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Fairfield Intermediate
Fairfield Intermediate, sometimes shortened to FIS, is a year 7-8 school located in Fairfield, Hamilton, New Zealand. It has a roll of as of and has a decile rating of 5. The principal is Angela Walters. History The school was founded in 1963 and was and still is the only school in North-East Hamilton that caters to year 7-8 students. The school has for many years gone to Port Waikato and Pauanui for school camps. This has been changed for the 2013 camps where Pauanui is no longer used for the trips. Notable alumni Notable alumni of Fairfield Intermediate include Stan Walker (2002–2003), an actor and Australian Idol-winning singer, and Scott Styris (1987–1988), an all-rounder who has played for the Black Caps and Northern Districts. Extracurricular activities Fairfield Intermediate offers many opportunities in sport and music with yearly productions and successful sports teams. Their chess team has traditionally done well, winning many regional tournaments in the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fairfield, Waikato
Fairfield is a suburb to the northeast of central Hamilton, New Zealand. Fairfield is named after the dairy farm of John Davies, who bought 100 acres (0.40 km2) from F. R. Claude. This area experienced rapid growth in the 1950s and 60s. History Fairfield is named after the dairy farm of John Davies, who bought from F. R. Claude. This area experienced rapid growth in the 1950s and 60s. Features of Fairfield Fairfield Bridge Fairfield Bridge crosses the Waikato River and connects Fairfield with suburbs west of the river. It is a reinforced concrete road bridge, and well-known landmark. The bridge was built by Caesar Roose in 1936. It has a twin further north on the Waikato River at Tuakau. Demographics Fairfield covers and had an estimated population of as of with a population density of people per km2. Fairfield had a population of 4,383 at the 2018 New Zealand census, an increase of 390 people (9.8%) since the 2013 census, and an increase of 435 people (11.0%) sin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngauruhoe
Mount Ngāuruhoe (also spelled Ngauruhoe; Māori: ''Ngāuruhoe'') is a volcanic cone in New Zealand. It is the youngest vent in the Tongariro stratovolcano complex on the Central Plateau of the North Island and first erupted about 2,500 years ago. Although often regarded as a separate mountain, geologically, it is a secondary cone of Mount Tongariro. The volcano lies between the active volcanoes of Mount Tongariro to the north and Mount Ruapehu to the south, to the west of the Rangipo Desert and 25 kilometres to the south of the southern shore of Lake Taupō. Etymology The local Māori traditions state that the volcano was named by Ngātoro-i-rangi, an ancestor of the local Māori iwi, Ngāti Tūwharetoa. Ngātoro-i-rangi called volcanic fire from his homeland Hawaiki, which eventually emerged at Ngāuruhoe. The name given by Ngātoro-i-rangi (Ngāuruhoe) either commemorates his slave, who had died from the cold before the fire arrived, or refers to the insertion ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puriri
''Vitex lucens'', or pūriri, is an evergreen tree endemic to New Zealand. History Pūriri was first collected (by Europeans) at Tolaga Bay by Banks and Solander during Cook's first visit in 1769. The plant was excellently described by Solander in his manuscript "Primitae Florae Novae Zelandiae" under the name ''Ephielis pentaphylla'', and a drawing of considerable artistic merit was also prepared.Cheeseman (1914) Illustrations of the New Zealand Flora. Vol 2. The next botanist to notice pūriri, Allan Cunningham, did not do so until 1826 when he observed it on "the rocky shores of Bay of Islands, growing frequently within the range of salt water." Cunningham named it ''Vitex littoralis'', correctly assigning it to the genus ''Vitex'' but overlooking that "littoralis" had been used for a Malayan species 4 years earlier. Thomas Kirk proposed ''V. lucens'' in 1897 after attention had been drawn to the fact that ''V. littoralis'' was taken.A.C. Dijkgraaf (1994) Propagation and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Totara
''Podocarpus totara'' (; from the Maori-language ; the spelling "totara" is also common in English) is a species of podocarp tree endemic to New Zealand. It grows throughout the North Island and northeastern South Island in lowland, montane and lower subalpine forest at elevations of up to 600 m. Tōtara is commonly found in lowland areas where the soil is fertile and well drained. Description The tōtara is a medium to large tree, which grows slowly to around 20 to 25 m, exceptionally to 35 m; it is noted for its longevity and the great girth of its trunk. The bark peels off in papery flakes, with a purplish to golden brown hue. The sharp, dull-green, needle-like leaves are stiff and leathery, 2 cm long. This plant produces highly modified cones with two to four fused, fleshy, berry-like, juicy scales, bright red when mature. The cone contains one or two rounded seeds at the apex of the scales. The largest known living tōtara, the Pouakani Tree, near Pureora in the ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rimu
''Dacrydium cupressinum'', commonly known as rimu, is a large evergreen coniferous tree endemic to the forests of New Zealand. It is a member of the southern conifer group, the podocarps. The Māori name ''rimu'' comes from the Polynesian term ''limu'' which the tree's foliage were reminded of, ultimately from Proto-Austronesian *''limut'' meaning "moss". The former name "red pine" has fallen out of common use. Distribution Rimu grows throughout New Zealand, in the North Island, South Island and Stewart Island/Rakiura. This species is common in lowland and montane forest. Although the largest concentration of trees is now found on the West Coast of the South Island, the biggest trees tend to be in mixed podocarp forest near Taupō (e.g., Pureora, Waihaha, and Whirinaki Forests). A typical North Island habitat is in the Hamilton Ecological District, where '' Fuscospora truncata'' and rimu form the overstory. Associate ferns on the forest floor are ''Blechnum discolor'', ''B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kauri
''Agathis'', commonly known as kauri or dammara, is a genus of 22 species of evergreen tree. The genus is part of the ancient conifer family Araucariaceae, a group once widespread during the Jurassic and Cretaceous periods, but now largely restricted to the Southern Hemisphere except for a number of extant Malesian ''Agathis''.de Laubenfels, David J. 1988. Coniferales. P. 337–453 in Flora Malesiana, Series I, Vol. 10. Dordrecht: Kluwer Academic. Description Mature kauri trees have characteristically large trunks, with little or no branching below the crown. In contrast, young trees are normally conical in shape, forming a more rounded or irregularly shaped crown as they achieve maturity.Whitmore, T.C. 1977. ''A first look at Agathis''. Tropical Forestry Papers No. 11. University of Oxford Commonwealth Forestry Institute. The bark is smooth and light grey to grey-brown, usually peeling into irregular flakes that become thicker on more mature trees. The branch structu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nikau
''Rhopalostylis sapida'', commonly known as nīkau ( mi, nīkau), is a palm tree endemic to New Zealand, and the only palm native to mainland New Zealand. Etymology is a Māori word; in the closely related Eastern Polynesian languages of the tropical Pacific, it refers to the fronds or the midrib of the coconut palm. Distribution The nīkau palm is the only palm species endemic to mainland New Zealand. Its natural range is coastal and lowland forest on the North Island, and on the South Island as far south as Okarito (43°20′S) in the west and Banks Peninsula (43°5′S) in the east. It also occurs on Chatham Island and Pitt Island/Rangiauria to the south-east of New Zealand, where it is the world's southernmost palm at 44° 18'S latitude.Esler, A. E. 'The Nikau Palm', ''New Zealand's Nature Heritage'', Vol.2 Part 19 p.532, 1974 Nīkau grow up to 15 m tall, with a stout, green trunk which bears grey-green leaf scars. The trunk is topped by a smooth, bulging crownshaft ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Taranaki
Mount Taranaki (), also known as Mount Egmont, is a dormant stratovolcano in the Taranaki region on the west coast of New Zealand's North Island. It is the second highest point in the North Island, after Mount Ruapehu. The mountain has a secondary cone, Fanthams Peak ( mi, Panitahi), , on its south side. Name The name ''Taranaki'' comes from the Māori language. The Māori word means mountain peak, and is thought to come from , meaning "shining", a reference to the snow-clad winter nature of the upper slopes. It was also named and by iwi who lived in the region in "ancient times". Captain Cook named it Mount Egmont on 11 January 1770 after John Perceval, 2nd Earl of Egmont, a former First Lord of the Admiralty who had supported the concept of an oceanic search for ''Terra Australis Incognita''. Cook described it as "of a prodigious height and its top cover'd with everlasting snow," surrounded by a "flat country ... which afforded a very good aspect, being clothed with wood ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tongariro
Mount Tongariro (; ) is a compound volcano in the Taupō Volcanic Zone of the North Island of New Zealand. It is located to the southwest of Lake Taupō, and is the northernmost of the three active volcanoes that dominate the landscape of the central North Island. Geology Mount Tongariro is part of the Tongariro volcanic centre, which consists of four massifs made of andesite: Tongariro, Kakaramea-Tihia Massif, Pihanga, and Ruapehu at the southern end of the North Island Volcanic Plateau. The andesitic eruptions formed Tongariro, a steep stratovolcano, reaching a height of . Tongariro is composed of layers of both lava and tephra and the eruptions that built the current stratovolcano commenced about 275,000 years ago. Tongariro consists of at least 12 cones. Ngāuruhoe, while often regarded as a separate mountain, is geologically a cone of Tongariro. It is also the most active vent, having erupted more than 70 times since 1839, the last episode in 1973 to 1975. Activity ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Ruapehu
Mount Ruapehu (; ) is an active stratovolcano at the southern end of the Taupō Volcanic Zone and North Island volcanic plateau in New Zealand. It is northeast of Ohakune and southwest of the southern shore of Lake Taupō, within the Tongariro National Park. The North Island's major ski resorts and only glaciers are on its slopes. Ruapehu, the largest active volcano in New Zealand, has the highest point in the North Island and has three major peaks: Tahurangi (2,797 m), Te Heuheu (2,755 m) and Paretetaitonga (2,751 m). The deep, active volcanic crater, crater is between the peaks and fills with water between major eruptions, being known as Crater Lake ( mi, Te Wai ā-moe). The name ''Ruapehu'' means "pit of noise" or "exploding pit" in Māori language, Māori. Geography Ruapehu is located in the center of the North Island of New Zealand, northeast of Ohakune, New Zealand and southwest of the southern shore of Lake Taupō, within Tongariro National Park. Rua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamilton, New Zealand
Hamilton ( mi, Kirikiriroa) is an inland city in the North Island of New Zealand. Located on the banks of the Waikato River, it is the seat and most populous city of the Waikato region. With a territorial population of , it is the country's fourth most-populous city. Encompassing a land area of about , Hamilton is part of the wider Hamilton Urban Area, which also encompasses the nearby towns of Ngāruawāhia, Te Awamutu and Cambridge. In 2020, Hamilton was awarded the title of most beautiful large city in New Zealand. The area now covered by the city was originally the site of several Māori villages, including Kirikiriroa, from which the city takes its Māori name. By the time English settlers arrived, most of these villages, which sat beside the Waikato River, were abandoned as a result of the Invasion of Waikato and land confiscation (''Raupatu'') by the Crown. Initially an agricultural service centre, Hamilton now has a diverse economy and is the third fastest growing urba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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