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Barrett Reef
The cluster of rocks that is Barrett Reef (often known as ''Barrett's Reef'') is one of the most hazardous reefs in New Zealand. It lies on the western side of the entrance of Wellington Harbour, on the approaches to the city of Wellington, at coordinates . The reef is named after Dicky Barrett (trader), Richard (Dicky) Barrett (1807–1847), a whaler and trader. Its Māori language, Māori name is ''Tangihanga-a-Kupe, (Mourning of Kupe)'', which may refer to the reef's similarity to a line of mourners at a tangi, the sad sound of the water around the reef, or Kupe crying for people he left behind in his travels. The reef is popular with recreational divers. Dangerous entrance The reef, much of which is exposed even at high tide, is located to the west of the two-kilometre-wide channel that links Cook Strait with Wellington Harbour, close to the shore of the Miramar Peninsula. The shipping channel lies between the reef and Pencarrow to the east. The area to the west between the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reef
A reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic component, abiotic (non-living) processes such as deposition (geology), deposition of sand or wave erosion planning down rock outcrops. However, reefs such as the coral reefs of tropical waters are formed by biotic component, biotic (living) processes, dominated by corals and coralline algae. Artificial reefs, such as shipwrecks and other man-made underwater structures, may occur intentionally or as the result of an accident. These are sometimes designed to increase the physical complexity of featureless sand bottoms to attract a more diverse range of organisms. They provide shelter to various aquatic animals which help prevent extinction. Another reason reefs are put in place is for aquaculture, and fish farmers who are looking to improve their businesses sometimes invest in them. Reefs are often quite n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Picton, New Zealand
Picton () is a town in the Marlborough Region of New Zealand's South Island. The town is located near the head of the Queen Charlotte Sound / Tōtaranui, north of Blenheim, New Zealand, Blenheim and west of Wellington. Waikawa, Marlborough, Waikawa lies just north-east of Picton and is considered to be a contiguous part of the Picton urban area. Picton is a major hub in New Zealand's transport network, connecting the South Island road and rail network with ferries across Cook Strait to Wellington and the North Island. The Picton urban area has a population of making it the second-largest town in the Marlborough Region behind Blenheim. It is the easternmost town in the South Island with a population of at least 1,000 people. Toponymy The town is named after Sir Thomas Picton, the Welsh military associate of the Arthur Wellesley, 1st Duke of Wellington, Duke of Wellington, who was killed at the Battle of Waterloo. Thomas Picton's connection to the slave trade and controve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reefs Of The Pacific Ocean
A reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic (non-living) processes such as deposition of sand or wave erosion planning down rock outcrops. However, reefs such as the coral reefs of tropical waters are formed by biotic (living) processes, dominated by corals and coralline algae. Artificial reefs, such as shipwrecks and other man-made underwater structures, may occur intentionally or as the result of an accident. These are sometimes designed to increase the physical complexity of featureless sand bottoms to attract a more diverse range of organisms. They provide shelter to various aquatic animals which help prevent extinction. Another reason reefs are put in place is for aquaculture, and fish farmers who are looking to improve their businesses sometimes invest in them. Reefs are often quite near to the surface, but not all definitions require t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cook Strait Ferry
Cook Strait () is a strait that separates the North and South Islands of New Zealand. The strait connects the Tasman Sea on the northwest with the South Pacific Ocean on the southeast. It is wide at its narrowest point,McLintock, A. H., ed. (1966''Cook Strait''from An Encyclopaedia of New Zealand, updated 18-Sep-2007. Note: This is the distance between the North Island and Arapaoa Island; some sources give a slightly larger reading of around , that between the North Island and the South Island. and has been described as "one of the most dangerous and unpredictable waters in the world". Regular ferry services run across the strait between Picton in the Marlborough Sounds and Wellington. The strait is named after James Cook, the first European commander to sail through it, in 1770. In Māori it is named ''Te Moana-o-Raukawa'', which means ''The Sea of Raukawa''. The waters of Cook Strait are dominated by strong tidal flows. The tidal flow through Cook Strait is unusual in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The Wellington Region
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steeple Rock
Steeple Rock/Te Aroaro-o-Kupe is a large rock off Seatoun at the west of the entrance to Wellington Harbour, rising above sea level. The rock plays a role in warning ships off the coast. It is the location of a marine light and an unbeaconed trig station (‘Steeple Rock Light’, Survey marker, geodetic code B0XX). Its Māori language, Māori name is Te Aroaro-o-Kupe (The front of Kupe or The presence of Kupe). The name was officially changed in 2009 from the English "Steeple Rock" to the current dual name of Steeple Rock/Te Aroaro-o-Kupe as part of the 2009 Treaty of Waitangi claims and settlements, Treaty of Waitangi settlement between Taranaki Whānui ki te Upoko o te Ika and the New Zealand government. The previous Māori name of the rock was Te Ure o Kupe (The penis of Kupe). Kupe, the legendary discoverer of Aotearoa, is said to have injured himself on the rock while swimming. In earlier times Steeple Rock was also known as Pinnacle Rock. This should not be confused with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hikitia
''Hikitia'' is a self-propelled floating steam crane in Wellington Harbour, New Zealand. She is thought to be the only working steam crane of her type in the world. She is also the sister ship to the '' Rapaki'', formerly of the Port of Lyttelton, which was put on display at the New Zealand Maritime Museum after being taken out of service, and then scrapped in January 2019. Some parts from ''Rapaki'' were given to ''Hikitia''. Delivery voyage The ''Hikitia'' was built by Fleming & Ferguson of Paisley, Scotland. After completing trials, the vessel left Greenock on 29 September 1926. The delivery voyage took 82 days, travelling via the Panama Canal to reach New Zealand. The vessel travelled with the crane fully erected, and arrived in Wellington Harbour on 21 December 1926. Engines Twin screws are driven by surface-condensing direct-drive compound engine A compound engine is an engine that has more than one stage for recovering energy from the same working fluid, with t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taranaki Herald
The ''Taranaki Herald'' was an afternoon daily newspaper, published in New Plymouth, New Zealand. It began publishing as a four-page tabloid on 4 August 1852. It was the first newspaper published in Taranaki and it became the country's oldest daily newspaper when the ''Lyttelton Times'' closed in 1935. The ''Taranaki Herald'' ceased publication in 1989. History The newspaper was founded by William Collins and Garland William Woon, who hired William Morgan Crompton as its first editor. It began as a weekly paper, moved to twice-weekly publication in 1867 and began appearing daily in 1877. Crompton was replaced as editor in 1854 by Richard Pheney, who quit in November 1856 when he opposed the newspaper owner's support for George Cutfield over Charles Brown as Taranaki Superintendent. In May 1857 Pheney was appointed as the first editor of a rival newspaper, the '' Taranaki News'', which changed its name to the ''Taranaki Daily News'' when it began daily publication three years ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Evans Bay, New Zealand
Evans Bay () is a large bay at the southern end of Wellington Harbour, New Zealand. Located between the Miramar Peninsula and Hataitai, it was the site of New Zealand's first patent slip and served as Wellington's international flying boat, flying-boat terminal from 1938 until 1956. It is named after George Evans (Australian politician), George Samuel Evans, an early Wellington settler. Geography Evans Bay is a large U-shaped bay within Wellington Harbour. Within the bay are smaller features such as Balaena Bay, Hataitai Beach and Shelly Bay. Prior to the Haowhenua earthquake in about 1460 AD, Miramar was an island and Evans Bay would have been open to Lyall Bay. Today it is bounded by the Miramar peninsula to the east, the Rongotai isthmus to the south, and a hilly ridge forming part of Hataitai to the west. Formerly the Waipapa Stream flowed from the valley in Hataitai into the head of Evans Bay near the bluff at Wellington Road, creating a large swampy delta. The shorelin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland Star
The ''Auckland Star'' was an evening daily newspaper published in Auckland, New Zealand, from 24 March 1870 to 16 August 1991. Survived by its Sunday edition, the ''Sunday Star'', part of its name endures in ''The Sunday Star-Times'', created in the 1994 merger of the ''Dominion Sunday Times'' and the ''Sunday Star''. Originally published as the ''Evening Star'' from 24 March 1870 to 7 March 1879, the paper continued as the ''Auckland Evening Star'' between 8 March 1879 and 12 April 1887, and from then on as the ''Auckland Star''. One of the paper's notable investigative journalists was Pat Booth, who was responsible for notable coverage of the Crewe murders and the eventual exoneration of Arthur Allan Thomas. Booth and the paper extensively reported on the Mr Asia case. In 1987, the owners of the ''Star'' launched a morning newspaper to more directly compete with ''The New Zealand Herald''. The '' Auckland Sun'' was affected by the 1987 stock market crash and folded a ye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Bank Arcade
The Old Bank Arcade is a retail and office complex on a corner site at Lambton Quay, Wellington, New Zealand. The property consists of four buildings built between 1883 and 1904. The most prominent is the Bank of New Zealand building (no. 1) on the wedge-shaped corner of Lambton Quay and Customhouse Quay. It was designed by Thomas Turnbull for the Bank of New Zealand and is located on the site of Plimmer's Ark. Built by T. Carmichael, it is a brickwork shell with timber flooring, pressed metal ceilings and plaster decoration. The Bank of New Zealand operated a branch on the ground floor of this building from its opening in 1901 until 1984. The banking hall was described by the ''New Zealand Mail'' of 1901 as "a handsome, lofty room, said to be one of the largest of its kind in the colonies". This building is classified as a "Category I" ("places of 'special or outstanding historical or cultural heritage significance or value'") historic place by the New Zealand Historic Place ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Plimmer
John Plimmer (28 June 1812 – 5 January 1905) was an English settler and entrepreneur in New Zealand who was the self-styled "Father of Wellington". Early life in England Plimmer was born at a village called in contemporary accounts "Upton-under-Amon" near Shrewsbury, Shropshire, England on 28 June 1812, youngest but one of 12 children of Isaac Plimmer, builder and timber merchant, and his wife Mary (''nee'' Roden). Identifiably the village is Upton Magna, which lies under Haughmond Hill, where he was baptised on 19 July that year. Educated at a local parish school, he was intended for teaching but preferred to train as a plasterer and master builder. He practised the trades at Willenhall, Staffordshire from after his father moved there until his own emigration and it was at Birmingham in that area he first married, to Mary Roden who was a probable cousin, in 1833. Life in New Zealand He arrived in Wellington from England on the ship ''Gertrude'' in 1841. As an entrepre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
