Fork Stream | |
---|---|
Location | |
Country | New Zealand |
Physical characteristics | |
Source | |
• location | Gamack Range |
Mouth | |
• location | Tekapo River |
The Fork Stream is a river in the Canterbury region of New Zealand. It arises in the Gamack Range and flows south-east into the Tekapo River, which exits at Lake Benmore and eventually via the Waitaki River into the Pacific Ocean. Fraser Stream is a tributary. [1] [2] A high proportion of the stream's flow comes from snow melt. [3]
There are trout in the stream. [4]
The Mackenzie Basin, popularly and traditionally known as the Mackenzie Country, is an elliptical intermontane basin located in the Mackenzie and Waitaki Districts, near the centre of the South Island of New Zealand. It is the largest such basin in New Zealand. Historically famous mainly for sheep farming, the sparsely populated area is now also a popular tourism destination.
The Waitaki River is a large braided river in the South Island of New Zealand. It drains the Mackenzie Basin and runs 209 kilometres (130 mi) south-east to enter the Pacific Ocean between Timaru and Oamaru on the east coast. It starts at the confluence of the Ōhau and Tekapo rivers, now at the head of the artificial Lake Benmore, these rivers being fed by three large glacial lakes, Pukaki, Tekapo, and Ōhau at the base of the Southern Alps. The Waitaki flows through Lake Benmore, Lake Aviemore and Lake Waitaki, these lakes being contained by hydroelectric dams, Benmore Dam, Aviemore Dam and Waitaki Dam. The Waitaki has several tributaries, notably the Ahuriri River and the Hakataramea River. It passes Kurow and Glenavy before entering the Pacific Ocean. The River lends its name the Waitaki District on the south side of the river bank.
Lake Tekapo is the second-largest of three roughly parallel lakes running north–south along the northern edge of the Mackenzie Basin in the South Island of New Zealand. It covers an area of 83 km2 (32 sq mi) and is at an altitude of 710 m (2,330 ft) above sea level.
Lake Tekapo is a small township located at the southern end of the lake of the same name in the inland South Island of New Zealand. It had 558 residents according to the 2018 census, being one of five settlements in the sparsely populated Mackenzie Basin.
The Hakataramea River flows generally south through the Hakataramea Valley, which is separated from the more inland Mackenzie Basin by the Kirkliston Range in Canterbury, New Zealand.
The Tekapo River flows occasionally through the Mackenzie Basin, Canterbury, in New Zealand's South Island, although the riverbed is now often dry in the upper reaches. It maintains a constant flow below the confluence of several tributaries, notably the Maryburn, Forks, and Grays rivers.
The Pukaki River flows through the Mackenzie Basin, Canterbury, in New Zealand's South Island.
The Grays River is a tributary of the Tekapo River in the Mackenzie Basin of New Zealand. It flows southwest for 25 kilometres (16 mi), joining the larger river southeast of Lake Pukaki.
Lake Alexandrina 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 midway down the lake. The outlet feeds into a smaller lake, Lake MacGregor before feeding into Lake Tekapo described as “Opaque and milky blue” in colour. In the desert terrain of the Mackenzie Plains, Lake Alexandrina is considered as an “oasis of life”. Lake Alexandrina is a Wildlife Refuge and a delight to a fisherman, well documented for its brown and rainbow trout and salmon.
South Canterbury is the area of the Canterbury Region of the South Island of New Zealand bounded by the Rangitata River in the north and the Waitaki River to the south. The Pacific Ocean and ridge of the Southern Alps form natural boundaries to the east and west respectively. Though the exact boundaries of the region have never been formalised, the term is used for a variety of government agencies and other entities. It is one of four traditional sub-regions of Canterbury, along with Mid Canterbury, North Canterbury, and Christchurch city.
Allan David Dick was a New Zealand politician of the National Party.
The Halswell River is a river in the Canterbury region of New Zealand.
The Kurow River is a river of North Otago, New Zealand. A tributary of the Waitaki River, it rises in Saint Marys Range and flows into that river downstream of Kurow.
The Little Awakino River is a river of North Otago, New Zealand. A tributary of the Waitaki River, it flows into that river a short distance downstream of Lake Waitaki.
The Macaulay River is a river of the Mackenzie Country of New Zealand's South Island. It flows south from the Two Thumb Range, part of the Southern Alps, its valley merging with that of the Godley River shortly before it enters the northern end of Lake Tekapo.
The Mistake River is a river of the Canterbury region of New Zealand's South Island. It flows south from the Hall Range to the northwest of Lake Tekapo, turning east at the southern end of the range to flow into the western edge of the lake.
The Twizel River is a river of the Mackenzie Basin, in the Canterbury region of New Zealand's South Island. It is part of the Waitaki River system. It was named for Twizel Bridge in Northumberland by John Turnbull Thomson, Chief Surveyor of Otago in the mid 1800s.
The Two Thumb Range is a range of mountains in the Canterbury Region of New Zealand's South Island. It is located to the east of Lake Tekapo and has several peaks which rise to around 2,500 metres (8,200 ft). The southern end of the range contains one of Canterbury's main skifields, Mount Dobson.
Bortons is a small settlement on the southern bank of the Waitaki River in New Zealand's South Island. It is located on SH 83, 7 km east of Duntroon.
44°00′16″S170°24′54″E / 44.00444°S 170.41500°E