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List Of Caves In 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 formation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
Caves or caverns are natural voids under the Earth's Planetary surface, surface. Caves often form by the weathering of rock and often extend deep underground. Exogene caves are smaller openings that extend a relatively short distance underground (such as rock shelters). 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, ''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, microorganisms, pressure, and atmospheric influences. Isotopic dating techniques can be applied to cave sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nettlebed Cave
__NOTOC__ Nettlebed Cave is a limestone cave located in the Mount Arthur (New Zealand), Mount Arthur region of the northwest South Island of New Zealand. The presence of ongaonga (''Urtica ferox''), an endemic tree nettle, near the bottom entrance gives the cave its name. Nettlebed Cave was connected to Stormy Pot in January 2014, making the system the deepest known cave in the Southern Hemisphere. Nettlebed Cave drops below its upper entrance (Big Friendly Giant, Stormy Pot) to its lower exit (the Pearse River resurgence) and is long. Exploration Nettlebed Cave was first explored by cavers in 1969 through the dry overflow passage of a large spring pouring into the Pearse River. By 1973 of passages had been mapped. It was not until 1979 that a flowstone squeeze known as the Hinkle-horn-honking-holes was passed, making further explorations possible. Five successive Christmas expeditions (1979–80 through 1983–84) utilising underground camps at Salvation Hall and Soft Rock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Rock Formations Of New Zealand
This is a list of rock formations in New Zealand based on their aesthetic and cultural importance. New Zealand's geomorphology is formed through an interaction between uplift, erosion and the underlying Geology of New Zealand, rock type. Most of the notable examples listed here are formed by selective erosion, for example waves and rivers can more easily erode sandstone than basalt and can also exploit Joint (geology), joints or Fault (geology), faults in the rock-mass. Some rocks like limestone (Waitomo Caves) and marble (Takaka Hill) can also be dissolved in water which forms a distinctive karst geomorphology. Notable rock formations are also formed through constructive processes such as geothermal and volcanic deposits, and sedimentary deposition. North Island formations South Island formations Formations elsewhere Maps See also * List of caves of New Zealand * List of rock formations * Stratigraphy of New Zealand * Geomorphology References {{DEFAULTSOR ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Caves
This is a list of caves of the world that have articles or that are properly cited. They are sorted by continent and then country. Caves which are in overseas territories on a different continent than the home country are sorted by the territory's continent and name. Africa Algeria * Aïn Taïba * Anou Achra Lemoun * Anou Boussouil * Anou Ifflis * Anou Timedouine * Gueldaman caves * Ghar Boumâaza (Rivière De La Tafna) * Grotte de Cervantes * Kef Al Kaous Botswana * Gcwihaba * Tsodilo#Rhino Cave, Rhino Cave Cameroon * Gouffre de Mbilibekon * Grottes de Linté * Grotte de Loung * Grotte de Mfouda * Grotte FovuFovu à Baham – Les grottes sacrées des Hautes Terres de L'Ouest Cameroun Grottesducameroun.org. Retrieved 15 September 2011. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aurora Cave
Aurora Cave is a limestone cave, part of the Te Ana-au Caves in Fiordland, in the South Island of New Zealand on the western side of a deep glacial trough containing Lake Te Anau. Aurora Cave is separated by a sump from Te Ana-au Cave (a tourist cave). The cave has been formed by the Tunnel Burn, which drains from Lake Orbell in the Takahe valley. Aurora Cave is 267 metres deep and 6 km. long. Around 1988, a of an extinct species of were discovered. It was named the Aurora frog ( |
Te Ana-au Caves
The Te Ana-au caves are a culturally and ecologically important system of limestone caves on the western shore of Lake Te Anau, in the southwest of New Zealand. They were re-discovered in 1948 by Lawson Burrows, who found the upper entry after three years of searching, following clues in old Māori mythology, Māori legends. It later became a major tourist attraction for the area, as the part of the caverns close to the lake shore is home to glowworms. The unofficial name used by the national caving association is ''Aurora''. The caves are geologically young (estimated 12,000 years) and hence there is only one tiny stalactite. The Māori language, Māori name Te Ana-au can be translated as "The Swirling Cave" (''te'': the; ''ana'': cave; ''au'': swirling) in reference to the water running through it. The water, Tunnel Burn, is the outflow of Lake Orbell. Lawson Burrows and his business partner Wilson Campbell set up Fiordland Travels as a tourism company for their venture. In ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngārua Caves
The Ngārua Caves are a series of limestone caves in the Tākaka Hill range south of Abel Tasman National Park. The caves are located close to Takaka Hill's summit, adjacent to State Highway 60 as it winds its way over the Takaka Hill between Motueka and Upper Takaka. Scheduled tours suitable for people of all ages are provided by a commercial operator from the car park and cafe situated at the cave entrance. The caves cannot be visited unattended. Ngārua Caves contain a variety of cave formations along a comfortable walkway through the caves, as well as notable displays of Moa bones remaining in the caves. Ngārua Caves is listed as one of the "101 Must-Do's for Kiwis". See also *Caving in New Zealand Caving in New Zealand is an established hobby as well as being a part of commercial tourism. Recreational caving is practised by several hundred members of caving associations all over New Zealand, who take advantage of the widespread limestone ... References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harwoods Hole
Harwoods Hole is a cave system located in the northwest of the South Island of New Zealand, in the Abel Tasman National Park. At , it is New Zealand's deepest vertical shaft. It was first explored in 1958, long after it was discovered. Formation Evidence suggests that run-off from an area of approximately 20 square km converged into a stream that then flowed down a dry valley to create what is now Harwoods Hole. Since then the river appears to have changed course. Subsequently, Harwoods Hole receives water through sinkholes and surrounding dry valleys; this water then percolates through surrounding rock ensuring it becomes saturated with calcite, before entering the cave where the calcite is deposited. This second phase means that rather than expanding, Harwoods Hole is being filled in. History It is one of several important cave systems in Tākaka Hill, between Golden Bay and Tasman Bay. Starting at the surface as a diameter entrance and descending , Harwoods Hole is New Z ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tākaka Hill
Tākaka Hill, previously also referred to as Marble Mountain, is a range of hills in the northwest of the South Island of New Zealand. Made of marble that has weathered into many strange forms and with numerous sinkholes, it is typical karst country. The marble is Ordovician in age and from the Tākaka terrane. There is only one road winding over and around the flanks of Tākaka Hill, New Zealand State Highway 60, State Highway 60, following the valleys of the Tākaka River to the northwest and the Riuwaka River to the southeast. In July 2020, the name of the pass was officially gazetted as Tākaka Hill Saddle by the New Zealand Geographic Board. It rises to 791 metres at its highest point and separates the coastal communities of Golden Bay / Mohua, Golden Bay from those of the more populous Tasman Bay to the southeast and because of its winding nature isolates Golden Bay from the rest of the South Island. Tākaka Hill is notable for its (now defunct) marble quarry and for many ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riwaka River
The Riuwaka River, formerly known as the Riwaka River, is located in the Nelson region in the northwest of New Zealand's South Island. It flows for 20 kilometres, entering Tasman Bay close to the town of Riwaka, 10 kilometres north of Motueka. The valleys of the Riuwaka and nearby Tākaka River form part of the pass over which the only road between Tasman Bay and Golden Bay runs. For part of its journey, the river flows underground through limestone caves, returning to the open air at ''The Riuwaka Resurgence''. This spot is popular with both holidaymakers and divers, as the water is always crystal clear, and is very cold even in the heat of mid-summer. The name of the river was officially altered to Riuwaka River in August 2014, following the Treaty of Waitangi settlements between the Crown and local iwi Ngāti Rārua and Te Atiawa o Te Waka-a-Māui. See also * List of caves in New Zealand The following is a list of some of the more well known caves and caverns in Ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rawhiti Cave
Rawhiti Cave, also known as Manson Cave, is a single large limestone cave in the hillside of the Dry Creek Valley southeast of Tākaka on the South Island of New Zealand. It is referred to as Manson Cave in the NZ Topo Map, after owners in the early 20th century,Information panel "Water Catcher", Department of Conservation NZ however the cave is known as Rawhiti Cave locally, and on DoC information panels and in brochures. The cave's entrance is one of the largest cave entrances in New Zealand with an opening of about wide and up to tall. The ceiling is densely covered in stalactites which become increasingly finer deeper down into the cave. A short walking track leads halfway down into the cavernous opening to a viewing platform. Flora The diverse twilight-zone flora near the entrance of Rawhiti Cave makes this cave nationally significant. Over long periods of time, plant growth on the cave formations causes them to grow towards the sunlight as more calcium carbonate is dep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bulmer Cavern
Bulmer Cavern is New Zealand's longest cave system, running for through Mount Owen in the Tasman region of the northwest South Island. (from Te Ara: The Encyclopedia of New Zealand) John Patterson discovered the cave on New Year's Day 1984, by dropping a rock down and counting the seconds until it reached the bottom. Bulmer Cavern was the location of a major cave rescue
Cave rescue is a highly specialized field of wilderness rescue in which injured, trapped or lost cave explorers are medically treated and extracted from various cave environments.
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