Storm Of 1897
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Storm Of 1897
The storm of 1897 was a severe storm that struck the lower to central North Island of New Zealand on 16 April 1897. It caused the ship ''Zuleika'' to run aground near Cape Palliser, with the loss of 12 lives, and severe flooding. At Clive the flooding caused the loss of a further 12 lives and one person was drowned near Kapiti. There were six further unconfirmed reports of drowning, bringing the total loss of life directly related to the storm event to between 25 and 31. Based on descriptions of the storm, particularly that of Captain Marten of the ''Waiapu'', it may have been an extratropical cyclone. The storm Prelude Weather reports on the 14 April indicated an approaching storm with a falling barometer especially in the south and with winds from a generally northerly direction. The barometer at Bluff registered . By 15 April, the wind was moving to the south, with barometric pressure being variable. Warnings were issued for southerly gales for the South Island and lower Nort ...
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Storm Wellington Harbour
A storm is any disturbed state of the natural environment or the atmosphere of an astronomical body. It may be marked by significant disruptions to normal conditions such as strong wind, tornadoes, hail, thunder and lightning (a thunderstorm), heavy precipitation ( snowstorm, rainstorm), heavy freezing rain ( ice storm), strong winds ( tropical cyclone, windstorm), wind transporting some substance through the atmosphere such as in a dust storm, among other forms of severe weather. Storms have the potential to harm lives and property via storm surge, heavy rain or snow causing flooding or road impassibility, lightning, wildfires, and vertical and horizontal wind shear. Systems with significant rainfall and duration help alleviate drought in places they move through. Heavy snowfall can allow special recreational activities to take place which would not be possible otherwise, such as skiing and snowmobiling. The English word comes from Proto-Germanic ''*sturmaz' ...
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Hydrabad (1865 Ship)
''Hydrabad'' was an iron cargo and passenger sailing ship, built in Scotland and launched in 1865. She was owned by several successive companies, and served until being wrecked off the coast of New Zealand in 1878. There were attempts to salvage her, but they all failed, and the wreck was left to deteriorate on the shoreline. Construction and early years She was built by Robert Duncan & Company, of Port Glasgow, Scotland and launched on 14 May 1865. She was completed in August 1865, and initially owned by the Bombay Iron Ship Company, of Bombay. She was later acquired by Stephens and Sons, of London. ''Hydrabad'' was a full-rigged ship with three masts, built of iron. She was long, had a beam of , and a draught of . She had two holds, and an ornately carved figurehead of a Hindu warrior. Her accommodation was lavishly furnished. Wreck ''Hydrabad'' was bound from Lyttelton to Adelaide, carrying broad gauge rolling stock which had been sold by the Canterbury Provincial Rail ...
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Waipawa
Waipawa is the second-largest town in Central Hawke's Bay in the east of the North Island of New Zealand. It has a population of At the 2013 census, it had a population of 1,965, a change of 2.2 percent from the 2006 census. The town is located northeast of Waipukurau and southwest of Hastings, on the northern bank of the Waipawa River, a tributary of the Tukituki River. Waipawa was settled in the early 1860s, and the Settler's Museum exhibits many of these historical collections. It holds the main office of the Central Hawke's Bay District Council, and is New Zealand's oldest inland European settlement. Frederick Abbot was one of the early settlers and Waipawa was originally called Abbotsford, when the township was being sold in 1859, and there is still a children's home in Waipawa named Abbotsford. However, it was often shown as Abbotsford, Waipawa and Waipawa was more commonly used alone after the opening of the Waipawa railway station and Waipawa Mail in the late 1870s. ...
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Palmerston North–Gisborne Line
The Palmerston North–Gisborne Line (PNGL) is a secondary main line railway in the North Island of New Zealand. It branches from the North Island Main Trunk at Palmerston North and runs east through the Manawatū Gorge to Woodville, where it meets the Wairarapa Line, and then proceeds to Hastings and Napier in Hawke's Bay before following the coast north to Gisborne. Construction began in 1872, but the entire line was not completed until 1942. The line crosses the runway of Gisborne Airport, one of the world's only railways to do so since Pakistan's Khyber Pass Railway closed. In conjunction with the Moutohora Branch that ran north from Gisborne between 1900 and 1959, the line was originally intended to connect to the East Coast Main Trunk, described in 1875 as the North Island trunk line, but the difficult inland section between the Tāneatua Branch in the Bay of Plenty and the Moutohora Branch was never completed. The line has been freight only since October 2001, whe ...
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Takapau
Takapau is a small rural community in the Central Hawkes Bay in New Zealand. It is located 20 kilometres west of Waipukurau, off State Highway 2, and has a population of more than 500. The original township was founded in 1876 by farmer Sydney Johnston from Oruawharo station. Johnston's family donated land for a school and churches, and built the local library, public hall and, later, Plunket rooms. Many streets are named after members of the family. Takapau was once the centre of a large flax milling industry, and the community takes its name from the flax that grew in the expansive Takapau plains. The Māori word translates literally as "mat" or "carpet". The largest business in Takapau is now the Silverfern Farms meat-processing plant, founded by the Hawke's Bay Farmers’ Meat Company in 1981. Kintail Honey, one of country's largest honey-packing and beekeeping operations, is also based in the town. There are two schools in Takapau. The Trappist monastery, the Southern ...
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Bulls, New Zealand
Bulls is a small town north west of Palmerston North on the west coast of the North Island of New Zealand. It is in a fertile farming area in the Rangitikei District at the junction of State Highways 1 and 3 about 135 kilometres (84 mi) north of Wellington. According to a Statistics New Zealand estimate, Bulls has a population of inhabitants. Recent marketing makes puns with the name, for example, "New Zealand gets its milk from Bulls" or the sign for the local police station "Const-a-bull". Etymology There are two recorded Māori toponyms for the area – Te Ara Taumaihi and Ō-hine-puhiawe. The origins of Te Ara Taumaihi have yet to be explicitly explored. Ō-hine-puhiawe, a land block where Parewahawaha marae is situated, acts as a synecdoche to refer to the current town area. The modern town name is named after James Bull who owned the first general store there. The town was originally called Bull Town, but this was changed to Clifton and then renamed back to Bulls a ...
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Portland Island (New Zealand)
Portland Island, also called Waikawa, is a small island off the southern tip of the Māhia Peninsula on the North Island of New Zealand. It is used for sheep farming. The area of the island fluctuates rapidly between high and low tides due to a shelf of rocks surrounding the east, north and west coast of the island. During low tide the area of the island can grow up to 3 km2, while during high tide it shrinks down to only 1.4 km2. This makes access by boat to the island rather difficult, despite it being only a kilometer offshore. See also * Lists of islands ** List of islands of New Zealand * Desert island A desert island, deserted island, or uninhabited island, is an island, islet or atoll that is not permanently populated by humans. Uninhabited islands are often depicted in films or stories about shipwrecked people, and are also used as stereot ... References Landforms of the Hawke's Bay Region Uninhabited islands of New Zealand Māhia Peninsula
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Cyclone
In meteorology, a cyclone () is a large air mass that rotates around a strong center of low atmospheric pressure, counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as viewed from above (opposite to an anticyclone). Cyclones are characterized by inward-spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. Cyclogenesis is the process of cyclone formation and ...
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Castlepoint
Castlepoint is a small beachside settlement on the Wairarapa coast of the Wellington Region of New Zealand. It is home to a lighthouse which stands near the top of the northern end of a reef. The reef is about one kilometre long. At the southern end of the reef, there is an island known locally as "seagull island", due to its large population of seagulls. The southern side of Castle Rock is known as Christmas Bay. Castlepoint is approximately one hour's drive from Masterton. Castlepoint was so named in 1770 by Captain Cook who was struck by the similarities of Castle Rock to the battlements of a castle. The Maori name for the area is Rangiwhakaoma, which translates as 'where the sky runs'. Smaller cetaceans such as dolphins frequent around Castlepoint while larger whales such as southern right whales and humpback whales may be visible from the shores during their migration seasons. A book chronicling the history of Castlepoint, including Castlepoint Station, Castle Point L ...
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Banks Peninsula
Banks Peninsula is a peninsula of volcanic origin on the east coast of the South Island of New Zealand. It has an area of approximately and encompasses two large harbours and many smaller bays and coves. The South Island's largest city, Christchurch, is immediately north of the peninsula. Geology Banks Peninsula forms the most prominent volcanic feature of the South Island, similar to — but more than twice as large as — the older Dunedin volcano (Otago Peninsula and Harbour) to the southwest. Geologically, the peninsula comprises the eroded remnants of two large (Lyttelton formed first, then Akaroa), and the smaller Mt Herbert Volcanic Group. These formed due to intraplate volcanism between approximately eleven and eight million years ago (Miocene) on a continental crust. The peninsula formed as offshore islands, with the volcanoes reaching to about 1,500 m above sea level. Two dominant craters formed Lyttelton and Akaroa Harbours. The Canterbury ...
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