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Cathedral Caves
The Cathedral Caves are two connected limestone sea caves located on Waipati Beach, south of Papatowai, on the Catlins Coast in the southeast corner of New Zealand's South Island. The two main cave systems join together within the cliff and one has a high ceiling. Often blue penguins and fur seals will emerge from the gloom at the far end of the cave. The 199m-long cave is formed in Jurassic sandstone (about 160 million years old) of the Murihiku Terrane, though the cave itself is much younger, ten to hundreds of thousands of years old. They were named by Thomas Hocken Thomas Morland Hocken (14 January 1836 – 17 May 1910) was a New Zealand collector, bibliographer and researcher. Early life He was born in Rutlandshire on 14 January 1836, the son of Wesleyan minister Joshua Hocken, and educated at Woodhouse ... who noted how the caves reverberated noise and their resemblance to European cathedrals. The caves are only accessible for an hour either side of low tide. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Department Of Conservation (New Zealand)
The Department of Conservation (DOC; Māori: ''Te Papa Atawhai'') is the public service department of New Zealand charged with the conservation of New Zealand's natural and historical heritage. An advisory body, the New Zealand Conservation Authority (NZCA) is provided to advise DOC and its ministers. In addition there are 15 conservation boards for different areas around the country that provide for interaction between DOC and the public. Function Overview The department was formed on 1 April 1987, as one of several reforms of the public service, when the ''Conservation Act 1987'' was passed to integrate some functions of the Department of Lands and Survey, the Forest Service and the Wildlife Service. This act also set out the majority of the department's responsibilities and roles. As a consequence of Conservation Act all Crown land in New Zealand designated for conservation and protection became managed by the Department of Conservation. This is about 30% of New Z ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Catlins
The Catlins (sometimes referred to as The Catlins Coast) comprises an area in the southeastern corner of the South Island of New Zealand. The area lies between Balclutha and Invercargill, straddling the boundary between the Otago and Southland regions. It includes the South Island's southernmost point, Slope Point. A rugged, sparsely populated area, the Catlins features a scenic coastal landscape and dense temperate rainforest, both of which harbour many endangered species of birds, most notably the rare yellow-eyed penguin. The coast attracts numerous marine mammals, among them New Zealand fur seals and Hooker's sea lions. In general terms the area enjoys a maritime temperate climate. Its exposed location leads to its frequently wild weather and heavy ocean swells, which are an attraction to big-wave surfers, and have also caused numerous shipwrecks. People have lived in the area since around 1350 AD. Prior to European settlement, the region was sparsely inhabited by nomadi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Caves
A sea cave, also known as a littoral cave, is a type of cave formed primarily by the wave action of the sea. The primary process involved is erosion. Sea caves are found throughout the world, actively forming along present coastlines and as relict sea caves on former coastlines. Some of the largest wave-cut caves in the world are found on the coast of Norway, but are now 100 feet or more above present sea level. These would still be classified as littoral caves. By contrast, in places like Thailand's Phang Nga Bay, solutionally formed caves in limestone have been flooded by the rising sea and are now subject to littoral erosion, representing a new phase of their enlargement. Some of the best-known sea caves are European. Fingal's Cave, on the island of Staffa in Scotland, is a spacious cave some 70 m long, formed in columnar basalt. The Blue Grotto of Capri, although smaller, is famous for the apparent luminescent quality of its water, imparted by light passing through underwate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Scenic Route
The Southern Scenic Route is a tourist highway in New Zealand linking Queenstown, Fiordland, Te Anau and the iconic Milford Road to Dunedin via, Riverton, Invercargill and The Catlins. An Australian travel magazine labelled it "one of the world's great undiscovered drives" in 2008. History and development The Southern Scenic Route concept and name were conceived at an informal gathering by Tuatapere residents John Fraser and Les Hutchins in November 1985 and confirmed at a public meeting in January 1986.Julie Walls (ed) ''Southern Scenic Route Visitor Publication'' 7ed, Focus Publications, Te Anau, November 2006 The promoters then negotiated with road and tourism authorities and local government. The project was a first for New Zealand and approval was a slow process. At one stage, traffic signs were installed in a clandestine operation. The Route opened officially on 6 November 1988, initially running between Te Anau in the west and Balclutha in the east. It was extende ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of New Zealand
The following is a list of some of the more well known caves and caverns in New Zealand. Not all caves have an official name as set by the New Zealand Geographic Board. The national caving association maintains maps of all known surveyed caves and the name is generally allocated by the group who first discovered the cave. North Island caves *Many lava tubes and lava caves in the Auckland volcanic field, including: ** Rangitoto lava caves **Wiri Lava Cave *Waitomo district: ** Aranui Cave ** Gardner's Gut ** Ruakuri Cave ** Waitomo Cave South Island caves * Broken River Cave * Cathedral Caves * Cave Stream * Clifden Limestone Caves *Honeycomb Hill Cave * Metro Cave / Te Ananui Cave * Mount Arthur caves: ** Ellis Basin cave system ** Nettlebed Cave * Moncks Cave * Mount Owen caves: ** Bohemia Cave ** Bulmer Cavern * Rawhiti Cave * Riwaka Resurgence * Tākaka Hill caves: ** Harwoods Hole ** Ngārua Caves * Te Ana-au Caves ** Aurora Cave See also *List of caves *List of rock f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastline Of New Zealand
New Zealand has of coastline making it the 9th longest in the world. The coastline borders the Tasman Sea and the Pacific Ocean. The northern and southernmost points of the coastline on the two main islands are Surville Cliffs and Slope Point respectively. Cape Reinga in the north and Bluff in the south are often incorrectly given as the extremities of the coastline on the North and South Islands. Coastal development, such as buildings and marine farms, has become contentious in recent decades. Geography The geography of the New Zealand coastline is varied. As well as sheltered sandy beaches there are rugged, remote and cliff lined sections typified by the Fiordland area. Ironsand gives the beaches on west coast of the North Island a black colouration. Pine plantation were established on some of the coastal dune sections. Woodhill, Riverhead and Bottle Lake Forest are such examples. Marram grass was planted for dune stabilisation displacing native plants such as Pingao. Co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Formations Of Otago
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in Wales * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, an islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāi Tahu
Ngāi Tahu, or Kāi Tahu, is the principal Māori (tribe) of the South Island. Its (tribal area) is the largest in New Zealand, and extends from the White Bluffs / Te Parinui o Whiti (southeast of Blenheim), Mount Mahanga and Kahurangi Point in the north to Stewart Island / Rakiura in the south. The comprises 18 (governance areas) corresponding to traditional settlements. Ngāi Tahu originated in the Gisborne District of the North Island, along with Ngāti Porou and Ngāti Kahungunu, who all intermarried amongst the local Ngāti Ira. Over time, all but Ngāti Porou would migrate away from the district. Several were already occupying the South Island prior to Ngāi Tahu's arrival, with Kāti Māmoe only having arrived about a century earlier from the Hastings District, and already having conquered Waitaha, who themselves were a collection of ancient groups. Other that Ngāi Tahu encountered while migrating through the South Island were Ngāi Tara, Rangitāne, Ngāti T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thomas Hocken
Thomas Morland Hocken (14 January 1836 – 17 May 1910) was a New Zealand collector, bibliographer and researcher. Early life He was born in Rutlandshire on 14 January 1836, the son of Wesleyan minister Joshua Hocken, and educated at Woodhouse Grove School and a school in Newcastle. He studied medicine at Durham University and Dublin University, and in 1859 became a member of the Royal College of Surgeons. Career The following year, he decided to leave England's cold climes for the sake of his health, and became a ship's surgeon. In 1862, he arrived in Dunedin, New Zealand where he set up practice, also becoming the city's coroner, a post which he held for over 20 years. During much of this time he was also president of the Otago branch of the New Zealand Medical Association, and lectured in surgery in the Otago Medical School. Hocken was married twice, to Julia Annia Daykne Simpson in 1867, and Bessie Buckland in July 1883 at Invercargill's St John's Church. Hocken's keen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Murihiku Terrane
The Southland Syncline is a major geological structure located in the Southland Region of New Zealand's South Island. The syncline folds the Mesozoic greywackes of the Murihiku Terrane. The northern limb of the fold is steep to overturned, while the southern limb dips shallowly to the northeast. The axial plan dips to the northeast and the axis plunges to the southeast. The Murihiku Terrane is formed predominantly from Permian to Jurassic sedimentary rocks with minor igneous intrusions, and is marked by prominent strike ridges particularly on its northern limb due to the steeper dip. These are created from the erosion of alternating strata of sandstone and mudstone. The northern edge of this fold system is marked by the Murihiku Escarpment, at the southern extreme of the Waimea Plains. Many of the names of stages and epochs in the Permian, Triassic, and Jurassic periods in the New Zealand geologic time scale are named for places within or close to the Southland Syncline and Murih ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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