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Onemana
Onemana is a 1970s beach village on the eastern side of the Coromandel Peninsula of New Zealand, with a beach, a surf club, fire station and dairy. It lies to the east of State Highway 25, south of Pauanui and north of Whangamatā. The Wharekawa River and Opoutere are just to the north and west. History The area was originally named Whitipirorua by Māori. The first known settlers of the area were the Ngāti Hei. They were supplanted by Ngāti Hako in the mid 17th century, but Ngā Puhi raids during the Musket Wars of the early 19th century left the area without a permanent population. By a variety of means the land was acquired by the government and sold to settlers. Archaeological evidence suggests that the area was first settled in the 1300s, with a pā located at the south of Onemana Beach. The area was important for the production of stone tools made of matā (chert) and matā tūhua (obsidian). The 364 section subdivision was created in the 1970s on the Bambury ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whitipirorua Point And The South End Of Onemana Beach
Onemana is a 1970s beach village on the eastern side of the Coromandel Peninsula of New Zealand, with a beach, a surf club, fire station and dairy. It lies to the east of State Highway 25, south of Pauanui and north of Whangamatā. The Wharekawa River and Opoutere are just to the north and west. History The area was originally named Whitipirorua by Māori. The first known settlers of the area were the Ngāti Hei. They were supplanted by Ngāti Hako in the mid 17th century, but Ngā Puhi raids during the Musket Wars of the early 19th century left the area without a permanent population. By a variety of means the land was acquired by the government and sold to settlers. Archaeological evidence suggests that the area was first settled in the 1300s, with a pā located at the south of Onemana Beach. The area was important for the production of stone tools made of matā (chert) and matā tūhua (obsidian). The 364 section subdivision was created in the 1970s on the Bambury fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whangamatā
The town of Whangamatā is on the southeast coast of the Coromandel Peninsula in the North Island of New Zealand. It is located 30 kilometres north of Waihi, to the north of the western extremity of the Bay of Plenty. In holiday times the population swells considerably: New Year's celebrations fill the town to over 25,000 though this falls soon after New Year's Day. A number of off-shore islands can be seen from the beach. ''Hauturu'' or Clark Island is accessible by wading at low tide and is popular in summer months for rock-pool fossickers and kayakers. ''Whenuakura'', sometimes known as Donut Island, sits about a kilometre east of the southern part of Whangamatā beach (Otahu Beach). Tuatara roamed on Whenuakura until fairly recently. Whenuakura Island has a large collapsed blow hole which has formed a small beach inside the island – hence the alternative name. The town has two ocean beaches, both of which are extremely safe for swimming and surfing. There is a safe boati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. 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 then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Obsidian
Obsidian () is a naturally occurring volcanic glass formed when lava extrusive rock, extruded from a volcano cools rapidly with minimal crystal growth. It is an igneous rock. Obsidian is produced from felsic lava, rich in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. It is commonly found within the margins of rhyolite, rhyolitic lava flows known as obsidian flows. These flows have a high content of silicon dioxide, silica, granting them a high viscosity. The high viscosity inhibits atomic diffusion, diffusion of atoms through the lava, which inhibits the first step (nucleation) in the formation of mineral crystals. Together with rapid cooling, this results in a natural glass forming from the lava. Obsidian is hard, Brittleness, brittle, and amorphous; it therefore Fracture (mineralogy)#Conchoidal fracture, fractures with sharp edges. In the past, it was used to manufacture cutting and piercing tools, and it has been used experimentally as surgic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landfill
A landfill site, also known as a tip, dump, rubbish dump, garbage dump, or dumping ground, is a site for the disposal of waste materials. Landfill is the oldest and most common form of waste disposal, although the systematic burial of the waste with daily, intermediate and final covers only began in the 1940s. In the past, refuse was simply left in piles or thrown into pits; in archeology this is known as a midden. Some landfill sites are used for waste management purposes, such as temporary storage, consolidation and transfer, or for various stages of processing waste material, such as sorting, treatment, or recycling. Unless they are stabilized, landfills may undergo severe shaking or soil liquefaction of the ground during an earthquake. Once full, the area over a landfill site may be reclaimed for other uses. Operations Operators of well-run landfills for non-hazardous waste meet predefined specifications by applying techniques to: # confine waste to as small an area as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent to granite. Rhyolitic magma is extremely viscous, due to its high silica content. This favors explosive eruptions over effusive eruptions, so this type of magma is more often erupted as pyroclastic rock than as lava flows. Rhyolitic ash-flow tuffs are among the most voluminous of continental igneous rock formations. Rhyolitic tuff has been extensively used for construction. Obsidian, which is rhyolitic volcanic glass, has been used for tools from prehistoric times to the present day because it can be shaped to an extremely sharp edge. Rhyolitic pumice finds use as an abrasive, in concrete, and as a soil amendment. Description Rhyolite i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Well
A well is an excavation or structure created in the ground by digging, driving, or drilling to access liquid resources, usually water. The oldest and most common kind of well is a water well, to access groundwater in underground aquifers. The well water is drawn up by a pump, or using containers, such as buckets or large water bags that are raised mechanically or by hand. Water can also be injected back into the aquifer through the well. Wells were first constructed at least eight thousand years ago and historically vary in construction from a simple scoop in the sediment of a dry watercourse to the qanats of Iran, and the stepwells and sakiehs of India. Placing a lining in the well shaft helps create stability, and linings of wood or wickerwork date back at least as far as the Iron Age. Wells have traditionally been sunk by hand digging, as is still the case in rural areas of the developing world. These wells are inexpensive and low-tech as they use mostly manual labour, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Groundwater
Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, perma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Christianity In New Zealand
Christianity in New Zealand dates to the arrival of missionaries from the Church Missionary Society who were welcomed onto the beach at Rangihoua Bay in December 1814. It soon became the predominant belief amongst the indigenous people with an estimated 60% of Māori pledging allegiance to the Christian message within the first 35 years. It remains New Zealand's largest religious group despite there being no official state church. Today, slightly less than half the population identify as Christian. The largest Christian groups are Catholic, Anglican and Presbyterian. Christian organisations are the leading non-government providers of social services in New Zealand. History The first Christian services conducted in New Zealand were carried out by Father Paul-Antoine Léonard de Villefeix, the Dominican chaplain on the ship ''Saint Jean Baptiste'' commanded by the French navigator and explorer Jean-François-Marie de Surville. Villefeix was the first Christian minister to set ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pasifika New Zealanders
Pasifika New Zealanders are a pan-ethnic group of New Zealanders associated with, and descended from, the indigenous peoples of the Pacific Islands outside of New Zealand itself (also known as Pacific Islanders). They form the fourth-largest ethnic grouping in the country, after European-descended Pākehā, indigenous Māori, and Asian New Zealanders. There are over 380,000 Pasifika people in New Zealand, with the majority living in Auckland. 8% of the population of New Zealand identifies as being of Pacific origin. History Prior to the Second World War Pasifika in New Zealand numbered only a few hundred. Wide-scale Pasifika migration to New Zealand began in the 1950s and 1960s, typically from countries associated with the Commonwealth and the Realm of New Zealand, including Western Samoa (modern-day Samoa), the Cook Islands and Niue. In the 1970s, governments (both Labour and National), migration officials, and special police squads targeted Pasifika illegal overstayers. Paci ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pākehā
Pākehā (or Pakeha; ; ) is a Māori term for New Zealanders primarily of European descent. Pākehā is not a legal concept and has no definition under New Zealand law. The term can apply to fair-skinned persons, or to any non-Māori New Zealander. Papa'a has a similar meaning in Cook Islands Māori. Historically before the arrival of other ethnic groups the word Māori meant 'ordinary' or 'normal'. The arrival of Europeans led to the formation of a new term to distinguish the self-regarded 'ordinary' or 'normal' Māori from the new arrivals. The etymology of the word ''Pākehā'' remains unclear, but the term was in use by the late-18th century. In December 1814 the Māori children at Rangihoua in the Bay of Islands were "no less eager to see the ''packaha'' than the grown folks". In Māori, plural noun-phrases of the term include (the definite article) and (the indefinite article). When the word was first adopted into English, the usual plural was 'Pakehas'. However, spe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2006 New Zealand Census
The New Zealand Census of Population and Dwellings ( mi, Te Tatauranga o ngā Tāngata Huri Noa i Aotearoa me ō rātou Whare Noho) is a national population and housing census conducted by government department Statistics New Zealand every five years. There have been 34 censuses since 1851. In addition to providing detailed information about national demographics, the results of the census play an important part in the calculation of resource allocation to local service providers. The 2018 census took place on Tuesday 6 March 2018. The next census is expected in March 2023. Census date Since 1926, the census has always been held on a Tuesday and since 1966, the census always occurs in March. These are statistically the month and weekday on which New Zealanders are least likely to be travelling. The census forms have to be returned by midnight on census day for them to be valid. Conducting the census Until 2018, census forms were hand-delivered by census workers during the lead ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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