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State Highway 5 (New Zealand)
State Highway 5 (SH 5), one of New Zealand's eight national highways, runs from State Highway 1 at Tīrau, in the south Waikato, to State Highway 2, close to the Hawkes Bay coast at Bay View, 10 km north of Napier. It is the second shortest of the national highways. SH 5 is a two-lane single carriageway, except for a two-kilometre section of dual carriageway in Rotorua, and has at-grade intersections and property accesses in both rural and urban areas. The NZ Transport Agency classifies SH 5 as a regional strategic highway, except for the section concurrent with SH 1 around Taupō, where it is classified as a national strategic road. Route SH 5 leaves SH 1 at a roundabout just south-east of the town of Tīrau in the south Waikato and heads east, crossing over the Mamaku Ranges to Lake Rotorua. The highway skirts the southwestern edge of the lake, entering the city of Rotorua and continuing south through the Rotorua-Taupō thermal area to the upper reaches of the Waika ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thermal Explorer Highway
A thermal column (or thermal) is a rising mass of buoyant air, a convective current in the atmosphere, that transfers heat energy vertically. Thermals are created by the uneven heating of Earth's surface from solar radiation, and are an example of convection, specifically atmospheric convection. Thermals on Earth The Sun warms the ground, which in turn warms the air directly above. The warm air near the surface expands, becoming less dense than the surrounding air. The lighter air rises and cools due to its expansion in the lower pressure at higher altitudes. It stops rising when it has cooled to the same temperature, thus density, as the surrounding air. Associated with a thermal is a downward flow surrounding the thermal column. The downward-moving exterior is caused by colder air being displaced at the top of the thermal. The size and strength of thermals are influenced by the properties of the lower atmosphere (the ''troposphere''). When the air is cold, bubbles of warm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Opepe, New Zealand
Opepe was a settlement in New Zealand, a few miles southeast of Taupō. It was the scene of an attack on European militia by Maori on 7 June 1869, in which nine members of the militia were killed. The Opepe Maori settlement was at the intersection of two major pre-European walking tracks (Taupo- Napier and Urewera-Tokaanu). It was the birthplace of the Maori leader Te Rangitahau. The New Zealand Ministry for Culture and Heritage gives a translation of "place of the moth" for ''Ōpepe''. During Te Kooti's War, in early June 1869 Te Kooti and about 150 of his supporters moved towards Lake Taupō in the center of the North Island. At Opepe, just short of Taupō, they ran into party of fourteen Militia, who were camped in the abandoned village. Nine of the militia were killed with no loss to Te Kooti. One of the men, who was drying his uniform, escaped completely naked across rough country in mid-winter, and was awarded the New Zealand Medal. A military stockade was built at Opepe in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wind Farm
A wind farm or wind park, also called a wind power station or wind power plant, is a group of wind turbines in the same location used Wind power, to produce electricity. Wind farms vary in size from a small number of turbines to several hundred wind turbines covering an extensive area. Wind farms can be either onshore or offshore. Many of the largest operational onshore wind farms are located in China, India, and the United States. For example, the List of onshore wind farms, largest wind farm in the world, Gansu Wind Farm in China had a capacity of over 6,000 megawatt, MW by 2012,Watts, Jonathan & Huang, CecilyWinds Of Change Blow Through China As Spending On Renewable Energy Soars ''The Guardian'', 19 March 2012, revised on 20 March 2012. Retrieved 4 January 2012. with a goal of 20,000 MWFahey, JonathanIn Pictures: The World's Biggest Green Energy Projects ''Forbes'', 9 January 2010. Retrieved 19 June 2019. by 2020.Kanter, DougGansu Wind Farm ''Forbes''. Retrieved 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mohaka River
The Mohaka river is on the North Island of New Zealand in the east central region of Hawke’s Bay. Mohaka is a Maori word, roughly translated it means “place for dancing”. The iwi (Māori tribes) associated with the Mohaka River are Ngāti Pāhauwera, Ngāti Hineuru, Ngāti Tūwharetoa and Mana Ahuriri. The headwaters are found in the Kaweka and Kaimanawa ranges. From the range it winds southeast before twisting northeast and finally southeast again to empty into the Pacific Ocean near the town of Mohaka. There are many gorges on the Mohaka; some as steep as 200m (656 feet). Its main tributaries are the Waipunga, Taharua, Hautapu rivers. The full length is and it drains a basin of . HistoryNgati Pahauwera s traditional tribal territory is from the Te Hoe river junction to its mouth. The river, including its waters, bed and fisheries, is a taonga of Ngati P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waipunga River
The Waipunga River is a tributary of the Mohaka River, located between Taupō and Napier in New Zealand's North Island. It runs roughly 50 km from its source near the eastern edge of the Volcanic Plateau A volcanic plateau is a plateau produced by volcanic activity. There are two main types: lava plateaus and pyroclastic plateaus. Lava plateau Lava plateaus are formed by highly fluid basaltic lava during numerous successive eruptions throu ... to its junction with the Mohaka, of which some 15 km follow alongside the Napier-Taupō highway ( State Highway 5). The scenic Waipunga Falls are visible from a rest stop along the highway. Rivers of the Hawke's Bay Region Rivers of New Zealand {{HawkesBay-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Island Volcanic Plateau
The North Island Volcanic Plateau (often called the Central Plateau and occasionally the Waimarino Plateau) is a volcanic plateau covering much of central North Island of New Zealand with volcanoes, lava plateaus, and crater lakes. It contains the Taupō caldera complex, Okataina caldera complex and Tongariro Volcanic Centre being currently the most frequently active and productive area of silicic volcanism on Earth. New Zealand is part of the Pacific Ring of Fire. Location and description The plateau is approximately east–west and the north–south distance is about . Extensive ignimbrite sheets spread east and west from the Central Taupō Volcanic Zone, centred on the huge active supervolcanic caldera of Lake Taupō, now the largest lake in New Zealand. This last erupted less than 2000 years ago. The volcanic area includes the three active peaks of Mount Tongariro, Mount Ngāuruhoe, and Mount Ruapehu in the south, and extends beyond Rotorua in the north reaching ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rangitaiki River
The Rangitaiki River is the longest river in the Bay of Plenty region in New Zealand's North Island. It is long, and rises inland from northern Hawkes Bay to the east of the Kaingaroa Forest. The Rangitaiki catchment covers an area of 3005 km. It flows in a generally northeastward direction, passing through the town of Murupara and skirting close to the western edge of Te Urewera National Park before turning northwards, flowing past Edgecumbe and into the Bay of Plenty close to Thornton. There are two man-made lakes on the Rangitaiki formed by hydro-electric dams, Lake Āniwaniwa (formerly Lake Aniwhenua). and Lake Matahina. History In April 2017, remnants of Cyclone Debbie caused heavy rainfall in the region. At 8:30 am on April 6, water from the Rangitaiki River breached the College Road floodwall at Edgecumbe, causing widespread flooding across the township. A state of emergency was declared for the Whakatane District, and around 2,000 people were evacuated to Ka ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iwitahi
Iwitahi is a rural locality in the Taupo District and Bay of Plenty Region of New Zealand's North Island. It is situated on State Highway 5 between Taupo and Napier, about 20 km southeast of Taupo. It is a farming area, largely surrounded by forest, close to the plains of the upper Rangitaiki River The Rangitaiki River is the longest river in the Bay of Plenty region in New Zealand's North Island. It is long, and rises inland from northern Hawkes Bay to the east of the Kaingaroa Forest. The Rangitaiki catchment covers an area of 3005&nb .... The locality was formerly known as ''Iwatahi''.''Wise's New Zealand guide'' (1969) Dunedin: H. Wise & Co, p. 106 References Taupō District Populated places in the Bay of Plenty Region {{BayofPlenty-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hatepe Eruption
The Hatepe eruption, named for the Hatepe Plinian pumice tephra layer, sometimes referred to as the Taupō eruption or Horomatangi Reef Unit Y eruption, is dated to 232 CE ± 10 and was Taupō Volcano's most recent major eruption. It is thought to be New Zealand's largest eruption within the last 20,000 years. The eruption ejected some of material, of which just over was ejected in a few minutes. This makes it one of the largest eruptions in the last 5,000 years, comparable to the Minoan eruption in the 2nd millennium BCE, the 946 eruption of Paektu Mountain, the 1257 eruption of Mount Samalas, and the 1815 eruption of Mount Tambora. Stages of the eruption The eruption went through several stages, with six distinct marker horizons identified. Despite the uniform composition of the erupted magma, a wide variety of eruptive styles were displayed, including weak phreatomagmatism, Plinian eruptions, and a huge pyroclastic flow. Rhyolitic lava domes were extruded some ye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaingaroa Forest
Kaingaroa Forest covers 2900 km² of the Bay of Plenty region of New Zealand, and is the largest forest plantation in New Zealand, and the second largest in the Southern Hemisphere (after the 6000km² Sabie/Graskop plantation in South Africa). The forest stretches from Lake Taupō in the south to Kawerau to the north. The headquarters of the forest are at the small settlement of Kaingaroa, Bay of Plenty, 50 kilometres southeast of Rotorua. Prior to planting the area was a tussock and scrub plateau (ranging between and high), formed on volcanic ash. The New Zealand Ministry for Culture and Heritage gives a translation of "long area of land" for ''Kāingaroa''. The forest was first planted in the late 1920s and owned as a state asset by the New Zealand government. Experimental planting of douglas fir and radiata pine began on a block at Kaingaroa in 1901 and continued from 1906 using Waiotapu prison labour. By 1932 the pines averaged high and in diameter. Later plan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
