Charles Sound
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Charles Sound
Taiporoporo / Charles Sound is a fiord of the South Island of New Zealand. It is one of the fiords that form the coast of Fiordland. Geography The fiord is located between Taitetimu / Caswell Sound and Hinenui / Nancy Sound, on the central Fiordland coast. It is 14 kilometres in length, and extends in a roughly northwestern direction. In its upper reaches the fiord splits into two arms of similar length, the Emelius Arm (to the north) and the Gold Arm (to the south). The Gold Arm is protected by the Kahukura (Gold Arm) Marine Reserve. Other parts of the fiord are included in the Taumoana (Five Fingers Peninsula) Marine Reserve. The Irene and Windward Rivers flow respectively into the ends of the Emelius and Gold Arms. The short Juno River enters to Tasman Sea just to the north of the fiord's mouth. Several small islands are located within the fiord, including Catherine Island and Fanny Island in the Gold Arm and Eleanor Island at the mouth of the Emelius Arm. History C ...
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Tasman Sea
The Tasman Sea (Māori: ''Te Tai-o-Rēhua'', ) is a marginal sea of the South Pacific Ocean, situated between Australia and New Zealand. It measures about across and about from north to south. The sea was named after the Dutch explorer Abel Janszoon Tasman, who in 1642 was the first known person to cross it. British explorer Lieutenant James Cook later extensively navigated the Tasman Sea in the 1770s during his three voyages of exploration. The Tasman Sea is informally referred to in both Australian and New Zealand English as the Ditch; for example, "crossing the Ditch" means travelling to Australia from New Zealand, or vice versa. The diminutive term "the Ditch" used for the Tasman Sea is comparable to referring to the North Atlantic Ocean as "the Pond". Climate The south of the sea is passed over by depressions going from west to east. The northern limit of these westerly winds is near to 40°S. During the southern winter, from April to October, the northern branch ...
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Irene River (New Zealand)
The Irene River is a river of New Zealand, flowing into Charles Sound, Fiordland. The river flows generally north from the Irene Pass, a saddle in the Museum Range of the Southern Alps. It follows a roughly semicircular path, initially flows northeast before turning north, northwest, and finally west before entering the northern (Emelius) arm of Charles Sound.Dowling, P. (ed.) (2004) ''Reed New Zealand atlas.'' Auckland: Reed Publishing. Map 96. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Rivers of Fiordland {{Fiordland-river-stub ...
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Windward River
The Windward River is a river in Fiordland, New Zealand, flowing into Gold Arm, Charles Sound. The estuary of the Windward River is protected by the Kahukura (Gold Arm) Marine Reserve. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Rivers of Fiordland {{Fiordland-river-stub ...
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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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Fiord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords when floo ...
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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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Fiordland
Fiordland is a geographical region of New Zealand in the south-western corner of the South Island, comprising the westernmost third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name "Fiordland" comes from a variant spelling of the Scandinavian word for this type of steep valley, "fjord". The area of Fiordland is dominated by, and very roughly coterminous with, Fiordland National Park, New Zealand's largest National Park. Due to the often steep terrain and high amount of rainfall supporting dense vegetation, the interior of the Fiordland region is largely inaccessible. As a result, Fiordland was never subjected to notable logging operations, and even attempts at whaling, seal hunting, and mining were on a small scale and short-lived, partly also because of the challenging weather. Today, Fiordland contains by far the greatest extent of u ...
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Taitetimu / Caswell Sound
Taitetimu / Caswell Sound is a fiord of the South Island of New Zealand. It is one of the fiords that form the coast of Fiordland. Geography The fiord is located between Te Houhou / George Sound and Taiporoporo / Charles Sound, on the central Fiordland coast. It is 16 kilometres in length, and extends in a roughly west-northwestern direction. The fiord is relatively straight except near its mouth, when it turns northward, and has no major arms or indentations. A small island, Styles Island, sits close to the southern shore at the fiord's entrance to the Tasman Sea. A straight ridge of peaks lies parallel with the fiord's south shore, between it and the valley of the Juno River. The highest point of these peaks, at , lies just to the west of the small mountain lake, Lake Shirley, which flows into the fiord over the Shirley Falls. Mountains also stand against the northern shore of the fiord, several of them rising above . Several small rivers enter the fiord along its s ...
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Hinenui / Nancy Sound
Hinenui / Nancy Sound is a fiord on the South Island of New Zealand. It is one of the fiords that form the coast of Fiordland. Geography Hinenui / Nancy Sound is located between Taiporoporo / Charles Sound and Te Awa-o-Tū / Thompson Sound, part of the Doubtful Sound complex. The fiord runs straight in a northwesterly direction for most of its 15.4 kilometre length, with the exception of a bend to the west near its entrance and a nearly right-angle bend near its head. This section, known as 'Foot Arm' due to its resemblance to a human foot (along with similarly-named 'Heel Cove' and 'Toe Cove' at their respective positions), runs in a southwesterly direction before turning at Heel Cove to join the main channel of the Fiord. The fiord has two small islands at its entrance. One of these, the aptly-named Entrance Island, sits to the north of the main channel, off the coast of Burnett Point. The other, Anxiety Island, is in a similar position to the south, sitting just north of ...
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Fiordland's Marine Reserves
Fiordland is a geographical region of New Zealand in the south-western corner of the South Island, comprising the westernmost third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name "Fiordland" comes from a variant spelling of the Scandinavian word for this type of steep valley, "fjord". The area of Fiordland is dominated by, and very roughly coterminous with, Fiordland National Park, New Zealand's largest National Park. Due to the often steep terrain and high amount of rainfall supporting dense vegetation, the interior of the Fiordland region is largely inaccessible. As a result, Fiordland was never subjected to notable logging operations, and even attempts at whaling, seal hunting, and mining were on a small scale and short-lived, partly also because of the challenging weather. Today, Fiordland contains by far the greatest extent of ...
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Juno River
The Juno River is a river of Fiordland, New Zealand. It rises west of Lake Shirley and flows westward into the Tasman Sea between Taitetimu / Caswell Sound and Taiporoporo / Charles Sound. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Rivers of Fiordland {{Fiordland-river-stub ...
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Seal Hunting
Seal hunting, or sealing, is the personal or commercial hunting of seals. Seal hunting is currently practiced in ten countries: United States (above the Arctic Circle in Alaska), Canada, Namibia, Denmark (in self-governing Greenland only), Iceland, Norway, Russia, Finland and Sweden. Most of the world's seal hunting takes place in Canada and Greenland. The Canadian Department of Fisheries and Oceans (DFO) regulates the seal hunt in Canada. It sets quotas (total allowable catch – TAC), monitors the hunt, studies the seal population, works with the Canadian Sealers' Association to train sealers on new regulations, and promotes sealing through its website and spokespeople. The DFO set harvest quotas of over 90,000 seals in 2007; 275,000 in 2008; 280,000 in 2009; and 330,000 in 2010. The actual kills in recent years have been less than the quotas: 82,800 in 2007; 217,800 in 2008; 72,400 in 2009; and 67,000 in 2010. In 2007, Norway claimed that 29,000 harp seals were killed, Russ ...
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