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Geologic Formation Attractions In New Zealand

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New Zealand is a sovereign island country in the southwestern Pacific Ocean. The country geographically comprises two main landmasses—the North Island , and the South Island —and around 600 smaller islands. New Zealand is situated some 1,500 kilometres east of Australia across the Tasman Sea and roughly 1,000 kilometres south of the Pacific island areas of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinct biodiversity of animal, fungal, and plant life. The country's varied topography and its sharp mountain peaks, such...
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Geologic Formation Attractions In New Zealand

  • 1. Rere Rockslide Gisborne
    Rere is a small community in the northeast of New Zealand's North Island. it is located in the upper valley of the Wharekopae River in remote country in the foothills of the Huiarau Range, inland from Gisborne. It is notable for the Rere Falls and Rere Rock Slide, both on the Wharekopae River. Rere Falls, while not very tall at 5 metres , is a picturesque 20 metres wide waterfall. It is possible to walk behind its cascading curtain of water, although the rock face can be slippery. Rere Rock Slide has been included in the NZ Automobile Association's 101 Must-do places for Kiwis. It is a smooth, natural rock formation 60 metres long, at an angle of about 30°, over which the Wharekopae River rushes like water in a giant water slide. With a little care, it can be slid down on boogie boards, t...
    From Wikipedia, the free encyclopedia.
  • 3. Moeraki Boulders Moeraki
    The Moeraki Boulders are unusually large and spherical boulders lying along a stretch of Koekohe Beach on the wave-cut Otago coast of New Zealand between Moeraki and Hampden. They occur scattered either as isolated or clusters of boulders within a stretch of beach where they have been protected in a scientific reserve. The erosion by wave action of mudstone, comprising local bedrock and landslides, frequently exposes embedded isolated boulders. These boulders are grey-colored septarian concretions, which have been exhumed from the mudstone enclosing them and concentrated on the beach by coastal erosion.In 1848 W. B. D. Mantell sketched the beach and its boulders, more numerous than now. The picture is now in the Alexander Turnbull Library in Wellington. The boulders were described in 1850 ...
    From Wikipedia, the free encyclopedia.
  • 4. The Boulder Bank Tasman
    A Mw 6.2 earthquake occurred in Christchurch on 22 February 2011 at 12:51 p.m. local time . The earthquake struck the Canterbury Region in New Zealand's South Island and was centred 2 kilometres west of the port town of Lyttelton, and 10 kilometres south-east of the centre of Christchurch, at the time New Zealand's second-most populous city. The earthquake caused widespread damage across Christchurch, killing 185 people in the nation's fifth-deadliest disaster. Christchurch's central city and eastern suburbs were badly affected, with damage to buildings and infrastructure already weakened by the magnitude 7.1 Canterbury earthquake of 4 September 2010 and its aftershocks. Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt. The earthquake was felt ...
    From Wikipedia, the free encyclopedia.
  • 5. Craters of the Moon Taupo
    Craters of the Moon Thermal Area is a region with geothermal activity north of Taupo, New Zealand. It is a part of Wairakei, the largest geothermal field in New Zealand, with a surface area of about 25 km2, which lies in the Taupo Volcanic Zone. The name springs from the many hydrothermal eruption craters, which are in part barren and which have bright colours. Combined with the numerous steam vents, constantly shifting, collapsing and reforming giving the whole area desolate appearance, and the sulphur smell, the whole area has an “unearthly” atmosphere. The craters are a relatively recent feature of the area and appeared as a result of human activity in the region. The site is Crown Land, administered by the Department of Conservation, with help from the Craters of the Moon Trust, a ...
    From Wikipedia, the free encyclopedia.
  • 6. Sumner Beach (Cave Rock) Christchurch
    Sumner is a coastal seaside suburb of Christchurch, New Zealand and was surveyed and named in 1849 in honour of John Bird Sumner, the then newly appointed Archbishop of Canterbury and president of the Canterbury Association. Originally a separate borough, it was amalgamated with the city of Christchurch as communications improved and the economies of scale made small town boroughs uneconomic to operate.
    From Wikipedia, the free encyclopedia.
  • 12. Mangapohue Natural Bridge Walk Waitomo Caves
    The Mangapohue Natural Bridge consists of two rock arches formed by the Mangapohue Stream in the Marokopa River valley near Waitomo, New Zealand. The 17 m high limestone arches are a remnant of an ancient cave system. The smaller lower rock arch spans the Mangapohue Stream and cannot be walked through, while the larger upper arch is situated straight above the lower arch and contains a platform to view the stalactites on the upper arch's ceiling. The arches can be reached by the sealed Te Anga Road from State Highway 3 approximately 25 km west of the Waitomo Caves. From the carpark, the wheelchair-friendly walk takes 5 minutes to reach the natural bridge. The walk leads through a scenic limestone gorge, crossing the stream once on a timber bridge, and ending at a viewing platform below the...
    From Wikipedia, the free encyclopedia.

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