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Pukekiwiriki
The Pukekiwiriki (alternatively spelled and pronounced Pukekoiwiriki), also known as Red Hill, is the northernmost volcano of the South Auckland volcanic field in New Zealand, located east of Papakura, which erupted an estimated one million years ago. The hill was the site of a major Tāmaki Māori pā, and the Te Ākitai Waiohua village Te Aparangi in the 19th century. Etymology The name in Māori literally means "the Hill of the Little Kiwi", but is also known by the name Pukekōiwiriki. This name, directly translated as "hill" (''puke''-) "bones" (''koiwi''-) "of the Riki people" (''riki'') or sometimes as "the Hill of the Small Skeleton", refers to the remains of ancient chiefs found at this hill, and the red soil, stained by their deaths. The English language name, Red Hill, refers to the red volcanic soils on the volcano's slopes. Geology and biodiversity Pukekiwiriki is a basalt volcano that erupted an estimated 1,000,000 years ago. The eruption flowed west towar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Auckland Volcanic Field
The South Auckland volcanic field, also known as the Franklin Volcanic Field, is an area of extinct monogenetic volcanoes around Pukekohe, the Franklin area and north-western Waikato, south of the Auckland volcanic field. The field contains at least 82 volcanoes, which erupted between 550,000 and 1,600,000 years ago. Features The field extends from Pukekiwiriki east of Papakura in the north and Pukekawa in the south. The field contains at least 82 volcanoes, and is older than the Auckland volcanic field to the north. The youngest volcanoes are likely the Bombay Hills shield volcano, which erupted an estimated 600,000 years ago, and Pukekohe Hill, the largest shield volcano of the field, which erupted an estimated 550,000 years ago. The largest tuff ring in the field is Onewhero maar which is in diameter and was formed 880,000 years ago.The field can be divided into three broad geographic areas: the north-eastern section, which consists of eroded remnants of lava flows and sco ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Invasion Of The Waikato
The Invasion of the Waikato became the largest and most important campaign of the 19th-century New Zealand Wars. Hostilities took place in the North Island of New Zealand between the military forces of the colonial government and a federation of Māori tribes known as the Kingitanga Movement. The Waikato is a territorial region with a northern boundary somewhat south of the present-day city of Auckland. The campaign lasted for nine months, from July 1863 to April 1864. The invasion was aimed at crushing Kingite power (which European settlers saw as a threat to colonial authority) and also at driving Waikato Māori from their territory in readiness for occupation and settlement by European colonists. The campaign was fought by a peak of about 14,000 Imperial and colonial troops and about 4,000 Māori warriors drawn from more than half the major North Island tribal groups. Plans for the invasion were drawn up at the close of the First Taranaki War in 1861 but the Colonial Off ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manukau Harbour
The Manukau Harbour is the second largest natural harbour in New Zealand by area. It is located to the southwest of the Auckland isthmus, and opens out into the Tasman Sea. Geography The harbour mouth is between the northern head ("Burnett Head" / "Ohaka Head") located at the southern end of the Waitākere Ranges and South Head at the end of the Āwhitu Peninsula reaching up from close to the mouth of the Waikato River. The mouth is only 1800 metres wide, but after a nine kilometre channel it opens up into a roughly square basin 20 kilometres in width. The harbour has a water surface area of 394 square kilometres. There is a tidal variation of up to 4 metres, a very substantial change, especially since the harbour, being silted up with almost 10 million years of sedimentation, is rather shallow itself.Manukau Ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism Of New Zealand
The volcanism of New Zealand has been responsible for many of the country's geographical features, especially in the North Island and the country's outlying islands. While the land's volcanism dates back to before the Zealandia microcontinent rifted away from Gondwana 60–130 million years ago, activity continues today with minor eruptions occurring every few years. This recent activity is primarily due to the country's position on the boundary between the Indo-Australian and Pacific Plates, a part of the Pacific Ring of Fire, and particularly the subduction of the Pacific Plate under the Indo-Australian Plate. New Zealand's rocks record examples of almost every kind of volcanism observed on Earth, including some of the world's largest eruptions in geologically recent times. None of the South Island's volcanoes are active. Major eruptions New Zealand has been the site of many large explosive eruptions during the last two million years, including several of supervol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Auckland Region
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The Auckland Region
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, Stratum, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic Waterbody, waterbodies and sub-surface features. Mountains, hills, Plateau, plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Auckland
Auckland (pronounced ) ( mi, Tāmaki Makaurau) is a large metropolitan city in the North Island of New Zealand. The most populous urban area in the country and the fifth largest city in Oceania, Auckland has an urban population of about It is located in the greater Auckland Region—the area governed by Auckland Council—which includes outlying rural areas and the islands of the Hauraki Gulf, and which has a total population of . While European New Zealanders, Europeans continue to make up the plurality of Auckland's population, the city became multicultural and cosmopolitan in the late-20th century, with Asians accounting for 31% of the city's population in 2018. Auckland has the fourth largest foreign-born population in the world, with 39% of its residents born overseas. With its large population of Pasifika New Zealanders, the city is also home to the biggest ethnic Polynesian population in the world. The Māori-language name for Auckland is ', meaning "Tāmaki ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Papakura Local Board Area
Papakura is a southern suburb of Auckland, in northern New Zealand. It is located on the shores of the Pahurehure Inlet, approximately 32 kilometres south of the Auckland CBD. It is under the authority of the Auckland Council. Papakura is a Māori word believed to have originated from ''papa'', meaning ''earth'' or ''flat'' (abbreviation of ''Papatūānuku'') and ''kura'' meaning ''red'', reflecting the rich, fertile soil upon which the community was founded. History A village was established at Papakura in the late 1840s by a small group of settler families who sought to farm in the area. Among these early settlers was George Cole, a Welsh immigrant whose legacy in the town has been preserved through ''Coles Crescent'', one of the major thoroughfares in the town centre. The tract of land that was initially purchased was subdivided in 1853, with the street layout that was built initially remaining largely in place today. In 1862, construction of the Great South Road, from Au ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Environmental Protection Authority (New Zealand)
The Environmental Protection Authority (EPA) (Māori Māori or Maori can refer to: Relating to the Māori people * Māori people of New Zealand, or members of that group * Māori language, the language of the Māori people of New Zealand * Māori culture * Cook Islanders, the Māori people of the C ...: ''Te Mana Rauhī Taiao'') is New Zealand government agency (Crown entity/agent) It is New Zealand's national-level environmental regulator. Its vision is "an environment protected, enhancing our way of life and the economy." As a Crown agent under the Crown entity model, the EPA operates at arm’s length from Ministers. Its independence in decision making is protected by statute and the established governance structures. A letter of expectations is issued annually by its responsible Ministers which, within the context of its independence, sets out the broad expectations of the Government of the day. History The Environmental Protection Authority was established on 1 July 201 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Te Ata Waiohua
Ngāti Te Ata Waiohua is a Māori iwi from the area around the Manukau Harbour in the Auckland Region of New Zealand. Ngāti Te Ata Waiohua were traditionally known as Te Ruakaiwhare, after the tribal guardian Kaiwhare, who protects the waters of the Manukau Harbour. They occupy the area around Waiuku, Glenbrook, Akaaka, Ōtaua, Te Puni, Whakaūpoko, Mauku, Patumāhoe, Pukekohe, Paerātā, Waiau Pā, Clark's Beach, Āwhitu Peninsula, Huia and the Waitākere Ranges. The iwi gets its name from the famous Waiohua chieftainess Te Atairehia, a granddaughter of the founding Te Wai-o-Hua chief Te Hua-o-kaiwaka and daughter of Huatau. She was given land in Waiuku after helping the local hapū (sub-tribe) Ngāti Kahukōkā in its fight against other tribes. Te Atairehia married Tapaue, a Ngāti Mahuta chief who was killed after winning control of a stretch of the Waikato River from Taupiri to Port Waikato. His death was avenged by his son Pāpaka, who secured Waiuku for Ngāti Te Ata Waio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taro
Taro () (''Colocasia esculenta)'' is a root vegetable. It is the most widely cultivated species of several plants in the family Araceae that are used as vegetables for their corms, leaves, and petioles. Taro corms are a food staple in African, Oceanic, and South Asian cultures (similar to yams). Taro is believed to be one of the earliest cultivated plants. Names and etymology The English term ''taro'' was borrowed from the Māori language when Captain Cook first observed ''Colocasia'' plantations there in 1769. The form ''taro'' or ''talo'' is widespread among Polynesian languages:*''talo'': taro (''Colocasia esculenta'') – entry in the ''Polynesian Lexicon Project Online'' (Pollex). in Tahitian; in < ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sweet Potato Cultivation In Polynesia
Sweet potato cultivation in Polynesia as a crop began around 1000 AD in central Polynesia. The plant became a common food across the region, especially in Hawaii, Easter Island and New Zealand, where it became a staple food. By the 1600s in central Polynesia, traditional cultivars were being replaced with hardier and larger varieties from the Americas (a process which began later in New Zealand, in the early 1800s). Many traditional cultivars are still grown across Polynesia, but they are rare and are not widely commercially grown. It is unknown how sweet potato began to be cultivated in the Pacific, but the current scholarly consensus is that the presence of sweet potato in Polynesia is evidence of Polynesian contact with South America. However, some genetic studies of traditional cultivars suggest that sweet potato was first dispersed to Polynesia before human settlement. History The sweet potato plant (''Ipomoea batatas'') is originally from the Americas, and became w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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