Newdicks Beach
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Newdicks Beach
Newdicks Beach is located on the southeastern side of Okurei Point (Town point) in the Bay of Plenty in the North Island of New Zealand. The beach is approximately 2 km long and is a predominantly sandy beach. The sand is predominantly quartz giving it a light coloured appearance. The occasional black patches of sand are due to the mineral titanomagnitite which comes from andesitic volcanoes. The road which leads to the beach is privately owned (initially by the Newdicks family) and payment is required to drive down the gravel road, although it can be walked for free. Newdicks beach borders two pa sites (ancient 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 ... fortifications). Western Bay of Plenty District Beaches of the Bay of Plenty Region {{Bayo ...
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Bay Of Plenty
The Bay of Plenty ( mi, Te Moana-a-Toi) is a region of New Zealand, situated around a bight of the same name in the northern coast of the North Island. The bight stretches 260 km from the Coromandel Peninsula in the west to Cape Runaway in the east. The Bay of Plenty Region, governed by the Bay of Plenty Regional Council, incorporates several large islands in the bay, in addition to the mainland area. Called ''Te Moana-a-Toi'' (the Sea of Toi) in the Māori language after Toi, an early ancestor, the name 'Bay of Plenty' was bestowed by James Cook in 1769 when he noticed the abundant food supplies at several Māori villages there, in stark contrast to observations he had made earlier in Poverty Bay. History According to local Māori traditions, the Bay of Plenty was the landing point of several migration canoes that brought Māori settlers to New Zealand. These include the ''Mātaatua'', ''Nukutere'', ''Tākitimu'', '' Arawa'' and ''Tainui'' canoes. Many of the de ...
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North Island
The North Island, also officially named Te Ika-a-Māui, is one of the two main islands of New Zealand, separated from the larger but much less populous South Island by the Cook Strait. The island's area is , making it the world's 14th-largest island. The world's 28th-most-populous island, Te Ika-a-Māui has a population of accounting for approximately % of the total residents of New Zealand. Twelve main urban areas (half of them officially cities) are in the North Island. From north to south, they are Whangārei, Auckland, Hamilton, Tauranga, Rotorua, Gisborne, New Plymouth, Napier, Hastings, Whanganui, Palmerston North, and New Zealand's capital city Wellington, which is located at the south-west tip of the island. Naming and usage Although the island has been known as the North Island for many years, in 2009 the New Zealand Geographic Board found that, along with the South Island, the North Island had no official name. After a public consultation, the board officially ...
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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 country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ...
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Andesitic
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the feldsp ...
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Pa (Māori)
Pa, pa, PA, P.A. or pA may refer to: Businesses and organisations Government and military * Palestinian National Authority, also called Palestinian Authority, interim governing body of the Gaza Strip and part of the West Bank * Pakistan Army * People's Association (Singapore), a Singaporean grassroots statutory board * Philippine Army * Patrulla Águila * Planning Authority, a government agency of Malta Airlines * Pan American World Airways, IATA airline designator PA (to 1991) * Florida Coastal Airlines, IATA airline designator PA (1995–2010) * Airblue, IATA airline designator PA (from 2003) Other * Progressive Alliance, a political international of social-democratic, socialist and progressive political parties and organisations * Professional association, a type of business organization * PA Consulting Group * PA Media, a news agency in the UK and Ireland, formerly the Press Association * Produttori Associati, an Italian record label Linguistics * Pa (cuneiform), a cunei ...
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Māori People
The Māori (, ) are the indigenous Polynesian people of mainland New Zealand (). Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed their own distinctive culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Initial contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi in 1840, the two cultures coexisted for a generation. Rising tensions over disputed land sales led to conflict in the 1860s, and massive land confiscations, to which ...
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Western Bay Of Plenty District
Western Bay of Plenty District is a territorial district within the Bay of Plenty Region of New Zealand. The district envelops Tauranga City by land, and includes Matakana Island, at the entrance to Tauranga Harbour. Local government The seat of the Western Bay of Plenty District Council is at Greerton in Tauranga City (which is a separate area that is not part of the district). The district came into being in the local government reorganisation of 1989; with minor modifications to the boundaries, it merged the old Tauranga County and Te Puke Borough. The greatest changes were in the northwest, with Waihi Beach being transferred to the district from the old Ohinemuri County, and in the vicinity of Tauranga City, where some of the hinterland, formerly in the county, was transferred to the city. The wards (for the purposes of electing district councillors) are the following: * Waihi Beach-Katikati Ward: (seat at Katikati) ** Waihi Beach Sub-Division ** Katikati Sub-Division * Kai ...
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