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Riuwaka 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 / Te Tai-o-Aorere 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 Te Atiawa o Te Waka-a-Māui is a Māori iwi (tribe) in the upper South Island of New Zealand. Its rohe (triba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Resurgence '', a 1981 album by jazz saxophonist David "Fathead" Newman
* ''Resurgence'' (magazine), a British publication, merged with ''The Ecologist'' in 2012
* Resurgence may refer to: *Resurgence (spring), spring discharge, where water comes from the ground *Resurgence (pest) of (usually agricultural) pests, due for example, to the misuse of pesticides *Resurgence (Dutch Revolt), the period between 1572 and 1585 in the Dutch Revolt *Risorgimento, meaning the Resurgence, Italian unification *The Resurgence (organization), a Christian ministry associated with Mars Hill Church and Mark Driscoll Media *''Resurgence! ''Resurgence!'' is an album by saxophonist David "Fathead" Newman recorded in 1981 and released on the Muse label. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Underwater Diving
Underwater diving, as a human activity, is the practice of descending below the water's surface to interact with the environment. It is also often referred to as diving, an ambiguous term with several possible meanings, depending on context. Immersion in water and exposure to high ambient pressure have physiological effects that limit the depths and duration possible in ambient pressure diving. Humans are not physiologically and anatomically well-adapted to the environmental conditions of diving, and various equipment has been developed to extend the depth and duration of human dives, and allow different types of work to be done. In ambient pressure diving, the diver is directly exposed to the pressure of the surrounding water. The ambient pressure diver may dive on breath-hold (freediving) or use breathing apparatus for scuba diving or surface-supplied diving, and the saturation diving technique reduces the risk of decompression sickness (DCS) after long-duration deep dives ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The Tasman District
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of The Tasman District
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, microorganism ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Atiawa O Te Waka-a-Māui
Te Atiawa o Te Waka-a-Māui is a Māori iwi (tribe) in the upper South Island of New Zealand. Its rohe (tribal area) extends from Golden Bay and Marlborough Sounds at the top of the South Island to Cape Campbell, St Arnaud and Westport. Marae and wharenui There are four marae and wharenui associated with Te Atiawa o Te Waka-a-Māui: * Onetahua Kōkiri Marae (Te Ao Marama wharenui), Takaka * Te Āwhina marae (Turangāpeke wharenui), Motueka * Waikawa marae (Arapaoa wharenui), Picton * Whakatū marae (Kākāti), Nelson Governance Te Atiawa o Te Waka-a-Māui Trust is recognised by the New Zealand Government as the governance entity of the iwi, following its Treaty of Waitangi settlement with the Crown under the Ngāti Kōata, Ngāti Rārua, Ngāti Tama ki Te Tau Ihu, and Te Ātiawa o Te Waka-a-Māui Claims Settlement Act 2014. The trust is a mandated iwi organisation in the Māori Fisheries Act, an iwi aquaculture organisation under the Māori Commercial Aquaculture Claims Settl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Rārua
Ngāti Rārua are a Māori iwi (tribe) of the Tainui tribal confederation, descendants of the people who arrived in Aotearoa aboard the ''Tainui'' waka (canoe). Ngāti Rārua stem from the marriage of Rārua-ioio and Tū-pāhau and had their original home at Kāwhia, Marokopa and Waikawau on the West Coast of the Waikato King Country region. In 1821 Ngāti Rārua migrated southwards in a series of ''heke'' (migrations) led by Te Rauparaha of Ngāti Toa which saw the iwi relocate to Nelson Marlborough. Ngāti Rārua tribal lands (rohe) overlap those of Ngāti Koata, Ngāti Tama, Te Āti Awa, Ngāti Kuia, Ngāti Apa ki te Rā Tō and Rangitāne. Since the arrival in Te Tau Ihu, Ngāti Rārua have maintained continuous '' ahi kā'' in Golden Bay, various locations in the Abel Tasman National Park, Mārahau, Kaiteriteri, Riwaka, Motueka, Nelson, and Wairau. Hapū * Ngāti Tūrangāpeke * Ngāti Pare-Te-Ata * Ngāti Paretona * Ngāti Kairārunga * Te Arawāere Marae * Te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Crown
The Crown is the state in all its aspects within the jurisprudence of the Commonwealth realms and their subdivisions (such as the Crown Dependencies, overseas territories, provinces, or states). Legally ill-defined, the term has different meanings depending on context. It is used to designate the monarch in either a personal capacity, as Head of the Commonwealth, or as the king or queen of their realms (whereas the monarchy of the United Kingdom and the monarchy of Canada, for example, are distinct although they are in personal union). It can also refer to the rule of law; however, in common parlance 'The Crown' refers to the functions of government and the civil service. Thus, in the United Kingdom (one of the Commonwealth realms), the government of the United Kingdom can be distinguished from the Crown and the state, in precise usage, although the distinction is not always relevant in broad or casual usage. A corporation sole, the Crown is the legal embodiment of execut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Treaty Of Waitangi Claims And Settlements
Claims and settlements under the Treaty of Waitangi have been a significant feature of New Zealand politics since the Treaty of Waitangi Act 1975 and the Waitangi Tribunal that was established by that act to hear claims. Successive governments have increasingly provided formal legal and political opportunity for Māori to seek redress for what are seen as breaches by the Crown of guarantees set out in the Treaty of Waitangi. While it has resulted in putting to rest a number of significant longstanding grievances, the process has been subject to criticisms including those who believe that the redress is insufficient to compensate for Māori losses. The settlements are typically seen as part of a broader Māori Renaissance. The Waitangi Tribunal was set up as the primary means of registering and researching claims because the Treaty of Waitangi itself has little legal standing. The primary means of settling those claims is through direct negotiations with the government of the day. ... [...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] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Golden Bay / Mohua
Golden Bay / Mohua is a shallow, paraboloid-shaped bay in New Zealand, near the northern tip of the South Island. An arm of the Tasman Sea, the bay lies northwest of Tasman Bay / Te Tai-o-Aorere and Cook Strait. It is protected in the north by Farewell Spit, a 26 km long arm of fine golden sand that is the country's longest sandspit. The Aorere and Tākaka rivers are the major waterways to flow into the bay from the south and the west. It is part of the Tasman Region, one of the territorial authorities of New Zealand. The bay was once a resting area for migrating whales and dolphins such as southern right whales and humpback whales, and pygmy blue whales may be observed off the bay as well. The west and northern regions of the bay are largely unpopulated. Along its southern coast are the towns of Tākaka and Collingwood, and the Abel Tasman National Park. Separation Point, the natural boundary between Golden and Tasman Bays, is in the park. North-eastern parts of K ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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