| 词条 | Lake Grassmere |
| 释义 |
| name = Lake Grassmere / Kapara Te Hau | image = Cape Campbell sunrise.jpg | caption = | image_bathymetry = | caption_bathymetry = | location = Marlborough Region, South Island | coords = {{coord|41|44|S|174|10|E|region:NZ_type:waterbody|display=inline,title}} | type = lagoon | inflow = none | outflow = | catchment = | basin_countries = New Zealand | length = | width = | area = {{convert|17|km2|mi2|abbr=on}} | depth = | max-depth = | volume = | residence_time = | shore = | elevation = | islands = | cities = }} Lake Grassmere / Kapara Te Hau is a New Zealand lake in the northeastern South Island, close to Cook Strait. The lake is used for the production of salt. GeographyLake Grassmere, {{convert|25|mi|km}} south of Blenheim and {{convert|6|mi|km|0}} south of the mouth of the Awatere River, is a shallow lagoon protected from the open sea by a single barrier beach covered by sand dunes. It is on the north-easterly extension of the Ward depression. Covering an area of {{convert|17|km2|mi2}}, it has no natural inflow and is prone to strong warm winds. Close to the sea, it also has a very high salinity. Because of these geographical characteristics, it is ideal for natural salt extraction. Grassmere has been divided into solar evaporation ponds. Seawater is pumped in, and moved between ponds over several months, increasing in salinity with each successive evaporation period. As salinity increases, crystallised salt forms and is extracted. Grassmere's area varies between {{convert|3500|and|4400|acre|km2}}; this maximum is attained only in rare floods. The watershed is small. The climate, with a low average rainfall of {{convert|585|mm|in}} and prevailing strong and dry north-westerly winds, provides Lake Grassmere with the suitable conditions required for natural economic salt production. Early historyThe Māori name for the lake is Kapara Te Hau ("wind-blown lake"). Early whalers on the coast rendered this name “Cobblers' Hole”. According to Māori oral tradition, the lake occupies the site of early cultivations. Kupe, the navigator, is said to have poured salt water on these cultivations, thus creating the lake. In pre-European times it was used as a ready source of food, as it attracts a wide range of waterfowl. In 1832–33, a year after Ngāti Toa under the leadership of Te Rauparaha had defeated Ngāi Tahu at Kaiapoi and Banks Peninsula, Ngāti Toa visited the lake to take moulting ducks. A Ngāi Tahu force, having learned of this impending visit, laid an ambush. Scouts from Te Rauparaha's party found the locality apparently uninhabited and the canoes were driven ashore. On landing, the visitors were taken by surprise and sustained heavy casualties. Te Rauparaha was seized by Tūhawaiki, who was anxious to take him alive. The captive, however, after feigning resignation, was less tightly held. He then slipped out of his flax garment, swam to a canoe and made his escape. Salt industryUntil the 1940s Grassmere's bed was a mud bath in winter and a dustbowl in summer, with the occasional natural deposit of salt. The salt industry began in 1943 and now occupies one-third of the suitable lake area of {{convert|3800|acre|km2|order=flip}}. The 1960 production was 17,000 tons.
In addition to low rainfall, Grassmere is perfectly suited to solar salt production.
In the mid 1960s harvests were carried out with a new pattern of crystallising ponds which have special provision for draining off rainwater before it has had time to mix with the brine concentrate. The harvest for 1964–65 reached 30,000 tons, a record at the time. By 1970 the harvest had increased to almost 52,000 tonnes, but this could not match demand, which had grown with industrial development (especially from freezing works and pulp and paper mills). It became evident that Grassmere could not meet New Zealand's salt requirements. Bulk shipments of salt from the Caribbean and Australia were landed at Mt Maunganui, where a vacuum salt plant was built. This produced the high-purity salt needed by producers in the dairy and pharmaceutical industries. A second, smaller vacuum plant was built at Grassmere. Some rolling stock from the railway at Grassmere salt works is preserved at the Ferrymead Two Foot Railway. EconomicsA large range of salts with slightly different chemical compositions, grain sizes and shapes are produced at Lake Grassmere. All table salt produced in New Zealand is solar salt, and both iodised and non-iodised table salt are available. Iodised salt contains added iodine (to prevent goitre) and silicon dioxide (to make the salt run). Specialty salts, including flaky salt, are also produced at Lake Grassmere. Animal health products such as salt licks for farm animals are produced at Grassmere and Mt Maunganui. At the end of summer Grassmere's gleaming white salt piles are easily seen from State Highway 1. This seasonal landmark forms a vivid contrast to the burnt brown of the Marlborough hills. Seismic activityA fault running underneath Lake Grassmere triggered a magnitude 6.6 earthquake on Friday, August 16, 2013 at 2:31:05 pm.[1] The quake was {{convert|8|km|mi|0}} deep and was strike-slip fault similar to the 2013 Seddon earthquake on July 21, thus considered a doublet earthquake. Official nameThe official name of the lake become a dual name as a result of the Ngāi Tahu Claims Settlement Act 1998.[2] References1. ^http://info.geonet.org.nz/display/home/M6.6+Lake+Grassmere+earthquake M6.6 Lake Grassmere earthquake 2. ^{{cite web|url=http://www.nzlii.org/nz/legis/hist_act/ntcsa19981998n97295|title=Ngai Tahu Claims Settlement Act 1998}} External links
3 : Lakes of New Zealand|Landforms of the Marlborough Region|Saline lakes of Oceania |
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