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Honeycomb Hill Cave
Honeycomb Hill Cave is located in the Oparara Basin, on the northwestern edge of the South Island of New Zealand. The Oparara River flows through a section of the cave. The cave was discovered in 1976 by the Buller Caving Group. Since then, 14 km of passages have been mapped, and several important deposits of moa bones have been discovered in the caves. In 2008 an extra 38 hectares of Kahurangi National Park was included in the Honeycomb Hill Caves Specially Protected Area to protect the cave system. See also *Caving in New Zealand References External linksWelcome New Zealand Speleological Society (NZSS)
(umbrella organisation of the New Zealand caving clubs) Caves of New Zealand Landforms of the West Coast, New Zealand Paleontological sites of New Zealand Kahurangi National Park Buller District {{Oceania-archaeology-stub ...
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Gradungula Crawl A
''Gradungula'' is a monotypic taxon, monotypic genus of Oceania, South Pacific Gradungulidae, large-clawed spiders containing the single species, ''Gradungula sorenseni''. It is only found in New Zealand. __TOC__ Etymology The genus name is derived from Latin ' "step" and ' "claw", referring to the enlarged front leg claws of this species. These claws also occur in other species of the family Gradungulidae. The species name "''sorenseni''" is named after Jack Sorensen, the discoverer of the species. Taxonomy ''Gradungula sorenseni'' was first described by Raymond Robert Forster in 1955. Distribution ''Gradungula sorenseni'' is distributed in forests throughout the western South Island and throughout Stewart Island. Forster, R. R., Platnick, N. I. & Gray, M. R. (1987). A review of the spider superfamilies Hypochiloidea and Austrochiloidea (Araneae, Araneomorphae). ''Bulletin of the American Museum of Natural History'' 185: 1-116. References

Gradungulidae Monotypic ...
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Bees Knees 2 A
Bees are winged insects closely related to wasps and ants, known for their roles in pollination and, in the case of the best-known bee species, the western honey bee, for producing honey. Bees are a monophyletic lineage within the superfamily Apoidea. They are presently considered a clade, called Anthophila. There are over 16,000 known species of bees in seven recognized biological families. Some speciesincluding honey bees, bumblebees, and stingless beeslive socially in colonies while most species (>90%)including mason bees, carpenter bees, leafcutter bees, and sweat beesare solitary. Bees are found on every continent except Antarctica, in every habitat on the planet that contains insect-pollinated flowering plants. The most common bees in the Northern Hemisphere are the Halictidae, or sweat bees, but they are small and often mistaken for wasps or flies. Bees range in size from tiny stingless bee species, whose workers are less than long, to '' Megachile pluto'', ...
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Oparara Basin
''Oparara'' is a genus of South Pacific intertidal spiders first described by Raymond Robert Forster & C. L. Wilton in 1973. it contains only two species, both found in 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 count .... References Araneomorphae genera Desidae Spiders of New Zealand Taxa named by Raymond Robert Forster {{Araneomorphae-stub ...
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South Island
The South Island, also officially named , is the larger of the two major islands of New Zealand in surface area, the other being the smaller but more populous North Island. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, and to the south and east by the Pacific Ocean. The South Island covers , making it the world's 12th-largest island. At low altitude, it has an oceanic climate. The South Island is shaped by the Southern Alps which run along it from north to south. They include New Zealand's highest peak, Aoraki / Mount Cook at . The high Kaikōura Ranges lie to the northeast. The east side of the island is home to the Canterbury Plains while the West Coast is famous for its rough coastlines such as Fiordland, a very high proportion of native bush and national parks, and the Fox and Franz Josef Glaciers. The main centres are Christchurch and Dunedin. The economy relies on agriculture and fishing, tourism, and general manufacturing and services. ...
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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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Oparara River
''Oparara'' is a genus of South Pacific intertidal spiders first described by Raymond Robert Forster & C. L. Wilton in 1973. it contains only two species, both found in 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 count .... References Araneomorphae genera Desidae Spiders of New Zealand Taxa named by Raymond Robert Forster {{Araneomorphae-stub ...
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Kahurangi National Park
Kahurangi National Park in the northwest of the South Island of New Zealand is the second largest of the thirteen national parks of New Zealand. It was gazetted in 1996 and covers , ranging to near Golden Bay in the north. Much of what was the North-west Nelson Forest Park formed the basis of the new park. Kahurangi Point, regarded as the boundary between the West Coast and Tasman Regions, is located in the park, as is Mount Owen. The main tramping tracks in the park are the Heaphy Track and the Wangapeka Track. The park is administered by the Department of Conservation. Tramping, rafting and caving are popular activities in the park. After being prohibited for several years, mountainbiking was allowed on the Heaphy Track on a trial basis for the winters of 2011, 2012 and 2013. The effect of the cyclists on trampers and the wildlife were to determine whether the trial continued or not. Endangered takahē were reintroduced to the park in 2018, which was 100 years after they ...
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New Zealand Government
, background_color = #012169 , image = New Zealand Government wordmark.svg , image_size=250px , date_established = , country = New Zealand , leader_title = Prime Minister Jacinda Ardern , appointed = Governor-General , main_organ = , ministries = 32 ministries and departments , responsible = House of Representatives , budget = 119.3 billion (2018–19) , address = The Beehive and other locations across Wellington , url = The New Zealand Government ( mi, Te Kāwanatanga o Aotearoa) is the central government through which political authority is exercised in New Zealand. As in most other parliamentary democracies, the term "Government" refers chiefly to the executive branch, and more specifically to the collective ministry directing the executive. Based on the principle of responsible government, it operates within the framework that "the Queen reigns, but the government rules, so long as it has the support of the House of Representatives".Sir Kenneth Keith, qu ...
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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 karst cave systems present in the country, especially in the Waitomo District of the North Island and in the Nelson- Tasman region of the South Island. There are also several hundred thousands of visitors to various tourist caves in New Zealand per year,Caving tourism
(from Te Ara: The Encyclopedia of New Zealand. Accessed 2008-06-16.)
though a majority of these trips would not properly be called

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 ...
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Landforms Of The West Coast, New Zealand
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ...
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Paleontological Sites Of New Zealand
Paleontology (), also spelled palaeontology or palæontology, is the scientific study of life that existed prior to, and sometimes including, the start of the Holocene epoch (roughly 11,700 years before present). It includes the study of fossils to classify organisms and study their interactions with each other and their environments (their paleoecology). Paleontological observations have been documented as far back as the 5th century BC. The science became established in the 18th century as a result of Georges Cuvier's work on comparative anatomy, and developed rapidly in the 19th century. The term itself originates from Greek (, "old, ancient"), (, (gen. ), "being, creature"), and (, "speech, thought, study"). Paleontology lies on the border between biology and geology, but differs from archaeology in that it excludes the study of anatomically modern humans. It now uses techniques drawn from a wide range of sciences, including biochemistry, mathematics, and engineering. Us ...
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