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Taranaki Region
Taranaki is a region in the west of New Zealand's North Island. It is named after its main geographical feature, the stratovolcano of Mount Taranaki, also known as Mount Egmont. The main centre is the city of New Plymouth. The New Plymouth District is home to more than 65 per cent of the population of Taranaki. New Plymouth is in North Taranaki along with Inglewood and Waitara. South Taranaki towns include Hāwera, Stratford, Eltham, and Ōpunake. Since 2005, Taranaki has used the promotional brand "Like no other". Geography Taranaki is on the west coast of the North Island, surrounding the volcanic peak of Mount Taranaki. The region covers an area of 7258 km2. Its large bays north-west and south-west of Cape Egmont are North Taranaki Bight and South Taranaki Bight. Mount Taranaki is the second highest mountain in the North Island, and the dominant geographical feature of the region. A Māori legend says that Mount Taranaki previously lived with the Tongariro, ...
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Regions Of New Zealand
New Zealand is divided into sixteen regions () for local government purposes. Eleven are administered by regional councils (the top tier of local government), and five are administered by unitary authorities, which are territorial authorities (the second tier of local government) that also perform the functions of regional councils. The Chatham Islands Council is not a region but is similar to a unitary authority, authorised under its own legislation. Current regions History and statutory basis The regional councils are listed in Part 1 of Schedule 2 of the Local Government Act 2002, along with reference to the ''Gazette'' notices that established them in 1989. The Act requires regional councils to promote sustainable developmentthe social, economic, environmental and cultural well-being of their communities. The current regions and most of their councils came into being through a local government reform in 1989 that took place under the Local Government Act 1974. The ...
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Knightia Excelsa
''Knightia excelsa'', commonly called rewarewa (from Māori), is an evergreen tree endemic to the low elevation and valley forests of New Zealand's North Island and Marlborough Sounds (41° S) and the type species for the genus '' Knightia''. Rewarewa grows to 30 m tall, with a slender crown. The leaves are alternate, leathery, narrow oblong, 10 – 15 cm long and 2.5 - 3.5 cm wide, and without stipules. The flowers are 2 - 3.5 cm long, bright red, and borne in racemes 10 cm long. Produces dry woody follicles. It was called New Zealand honeysuckle by early European settlers but the name has fallen into disuse in preference for the Māori name. Rewarewa flowers are a great source for honey Honey is a sweet and viscous substance made by several bees, the best-known of which are honey bees. Honey is made and stored to nourish bee colonies. Bees produce honey by gathering and then refining the sugary secretions of plants (primar ... production. The rew ...
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Coriaria Arborea
''Coriaria arborea'' is a highly poisonous and common native shrub or small tree of New Zealand. The common name for this and the other New Zealand species of ''Coriaria'' is tutu. ''Coriaria arborea'' is found in scrub and open areas from the coast to the hills across the country. A straggling plant, it can grow to high. The leaves grow opposite on slender stems while flowers are arranged in drooping racemes. ''C. arborea'' is capable of nitrogen fixation. Ecology ''C. arborea'' plays host to several species of New Zealand endemic moth including '' Izatha austera'', ''I. churtoni'', '' I. mesoschista'' and '' I. peroneanella''. Uses In spite of its toxicity, Tutu was consumed by Māori, specifically the extracted juice from the fleshy flower petals. The gathered berries were placed in specially woven baskets lined with the flower heads of Toetoe, acting as a sieve to separate the poisonous seeds from the squeezed juice. The extracted juice is used as a sweetener to food ...
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Bracken
Bracken (''Pteridium'') is a genus of large, coarse ferns in the family Dennstaedtiaceae. Ferns (Pteridophyta) are vascular plants that have alternating generations, large plants that produce spores and small plants that produce sex cells (eggs and sperm). Brackens are noted for their large, highly divided leaves. They are found on all continents except Antarctica and in all environments except deserts, though their typical habitat is moorland. The genus probably has the widest distribution of any fern in the world. The word ''bracken'' is of Old Norse origin, related to Swedish ''bräken'' and Danish ''bregne'', both meaning fern. In the past, the genus was commonly treated as having only one species, ''Pteridium aquilinum'', but the recent trend is to subdivide it into about ten species. Like other ferns, brackens do not have seeds or fruits, but the immature fronds, known as '' fiddleheads'', are sometimes eaten, although some are thought to be carcinogenic. Description a ...
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Coastal Plain
A coastal plain is flat, low-lying land adjacent to a sea coast. A fall line commonly marks the border between a coastal plain and a piedmont area. Some of the largest coastal plains are in Alaska and the southeastern United States. The Gulf Coastal Plain of North America extends northwards from the Gulf of Mexico along the Lower Mississippi River to the Ohio River, which is a distance of about . The Atlantic Coastal Plain runs from the New York Bight to Florida. The Coastal Plains of India lie on either side of the Deccan Plateau, along the western and eastern coasts of India. They extend for about 6,150 km from the Rann of Kutch in the west to West Bengal in the east. They are broadly divided into the Western Coastal Plains and the Eastern Coastal Plains. The two coastal plains meet at Kanyakumari, the southernmost tip of the Indian mainland. The eastern coastal plain is located between The Bay of Bengal and the eastern Ghats and the western coastal plain is located betwee ...
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Egmont National Park
Egmont National Park () is located south of New Plymouth, close to the west coast of the North Island of New Zealand. The park covers Mount Taranaki and its slopes. The park was first created in 1881 as a forest reserve and went on to become New Zealand’s second national park in 1900. The forest reserve was created within a 6-mile (9.6-kilometre) radius around the cone of the dormant volcano. Areas encompassing the older volcanic remnants of Pouakai and Kaitake were later added to the reserve at the northwest side. The forest is surrounded on all sides by pasture, giving it a distinctly circular shape. Ecology The park receives massive annual rainfall. Moist westerlies from the Tasman Sea form Orographic precipitation when they reach Mount Taranaki and the adjacent Pouakai and Kaitake ranges. Since the area has high annual rainfall and a mild coastal climate there is a lush rainforest covering the foothills, a forest that is nationally significant for the total absence of ...
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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 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. 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. Ruapehu is the largest and southernm ...
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Mount 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 ...
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Mount 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 ...
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Mount Taranaki Legend
In Māori legend, Taranaki is a mountain being that lived peacefully for many centuries in the centre of Aotearoa's Te Ika-a-Māui with four other mountains. Of the four mountains Tongariro, Ngauruhoe and Ruapehu were still fighting. Nearby stood Mount Pihanga. Covered in a cloak of deep green forest she presented a stunning sight and all the mountain gods were in love with her. Taranaki dared to make advances to Pihanga and was reproached by Tongariro and a mighty battle ensued between them. The earth shook and the sky became dark as the mountains belched forth their anger. When the battle ended the lovely Pihanga stood close by Tongariro's side. Taranaki, wild with grief and jealously, angrily wrenched his roots from the ground and left the other mountains. Weeping, he plunged towards the setting sun, gouging out a deep wide trench. When he reached the sea he turned north and stumbled up the coast. As he slept that night the Pouakai Ranges snared and trapped Taranaki in the ...
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Taranaki Satellite
Taranaki is a region in the west of New Zealand's North Island. It is named after its main geographical feature, the stratovolcano of Mount Taranaki, also known as Mount Egmont. The main centre is the city of New Plymouth. The New Plymouth District is home to more than 65 per cent of the population of Taranaki. New Plymouth is in North Taranaki along with Inglewood and Waitara. South Taranaki towns include Hāwera, Stratford, Eltham, and Ōpunake. Since 2005, Taranaki has used the promotional brand "Like no other". Geography Taranaki is on the west coast of the North Island, surrounding the volcanic peak of Mount Taranaki. The region covers an area of 7258 km2. Its large bays north-west and south-west of Cape Egmont are North Taranaki Bight and South Taranaki Bight. Mount Taranaki is the second highest mountain in the North Island, and the dominant geographical feature of the region. A Māori legend says that Mount Taranaki previously lived with the Tongariro, Ngaur ...
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