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Bowen River (New Zealand)
The Bowen River is a river in northern Fiordland, New Zealand. The river originates near Mount Grave and is joined by many small streams on its way south through the valley. After close to , the river plunges from the hanging valley over the Lady Bowen Falls and drains into the head of Milford Sound. The falls are named for Diamantina Bowen, wife of George Bowen, the fifth Governor of New Zealand. As one of only two permanent waterfalls in Milford Sound, the falls provide electricity for the Milford Sound settlement by feeding a small hydroelectric scheme, and are also the water source for the settlement. A track leading to the base of the falls was closed in 2003 due to rock falls and instability, but was partly re-opened in 2018 with the first section of the track now replaced by a short ride in a small boat from the Freshwater Basin Terminal in Milford. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan Rive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diamantina Bowen
Diamantina, Lady Bowen (; 1832/1833–1893), was a noble from the formerly Venetian Ionian Islands who became the wife of Sir George Bowen, the first Governor of Queensland. Personal life The '' Contessa'' Diamantina di Roma was born in 1832 or 1833 on Zakynthos, the United States of the Ionian Islands, then a British protectorate, today in Greece. Her place of birth was Ithaca, as many landmarks in throughout Queensland are named in her honor, “Diamantina”, “Ithaca” and “Roma”. Her parents were Count and his wife Countess Orsola, née di Balsamo. Diamantina was the tenth of their eleven children. Her aristocratic family were descended from the Venetians who had settled in the Ionian Islands for centuries as part of the Stato da Màr. Her father was the President of the Ionian Senate (1850–56), titular Head of State of the United States of the Ionian Islands. He was also appointed a Poet Laureate by Queen Victoria. With such a family, Diamantina had a priv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Milford Sound
Milford Sound / Piopiotahi is a fiord in the south west of New Zealand's South Island within Fiordland National Park, Piopiotahi (Milford Sound) Marine Reserve, and the Te Wahipounamu World Heritage site. It has been judged the world's top travel destination in an international survey (the ''2008 Travelers' Choice Destinations Awards'' by TripAdvisor) and is acclaimed as New Zealand's most famous tourist destination."Real Journeys rapt with Kiwi Must-Do's" ''Scoop'', 13 February 2007. had previously called it the |
Darran Mountains
The Darran Mountains are a prominent range within New Zealand's Fiordland National Park, the country's biggest national park. They contain the park's highest peak, Mount Tūtoko (). The range lies between Milford Sound (Piopiotahi) and the valley of the Cleddau River (to the west) and the broad valley of the Hollyford River to the east at the northern end of the national park. They are bounded to the south by the Homer Saddle, which separates them from the Wick Mountains, and to the north by the coast of the Tasman Sea. The Homer Tunnel lies under the southwesternmost extreme of the range.Dowling, P. (ed.) (2004). ’’Reed New Zealand atlas’’. Auckland: Reed Publishing. Map 89. Other than Mount Tūtoko, other prominent peaks in the range include Mount Madeline () and Mount Christina (). Numerous lakes and tarns are found within the range, among the largest being Lake Adelaide and Lake Marian Lake Marian is an alpine lake at the southern end of the Darran Mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fiordland
Fiordland is a geographical region of New Zealand in the south-western corner of the South Island, comprising the westernmost third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name "Fiordland" comes from a variant spelling of the Scandinavian word for this type of steep valley, "fjord". The area of Fiordland is dominated by, and very roughly coterminous with, Fiordland National Park, New Zealand's largest National Park. Due to the often steep terrain and high amount of rainfall supporting dense vegetation, the interior of the Fiordland region is largely inaccessible. As a result, Fiordland was never subjected to notable logging operations, and even attempts at whaling, seal hunting, and mining were on a small scale and short-lived, partly also because of the challenging weather. Today, Fiordland contains by far the greatest extent of u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Land Information New Zealand
Toitū Te Whenua Land Information New Zealand (LINZ) is the public service department of New Zealand charged with geographical information and surveying functions as well as handling land titles, and managing Crown land and property. The minister responsible is the Minister for Land Information, and was formerly the Minister of Survey and Land Information. LINZ was established in 1996 following the restructure of the Department of Survey and Land Information (DOSLI), which was itself one of the successor organisations to the Department of Lands and Survey. The New Zealand Geographic Board secretariat is part of LINZ and provides the Board with administrative and research assistance and advice. The Minister for Land Information is Damien O'Connor. Gaye Searancke was appointed Chief Executive of Land Information New Zealand in August 2019. She succeeded Andrew Crisp, who had been in the post since 2016. Nature and scope of functions LINZ's purpose is to: *Maintain and build co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Mouth
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hanging Valley
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bowen Falls
The Bowen Falls ( mi, Hineteawa), also known as Lady Bowen Falls, is a popular tourist attraction at Milford Sound, a fiord in New Zealand. The long Bowen River located in Fiordland National Park supplies the waterfall with water; the Bowen River is also used to generate electricity and supply drinking water to the nearby locality also named Milford Sound. Bowen Falls is one of just two permanent waterfalls that discharge into the fiord, and, at , it is the tallest. The river and waterfalls were named for Diamantina Bowen (Lady Bowen), the wife of the fifth governor of New Zealand, George Bowen Sir George Ferguson Bowen (; 2 November 1821 – 21 February 1899), was an Irish author and colonial administrator whose appointments included postings to the Ionian Islands, Queensland, New Zealand, Victoria, Mauritius and Hong Kong.R. B. Joy .... The governor visited Milford Sound aboard in 1871 and Bowen Falls was named to mark the occasion. The track from the Milford Sound wha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
George Bowen
Sir George Ferguson Bowen (; 2 November 1821 – 21 February 1899), was an Irish author and colonial administrator whose appointments included postings to the Ionian Islands, Queensland, New Zealand, Victoria, Mauritius and Hong Kong.R. B. Joyce,Bowen, Sir George Ferguson (1821–1899)', ''Australian Dictionary of Biography'', Vol. 3, Melbourne University Press, 1969, pp 203–207. Retrieved 18 April 2010 Early life Bowen was born the eldest son of the Rev. Edward Bowen,Death of Sir George Bowen , Wanganui Herald, Volume XXXIII, Issue 9676, 23 February 1899, Page 2 Rector of |
Hydroelectric
Hydroelectricity, or hydroelectric power, is electricity generated from hydropower (water power). Hydropower supplies one sixth of the world's electricity, almost 4500 TWh in 2020, which is more than all other renewable sources combined and also more than nuclear power. Hydropower can provide large amounts of low-carbon electricity on demand, making it a key element for creating secure and clean electricity supply systems. A hydroelectric power station that has a dam and reservoir is a flexible source, since the amount of electricity produced can be increased or decreased in seconds or minutes in response to varying electricity demand. Once a hydroelectric complex is constructed, it produces no direct waste, and almost always emits considerably less greenhouse gas than fossil fuel-powered energy plants. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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