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Rangipo
Te Onetapu (), commonly known as the Rangipo Desert (), is a barren desert-like environment located in New Zealand, located in the Ruapehu District on the North Island Volcanic Plateau; to the east of the three active peaks of Mount Tongariro, Mount Ngauruhoe, and Mount Ruapehu, and to the west of the Kaimanawa Range. Etymology Two main names have been given to the desert, both of which are derived from te reo Māori and describe the area's history. The first of these, Te Onetapu, is derived from the words - beach or sand, and - sacred. This name refers to the death of Taiteariki, an ancestor of the Ngāti Rangi iwi who was killed at a location in the desert in early Māori history after conflict arose between him and two children of Houmea, Tura and Rotuia. Following Pākehā settlement and expansion into the region, the desert became known as Rangipo, from the Māori words , meaning sky, and , meaning night or darkness. This name references the story of Ngātoro-i-rangi, ... [...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 Volcano, Taupō caldera complex, Ōkataina Caldera, Ōkataina caldera complex and Mount Tongariro, Tongariro Volcanic Centre resulting in it 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 supervolcano, 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 Ngauruhoe, and M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Ruapehu
Mount Ruapehu (; English ) is an active stratovolcano at the southern end of the Taupō Volcanic Zone and North Island North Island Volcanic Plateau, volcanic plateau in New Zealand. It is northeast of Ohakune and southwest of the southern shore of Lake Taupō, within 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 (). The name ''Ruapehu'' means "pit of noise" or "exploding pit" in Māori language, Māori. Geography Ruapehu is located in the centre of the North Island of New Zealand, northeast of Ohakune, New Zealand, and southwest of the southern shore of Lake Taupō, within Tongariro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Desert
A volcanic desert is an area largely or completely devoid of vegetation because of volcanic activity. The term is usually applied to larger areas such as the Highlands of Iceland, the Rangipo Desert in New Zealand or Cordón Caulle in Chile. Occasionally though, it is used for relatively small regions such as the Kaʻū Desert on the island of Hawaiʻi. Volcanic deserts may have enough precipitation to sustain vegetation, but due to repeated covering of tephra and acid rain after eruptions and high percolation and infiltration rates of water, vegetation is scarce. In addition to this volcanic desert shows often poor or little soil formation due to slow chemical weathering caused by cold climate or coarse tephra. This is how the Plaine des Sables, on the island of Réunion, can find itself close to the Commerson Crater, a place which holds several world records of rainfall. Examples * Highlands of Iceland, in Iceland. * Plaine des Sables, in France. * Kaʻū Desert, in Ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ruapehu District
Ruapehu District is a Territorial authorities of New Zealand, territorial authority in the centre of New Zealand's North Island. It has an area of 6,734 square kilometers and the district's population in was . Features The district is landlocked, and contains the western half of the Tongariro National Park, including Mount Ruapehu and the western sides of Mount Ngauruhoe and Mount Tongariro, as well as part of the Whanganui National Park. The district is also home to the world-famous Raurimu Spiral on the North Island Main Trunk, North Island Main Trunk railway line. The tourist towns of Raetihi, Whakapapa Village, National Park, and Ohakune are located near Mount Ruapehu in the south-east of the district. Waiouru, with an elevation of 815 metres, is in the extreme south-east of the district and houses the large Waiouru Army Camp. The southern section of the infamous Desert Road section of State Highway 1 (New Zealand), State Highway 1 runs through the east of the district, fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Desert
A volcanic desert is an area largely or completely devoid of vegetation because of volcanic activity. The term is usually applied to larger areas such as the Highlands of Iceland, the Rangipo Desert in New Zealand or Cordón Caulle in Chile. Occasionally though, it is used for relatively small regions such as the Kaʻū Desert on the island of Hawaiʻi. Volcanic deserts may have enough precipitation to sustain vegetation, but due to repeated covering of tephra and acid rain after eruptions and high percolation and infiltration rates of water, vegetation is scarce. In addition to this volcanic desert shows often poor or little soil formation due to slow chemical weathering caused by cold climate or coarse tephra. This is how the Plaine des Sables, on the island of Réunion, can find itself close to the Commerson Crater, a place which holds several world records of rainfall. Examples * Highlands of Iceland, in Iceland. * Plaine des Sables, in France. * Kaʻū Desert, in Ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaimanawa Range
The Kaimanawa Range, officially called the Kaimanawa Mountains since 16 July 2020, is a range of mountains in the central North Island of New Zealand. They extend for 50 kilometres in a northeast–southwest direction through largely uninhabited country to the south of Lake Taupō, east of the "Desert Road". Their slopes form part of the North Island Volcanic Plateau. The New Zealand Ministry for Culture and Heritage gives a translation of "breath for food" for ''Kaimanawa''. The lands around the mountains are scrubby. To the west, where the Rangipo Desert is located, the soils are poor quality. To the east, the soils are more fertile, but the land is very rough. A population of feral horses, the Kaimanawa horses, roam free on the ranges. Unlike the majority of mountain ranges in New Zealand, the Kaimanawa Range is divided into private land. Considerable areas of the Rangipo Desert are used by the New Zealand Army for training. Demographics Kaimanawa covers and had an estimate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Ngauruhoe
Mount Ngauruhoe () is a volcanic cone in New Zealand. It is the youngest vent in the Mount Tongariro, Tongariro stratovolcano complex on the Central Plateau, New Zealand, 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 to the south of the southern shore of Lake Taupō. Etymology Before the initial mapping of the area introduced labelling confusion, the local Māori name for the cone was Tongariro, and its summit crater was known as Ngāuruhoe. 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 Ngauruhoe. The name ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Treaty Of Waitangi
The Treaty of Waitangi (), sometimes referred to as ''Te Tiriti'', is a document of central importance to the history of New Zealand, Constitution of New Zealand, its constitution, and its national mythos. It has played a major role in the treatment of the Māori people in New Zealand by successive governments and the wider population, something that has been especially prominent from the late 20th century. The treaty document is an agreement, not a treaty as recognised in international law. It was first signed on 6 February 1840 by Captain William Hobson as Administrative consul, consul for the British Crown and by Māori chiefs () from the North Island of New Zealand. The treaty's quasi-legal status satisfies the demands of biculturalism in contemporary New Zealand society. In general terms, it is interpreted today as having established a partnership between equals in a way the Crown likely did not intend it to in 1840. Specifically, the treaty is seen, first, as entitling M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Treaty Of Waitangi Claims And Settlements
Claims and settlements under the Treaty of Waitangi () have been a significant feature of New Zealand politics since the Treaty of Waitangi Act 1975 and the Waitangi Tribunal that was established by that act to hear claims. Successive governments have increasingly provided formal legal and political opportunity for Māori to seek redress for what are seen as breaches by the Crown of guarantees set out in the Treaty of Waitangi. While it has resulted in putting to rest a number of significant longstanding grievances, the process has been subject to criticisms including those who believe that the redress is insufficient to compensate for Māori losses. The settlements are typically seen as part of a broader Māori Renaissance. The Waitangi Tribunal was set up as the primary means of registering and researching claims because the Treaty of Waitangi itself has little legal standing. The primary means of settling those claims is through direct negotiations with the government of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Soil Quality
Soil quality refers to the condition of soil based on its capacity to perform ecosystem services that meet the needs of human and non-human life.Tóth, G., Stolbovoy, V. and Montanarella, 2007. Soil Quality and Sustainability Evaluation - An integrated approach to support soil-related policies of the European Union", EUR 22721 EN. 40 pp. Office for Official Publications of the European Communities, Luxembourg. . Soil quality reflects how well a soil performs the functions of maintaining biodiversity and productivity, partitioning water and solute flow, filtering and buffering, nutrient cycling, and providing support for plants and other structures. Soil management has a major impact on soil quality. Soil quality relates to soil functions. Unlike water or air, for which established standards have been set, soil quality is difficult to define or quantify. Indicators of soil quality Soil quality can be evaluated using the Soil Management Assessment Framework. Soil quality in agric ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
