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Moturoa (island)
Moturoa is a steeply sloped island off the coast of Taranaki, New Zealand. It is the easternmost and largest of the Sugar Loaf Islands, hence its name, which is Māori for "long island". Moturoa is 120 metres long at its longest point, and around 100 metres wide. It is separated from the Taranaki coast of the North Island mainland by an wide channel. The entrance to Port Taranaki lies just to the east. The island has lent its name to Moturoa, a suburb of New Plymouth, which lies on the mainland 1.5 kilometres to the southeast. A cluster of smaller islands, of which Whareumu (Lion Rock) is the largest, lies some 60 metres off the island's southwest coast. Habitation Moturoa is uninhabited, but it and several of the other Sugar Loaf Islands were hunting, fishing and gathering grounds and places of refuge for local inhabitants and the Taranaki and Te Āti Awa for hundreds of years. Blasting Moturoa and Whareumu In the early 20th century Moturoa and Whareumu were blasted with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port Taranaki
Port Taranaki is a port complex located in New Plymouth, New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island count .... It is the only deep water port on the west coast of New Zealand, and is owned by the Taranaki Regional Council. The port handles a wide range of coastal and international cargoes, mostly relating to the farming, engineering and petrochemical industries. Adjacent features include the city of New Plymouth, the New Plymouth Power Station and the Sugar Loaf Islands Marine Protected Area (SLIMPA). History The port was established in 1875, and construction of the main breakwater began in 1881 with Frederic Carrington ceremoniously laying the first stone. In 2007, Port Taranaki became the first port in New Zealand to receive official recognition for its har ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Plugs Of New Zealand
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Islands Of New Zealand
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uninhabited Islands Of New Zealand
The list of uninhabited regions includes a number of places around the globe. The list changes year over year as human beings migrate into formerly uninhabited regions, or migrate out of formerly inhabited regions. List As a group, the list of uninhabited places are called the "nonecumene". This is a special geography term which means the uninhabited area of the world. * Virtually all of the Ocean *Virtually all of Antarctica *Most of The Arctic *Most of Greenland *Most of The Sahara * Antipodes Islands * Ashmore and Cartier Islands * Bajo Nuevo Bank * Baker Island * Ball's Pyramid * Balleny Islands * Big Major Cay * Bouvet Island * Much of the interior of Brazil * Caroline Island * Clipperton Island * The semi-arid regions and deserts of Australia * Devon Island * Much of Eastern Oregon * Elephant Island * Elobey Chico * Ernst Thälmann Island * Much of Fiordland, New Zealand * Goa Island * Gough Island * Hans Island * Harmil * Hashima Island * Hatutu * Heard Island a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of Taranaki
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Islands Of Taranaki
An island or isle is a piece of subcontinental land completely surrounded by water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. Sedimentary islands in the Ganges Delta are called chars. A grouping of geographically or geologically related islands, such as the Philippines, is referred to as an archipelago. There are two main types of islands in the sea: continental islands and oceanic islands. There are also artificial islands (man-made islands). There are about 900,000 official islands in the world. This number consists of all the officially-reported islands of each country. The total number of islands in the world is unknown. There may be hundreds of thousands of tiny islands that are unknown and uncounted. The number of sea islands in the world is estimated to be more than 200,000. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Islands
This is a list of the lists of islands in the world grouped by country, by continent, by body of water A body of water or waterbody (often spelled water body) is any significant accumulation of water on the surface of Earth or another planet. The term most often refers to oceans, seas, and lakes, but it includes smaller pools of water such a ..., and by other classifications. For rank-order lists, see the other lists of islands below. Lists of islands by country Africa Antarctica Asia Europe North America Oceania South America Lists of islands by continent Lists of islands by body of water By ocean: By other bodies of water: List of ancient islands Other lists of islands External links Island Superlatives {{DEFAULTSORT:List Of Islands * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Desert Island
A desert island, deserted island, or uninhabited island, is an island, islet or atoll that is not permanently populated by humans. Uninhabited islands are often depicted in films or stories about shipwrecked people, and are also used as stereotypes for the idea of "paradise". Some uninhabited islands are protected as nature reserves, and some are privately owned. Devon Island in Canada's far north is the largest uninhabited island in the world. Small coral atolls or islands usually have no source of fresh water, but occasionally a freshwater lens can be reached with a well. Terminology Uninhabited islands are sometimes also called "deserted islands" or "desert islands". In the latter, the adjective '' desert'' connotes not desert climate conditions, but rather "desolate and sparsely occupied or unoccupied". The word ''desert'' has been "formerly applied more widely to any wild, uninhabited region, including forest-land", and it is this archaic meaning that appears in the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Āti Awa
Te Āti Awa is a Māori iwi with traditional bases in the Taranaki and Wellington regions of New Zealand. Approximately 17,000 people registered their affiliation to Te Āti Awa in 2001, with around 10,000 in Taranaki, 2,000 in Wellington and around 5,000 of unspecified regional location. Geographical landmarks Te Āti Awa recognise Taranaki as their ancestral homeland. Mount Taranaki dominates the regional landscape, and many of the eight local iwi, including Te Āti Awa, regard it as sacred. The iwi also maintains a cultural association with several waterways in the region, including Wai-o-ngana, Waiwakaiho, and the Waitara River in the Taranaki region. Historical tapu in the Wellington region include the Hutt River delta and Lowry Bay (Eastbourne); plus Waikawa, Motueka and Golden Bay in the South Island. History Foundations Te Awanuiarangi is recognised as the founding ancestor of Te Āti Awa. According to Te Āti Awa traditions, he was the product of a union between Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sugar Loaf Islands
The Sugar Loaf Islands (often Sugarloaf; mi, Ngā Motu, ) are a collection of five small uninhabited islands and several sea stacks near Port Taranaki, New Zealand. The largest, Moturoa Island, covers approximately . Motumahanga is the island furthest from shore, at approximately . Ngā Motu was one of the first areas inhabited by descendants of Te Whiti o Rongomai, and the islands and reefs were all named by Ngāti Te Whiti. The island group was given its English name in 1770 by James Cook because the reminded him of the way sugar was stored in heaps in Europe. The Sugar Loaf Islands Marine Protected Area (SLIMPA) was established in 1991 to protect the area from oil exploration. This strengthened the protection that had been in place since the formation of a marine park in 1986. In 2013 New Plymouth district councillors unanimously agreed to gift the protected area back to the government for Treaty of Waitangi claims and settlements, treaty settlement negotiations with Taranak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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