures to check the phosphorus content in the lake received priority attention of the Government of New Zealand.[2]

Conservation measures

In order to take adequate remedial measures to check the inflow of nutrients into the lake, which had raised the phosphorus content in the lake waters to unacceptable levels, in 1984, the "Lake Alexandrina Steering Committee" was set up which identified the problem areas causing deterioration of water quality as due to phosphorus as also from the hut settlements at the outlet and south end, and from agricultural sources. The Taranaki Catchment Commission and the Waitaki Catchment Commission, who examined this issue in 1987, also concluded that though the inflows exceeded outflows, but they did not contribute to the storage due the high sediment contribution which vitiated the storage. Consequent to their study of recorded high total phosphorus levels causing the blooms and creating threats to wildlife and the recreational fisheries, the Commission prescribed interim management guidelines such as: Total cessation of aerial top dressing within 500 metres (1,600 ft) of the eastern shore and 800 metres (2,600 ft) of the western shore and around the flow sources into the lake; restrictions on fertiliser use for agriculture; access to streams for spawning activities and to establish a "deer fence" on the northern end of the wetland; stop all activities related to cultivation on the shores of the lake; stop building of the hut settlements around the lake; install individual household effluent storage or septic tanks; and diversion of sewage outside the catchment. These measures were implemented by the Mackenzie District Council under a District Plan 1997, under the title "Lake Side Protection Area around Lake Alexandrina". Progressively implemented since 1985, the redeeming feature of these actions is that the heavy algal blooms of the 1980s are now infrequent and limited to a frequency occurrence of once in three years.[2]

Tourism

In 1881, 10,000 trout were brought to Mackenzie country and released into Lake Alexandrina, as well as some other lakes, creeks and streams.[15] After the trout grew and prospered, fishing licenses were issued. Lake Alexandrina, now known for its attraction to fisherman, has a small number of fisherman's huts clustered at each end of the lake and near the outlet. Rowing boats are the only mode of transport on the lake as sail and motor boats are prohibited.[3]

Panoramas

Panoramic view of Lake Alexandrina shot from Mount John

References

  1. 1 2 New Zealand journal of marine and freshwater research. Dept. of Scientific and Industrial Research. 1984. p. 219. Retrieved 2 January 2011.
  2. 1 2 3 4 5 6 "Lake Manager's Handbook: Land-Water Interactions. June 2002.". Government of New Zealand. Retrieved January 2, 2010.
  3. 1 2 3 4 "Top Secret – Lake Alexandrina". AA Directions Magazine. March 2009. Retrieved January 2, 2011.
  4. 1 2 3 Orman, Tony (September 1994). 21 Great New Zealand Trout Waters. Stackpole Books. pp. 109–111. ISBN 978-0-8117-2567-5. Retrieved 4 March 2011.
  5. ↑ Wilson, Alexander; Union Steam Ship Company of New Zealand, ltd (1884). Maoriland: an illustrated handbook to New Zealand. G. Robertson. pp. 96–. Retrieved 3 January 2011.
  6. ↑ Phillips, John Charles (1986). A Natural History of the Ducks: Plectropterinae, Dendrocygninae, Anatinae (in part) (2 v.). Courier Dover Publications. p. 32. ISBN 978-0-486-25141-7. Retrieved 4 January 2011.
  7. 1 2 Angas, George French (1847). Savage life and scenes in Australia and New Zealand: being an artist's impressions of countries and people at the Antipodes... Smith, Elder, and co. pp. 122–. Retrieved 2 January 2011.
  8. ↑ University of Auckland. Field Club (1990). Tane. Auckland University Field Club. p. 137. Retrieved 2 January 2011.
  9. ↑ Stuart Chambers (2000). Birds of New Zealand: locality guide. Arun Books. p. 121. ISBN 978-0-473-07327-5. Retrieved 2 January 2011.
  10. ↑ University of Canterbury. Zoology Dept. New Zealand natural sciences. Zoology Dept., University of Canterbury. p. 61. Retrieved 2 January 2011.
  11. ↑ Zimmer, Carl (September 2000). Parasite rex: inside the bizarre world of nature's most dangerous creatures. Simon and Schuster. pp. 167–. ISBN 978-0-684-85638-4. Retrieved 3 January 2011.
  12. ↑ International Association of Theoretical and Applied Limnology (1988). Verhandlungen der Internationalen Vereinigung für Theoretische und Angewandte Limnologie. E. Schweizerbart'sche Verlagsbuchhandlung. Retrieved 2 January 2011.
  13. ↑ Rollett, F. Carr (1920). Angling in New Zealand. Whitcombe & Tombs. Retrieved 2 January 2011.
  14. ↑ Shaw, W. K. (22 May 2009). "Notice of Valid Crown Protected Area Names, Issue No. 73". linz.govt.nz. Land Information New Zealand. Retrieved 3 January 2011.
  15. ↑ Spackman, W. H. (1892). Trout in New Zealand: where to go and how to catch them. G. Didsbury, government printer. pp. 52–. Retrieved 3 January 2011.
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