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Turakirae Head
Turakirae Head is a promontory on the southern coast of New Zealand's 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 .... It is located at the western end of Palliser Bay, 20 kilometres southeast of Wellington, at the southern end of the Remutaka Range. The head is an excellent example of tectonic uplift within the Wellington region. There are a series of raised terraces which show where the shoreline existed prior to large seismic events. The Turakirae Head is also home to a seal colony and southern bull kelp. Turakirae also marks the southernmost coastal boundary point for the Ngāti Kahungunu tribe which extends as north as Paritu which is just north south of Gisborne. References Headlands of the Wellington Region Cook Strait {{Wellington-geo-st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 List of islands of New Zealand, smaller islands. It is the List of island countries, 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 of New Zealand, 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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 offi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palliser Bay
Palliser Bay is at the southern end of the North Island of New Zealand, to the southeast of Wellington. It runs for 40 kilometres along the Cook Strait coast from Turakirae Head at the southern end of the Remutaka Ranges to Cape Palliser, the North Island's southernmost point. The coastline is exposed to the weather and winds. Inland from the bay is the plain of the Ruamahanga River, which has its outflow in the bay. This river flows through Lake Wairarapa, 10 kilometres from the coast. There are several notable geographical features in the area, including the Putangirua Pinnacles, Kupe's Sail Kupe's Sail ( mi, Ngā Rā-a-Kupe) is a geological formation near the eastern end of Palliser Bay at the southern end of the North Island of New Zealand. It is composed of sedimentary rock which has been thrust up in an earthquake, resulting in ... and the Whatarangi Bluff, the erosion of which has had dramatic effects on the coastline. Some of these cliffs are made of mudstone and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wellington
Wellington ( mi, Te Whanganui-a-Tara or ) is the capital city of New Zealand. It is located at the south-western tip of the North Island, between Cook Strait and the Remutaka Range. Wellington is the second-largest city in New Zealand by metro area, and is the administrative centre of the Wellington Region. It is the world's southernmost capital of a sovereign state. Wellington features a temperate maritime climate, and is the world's windiest city by average wind speed. Legends recount that Kupe discovered and explored the region in about the 10th century, with initial settlement by Māori iwi such as Rangitāne and Muaūpoko. The disruptions of the Musket Wars led to them being overwhelmed by northern iwi such as Te Āti Awa by the early 19th century. Wellington's current form was originally designed by Captain William Mein Smith, the first Surveyor General for Edward Wakefield's New Zealand Company, in 1840. The Wellington urban area, which only includes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Remutaka Range
The Remutaka Range (spelled Rimutaka Range before 2017) is the southernmost range of a mountain chain in the lower North Island of New Zealand. The chain continues north into the Tararua, then Ruahine Ranges, running parallel with the east coast between Wellington and East Cape. The 555-metre summit of the road over the range at its northern saddle is named Remutaka Pass. The pass was formally named on 17 December 2015 when the Minister of Land Information confirmed the decision of the New Zealand Geographic Board. Following the passage of the Rangitāne Tū Mai Rā (Wairarapa Tamaki nui-ā-Rua) Claims Settlement Act 2017, the name of the range officially changed to Remutaka Range. Geography The Remutaka Range runs north-east to south-west for 55 kilometres from the upper reaches of the Hutt Valley (where the range's northern saddle abuts the southern end of the Tararuas) to Turakirae Head at the western end of Palliser Bay. The highest peak is Mount Matthews, at 940 metre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durvillaea
''Durvillaea'' is a genus of large brown algae in the monotypic family Durvillaeaceae. All members of the genus are found in the southern hemisphere, including Australia, New Zealand, South America, and various subantarctic islands. ''Durvillaea'', commonly known as southern bull kelps, occur on rocky, wave-exposed shorelines and provide a habitat for numerous intertidal organisms. Many species exhibit a honeycomb-like structure in their fronds that provides buoyancy, which allows individuals detached from substrates to raft alive at sea, permitting dispersal for hundreds of days over thousands of kilometres. ''Durvillaea'' species have been used for clothing, tools and as a food source by many indigenous cultures throughout the South Pacific, and they continue to play a prominent role in Chilean cuisine. Common name and etymology The common name for ''Durvillaea'' is southern bull kelp, although this is often shortened to bull kelp, which can generate confusion with the North ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Kahungunu
Ngāti Kahungunu is a Māori iwi located along the eastern coast of the North Island of New Zealand. The iwi is traditionally centred in the Hawke's Bay and Wairārapa regions. The tribe is organised into six geographical and administrative divisions: ''Wairoa'', ''Te Whanganui-ā-Orotū'', ''Heretaunga'', ''Tamatea'', ''Tāmaki-nui-a Rua'' and ''Wairarapa''. It is the third largest iwi in New Zealand by population, with 61,626 people (9.2% of the Māori population) identifying as Ngāti Kahungunu in the 2013 census. Early history Pre-colonisation Ngāti Kahungunu trace their origins to the ''Tākitimu'' waka. According to Ngāti Kahungunu traditions, ''Tākitimu'' arrived in Aotearoa around 1100–1200 AD as one of the ''waka'' in the great migration. Other ''waka'' included ''Tainui'', '' Te Arawa'', '' Tokomaru'', '' Ārai Te Uru'', '' Mataatua'', '' Kurahaupo'', '' Aotea'', '' Ngātokimatawhaorua'' and '' Horouta''. According to local legend, Tākitimu and its crew were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gisborne, New Zealand
Gisborne ( mi, Tūranga-nui-a-Kiwa "Great standing place of Kiwa") is a city in northeastern New Zealand and the largest settlement in the Gisborne District (or Gisborne Region). It has a population of The district council has its headquarters in Whataupoko, in the central city. The settlement was originally known as Turanga and renamed Gisborne in 1870 in honour of New Zealand Colonial Secretary William Gisborne. Early history First arrivals The Gisborne region has been settled for over 700 years. For centuries the region has been inhabited by the tribes of Te Whanau-a-Kai, Ngaariki Kaiputahi, Te Aitanga-a-Mahaki Rongowhakaata, Ngāi Tāmanuhiri and Te Aitanga-a-Hauiti. Their people descend from the voyagers of the Te Ikaroa-a-Rauru, Horouta and Tākitimu waka. East Coast oral traditions offer differing versions of Gisborne's establishment by Māori. One legend recounts that in the 1300s, the great navigator Kiwa landed at the Turanganui River first on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of The Wellington Region
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
