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Ngā Rā-a-Kupe
Ngā Rā-a-Kupe (), formerly known as Kupe's Sail, is a geological formation near the eastern end of Palliser Bay at the southern end of the North Island of New Zealand. It is composed of sedimentary rock which has been thrust up in an earthquake, resulting in a characteristic flat triangular ridge having the appearance of the kind of sail regularly used by Pacific explorers such as Kupe. According to Māori mythology Māori mythology and Māori traditions are two major categories into which the remote oral history of New Zealand's Māori people, Māori may be divided. Māori myths concern tales of supernatural events relating to the origins of what was the ..., the formation is the result of a sail-making competition between Kupe and his companion Ngake. After the sails were made, they were hung out to dry and were said to have formed the rock formation, which was then named after the legend. On 7 March 2023, the name of the rock formation was officially gazetted as Ng� ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff or rock face is an area of Rock (geology), rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and Dolomite (rock), dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Palliser / Mātakitaki-a-Kupe
Cape Palliser is a promontory on the southern coast of New Zealand's North Island and is the southernmost point of the North Island; it is in fact considerably farther south than Nelson or Blenheim in the South Island. It is located at the eastern end of Palliser Bay in the Wairarapa region, 50 kilometres southeast of Wellington – 100 kilometres by road. A small settlement, Ngawi, is situated near Cape Palliser, where the main income comes from crayfish (southern rock lobster) fishing. Fishing boats are pushed into the sea on their trailers by bulldozers. Ngā Rā-a-Kupe, previously known as Kupe's Sail, is a nearby triangular upthrust of sedimentary rock shaped like a sail. Māori history and the Kupe legend both feature Cape Palliser. Cape Palliser was named in 1770 by Captain James Cook in honour of his friend Admiral Sir Hugh Palliser of the British Royal Navy. On 7 March 2023, the name of the cape was officially gazetted as Cape Palliser / Mātakitaki-a-Kupe, followi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonic Uplift
Tectonic uplift is the orogeny, geologic uplift of Earth#Surface, Earth's surface that is attributed to plate tectonics. While Isostasy, isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of Thrust tectonics, crustal thickening (such as Mountain formation, mountain building events), changes in the density distribution of the crust and underlying Mantle (geology), mantle, and flexural support due to the bending of rigid lithosphere. Tectonic uplift results in denudation (processes that wear away the earth's surface) by raising buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting an isostatic response in the region of denudation (which can cause local bedrock uplift). The timing, magnitude, and rate of denudation can be estimated by geologists using pressure-temperature studies. Crustal thickening C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Language
Māori (; endonym: 'the Māori language', commonly shortened to ) is an Eastern Polynesian languages, Eastern Polynesian language and the language of the Māori people, the indigenous population of mainland New Zealand. The southernmost member of the Austronesian language family, it is related to Cook Islands Māori, Tuamotuan language, Tuamotuan, and Tahitian language, Tahitian. The Māori Language Act 1987 gave the language recognition as one of New Zealand's official languages. There are regional dialects of the Māori language. Prior to contact with Europeans, Māori lacked a written language or script. Written Māori now uses the Latin script, which was adopted and the spelling standardised by Northern Māori in collaboration with English Protestant clergy in the 19th century. In the second half of the 19th century, European children in rural areas spoke Māori with Māori children. It was common for prominent parents of these children, such as government officials, to us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kupe
Kupe was a legendary Polynesian explorer who, according to Māori oral history, was the first person to discover New Zealand. He is generally held to have been born to a father from Rarotonga and a mother from Raiatea, and probably spoke a Māori proto-language similar to Cook Islands Māori or Tahitian. His voyage to New Zealand ensured that the land was known to the Polynesians, and he would therefore be responsible for the genesis of the Māori people. Kupe was born in the geographically uncertain Māori homeland of Hawaiki, to a father from Rarotonga and a mother from Raiatea, between 40 and 23 generations ago. The more specific reasons for Kupe's semi-legendary journey, and the migration of Māori in general, have been contested. Māori oral history recounts that Hawaiki and other Polynesian islands were experiencing considerable internal conflict during his time, which is thought to have possibly caused an exodus. Kupe features prominently in the mythology and or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geographic Board
The New Zealand Geographic Board Ngā Pou Taunaha o Aotearoa (NZGB) is the authority over geographical and hydrographic names within New Zealand and its territorial waters. This includes the naming of small urban settlements, localities, mountains, lakes, rivers, waterfalls, harbours and natural features and may include researching local Māori names. It has named many geographical features in the Ross Sea region of Antarctica. It has no authority to alter street names (a local body responsibility) or the name of any country. The board was established by the New Zealand Geographic Board Act 1946, which has since been replaced by the New Zealand Geographic Board (Ngā Pou Taunaha o Aotearoa) Act 2008. Although an independent institution, it is responsible to the Minister for Land Information. The NZGB secretariat is part of Toitū Te Whenua Land Information New Zealand (LINZ) and provides the board with administrative and research assistance and advice. The New Zealand Geogra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kupe's Sail
Ngā Rā-a-Kupe (), formerly known as Kupe's Sail, is a geological formation near the eastern end of Palliser Bay at the southern end of the North Island of New Zealand. It is composed of sedimentary rock which has been thrust up in an earthquake, resulting in a characteristic flat triangular ridge having the appearance of the kind of sail regularly used by Pacific explorers such as Kupe. According to Māori mythology Māori mythology and Māori traditions are two major categories into which the remote oral history of New Zealand's Māori people, Māori may be divided. Māori myths concern tales of supernatural events relating to the origins of what was the ..., the formation is the result of a sail-making competition between Kupe and his companion Ngake. After the sails were made, they were hung out to dry and were said to have formed the rock formation, which was then named after the legend. On 7 March 2023, the name of the rock formation was officially gazetted as Ng� ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palliser Bay
Palliser Bay is at the southern end of the North Island of New Zealand, to the southeast of Wellington. It runs for 40 kilometres along the Cook Strait coast from Turakirae Head at the southern end of the Remutaka Ranges to Cape Palliser, the North Island's southernmost point. The coastline is exposed to the weather and winds. Inland from the bay is the plain of the Ruamahanga River, which has its outflow in the bay. This river flows through Lake Wairarapa, 10 kilometres from the coast. There are several notable geographical features in the area, including the Pūtangirua Pinnacles, Kupe's Sail Ngā Rā-a-Kupe (), formerly known as Kupe's Sail, is a geological formation near the eastern end of Palliser Bay at the southern end of the North Island of New Zealand. It is composed of sedimentary rock which has been thrust up in an earthq ... and the Whatarangi Bluff, the erosion of which has had dramatic effects on the coastline. Some of these cliffs are made of mudstone a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand
New Zealand () is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and List of islands of New Zealand, over 600 smaller islands. It is the List of island countries, sixth-largest island country by area and lies east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The Geography of New Zealand, country's varied topography and sharp mountain peaks, including the Southern Alps (), owe much to tectonic uplift and volcanic eruptions. Capital of New Zealand, New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and subsequently developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Mythology
Māori mythology and Māori traditions are two major categories into which the remote oral history of New Zealand's Māori people, Māori may be divided. Māori myths concern tales of supernatural events relating to the origins of what was the observable world for the pre-European Māori, often involving gods and demigods. Māori tradition concerns more folkloric legends often involving historical or semi-historical forebears. Both categories merge in to explain the overall origin of the Māori and their connections to the world which they lived in. The Māori did not have a writing system before European contact, beginning in 1769, therefore they relied on oral retellings and recitations memorised from generation to generation. The three forms of expression prominent in Māori and Polynesian oral literature are genealogical recital, poetry, and narrative prose. Experts in these subjects were broadly known as . The rituals, beliefs, and general worldview of Māori society were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
