Ahuriri Lagoon
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Ahuriri Lagoon
Ahuriri Lagoon ( mi, Te Whanganui-a-Orotū) was a large tidal lagoon at Napier, on the east coast of New Zealand's North Island, that largely drained when the area was raised by the 1931 Hawke's Bay earthquake. Before the earthquake, the lagoon stretched several kilometres from north to south, and covered roughly 4000 hectares (ha), or 40 km². The Tūtaekurī River flowed into the southern end, and the Esk River into the northern end. Following the earthquake, the Esk was no longer able to flow into the lagoon and ran more directly to the sea. The Tūtaekurī still flowed into the lagoon after the earthquake but it caused flooding for the next few years, and by the end of the 1930s it had been diverted away from the lagoon to enter the sea at the mouth of the Ngaruroro River. The land rise in the earthquake drained much of the lagoon, leaving a smaller estuary. Land reclamation and drainage work further reduced the estuary to its present size of 470 ha. Cultural history ...
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Ahuriri Lagoon Map Before After 1931 Hawke's Bay Earthquake Crude
Ahuriri is a suburb of the city of Napier, in the Hawke's Bay region of New Zealand's eastern North Island.NOTE: the term Ahuriri is also used as an alternative Māori language name for the city of Napier overall. The area was a major site of Māori and European settlement, and the site of the Port of Napier until the 1931 Hawke's Bay earthquake. It has since been redeveloped as a mixed commercial and residential area. Demographics Ahuriri had a population of 1,161 at the 2018 New Zealand census, an increase of 72 people (6.6%) since the 2013 census, and an increase of 303 people (35.3%) since the 2006 census 6 (six) is the natural number following 5 and preceding 7. It is a composite number and the smallest perfect number. In mathematics Six is the smallest positive integer which is neither a square number nor a prime number; it is the second small .... There were 510 households. There were 528 males and 630 females, giving a sex ratio of 0.84 males per female. The medi ...
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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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Lagoons Of New Zealand
A lagoon is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, or isthmuses. Lagoons are commonly divided into ''coastal lagoons'' (or ''barrier lagoons'') and ''atoll lagoons''. They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries. Lagoons are common coastal features around many parts of the world. Definition and terminology Lagoons are shallow, often elongated bodies of water separated from a larger body of water by a shallow or exposed shoal, coral reef, or similar feature. Some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity. The distinction between "lagoon" and "estuary" also varies between authorities. Richard A. Davis Jr. restricts "l ...
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History Of The Hawke's Bay Region
History (derived ) is the systematic study and the documentation of the human activity. The time period of event before the invention of writing systems is considered prehistory. "History" is an umbrella term comprising past events as well as the memory, discovery, collection, organization, presentation, and interpretation of these events. Historians seek knowledge of the past using historical sources such as written documents, oral accounts, art and material artifacts, and ecological markers. History is not complete and still has debatable mysteries. History is also an academic discipline which uses narrative to describe, examine, question, and analyze past events, and investigate their patterns of cause and effect. Historians often debate which narrative best explains an event, as well as the significance of different causes and effects. Historians also debate the nature of history as an end in itself, as well as its usefulness to give perspective on the problems of the p ...
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State Highway 2 (New Zealand)
State Highway 2 (SH 2) runs north–south through eastern parts of the North Island of New Zealand from the outskirts of Auckland to Wellington. It runs through Tauranga, Gisborne, Napier, Hastings and Masterton. It is the second-longest highway in the North Island, after State Highway 1, which runs the length of both of the country's main islands. For most of its length it consists of a two-lane single carriageway, with frequent passing lanes. There are sections of four-lane dual-carriageway expressway at Maramarua, Tauranga and Wellington. Route SH 2 leaves just north of Pōkeno, south of central Auckland. It heads east, crossing the Hauraki Plains before running the length of the Karangahake Gorge, a break in the hills between the Coromandel Peninsula and Kaimai Ranges. From the mining town of Waihi it runs southeast, skirting the edge of Tauranga Harbour, which it crosses on the Tauranga Harbour Bridge before connecting to the Tauranga Eastern Link, a four lan ...
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Westshore, New Zealand
Westshore is a northern coastal suburb of the city of Napier in Hawke's Bay, New Zealand. History The first European settlers built houses on Westshore in 1850, when it was little more than a sandspit. Prior to the 1931 Hawke's Bay earthquake, Westshore was already a popular seaside resort, a long-time popular spot for yachting and boating activities. In 1931 the earthquake struck Napier, reclaiming the Ahuriri Lagoon. This freed up land and allowed Westshore to expand as a suburb, as previously a narrow shingle spit was the only land available. The earthquake also transformed the previously dangerous and shingly seashore into a safe and sandy swimming beach. Projects such as beach front beautification, landscaping and other improvements have helped to make Westshore one of the most popular and preferred beaches in Napier. The Napier Swimming and Lifesaving Club was amongst the earliest Surf Lifesaving Clubs active in New Zealand, beginning in the 1910s. In October, 1958 the new ...
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Ahuriri
Ahuriri is a suburb of the city of Napier, in the Hawke's Bay region of New Zealand's eastern North Island.NOTE: the term Ahuriri is also used as an alternative Māori language name for the city of Napier overall. The area was a major site of Māori and European settlement, and the site of the Port of Napier until the 1931 Hawke's Bay earthquake. It has since been redeveloped as a mixed commercial and residential area. Demographics Ahuriri had a population of 1,161 at the 2018 New Zealand census, an increase of 72 people (6.6%) since the 2013 census, and an increase of 303 people (35.3%) since the 2006 census 6 (six) is the natural number following 5 and preceding 7. It is a composite number and the smallest perfect number. In mathematics Six is the smallest positive integer which is neither a square number nor a prime number; it is the second small .... There were 510 households. There were 528 males and 630 females, giving a sex ratio of 0.84 males per female. The medi ...
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Hawke Bay
Hawke Bay ( mi, Te Matau-a-Māui), formerly named ''Hawke's Bay'', is a large bay on the east coast of the North Island of New Zealand, surrounded by the Hawke's Bay region. It stretches from Māhia Peninsula in the northeast to Cape Kidnappers / Te Kauwae-a-Māui in the southwest, a distance of some . Captain James Cook, sailing in HMS ''Endeavour'', entered the bay on 12 October 1769. After exploring it, he named it for Sir Edward Hawke, First Lord of the Admiralty, on 15 October 1769, describing it as some 13 leagues (about ) across. Hawke had decisively defeated the French at the Battle of Quiberon Bay in 1759. This part of the New Zealand coast is subject to tectonic uplift, with the land being raised out of the sea. For this reason, the coastal land in this area has significant marine deposits, with both marine and land dinosaur fossils having been found inland. The Napier earthquake of 3 February 1931 resulted in several parts of the seabed close to the city of ...
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Hawke's Bay Airport
Hawke's Bay Airport , commonly referred to as Napier Airport, is Hawke's Bay's main commercial airport, serving domestic flights to the main centres of Auckland, Wellington and Christchurch as well as smaller centres such as Gisborne, Wairoa and Blenheim. The airport is located 5.8 km from Napier and 20.7 km from Hastings. The airport is permitted to allow limited international flights for aircraft with up to fourteen people on board by prior arrangement with Air Napier or Skyline Aviation. 452,000 travellers passed through the terminal in the 12 months to June 2013. This increased to 652,426 in the 12 months to June 2017. History The airport is located in the Napier suburb of Westshore, and is sometimes referred to as Napier Airport. It is sited on the former Ahuriri Lagoon, an area which was raised above sea level by the 1931 Hawke's Bay earthquake. In 2010/11 the main runway was extended to 1750 metres with 240-metre Runway End Safety Areas at either end which is long ...
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Napier Hill
Napier Hill ( mi, Mataruahou) is a limestone outcrop and suburb rising above the lowland districts of the city of Napier, New Zealand, Napier on New Zealand's North Island. The north-east end, Bluff Hill, has a steep cliff face overlooking the Port of Napier. It features Napier Girls' High School, the historic former Napier Prison and a scenic walk. The western end, Hospital Hill, was the site of the former Napier Hospital, whose services were transferred to Hawke's Bay Hospital in Hastings, New Zealand, Hastings in 1999. The building was demolished in 2015 after years of sitting derelict and the land has recently been purchased (December 2020) by the Napier City Council to be developed for use as a new reservoir to replace the current ageing water source on Enfield Road. European settlement on the hill began in 1855. Most homes on the hill were built in the 1920s. Prior to the 1931 Hawke's Bay earthquake, the hill was almost surrounded with water, with just two shingle spits ru ...
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Scinde Island
Napier Hill ( mi, Mataruahou) is a limestone outcrop and suburb rising above the lowland districts of the city of Napier on New Zealand's North Island. The north-east end, Bluff Hill, has a steep cliff face overlooking the Port of Napier. It features Napier Girls' High School, the historic former Napier Prison and a scenic walk. The western end, Hospital Hill, was the site of the former Napier Hospital, whose services were transferred to Hawke's Bay Hospital in Hastings in 1999. The building was demolished in 2015 after years of sitting derelict and the land has recently been purchased (December 2020) by the Napier City Council to be developed for use as a new reservoir to replace the current ageing water source on Enfield Road. European settlement on the hill began in 1855. Most homes on the hill were built in the 1920s. Prior to the 1931 Hawke's Bay earthquake, the hill was almost surrounded with water, with just two shingle spits running north and south, and was known as Sci ...
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Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bays, ...
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