Cape Fournier
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Cape Fournier
Cape Fournier is a headland on Chatham Island, in New Zealand's Chatham Islands group. It is the southeasternmost point in the island, and is the closest point on the island to the second largest of the Chatham Islands, Pitt Island, which lies 20 kilometres to the south-southeast across Pitt Strait Pitt Strait is a channel, wide, separating Chatham Island and Pitt Island, the two largest islands in New Zealand's Chatham Islands The Chatham Islands ( ) (Moriori: ''Rēkohu'', 'Misty Sun'; mi, Wharekauri) are an archipelago in the Pac .... References Fournier Chatham Island {{OutlyingNZ-geo-stub ...
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Cape Fournier
Cape Fournier is a headland on Chatham Island, in New Zealand's Chatham Islands group. It is the southeasternmost point in the island, and is the closest point on the island to the second largest of the Chatham Islands, Pitt Island, which lies 20 kilometres to the south-southeast across Pitt Strait Pitt Strait is a channel, wide, separating Chatham Island and Pitt Island, the two largest islands in New Zealand's Chatham Islands The Chatham Islands ( ) (Moriori: ''Rēkohu'', 'Misty Sun'; mi, Wharekauri) are an archipelago in the Pac .... References Fournier Chatham Island {{OutlyingNZ-geo-stub ...
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Chatham Island
Chatham Island ( ) (Moriori: ''Rēkohu'', 'Misty Sun'; mi, Wharekauri) is by far the largest island of the Chatham Islands group, in the south Pacific Ocean off the eastern coast of New Zealand's South Island. It is said to be "halfway between the equator and the pole, and right on the International Date Line", though the point (180°, 45°S) in fact lies ca. 173 miles WSW of the island's westernmost point. The island is called ''Rekohu'' ("misty skies") in Moriori, and ''Wharekauri'' in Māori.Government of New Zealand, Dept. of Conservation (1999) Chatham IslandsConservation Management Strategy''. Retrieved 13 July 2012. The island was named after the survey ship HMS ''Chatham'' which was the first European ship to locate the island in 1791. It covers an area of . Chatham Island lies south-east of Cape Turnagain, the nearest point of mainland New Zealand to the island. Geography The geography of the roughly T-shaped island is dominated by three features: two bays a ...
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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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Chatham Islands
The Chatham Islands ( ) (Moriori: ''Rēkohu'', 'Misty Sun'; mi, Wharekauri) are an archipelago in the Pacific Ocean about east of New Zealand's South Island. They are administered as part of New Zealand. The archipelago consists of about ten islands within an approximate radius, the largest of which are Chatham Island and Pitt Island (Rangiauria). They include New Zealand's easternmost point, the Forty-Fours. Some of the islands, formerly cleared for farming, are now preserved as nature reserves to conserve some of the unique flora and fauna. The islands were uninhabited when the Moriori people arrived around 1500 CE and developed a peaceful way of life. In 1835 members of the Ngāti Mutunga and Ngāti Tama Māori iwi from the North Island of New Zealand invaded the islands and nearly exterminated the Moriori, enslaving the survivors. Later during the period of European colonisation of New Zealand, the New Zealand Company claimed that the British Crown had never include ...
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Pitt Island
Pitt Island is the second largest island in the Chatham Islands, Chatham Archipelago, New Zealand. It is called ''Rangiauria'' in Māori language, Māori and ''Rangiaotea'' in ''Moriori language, Moriori.Government of New Zealand, Dept. of Conservation (1999) Chatham IslandsConservation Management Strategy map 6. Retrieved 13 July 2012. Pitt Island has an area of . It lies about to the east of New Zealand's main islands, and about to the southeast of Chatham Island, from which it is separated by Pitt Strait. The island is hilly; its highest point (Waihere Head) rises to above sea level. , Pitt Island had a population of about 38 people. Pitt Island's Kahuitara Point is the first populated location on earth to observe a sunrise in each new year, based on local time zone. History Pitt Island was originally inhabited by the Moriori people, Moriori, the indigenous peoples of the Chatham Islands, who called it ''Rangiaotea'' or ''Rangihaute''. Their archaeology, archaeologic ...
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Pitt Strait
Pitt Strait is a channel, wide, separating Chatham Island and Pitt Island, the two largest islands in New Zealand's Chatham Islands The Chatham Islands ( ) (Moriori: ''Rēkohu'', 'Misty Sun'; mi, Wharekauri) are an archipelago in the Pacific Ocean about east of New Zealand's South Island. They are administered as part of New Zealand. The archipelago consists of about te .... References Geography of the Chatham Islands Straits of New Zealand Chatham Island {{OutlyingNZ-geo-stub ...
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Headlands Of The Chatham Islands
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 th ...
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