|
List Of Sounds And Inlets Of Fiordland
The following is a list of the sounds and inlets or similar features which punctuate the coast of Fiordland, in southwestern New Zealand, in geographic order from north to south: * Big Bay *Martins Bay *Milford Sound *Poison Bay * Sutherland Sound * Hāwea / Bligh Sound **Bounty Haven * George Sound **South West Arm *Looking Glass Bay *Caswell Sound *Charles Sound **Emelius Arm * Hinenui / Nancy Sound **Foot Arm * Thompson Sound ** Bradshaw Sound (also Doubtful Sound) ***Precipice Cove ***Gaer Arm *Doubtful Sound / Patea, and its arms: **Malaspina Reach ***Hall Arm ***Crooked Arm **First Arm * Dagg Sound **Anchorage Arm *Breaksea Sound, and its arms: **Vancouver Arm **Broughton Arm **Acheron Passage (linked to Dusky Sound) ***Wet Jacket Arm *Tamatea / Dusky Sound **Supper Cove **Fanny Bay **Cascade Cove *Taiari / Chalky Inlet, and its arms: ** Moana-whenua-pōuri / Edwardson Sound **Te Korowhakaunu / Kanáris Sound *Rakituma / Preservation Inlet, and its arms: ** Isthmus Sound **U ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Map Of Fiordland National Park (12485990223)
A map is a symbolic depiction emphasizing relationships between elements of some space, such as objects, regions, or themes. Many maps are static, fixed to paper or some other durable medium, while others are dynamic or interactive. Although most commonly used to depict geography, maps may represent any space, real or fictional, without regard to context or scale, such as in brain mapping, DNA mapping, or computer network topology mapping. The space being mapped may be two dimensional, such as the surface of the earth, three dimensional, such as the interior of the earth, or even more abstract spaces of any dimension, such as arise in modeling phenomena having many independent variables. Although the earliest maps known are of the heavens, geographic maps of territory have a very long tradition and exist from ancient times. The word "map" comes from the , wherein ''mappa'' meant 'napkin' or 'cloth' and ''mundi'' 'the world'. Thus, "map" became a shortened term referrin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dual Naming
Dual naming is the adoption of an official place name that combines two earlier names, or uses both names, often to resolve a disagreement over which of the two individual names is more appropriate. In some cases, the reasons are political. Sometimes the two individual names are from different languages; in some cases this is because the country has more than one official language, and in others, one language has displaced another. In several countries, dual naming has begun to be applied only recently. This has come about in places where a colonial settler community had displaced the indigenous peoples and started using names in the settler language centuries ago, and more recent efforts have been made to use names in the indigenous language alongside the colonial names, as an act of reconciliation. Australia In Australia, a dual naming policy is often now used officially to name landmarks that are of significance to local Indigenous Australians, but for which the most common ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Hakapoua
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Awaroa / Long Sound
Rakituma / Preservation Inlet is the southernmost fiord in Fiordland National Park and lies on the southwest corner of the South Island of New Zealand. With an area of , it is the fourth largest fiord in New Zealand, after Tamatea / Dusky Sound, Doubtful Sound / Patea, and the neighbouring Taiari / Chalky Inlet to the north. Rakituma was briefly the site of an attempted fishing and gold mining settlement at Cromarty during the 19th century, however this was quickly abandoned once the level of gold declined in relation to more promising fields elsewhere. Geography As with Taiari / Chalky Inlet immediately to the north, Rakituma / Preservation Inlet has reasonably complex geography, resembling an inlet in its outer reaches more than the well-defined fiords to the north. According to Māori legend, these fiords were carved by the demigod Tū-te-raki-whānoa using his adze, Te Hamo. Starting from the south with Rakituma, his initial efforts were rough and resulted in rough coa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isthmus Sound
An isthmus (; ; ) is a narrow piece of land connecting two larger areas across an expanse of water by which they are otherwise separated. A tombolo is an isthmus that consists of a spit or bar, and a strait is the sea counterpart of an isthmus. Isthmus vs land bridge vs peninsula ''Isthmus'' and ''land bridge'' are related terms, with isthmus having a broader meaning. A land bridge is an isthmus connecting Earth's major landmasses. The term ''land bridge'' is usually used in biogeology to describe land connections that used to exist between continents at various times and were important for migration of people and various species of animals and plants, e.g. Beringia and Doggerland. An isthmus is a land connection between two bigger landmasses, while a peninsula is rather a land protrusion which is connected to a bigger landmass on one side only and surrounded by water on all other sides. Technically, an isthmus can have canals running from coast to coast (e.g. the Panama Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rakituma / Preservation Inlet
Rakituma / Preservation Inlet is the southernmost fiord in Fiordland National Park and lies on the southwest corner of the South Island of New Zealand. With an area of , it is the fourth largest fiord in New Zealand, after Tamatea / Dusky Sound, Doubtful Sound / Patea, and the neighbouring Taiari / Chalky Inlet to the north. Rakituma was briefly the site of an attempted fishing and gold mining settlement at Cromarty during the 19th century, however this was quickly abandoned once the level of gold declined in relation to more promising fields elsewhere. Geography As with Taiari / Chalky Inlet immediately to the north, Rakituma / Preservation Inlet has reasonably complex geography, resembling an inlet in its outer reaches more than the well-defined fiords to the north. According to Māori legend, these fiords were carved by the demigod Tū-te-raki-whānoa using his adze, Te Hamo. Starting from the south with Rakituma, his initial efforts were rough and resulted in rough coast ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Korowhakaunu / Kanáris Sound
Taiari / Chalky Inlet is one of the southernmost fiords in Fiordland, in the southwestern corner of New Zealand's South Island and part of Fiordland National Park. As with the neighbouring fiords of Tamatea / Dusky Sound to the north and Rakituma / Preservation Inlet to the south, Taiari / Chalky Inlet is a complex fiord with many channels and islands along its roughly length. Most notably, this includes the sections Moana-whenua-pōuri / Edwardson Sound and Te Korowhakaunu / Kanáris Sound, which split at Divide Head in the middle of Taiari and each extend for roughly inland in a V-shape. Despite its remoteness, Taiari / Chalky Inlet has seen frequent waves of human interaction. Early European accounts suggest that a population of Māori inhabited the fiord for a time, while battles between iwi (tribes) are said to have taken place in neighbouring Rakituma, but the extent of this habitation is not known. The fiord was regularly visited by Europeans during the late 18th and ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moana-whenua-pōuri / Edwardson Sound
Taiari / Chalky Inlet is one of the southernmost fiords in Fiordland, in the southwestern corner of New Zealand's South Island and part of Fiordland National Park. As with the neighbouring fiords of Tamatea / Dusky Sound to the north and Rakituma / Preservation Inlet to the south, Taiari / Chalky Inlet is a complex fiord with many channels and islands along its roughly length. Most notably, this includes the sections Moana-whenua-pōuri / Edwardson Sound and Te Korowhakaunu / Kanáris Sound, which split at Divide Head in the middle of Taiari and each extend for roughly inland in a V-shape. Despite its remoteness, Taiari / Chalky Inlet has seen frequent waves of human interaction. Early European accounts suggest that a population of Māori inhabited the fiord for a time, while battles between iwi (tribes) are said to have taken place in neighbouring Rakituma, but the extent of this habitation is not known. The fiord was regularly visited by Europeans during the late 18th an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiari / Chalky Inlet
Taiari / Chalky Inlet is one of the southernmost fiords in Fiordland, in the southwestern corner of New Zealand's South Island and part of Fiordland National Park. As with the neighbouring fiords of Tamatea / Dusky Sound to the north and Rakituma / Preservation Inlet to the south, Taiari / Chalky Inlet is a complex fiord with many channels and islands along its roughly length. Most notably, this includes the sections Moana-whenua-pōuri / Edwardson Sound and Te Korowhakaunu / Kanáris Sound, which split at Divide Head in the middle of Taiari and each extend for roughly inland in a V-shape. Despite its remoteness, Taiari / Chalky Inlet has seen frequent waves of human interaction. Early European accounts suggest that a population of Māori inhabited the fiord for a time, while battles between iwi (tribes) are said to have taken place in neighbouring Rakituma, but the extent of this habitation is not known. The fiord was regularly visited by Europeans during the late 18th and ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tamatea / Dusky Sound
Tamatea / Dusky Sound is a fiord on the southwest corner of New Zealand, in Fiordland National Park. Geography One of the most complex of the many fiords on this coast, it is also the largest at 40 kilometres in length and eight kilometres wide at its widest point. To the north of its mouth is the large Resolution Island, whose Five Fingers Peninsula shelters the mouth of the sound from the northwest; along the east coast of the island, Acheron Passage connects Dusky Sound with Breaksea Sound, to the north. Several large islands lie in the sound, notably Anchor Island, Long Island, and Cooper Island. The upper reaches of the sound are steep-sided, and the high precipitation of the region leads to hundreds of waterfalls cascading into the sound during the rainy season. Seals and dolphins are often sighted in the sound's waters and occasionally visited by whales where the area especially nearby Preservation Inlet was one of earliest shore-based whaling ground for southern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Acheron Passage
The Acheron (; grc, Ἀχέρων ''Acheron'' or Ἀχερούσιος ''Acherousios''; ell, Αχέροντας ''Acherontas'') is a river located in the Epirus region of northwest Greece. It is long, and its drainage area is . Its source is near the village Zotiko, in the southwestern part of the Ioannina regional unit, and it flows into the Ionian Sea in Ammoudia, near Parga. The Acheron also features prominently in Greek mythology, where it is often depicted as the entrance to the Greek Underworld where souls must be ferried across by Charon (although some later sources, such as Roman poets, assign this role to the river Styx). Mythology Ancient Greek mythology saw the Acheron, sometimes known as the "river of woe", as one of the five rivers of the Greek underworld. The name is of uncertain etymology. Most classical accounts, including Pausanias (10.28) and later Dante's ''Inferno'' (3.78), portray the Acheron as the entrance to the Underworld and depict Charon ferryi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> List Of Sounds And Inlets Of Fiordland")
.jpg "Click for more on -> Tamatea / Dusky Sound")