Bradshaw Sound
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Bradshaw Sound
Kaikiekie / Bradshaw Sound is one of the larger New Zealand fiords. It is one of the sub fiords/arms that make up the Doubtful Sound/ Thompson Sound complex and forms the northernmost of the blind or dead end fiords in this system. History It was named by Captain Stokes of HMS ''Acheron'', who gifted the name to R. Bradshaw, his first mate. The Māori call the fiord Kaikiekie, which translates as “to eat kiekie”, the kiekie being a native climbing plant. In October 2019, the name of the fiord was officially altered to Kaikiekie / Bradshaw Sound. Geography At the upper reaches of the sound, it sub divides into two smaller arms. To the north is the short Precipice Cove, and to the south the longer Kutu Parera (Gaer Arm). The northern inlet Precipice Cove is guarded at its southern entrance by Macdonell Island. It offers sheltered anchorage from the prevailing westerly and as such Several small tour companies ( such aFiordland Expeditionsand Real Journeys) use this as ...
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Tasman Sea
The Tasman Sea (Māori: ''Te Tai-o-Rēhua'', ) is a marginal sea of the South Pacific Ocean, situated between Australia and New Zealand. It measures about across and about from north to south. The sea was named after the Dutch explorer Abel Janszoon Tasman, who in 1642 was the first known person to cross it. British explorer Lieutenant James Cook later extensively navigated the Tasman Sea in the 1770s during his three voyages of exploration. The Tasman Sea is informally referred to in both Australian and New Zealand English as the Ditch; for example, "crossing the Ditch" means travelling to Australia from New Zealand, or vice versa. The diminutive term "the Ditch" used for the Tasman Sea is comparable to referring to the North Atlantic Ocean as "the Pond". Climate The south of the sea is passed over by depressions going from west to east. The northern limit of these westerly winds is near to 40°S. During the southern winter, from April to October, the northern branch ...
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Camelot River
The Camelot River is a river of Fiordland National Park, 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 count .... It is formed from the confluence of the Elaine Stream and Cozette Burn and flows west into the Gaer Arm of Kaikiekie / Bradshaw Sound. The estuary is protected by the Kutu Parera (Gaer Arm) Marine Reserve. See also * List of rivers of New Zealand ReferencesLand Information New Zealand- Search for Place Names Rivers of Fiordland {{Fiordland-river-stub ...
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Misty River
The Misty River is a river in Fiordland, New Zealand. It rises to the east of Irene Pass and flows westward into Teardrop Lake and on to Kaikiekie / Bradshaw Sound Kaikiekie / Bradshaw Sound is one of the larger New Zealand fiords. It is one of the sub fiords/arms that make up the Doubtful Sound/ Thompson Sound complex and forms the northernmost of the blind or dead end fiords in this system. History It .... See also * List of rivers of New Zealand References Rivers of Fiordland Fiordland National Park {{Fiordland-river-stub ...
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Rum River (New Zealand)
The Rum River is a slow, meandering stream that connects Minnesota's Mille Lacs Lake with the Mississippi River. It runs for U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed October 5, 2012 through the communities of Onamia, Milaca, Princeton, Cambridge, Isanti, and St. Francis before ending at the city of Anoka, roughly 20 miles northwest of Minneapolis. It is one of the six protected Wild and Scenic rivers in Minnesota. History The early explorer Louis Hennepin is credited with being the first European to lay eyes upon the Rum. He was taken to see it during the spring of 1680, while under the captivity of a party of Dakota. He referred to it as the St. Francis river in his published journals, although obviously the name didn't stick. The current river bearing the name St. Francis River, located 12 miles west of the Rum, parallels the flow of the Rum. The Rum River makes a sharp turn southward at Cambridge, Minne ...
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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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Fiords Of New Zealand
The fiords of New Zealand are all located in the southwest of the South Island, in a mountainous area known as Fiordland. A fiord is a narrow inlet of the sea between cliffs or steep slopes, which results from marine inundation of a glaciated valley. The spelling ''fiord'' is used in New Zealand rather than ''fjord'', although all the maritime fiords instead use the word ''sound'' in their name. The Marlborough Sounds, a series of deep indentations in the coastline at the northern tip of the South Island, are in fact drowned river valleys, or rias. The deeply indented coastlines of Northland and Auckland also host many rias, such as the Hokianga and Waitematā Harbours. New Zealand has fifteen named maritime fiords, listed here from northernmost to southernmost.Distance measured down centreline of fiord from coastline to head of longest arm of fiord. List Thompson Sound separates Secretary Island from the mainland and connects with Doubtful Sound and Bradshaw Sound at its i ...
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Doubtful Sound
Doubtful Sound / Patea is a fiord in Fiordland, in the far south west of New Zealand. It is located in the same region as the smaller but more famous and accessible Milford Sound / Piopiotahi. It took second place after Milford Sound as New Zealand's most famous tourism destination. At long, Doubtful Sound / Patea is the second longest, and with a depth of up to the deepest of the South Island's fiords. In comparison with Milford Sound, it is more widespread, with the cliffs not as dramatically tall and near vertical. However, the U-shaped profile of the fiord is obvious, in particular on the two innermost of the main fiord's arms and the hanging side valleys along the main fiord. Like most of Fiordland, Doubtful Sound receives a high amount of rainfall, ranging from an annual average of . The vegetation on the mountainous landscape surrounding the fiord is dense native rainforest. History Doubtful Sound was named 'Doubtful Harbour' in 1770 by Captain Cook, who did not ...
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Te Awa-o-Tū / Thompson Sound
Thompson Sound (; officially Te Awa-o-Tū / Thompson Sound) is a fiord of the South Island of New Zealand. It is one of the fiords that form the coast of Fiordland. Geography The fiord is connected at its farthest extent with Pendulo Reach, part of Doubtful Sound / Patea, and between them Thompson and Doubtful Sounds form the non-Tasman Sea coast of Secretary Island. It is 21 kilometres in length. Kaikiekie / Bradshaw Sound, which extends east from the junction of Doubtful and Thompson Sounds, is geographically and geologically an extension of Thompson Sound. Several small rivers flow into Thompson Sound, among them the Pandora and Namu Rivers. History Thompson Sound was given its European name by John Grono, a sealer who worked the Fiordland coast in the early 19th century, after his boat's owner, Andrew Thompson.Foster, A.Sounds Complicated, ''New Zealand Geographic'', 37, January–March 1998. Retrieved 30 September 2017. Grono himself is honoured in the name of the 119 ...
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John Lort Stokes
Admiral John Lort Stokes, RN (1 August 1811 – 11 June 1885)Although 1812 is frequently given as Stokes's year of birth, it has been argued by author Marsden Hordern that Stokes was born in 1811, citing a letter by fellow naval officer Crawford Pasco congratulating him on his birthday in 1852. was an officer in the Royal Navy who travelled on for close to eighteen years. Biography Born on 1 August 1811, son of Henry Stokes, of Scotchwell, near Haverfordwest, Pembrokeshire, and Anne, daughter of Dr George Phillips, Stokes joined the Royal Navy on 20 September 1824. The first ship he served on was , and then in October 1825 he joined the crew of ''Beagle'' under Captain Phillip Parker King. ''Beagle'' was involved in a survey of the waters of South America. In 1828 the commander of HMS ''Beagle'', Pringle Stokes (not related to John Lort Stokes), committed suicide and Robert FitzRoy assumed command; the ship returned to England in 1830 and was recommissioned. From 1831 to 1836 S ...
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HMS Acheron (1838)
HMS ''Acheron'' was the last wooden paddle sloop ordered for the Royal Navy. She was launched at Sheerness in 1838. She spent two commissions in the Mediterranean before being reclassed as a survey ship in 1847.Lyon Winfield, page 158 Between 1848 and 1851 she made a coastal survey of New Zealand, the first such survey since Captain Cook. She was paid off at Sydney and was tender to ''HMS Calliope''.Winfield She was sold at Sydney in 1855. ''Acheron'' was the second named vessel since it was used for an 8-gun Bomb, purchased in October 1803 then captured by the French in the Mediterranean and burnt on 3 February 1805. Construction She was initially ordered from Chatham Dockyard on 15 September 1837, but three days later this was changed to Sheerness Dockyard because the relevant tooling was already present there. The Vessel was named on 27 September and laid down in October. She was launched on 23 August 1838. She was completed for sea at Sheerness om 8 January 1839 at a firs ...
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Māori People
The Māori (, ) are the indigenous Polynesian people of mainland New Zealand (). Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed their own distinctive culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Initial contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi in 1840, the two cultures coexisted for a generation. Rising tensions over disputed land sales led to conflict in the 1860s, and massive land confiscations, to which ...
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Kiekie (plant)
Kiekie (''Freycinetia banksii'') is a densely branched, brittle, woody climber native to New Zealand. It is a member of the screwpalm family Pandanaceae. Kiekie has numerous cane-like stems up to 40 mm in diameter, which freely produce aerial roots. It climbs tree trunks, or forms dense tangles on the forest floor. Its stems and leaves are a dominant feature in many areas of New Zealand forest, the stems eventually reaching up to 30 m long. The leaves are long and slender, 60–90 cm long and 2-2.5 cm broad. Distribution Kiekie is found in forests throughout the North Island. In the South Island, kiekie is more common in higher rainfall areas, reaching its southern limit near the Clarence river in the east and in Fiordland in the west. Classification In 1973, B.C. Stone argued that ''F. banksii'' should be regarded as a subspecies of ''F. baueriana'' of Norfolk Island (Stone 1973). Subsequent to this, de Lange et al. (2005:591-592), countered Stone's argument ...
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