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Lion Rock (New Zealand)
Lion Rock is a rocky headland located on Piha Beach in the Waitākere Ranges area of the Auckland Region, New Zealand. Geography The rock is located to the south of Piha beach, close to the major settlement at Piha. The Piha Stream flows into the Tasman Sea directly south of the rock. Geology The island is a volcanic plug of the Miocene era Waitākere Volcano, composed of stratified rudite and intrusive andesite. The rock is what remains of one of the volcano's funnel-shaped vents on the eastern side of the mountain, which was uplifted from the sea 17 million years ago. As the volcano aged and eroded, the Lion Rock vent filled with collapsed lava, scoria and volcanic bombs, until it formed into its modern-day shape. History The traditional name for the rock is Te Piha, and is a name that was applied to the wider area. The name Te Piha came from the pattern made when waves hit against the rock. Lion Rock is in the rohe of Te Kawerau ā Maki, and was the location of islan ... [...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] |
Rohe
The Māori people of New Zealand use the word ''rohe'' to describe the territory or boundaries of ''iwi'' (tribes), although some divide their rohe into several ''takiwā''. The areas shown on the map (right) are indicative only, and some iwi areas may overlap. The term ''rohe'' also combines with other words to form more modern terms. These include ''rohe pōti'', meaning an electoral district or constituency, ''rohe wā'', meaning time zone, and ''whatunga rohe paetata'', meaning a local area network. The term ''rohe'' on its own has also been adopted to mean an internet domain. The term is also used for the mission districts (''rohe mihana'') of Te Pīhopatanga o Aotearoa, the Māori Anglican Church in Aotearoa/New Zealand. See also * List of Māori iwi This is a list of iwi (New Zealand Māori tribes). List of iwi This list includes groups recognised as iwi (tribes) in certain contexts. Many are also hapū (sub-tribes) of larger iwi. Moriori are included on this list. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Plugs Of New Zealand
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Formations Of New Zealand
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in Wales * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, an isl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of The Auckland Region
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Records Of The Auckland 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 muse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Traditional Textiles
Māori traditional textiles are the indigenous textiles of the Māori people of New Zealand. The organisation Te Roopu Raranga Whatu o Aotearoa, the national Māori weavers' collective, aims to preserve and foster the skills of making and using these materials. Textiles made from locally sourced materials were developed by Māori in New Zealand after migration from Polynesia as the plants used in the Pacific islands did not grow well in the New Zealand climate. In traditional Māori weaving of garments the main fibre is called muka and is made from harakeke. The Māori language terms for different types of weaving are commonly named as raranga, whatu and whiri. Raranga is a plaiting technique used for making baskets and mats; whatu is a pre-European finger weft twining weaving method used to make cloaks; and whiri is braiding to make cord. Most people weaving traditional Māori textiles were and are women. Traditionally, to become expert a young woman was initiated into Te Whare ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Midden
A midden (also kitchen midden or shell heap) is an old dump for domestic waste which may consist of animal bone, human excrement, botanical material, mollusc shells, potsherds, lithics (especially debitage), and other artifacts and ecofacts associated with past human occupation. These features provide a useful resource for archaeologists who wish to study the diets and habits of past societies. Middens with damp, anaerobic conditions can even preserve organic remains in deposits as the debris of daily life are tossed on the pile. Each individual toss will contribute a different mix of materials depending upon the activity associated with that particular toss. During the course of deposition sedimentary material is deposited as well. Different mechanisms, from wind and water to animal digs, create a matrix which can also be analysed to provide seasonal and climatic information. In some middens individual dumps of material can be discerned and analysed. Shells A shell mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tainui
Tainui is a tribal waka confederation of New Zealand Māori iwi. The Tainui confederation comprises four principal related Māori iwi of the central North Island of New Zealand: Hauraki, Ngāti Maniapoto, Ngāti Raukawa and Waikato. There are other Tainui iwi whose tribal areas lay outside the traditional Tainui boundaries – Ngāi Tai in the Auckland area, Ngāti Raukawa ki Te Tonga and Ngāti Toa in the Horowhenua, Kapiti region, and Ngāti Rārua and Ngāti Koata in the northern South Island. History Early history The Tainui iwi share a common ancestry from Polynesian migrants who arrived in New Zealand on the ''Tainui'' waka, which voyaged across the Pacific Ocean from Hawaiki to Aotearoa (North Island) approximately 800 years ago. According to Pei Te Hurinui Jones, the Tainui historian, Tainui first entered the Waikato about 1400 bringing with them kumara plants. By about 1450 they had conquered the last of the indigenous people in a battle at Atiamuri. Contact with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Whātua
Ngāti Whātua is a Māori iwi (tribe) of the lower Northland Peninsula of New Zealand's North Island. It comprises a confederation of four hapū (subtribes) interconnected both by ancestry and by association over time: Te Uri-o-Hau, Te Roroa, Te Taoū, and Ngāti Whātua-o-Ōrākei. The four hapū can act together or separately as independent tribes. Ngāti Whātua's territory or ''rohe'' is traditionally expressed as, "''Tāmaki ki Maunganui i te Tai Hauauru''" and "''Tāmaki ki Manaia i te Rawhiti''". The northern boundary is expressed as, "''Manaia titiro ki Whatitiri, Whatitiri titiro ki Tutamoe, Tutamoe titiro ki Maunganui''". The southern boundary is expressed as, "''Te awa o Tāmaki''". The area runs from Tāmaki River in the south to Maunganui Bluff (at the northern end of Aranga Beach on the west coast) in the north, and to Whangarei Harbour on the east coast. By the time of European settlement in New Zealand, Ngāti Whātua's territory was around the Kaipara Harbour an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Government
, background_color = #012169 , image = New Zealand Government wordmark.svg , image_size=250px , date_established = , country = New Zealand , leader_title = Prime Minister Jacinda Ardern , appointed = Governor-General , main_organ = , ministries = 32 ministries and departments , responsible = House of Representatives , budget = 119.3 billion (2018–19) , address = The Beehive and other locations across Wellington , url = The New Zealand Government ( mi, Te Kāwanatanga o Aotearoa) is the central government through which political authority is exercised in New Zealand. As in most other parliamentary democracies, the term "Government" refers chiefly to the executive branch, and more specifically to the collective ministry directing the executive. Based on the principle of responsible government, it operates within the framework that "the Queen reigns, but the government rules, so long as it has the support of the House of Representatives".Sir Kenneth Keith, qu ... [...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] |
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