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Swampy Summit
Swampy Summit is a prominent hill to the north of Dunedin, New Zealand. It reaches a height of . The hill's eastern slopes forms the western side of Leith Valley, the other side of which consists of the flank of Mount Cargill. The Leith Saddle is 2500 metres to the east of Swampy Summit's peak. Both the Water of Leith, New Zealand, Water of Leith and the Waitati River (which forms the valley on the north side of the Leith Saddle) have their sources on Swampy Summit's eastern flank. As the name suggests, a regionally significant of wetland lies to the southeast, close to the peak of Swampy Summit. The wetland is largely composed of peat bog which formed in a hollow near the summit, over which sphagnum moss has grown.Automobile Association New Zealand. (1987) ''AA Guide to Walkways: South Island, New Zealand.'' Willoughby, NSW: Weldon Publishing. pp. 205–209. Beyond the wetland lies a subordinate peak, Swampy Spur. To the west of Swampy Summit, the land falls away to form the ...
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The Silverpeaks
The Silverpeaks (sometimes spelt Silver Peaks) is an area of rough forest and tussock and scrub covered hill country inland and to the northwest of Dunedin, New Zealand. The area is largely uninhabited; the main indication of human activity is the Taieri Gorge Railway, which preserves the route of the former Otago Central Railway that runs along the steep-sided valley of the Taieri River. Much of the area lies within the Silverpeaks Scenic Reserve. Background A network of walking tracks crisscross the area. From Pulpit Rock, trampers descend the Devil's Staircase into a lush valley just a short distance from Jubilee Hut. Access to these tracks is mainly via Double Hill Road, a rural road that leaves SH1 close to Waitati, and from several rural roads that leave SH87 between Outram and Middlemarch. Several of the peaks rise to above 600 metres. The highest points in the Silverpeaks include Silver Peak (753 m), known in Māori as Huatea,Place names'' on Kāti Huirapa Run ...
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Peat Bog
A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; alkaline mires are called fens. A baygall is another type of bog found in the forest of the Gulf Coast states in the United States.Watson, Geraldine Ellis (2000) ''Big Thicket Plant Ecology: An Introduction'', Third Edition (Temple Big Thicket Series #5). University of North Texas Press. Denton, Texas. 152 pp. Texas Parks and Wildlife. Ecological Mapping systems of Texas: West Gulf Coastal Plain Seepage Swamp and Baygall'. Retrieved 7 July 2020 They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink. Bogs occur where the water at the ground surface is acidic and low in nutrients. In contrast to fens, they derive most of t ...
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Geography Of Dunedin
Dunedin ( ; mi, Ōtepoti) is the second-largest city in the South Island of New Zealand (after Christchurch), and the principal city of the Otago region. Its name comes from , the Scottish Gaelic name for Edinburgh, the capital of Scotland. The city has a rich Scottish, Chinese and Māori heritage. With an estimated population of as of , Dunedin is both New Zealand's seventh-most populous metro and urban area. For historic, cultural and geographic reasons the city has long been considered one of New Zealand's four main centres. The urban area of Dunedin lies on the central-eastern coast of Otago, surrounding the head of Otago Harbour, and the harbour and hills around Dunedin are the remnants of an extinct volcano. The city suburbs extend out into the surrounding valleys and hills, onto the isthmus of the Otago Peninsula, and along the shores of the Otago Harbour and the Pacific Ocean. Archaeological evidence points to lengthy occupation of the area by Māori prior to the ar ...
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Waikouaiti
Waikouaiti is a small town in East Otago, New Zealand, within the city limits of Dunedin. The town is close to the coast and the mouth of the Waikouaiti River. Today, Waikouaiti is a retail trade and servicing centre for the surrounding district, which has sheep farming as the principal primary activity. A major egg producer, Zeagold Foods, a branch of Mainland Poultry LTD has a 500,000-hen factory farming operation here and is in the process of expanding over the next year to meet demand for egg products. Hawksbury, 3 km southwest of Waikouaiti, has a cheese factory and shop, a swimming pool and housing developed from the old mental health institution, Cherry Farm. Karitane, 3 km to the southeast has a small fishing port. History Prior to the arrival of Europeans the area was occupied by Māori, who had a kaik, or unfortified settlement, at modern Karitane and a pa, or fortified settlement, on the adjacent Huriawa Peninsula. An 1826 sketch of the east Otago coast, ...
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Johnny Jones (pioneer)
John "Johnny" Jones (March 1809 – 16 March 1869) was a trader and settler in New Zealand. Born in Sydney, Jones was the third son of Thomas Jones, one of the early settlers in New South Wales. He spent his early life on sealing and whaling ships, before becoming a ferryman at Port Jackson. He had an entrepreneurial streak and invested his savings in a way that by the age of 20, he had interests in three whaling ships. He married Sarah Sizemore on 7 January 1828 in Sydney, and they had 11 children, although two died as infants. John Richard Jones was his eldest son. In 1835 Jones and Edwin Palmer went into a partnership to purchase a whaling station in New Zealand and a schooner for whaling. Within the next few years, his shrewd business skills allowed him to gain a controlling interest in seven New Zealand whaling stations. In 1838 he bought a whaling station and land near Waikouaiti, and also purchased a large area of land from Ngāi Tahu chief "Bloody Jack" Tuhawaiki, amoun ...
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Flagstaff, Otago
Flagstaff, known in Māori as Te Whanaupaki,Place names'' on Kāti Huirapa Runaka ki Puketeraki website, viewed 2012-01-04 is a prominent hill overlooking the northwest of the city of Dunedin, in New Zealand's South Island. Together with Mount Cargill, which lies to its northeast, it dominates the skyline of the city. Flagstaff lies seven kilometres to the north of Dunedin's city centre. The hill was known by the Māori as ''Whakari'', and an anglicised form of this name is still used for the Dunedin suburb of Wakari, which lies to the south of Flagstaff. The city's first road route to the Taieri Plains, which lie to the west, skirted the slopes of Flagstaff, and is still used as an alternative route out of the city. Flagstaff rises to a height of , and is part of the rim of the Dunedin Volcano, a long-extinct volcano of which the crater forms the Otago Harbour Otago Harbour is the natural harbour of Dunedin, New Zealand, consisting of a long, much-indented stretch of g ...
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Silver Stream
The Silver Stream (sometimes written Silverstream) is a small river flowing close to the town of Mosgiel in Otago, New Zealand. The Silver Stream, known in Māori as Whakaehu,Place names'' on Kāti Huirapa Runaka ki Puketeraki website, viewed 2012-01-04 rises in the Silverpeaks hills north of Dunedin, on the southern slope of Silver Peak itself, and flows initially southwards through a steep-sided forested valley which widens to become Whare Flat, before turning west at the eastern edge of the Taieri Plains at the foot of Three Mile Hill, close to Invermay Research Station. It continues in a southwesterly direction past the northern edge of Mosgiel, reaching the Taieri River two kilometres north of Allanton. Its total length is about . Silver Stream is the site of a historic water race. The Silver Stream Water Race was built between 1877 and 1881, and consisted of nearly of open races, sluices, tunnels, and weirs. The race began at a weir high on the river and traversed the s ...
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Sphagnum Moss
''Sphagnum'' is a genus of approximately 380 accepted species of mosses, commonly known as sphagnum moss, peat moss, also bog moss and quacker moss (although that term is also sometimes used for peat). Accumulations of ''Sphagnum'' can store water, since both living and dead plants can hold large quantities of water inside their cells; plants may hold 16 to 26 times as much water as their dry weight, depending on the species.Bold, H. C. 1967. Morphology of Plants. second ed. Harper and Row, New York. p. 225-229. The empty cells help retain water in drier conditions. As sphagnum moss grows, it can slowly spread into drier conditions, forming larger mires, both raised bogs and blanket bogs. Thus, sphagnum can influence the composition of such habitats, with some describing sphagnum as 'habitat manipulators'. These peat accumulations then provide habitat for a wide array of peatland plants, including sedges and ericaceous shrubs, as well as orchids and carnivorous plants.Keddy, P ...
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Waitati River
The Waitati River is a river in New Zealand, flowing into the Pacific Ocean at Blueskin Bay, north of Dunedin. The Dunedin Northern Motorway follows the valley of the Waitati between the Leith Saddle and Waitati. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākitio R ... References Rivers of Otago Rivers of New Zealand {{Otago-river-stub ...
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New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ...
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Water Of Leith, New Zealand
The Water of Leith (also known as Ōwheo, the River Leith or Leith Stream), is a small river in the South Island of New Zealand. It rises to the north of the city of Dunedin, flowing for southeast through the northern part of the city and the campus of the University of Otago before reaching the Otago Harbour. The name of the city of Dunedin is the anglicised form of ''Dùn Èideann'' which is the Scottish Gaelic form of the name ''Edinburgh'', and thus the river is also named for the Water of Leith which runs through the Scottish capital. The original Māori name for the stream was ''Ōwheo'' ("The place of Wheo"), Wheo being the name of a local chief whose village stood close to its mouth.Herd, J., and Griffiths, G.J. (1980). ''Discovering Dunedin.'' Dunedin: John McIndoe. This name is now rarely used (but the university's computer science department building is named after it). Course The Leith's source is close to the Dunedin Northern Motorway, part of State Highway 1, sou ...
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Leith Saddle
350px, Leith Saddle near Dunedin, New Zealand Leith Saddle is a saddle between the sources of the Water of Leith and the Waitati River, approximately halfway between Dunedin's northern suburb of Pine Hill and the outlying settlement of Waitati. The saddle is a strategic point where the Dunedin Northern Motorway, part of State Highway 1 traverses a fragile alpine forest. Proposed road works to straighten a dangerous corner here conflict with conservation values. Water supply pipelines, and popular tramping and cycling routes also converge at the saddle. The Water of Leith's source is 100 metres to the south of Leith Saddle, at a height of 380 metres above sea level.Hamel, A. (2008). ''Dunedin tracks and trails.'' Dunedin: Silver Peaks Press. The Leith Saddle Track is a 3.5 hour climb through native cloud forest to Swampy Spur and Swampy Summit with links to other walkways in the Silverpeaks and Dunedin's hills.
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