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Paorae
Paorae is the name of a migrating coastal dune, formerly located west of the Āwhitu Peninsula in the Auckland Region of New Zealand. Paorae was an important area for cultivating kūmara (sweet potato) and taro for Tāmaki Māori tribes Ngāiwi and Ngāoho, and later Waikato Tainui. The land eroded in the 18th century, becoming known as a legendary "Māori Atlantis" to European New Zealanders. Material from Paorae forms the Manukau Heads sandbars and the modern day beach at Whatipu, which began forming in the 1930s. Geology New Zealand geologist Bruce Hayward theorised that Paorae formed from accumulated volcanic material from the Hatepe eruption of the Taupō Volcano, which occurred 1,800 years ago. Sediment from the eruption washed down the Waikato River, forming a large sand bank north of the Waikato River mouth, along the Āwhitu Peninsula. The land eroded in the 18th century, but material from Paorae continues to move northwards up the west coast. History Māori his ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manukau Heads
The Manukau Heads is the name given to the two promontories that form the entrance to the Manukau Harbour – one of the two harbours of Auckland in New Zealand. The southern head, at the northern tip of Āwhitu Peninsula, is simply termed "The South Head", whereas the northern head is named "Burnett Head" (the term North Head is used to indicate a promontory in the nearby Waitematā Harbour). Both heads are hilly areas of land that rise steeply from the water to over 240m within less than 400m of the shoreline. History In Pre-European times, the west coast of the Āwhitu Peninsula was the site of Paorae, a flat sand dune land which was a major kūmara (sweet potato) cultivation site for Tāmaki Māori iwi. The land eroded during the 18th century, however the sand from the dune feature continued to move northwards, creating vast sand banks in the Manukau Heads and at Whatipu. The foot of the South Head cliffs is the location of the Matatuahu archaeological site, one of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whatipu
Whatipu is a remote beach on the west coast of the Auckland Region in the North Island of New Zealand. The Whatipu area has been managed as a scientific reserve by the Auckland Regional Council since 2002. The road to it is unsealed. To the south of Whatipu is Manukau Harbour. To the north is Karekare. Whatipu is located at the southern end of the Waitākere Ranges. Shifting sands have substantially changed the beach since the 1940s. Over 6 square kilometres has been added to the beach since then. Geography Between 3 and 5 million years ago, tectonic forces between the Pacific Plate and Australian Plate uplifted the Waitākere Ranges and subsided the Manukau Harbour. Major features of Whatipu include Te Toka-Tapu-a-Kupe / Ninepin Rock and Paratutae Island, which are remnants of the Miocene era Waitākere Volcano. From the 1930s to the 1960s, sandy material began accumulating at Whatipu, creating a 1.5km strip of sand, where plants and fresh water swamps developed. Much of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikato River
The Waikato River is the longest river in New Zealand, running for through the North Island. It rises on the eastern slopes of Mount Ruapehu, joining the Tongariro River system and flowing through Lake Taupō, New Zealand's largest lake. It then drains Taupō at the lake's northeastern edge, creates the Huka Falls, and flows northwest through the Waikato Plains. It empties into the Tasman Sea south of Auckland, at Port Waikato. It gives its name to the Waikato region that surrounds the Waikato Plains. The present course of the river was largely formed about 17,000 years ago. Contributing factors were climate warming, forest being reestablished in the river headwaters and the deepening, rather than widening, of the existing river channel. The channel was gradually eroded as far up river as Piarere, leaving the old Hinuera channel through the Hinuera Gap high and dry. The remains of the old course are seen clearly at Hinuera, where the cliffs mark the ancient river edges. The Wai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Erosion
Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural. On non-rocky coasts, coastal erosion results in rock formations in areas where the coastline contains rock layers or fracture zones with varying resistance to erosion. Softer areas become eroded much faster than harder ones, which typically result in landforms such as tunnels, bridges, columns, and pillars. Over time the coast generally evens out. The softer areas fill up with sediment eroded from hard areas, and rock formations are eroded away. Also erosion commonly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piha
Piha is a coastal settlement in West Auckland, on the western coast of the Auckland Region in New Zealand. It is one of the most popular beaches in the area and a major day-trip destination for Aucklanders throughout the year, and especially in summer. Piha is 39 kilometres west of Auckland city centre, on the Tasman Sea coast to the north of the Manukau Harbour, on the western edge of the Waitākere Ranges. Immediately to the north of Piha is Whites Beach, and immediately to the south is Mercer Bay; land access to both is only by foot. The nearest beaches accessible by road are Karekare to the south, and Anawhata to the north. History The area is traditionally a part of rohe of the Tāmaki Māori tribe Te Kawerau ā Maki. The area is named for Te Piha, the traditional name of Lion Rock which was later applied to the wider area, and refers to the pattern made when waves hit against the rock. The area was the location of many pā and villages, including a headland at Te Wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karekare, New Zealand
Karekare is a small coastal settlement in West Auckland, New Zealand, sandwiched between the Waitākere Ranges and a large black sand surf beach. Geography It is located west of Auckland city centre, south of the larger beach of Piha. It is north of Whatipu, south of Piha and west of the Centennial Memorial Park and Water Catchment area, which cover most of the native bushland Waitākere Ranges. Karekare Beach is the confluence of the Company Stream, which was traditionally known by the name Waiteahoaho, and the Karekare Stream. The Karekare Falls are located inland from the beach. The beach at Karekare is split into two sections separated by the, Karekare Stream, Karekare Beach to the south and Tāhoro / Union Bay, to the north. Two major geographical sites within Karekare are The Watchman, traditionally known by the names Te Matua and Te Tokamatua, a significant knoll on the beach's ridge, and Paratahi Island, located to the south of Karekare. Karekare is the remains of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otago Witness
The ''Otago Witness'' was a prominent illustrated weekly newspaper in the early years of the European settlement of New Zealand, produced in Dunedin, the provincial capital of Otago. Published weekly it existed from 1851 to 1932. The introduction of the Otago Daily Times followed by other daily newspapers in its circulation area lead it to focus on serving a rural readership in the lower South Island where poor road access prevented newspapers being delivered daily. It also provided an outlet for local fiction writers. It is notable as the first newspaper to use illustrations and photographs and was the first New Zealand newspaper to provide a correspondence column for children, which was known as "Dot's Little Folk". Together with the Auckland based ''Weekly News'' and the Wellington based ''New Zealand Free Lance'' it was one of the most significant illustrated weekly New Zealand newspapers in the 19th and early 20th centuries. History Background Nine months after the first immi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Kawerau ā Maki
Te Kawerau ā Maki, Te Kawerau a Maki, or Te Kawerau-a-Maki is a Māori ''iwi'' (tribe) of the Auckland Region of New Zealand. It had 251 registered adult members as of June 2017. Auckland Council gave it land for a marae at Te Henga (Bethells Beach) in 2018; it has no ''wharenui'' (meeting house) yet. History Te Kawerau ā Maki are the descendants of the ''rangatira'' (chief) Maki and his wife Rotu, who migrated with their family and followers from Kawhia to Tāmaki Makaurau (Auckland) in the early 1600s. Te Kawerau trace their ancestry from a number of Māori migration canoes, particularly the Tainui, but also Aotea, Tokomaru, Kahuitara and Kurahaupō. Tainui ancestors including Hoturoa and the tohunga Rakataura (Hape) are particularly important in Te Kawerau whakapapa, as is the ancient turehu ancestor and tohunga Tiriwa. Maki and his people were related to a number of groups who had occupied the Auckland region since the fourteenth century, including the Tainui ''hapū'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Records Of The Auckland Institute And Museum
The Auckland War Memorial Museum Tāmaki Paenga Hira (or simply the Auckland Museum) is one of New Zealand's most important museums and war memorials. Its collections concentrate on New Zealand history (and especially the history of the Auckland Region), natural history, and military history. The present museum building was constructed in the 1920s in the neo-classicist style, and sits on a grassed plinth (the remains of a dormant volcano) in the Auckland Domain, a large public park close to the Auckland CBD. Auckland Museum's collections and exhibits began in 1852. In 1867 Aucklanders formed a learned society – the Auckland Philosophical Society, later the Auckland Institute. Within a few years the society merged with the museum and ''Auckland Institute and Museum'' was the organisation's name until 1996. Auckland War Memorial Museum was the name of the new building opened in 1929, but since 1996 was more commonly used for the institution as well. From 1991 to 2003 the museu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kāinga
A kāinga ( Southern Māori ''kaika'' or ''kaik'') is the traditional form of village habitation of pre-European Māori in New Zealand. It was unfortified or only lightly fortified, and over time became less important to the well-defended pā. Description Kāinga were generally unfortified or only lightly fortified, as opposed to the well-defended pā. They were generally coastal, and often found near to a river mouth. The settlement was generally occupied by members of one ''hapū'' (sub-tribe), which would identify itself with the nearest mountain and river (even in modern Māori, when meeting someone new, "what is your mountain?" is not an unusual question). Kāinga were often regarded as only semi-permanent settlements, and they were often abandoned. Reasons for abandonment included invasion by other iwi or resource shortages. Traditionally, Māori were often semi-nomadic, with entire communities moving at harvest or to hunt, using the kāinga as a stable home base. An entir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The 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 year la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
