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Dagg Sound
Te Rā / Dagg Sound is a narrow fiord located in Fiordland, New Zealand. It lies south of Doubtful Sound / Patea and north of Te Puaitaha / Breaksea Sound Te Puaitaha / Breaksea Sound is a small fiord on the southwestern coast of South Island, New Zealand in the Tasman Sea. Breaksea Island in Fiordland National Park lies at its entrance. In the 1850s, early settlers Henry Hirst and John Watt .... Whales frequent the waters out from the entrance of the fiord, close to the edge of the continental shelf where the water depth suddenly drops to thousands of metres. The fiord is surrounded by steep cliffs and stretches inland for . Anchorage Arm branches off to the north of the fiord. At the eastern end of the fiord there is a short portage through to Crooked Arm in Doubtful Sound / Patea. Naming The fiord was named Dagg Sound after named after the Captain of the whaling boat, ''Scorpion'', who visited it in 1804. In October 2019, the name of the fiord was officiall ...
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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 br ...
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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 List of islands of New Zealand, smaller islands. It is the List of island countries, 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 of New Zealand, 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. ...
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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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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 ...
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Doubtful Sound / Patea
Doubtful Sound / Patea is a fiord in Fiordland, in the far south west of New Zealand. It is located in the same region as the smaller but more famous and accessible Milford Sound / Piopiotahi. It took second place after Milford Sound as New Zealand's most famous tourism destination. At long, Doubtful Sound / Patea is the second longest, and with a depth of up to the deepest of the South Island's fiords. In comparison with Milford Sound, it is more widespread, with the cliffs not as dramatically tall and near vertical. However, the U-shaped profile of the fiord is obvious, in particular on the two innermost of the main fiord's arms and the hanging side valleys along the main fiord. Like most of Fiordland, Doubtful Sound receives a high amount of rainfall, ranging from an annual average of . The vegetation on the mountainous landscape surrounding the fiord is dense native rainforest. History Doubtful Sound was named 'Doubtful Harbour' in 1770 by Captain Cook, who did not ...
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Te Puaitaha / Breaksea Sound
Te Puaitaha / Breaksea Sound is a small fiord on the southwestern coast of South Island, New Zealand in the Tasman Sea. Breaksea Island in Fiordland National Park lies at its entrance. In the 1850s, early settlers Henry Hirst and John Watts-Russell John Charles Watts-Russell JP (1825 – 2 April 1875) was a 19th-century New Zealand politician, a member of the Canterbury Provincial Council and a member of the Legislative Council. He was supposedly the wealthiest of the early settlers, and ... explored the area for flat land suitable for sheep farming, but they were unsuccessful. In October 2019, the name of the fiord was officially altered to Te Puaitaha / Breaksea Sound. References Fiords of New Zealand Sounds of Fiordland {{Fiordland ...
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Fiords Of New Zealand
The fiords of New Zealand are all located in the southwest of the South Island, in a mountainous area known as Fiordland. A fiord is a narrow inlet of the sea between cliffs or steep slopes, which results from marine inundation of a glaciated valley. The spelling ''fiord'' is used in New Zealand rather than ''fjord'', although all the maritime fiords instead use the word ''sound'' in their name. The Marlborough Sounds, a series of deep indentations in the coastline at the northern tip of the South Island, are in fact drowned river valleys, or rias. The deeply indented coastlines of Northland and Auckland also host many rias, such as the Hokianga and Waitematā Harbours. New Zealand has fifteen named maritime fiords, listed here from northernmost to southernmost.Distance measured down centreline of fiord from coastline to head of longest arm of fiord. List Thompson Sound separates Secretary Island from the mainland and connects with Doubtful Sound and Bradshaw Sound at its in ...
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