75-574: 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 93 square kilometres (36 sq mi), 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
150-741: A branch line railway from Invercargill was opened to Tuatapere and it became known as the Tuatapere Branch . On 20 October 1925, an extension was opened to Orawia , 14 kilometres to the north-east but the line continued to be known as the Tuatapere Branch and an engine depot was established in the town. It was used as the base for most operations on the line and the branch was operated as essentially two sections, one from Invercargill to Tuatapere and one from Tuatapere to Orawia. Until 1968, steam locomotives ran all trains to Tuatapere, but in June 1968,
225-588: A Germanic noun for a travel : North Germanic ferd or färd and of the verb to travel , Dutch varen , German fahren ; English to fare . As a loanword from Norwegian, it is one of the few words in the English language to start with the sequence fj . The word was for a long time normally spelled f i ord , a spelling preserved in place names such as Grise Fiord . The fiord spelling mostly remains only in New Zealand English , as in
300-617: A common Germanic origin of the word. The landscape consists mainly of moraine heaps. The Föhrden and some "fjords" on the east side of Jutland, Denmark are also of glacial origin. But while the glaciers digging "real" fjords moved from the mountains to the sea, in Denmark and Germany they were tongues of a huge glacier covering the basin of which is now the Baltic Sea. See Förden and East Jutland Fjorde . Whereas fjord names mostly describe bays (though not always geological fjords), straits in
375-451: A fjord as a kind of sea ( Māori : tai ) that runs by a bluff ( matapari , altogether tai matapari "bluff sea"). The term "fjord" is sometimes applied to steep-sided inlets which were not created by glaciers. Most such inlets are drowned river canyons or rias . Examples include: Some Norwegian freshwater lakes that have formed in long glacially carved valleys with sill thresholds, ice front deltas or terminal moraines blocking
450-451: A glacial river flows in. Velfjorden has little inflow of freshwater. In 2000, some coral reefs were discovered along the bottoms of the Norwegian fjords. These reefs were found in fjords from the north of Norway to the south. The marine life on the reefs is believed to be one of the most important reasons why the Norwegian coastline is such a generous fishing ground. Since this discovery
525-421: A highly productive group of phytoplankton that enable such fjords to be valuable feeding grounds for other species. It is possible that as climate change reduces long-term meltwater output, nutrient dynamics within such fjords will shift to favor less productive species, destabilizing the food web ecology of fjord systems. In addition to nutrient flux, sediment carried by flowing glaciers can become suspended in
600-518: A logging museum and is located on the Southern Scenic Route from Invercargill to Te Anau making it a well-travelled tourist stop. The Clifden Suspension Bridge and Clifden War Memorial are located near State Highway 99 outside Tuatapere. A group of Hungarians settled in Tuatapere, but were assimilated into the general population by the mid 20th century. On 1 October 1909,
675-515: A long, narrow inlet. In eastern Norway, the term is also applied to long narrow freshwater lakes ( Randsfjorden and Tyrifjorden ) and sometimes even to rivers (for instance in Flå Municipality in Hallingdal , the Hallingdal river is referred to as fjorden ). In southeast Sweden, the name fjard fjärd is a subdivision of the term 'fjord' used for bays, bights and narrow inlets on
750-534: A narrower sound is called sund . In the Finnish language , a word vuono is used although there is only one fjord in Finland. In old Norse genitive was fjarðar whereas dative was firði . The dative form has become common place names like Førde (for instance Førde ), Fyrde or Førre (for instance Førre ). The German use of the word Föhrde for long narrow bays on their Baltic Sea coastline, indicates
825-747: A population density of 270 people per km . It is part of the much larger Longwood Forest statistical area. Tuatapere had a population of 531 at the 2018 New Zealand census , a decrease of 27 people (−4.8%) since the 2013 census , and a decrease of 48 people (−8.3%) since the 2006 census . There were 240 households, comprising 273 males and 258 females, giving a sex ratio of 1.06 males per female, with 81 people (15.3%) aged under 15 years, 84 (15.8%) aged 15 to 29, 237 (44.6%) aged 30 to 64, and 138 (26.0%) aged 65 or older. Ethnicities were 90.4% European/ Pākehā , 19.2% Māori , 1.7% Pasifika , 2.3% Asian , and 2.3% other ethnicities. People may identify with more than one ethnicity. Although some people chose not to answer
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#1733085695987900-500: A protected passage almost the entire 1,601 km (995 mi) route from Stavanger to North Cape , Norway. The Blindleia is a skerry-protected waterway that starts near Kristiansand in southern Norway and continues past Lillesand . The Swedish coast along Bohuslän is likewise skerry guarded. The Inside Passage provides a similar route from Seattle , Washington , and Vancouver , British Columbia , to Skagway , Alaska . Yet another such skerry-protected passage extends from
975-658: A suffix in names of some Scandinavian fjords and has in same cases also been transferred to adjacent settlements or surrounding areas for instance Hardanger , Stavanger , and Geiranger . The differences in usage between the English and the Scandinavian languages have contributed to confusion in the use of the term fjord. Bodies of water that are clearly fjords in Scandinavian languages are not considered fjords in English; similarly bodies of water that would clearly not be fjords in
1050-639: Is 160 m (520 ft) deep with a threshold of only 1.5 m (4 ft 11 in), while the 1,300 m (4,300 ft) deep Sognefjorden has a threshold around 100 to 200 m (330 to 660 ft) deep. Hardangerfjord is made up of several basins separated by thresholds: The deepest basin Samlafjorden between Jonaneset ( Jondal ) and Ålvik with a distinct threshold at Vikingneset in Kvam Municipality . Hanging valleys are common along glaciated fjords and U-shaped valleys . A hanging valley
1125-564: Is 2,000 m (6,562 ft) below the surrounding regional topography. Fjord lakes are common on the inland lea of the Coast Mountains and Cascade Range ; notable ones include Lake Chelan , Seton Lake , Chilko Lake , and Atlin Lake . Kootenay Lake , Slocan Lake and others in the basin of the Columbia River are also fjord-like in nature, and created by glaciation in the same way. Along
1200-483: Is a tributary valley that is higher than the main valley and was created by tributary glacier flows into a glacier of larger volume. The shallower valley appears to be 'hanging' above the main valley or a fjord. Often, waterfalls form at or near the outlet of the upper valley. Small waterfalls within these fjords are also used as freshwater resources. Hanging valleys also occur underwater in fjord systems. The branches of Sognefjord are for instance much shallower than
1275-450: Is a long, narrow sea inlet with steep sides or cliffs, created by a glacier . Fjords exist on the coasts of Antarctica , the Arctic , and surrounding landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be 29,000 km (18,000 mi) long with its nearly 1,200 fjords, but only 2,500 km (1,600 mi) long excluding the fjords . A true fjord
1350-414: Is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or glacial rebound). In some cases, this rebound is faster than sea level rise . Most fjords are deeper than the adjacent sea ; Sognefjord , Norway , reaches as much as 1,300 m (4,265 ft) below sea level . Fjords generally have a sill or shoal (bedrock) at their mouth caused by
1425-412: Is also often described as a fjord, but is actually a freshwater lake cut off from the sea, so is not a fjord in the English sense of the term. Locally they refer to it as a "landlocked fjord". Such lakes are sometimes called "fjord lakes". Okanagan Lake was the first North American lake to be so described, in 1962. The bedrock there has been eroded up to 650 m (2,133 ft) below sea level, which
1500-430: Is at least 500 m (1,600 ft) deep and water takes an average of 16 years to flow through the lake. Such lakes created by glacial action are also called fjord lakes or moraine-dammed lakes . Some of these lakes were salt after the ice age but later cut off from the ocean during the post-glacial rebound . At the end of the ice age Eastern Norway was about 200 m (660 ft) lower (the marine limit). When
1575-456: Is borrowed from Norwegian , where it is pronounced [ˈfjuːr] , [ˈfjøːr] , [ˈfjuːɽ] or [ˈfjøːɽ] in various dialects and has a more general meaning, referring in many cases to any long, narrow body of water, inlet or channel (for example, see Oslofjord ). The Norwegian word is inherited from Old Norse fjǫrðr , a noun which refers to a 'lake-like' body of water used for passage and ferrying and
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#17330856959871650-615: Is closely related to the noun ferð "travelling, ferrying, journey". Both words go back to Indo-European *pértus "crossing", from the root *per- "cross". The words fare and ferry are of the same origin. The Scandinavian fjord , Proto-Scandinavian * ferþuz , is the origin for similar Germanic words: Icelandic fjörður , Faroese fjørður , Swedish fjärd (for Baltic waterbodies), Scots firth (for marine waterbodies, mainly in Scotland and northern England). The Norse noun fjǫrðr
1725-458: Is cut almost in two by the Svelvik "ridge", a sandy moraine that was below sea level when it was covered by ice, but after the post-glacial rebound reaches 60 m (200 ft) above the fjord. In the 19th century, Jens Esmark introduced the theory that fjords are or have been created by glaciers and that large parts of Northern Europe had been covered by thick ice in prehistory. Thresholds at
1800-487: Is dominated by two large islands, Weka / Long Island and Steep-to Island, while the northern half has many more smaller islands as part of the Cording Islands group. Towards the northeast of the lower portion of the fiord, it again splits in two. The upper half forms a roughly 5-kilometre-long arm known as Isthmus Sound, while the lower half forms a narrow channel to the inner fiord. After two further arms – Useless Bay to
1875-646: Is fairly new, little research has been done. The reefs are host to thousands of lifeforms such as plankton , coral , anemones , fish, several species of shark, and many more. Most are specially adapted to life under the greater pressure of the water column above it, and the total darkness of the deep sea. New Zealand's fjords are also host to deep-water corals , but a surface layer of dark fresh water allows these corals to grow in much shallower water than usual. An underwater observatory in Milford Sound allows tourists to view them without diving. In some places near
1950-458: 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 flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting
2025-500: Is located on the southern shore of Lake Superior in Michigan . The principal mountainous regions where fjords have formed are in the higher middle latitudes and the high latitudes reaching to 80°N (Svalbard, Greenland), where, during the glacial period, many valley glaciers descended to the then-lower sea level. The fjords develop best in mountain ranges against which the prevailing westerly marine winds are orographically lifted over
2100-465: Is the freshwater fjord Movatnet (Mo lake) that until 1743 was separated from Romarheimsfjorden by an isthmus and connected by a short river. During a flood in November 1743, the river bed eroded and sea water could flow into the lake at high tide. Eventually, Movatnet became a saltwater fjord and renamed Mofjorden ( Mofjorden ). Like fjords, freshwater lakes are often deep. For instance Hornindalsvatnet
2175-409: Is the isthmus with a village between Hornindalsvatnet lake and Nordfjord . Such lakes are also denoted fjord valley lakes by geologists. One of Norway's largest is Tyrifjorden at 63 m (207 ft) above sea level and an average depth at 97 m (318 ft) most of the lake is under sea level. Norway's largest lake, Mjøsa , is also referred to as "the fjord" by locals. Another example
2250-410: Is usually a large inflow of river water in the inner areas. This freshwater gets mixed with saltwater creating a layer of brackish water with a slightly higher surface than the ocean which in turn sets up a current from the river mouths towards the ocean. This current is gradually more salty towards the coast and right under the surface current there is a reverse current of saltier water from the coast. In
2325-602: The 2013 census , and an increase of 48 people (2.5%) since the 2006 census . There were 801 households, comprising 1,080 males and 918 females, giving a sex ratio of 1.18 males per female. The median age was 41.4 years (compared with 37.4 years nationally), with 417 people (20.9%) aged under 15 years, 321 (16.1%) aged 15 to 29, 960 (48.1%) aged 30 to 64, and 294 (14.7%) aged 65 or older. Ethnicities were 89.9% European/ Pākehā , 12.8% Māori , 1.5% Pasifika , 4.4% Asian , and 2.3% other ethnicities. People may identify with more than one ethnicity. The percentage of people born overseas
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2400-610: The British Columbia Coast , a notable fjord-lake is Owikeno Lake , which is a freshwater extension of Rivers Inlet . Quesnel Lake , located in central British Columbia, is claimed to be the deepest fjord formed lake on Earth. A family of freshwater fjords are the embayments of the North American Great Lakes. Baie Fine is located on the northwestern coast of Georgian Bay of Lake Huron in Ontario , and Huron Bay
2475-459: The Scandinavian sense of the term, are not universally considered to be fjords by the scientific community, because although glacially formed, most Finnmark fjords lack the steep-sided valleys of the more southerly Norwegian fjords. The glacial pack was deep enough to cover even the high grounds when they were formed. The Oslofjord , on the other hand, is a rift valley , and not glacially formed. The indigenous Māori people of New Zealand see
2550-598: The Straits of Magellan north for 800 km (500 mi). Fjords provide unique environmental conditions for phytoplankton communities. In polar fjords, glacier and ice sheet outflow add cold, fresh meltwater along with transported sediment into the body of water. Nutrients provided by this outflow can significantly enhance phytoplankton growth. For example, in some fjords of the West Antarctic Peninsula (WAP), nutrient enrichment from meltwater drives diatom blooms,
2625-535: The Viking settlers—though the inlet at that place in modern terms is an estuary , not a fjord. Similarly the name of Milford (now Milford Haven) in Wales is derived from Melrfjǫrðr ("sandbank fjord/inlet"), though the inlet on which it is located is actually a ria. Before or in the early phase of Old Norse angr was another common noun for fjords and other inlets of the ocean. This word has survived only as
2700-835: The Limfjord once was a fjord until the sea broke through from the west. Ringkøbing Fjord on the western coast of Jutland is a lagoon . The long narrow fjords of Denmark's Baltic Sea coast like the German Förden were dug by ice moving from the sea upon land, while fjords in the geological sense were dug by ice moving from the mountains down to the sea. However, some definitions of a fjord is: "A long narrow inlet consisting of only one inlet created by glacial activity". Examples of Danish fjords are: Kolding Fjord , Vejle Fjord and Mariager Fjord . The fjords in Finnmark in Norway, which are fjords in
2775-532: The Scandinavian sense have been named or suggested to be fjords. Examples of this confused usage follow. In the Danish language some inlets are called a fjord, but are, according to the English language definition, technically not a fjord, such as Roskilde Fjord . Limfjord in English terminology is a sound , since it separates the North Jutlandic Island (Vendsyssel-Thy) from the rest of Jutland . However,
2850-468: The Swedish Baltic Sea coast, and in most Swedish lakes. This latter term is also used for bodies of water off the coast of Finland where Finland Swedish is spoken. In Danish, the word may even apply to shallow lagoons . In modern Icelandic, fjörður is still used with the broader meaning of firth or inlet. In Faroese fjørður is used both about inlets and about broader sounds, whereas
2925-513: The bedrock. This may in particular have been the case in Western Norway where the tertiary uplift of the landmass amplified eroding forces of rivers. Confluence of tributary fjords led to excavation of the deepest fjord basins. Near the very coast, the typical West Norwegian glacier spread out (presumably through sounds and low valleys) and lost their concentration and reduced the glaciers' power to erode leaving bedrock thresholds. Bolstadfjorden
3000-514: The case of Hardangerfjord the fractures of the Caledonian fold has guided the erosion by glaciers, while there is no clear relation between the direction of Sognefjord and the fold pattern. This relationship between fractures and direction of fjords is also observed in Lyngen . Preglacial, tertiary rivers presumably eroded the surface and created valleys that later guided the glacial flow and erosion of
3075-405: The census's question about religious affiliation, 52.5% had no religion, 32.8% were Christian , 1.1% had Māori religious beliefs , and 0.6% were Hindu . Of those at least 15 years old, 39 (8.7%) people had a bachelor's or higher degree, and 162 (36.0%) people had no formal qualifications. 42 people (9.3%) earned over $ 70,000 compared to 17.2% nationally. The employment status of those at least 15
Rakituma / Preservation Inlet - Misplaced Pages Continue
3150-434: The deeper parts of the fjord the cold water remaining from winter is still and separated from the atmosphere by the brackish top layer. This deep water is ventilated by mixing with the upper layer causing it to warm and freshen over the summer. In fjords with a shallow threshold or low levels of mixing this deep water is not replaced every year and low oxygen concentration makes the deep water unsuitable for fish and animals. In
3225-459: The fiord sits to the north of the island and is 1.67 kilometres (1.04 mi) wide at its narrowest point. Otago Retreat separates Coal Island from the mainland to the south, which has an average width of less than a kilometre and just 375 metres (1,230 ft) at its narrowest point. Numerous smaller islands are located in the middle portion of the fiord, between Coal Island and the entrance to Te Awaroa / Long Sound. The southern half of this section
3300-551: The fiord's length, with Awaroa translating as "long river". At its head, this fiord is in turn fed by the outlet of Long Burn. Gray River flows nearby the inlet. A large part of the interior of Preservation Inlet is protected by the Te Tapuwae o Hua (Long Sound) Marine Reserve . Known to early sealers and whalers , it was named Port Preservation by Captain Eber Bunker in 1809. The first shore-based whaling station in New Zealand
3375-413: The fjord. Bolstadfjorden has a threshold of only 1.5 m (4 ft 11 in) and strong inflow of freshwater from Vosso river creates a brackish surface that blocks circulation of the deep fjord. The deeper, salt layers of Bolstadfjorden are deprived of oxygen and the seabed is covered with organic material. The shallow threshold also creates a strong tidal current. During the summer season, there
3450-489: The formation of sea ice. The study of phytoplankton communities within fjords is an active area of research, supported by groups such as FjordPhyto, a citizen science initiative to study phytoplankton samples collected by local residents, tourists, and boaters of all backgrounds. An epishelf lake forms when meltwater is trapped behind a floating ice shelf and the freshwater floats on the denser saltwater below. Its surface may freeze forming an isolated ecosystem. The word fjord
3525-468: The ice cap receded and allowed the ocean to fill valleys and lowlands, and lakes like Mjøsa and Tyrifjorden were part of the ocean while Drammen valley was a narrow fjord. At the time of the Vikings Drammensfjord was still four or five m (13 or 16 ft) higher than today and reached the town of Hokksund , while parts of what is now the city of Drammen was under water. After the ice age
3600-439: The inlet. No roads reach the coast at this point. However, a tramping track is available from Tuatapere to Big River, east of Preservation Inlet. After Big River there is no continuous track or marked route to the inlet. There is also access to the sound by sea or air. Fiord In physical geography , a fjord (also spelled fiord in New Zealand English ; ( / ˈ f j ɔːr d , f iː ˈ ɔːr d / )
3675-446: The level of the original sea level. In Eidfjord, Eio has dug through the original delta and left a 110 m (360 ft) terrace while lake is only 19 m (62 ft) above sea level. Such deposits are valuable sources of high-quality building materials (sand and gravel) for houses and infrastructure. Eidfjord village sits on the eid or isthmus between Eidfjordvatnet lake and Eidfjorden branch of Hardangerfjord. Nordfjordeid
3750-426: The line was dieselised , resulting in the closure of the Tuatapere engine depot. On 1 October 1970, a lack of traffic meant the line was truncated to Tuatapere, and it was further cut on 30 July 1976 when the section between Riverton and Tuatapere closed. Some relics from the railway have been preserved in Tuatapere, including structures in the station area such as the old station building and goods shed . Tuatapere
3825-471: The main fjord. The mouth of Fjærlandsfjord is about 400 m (1,300 ft) deep while the main fjord is 1,200 m (3,900 ft) nearby. The mouth of Ikjefjord is only 50 m (160 ft) deep while the main fjord is around 1,300 m (4,300 ft) at the same point. During the winter season, there is usually little inflow of freshwater. Surface water and deeper water (down to 100 m or 330 ft or more) are mixed during winter because of
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#17330856959873900-491: The marine limit. Like freshwater fjords, the continuation of fjords on land are in the same way denoted as fjord-valleys . For instance Flåmsdal ( Flåm valley) and Måbødalen . Outside of Norway, the three western arms of New Zealand 's Lake Te Anau are named North Fiord, Middle Fiord and South Fiord. Another freshwater "fjord" in a larger lake is Western Brook Pond , in Newfoundland's Gros Morne National Park ; it
3975-405: The most extreme cases, there is a constant barrier of freshwater on the surface and the fjord freezes over such that there is no oxygen below the surface. Drammensfjorden is one example. The mixing in fjords predominantly results from the propagation of an internal tide from the entrance sill or internal seiching. The Gaupnefjorden branch of Sognefjorden is strongly affected by freshwater as
4050-565: The mountainous regions, resulting in abundant snowfall to feed the glaciers. Hence coasts having the most pronounced fjords include the west coast of Norway, the west coast of North America from Puget Sound to Alaska, the southwest coast of New Zealand, and the west and to south-western coasts of South America , chiefly in Chile . Other regions have fjords, but many of these are less pronounced due to more limited exposure to westerly winds and less pronounced relief. Areas include: The longest fjords in
4125-462: The mouths and overdeepening of fjords compared to the ocean are the strongest evidence of glacial origin, and these thresholds are mostly rocky. Thresholds are related to sounds and low land where the ice could spread out and therefore have less erosive force. John Walter Gregory argued that fjords are of tectonic origin and that glaciers had a negligible role in their formation. Gregory's views were rejected by subsequent research and publications. In
4200-487: The north, and Revolver Bay to the south – the fiord changes from its predominant northeasterly direction to the northwest for 5.5 kilometres (3.4 mi). After this, the fiord turns back to its original orientation for the remainder of its length. This inner portion of the fiord, running for approximately 16.5 kilometres (10.3 mi), is known as Te Awaroa / Long Sound. Both the European and Māori portions of this name refer to
4275-506: 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 coastlines with many islands, before perfecting his technique by the time he created Piopiotahi at the north. The main body of Rakituma is connected to the Tasman Sea by two passages, separated by Coal Island . The main passage of
4350-448: The ocean was about 150 m (490 ft) at Notodden . The ocean stretched like a fjord through Heddalsvatnet all the way to Hjartdal . Post-glacial rebound eventually separated Heddalsvatnet from the ocean and turned it into a freshwater lake. In neolithic times Heddalsvatnet was still a saltwater fjord connected to the ocean, and was cut off from the ocean around 1500 BC. Some freshwater fjords such as Slidrefjord are above
4425-423: The outlet follow the Norwegian naming convention; they are frequently named fjords. Ice front deltas developed when the ice front was relatively stable for long time during the melting of the ice shield. The resulting landform is an isthmus between the lake and the saltwater fjord, in Norwegian called "eid" as in placename Eidfjord or Nordfjordeid . The post-glacial rebound changed these deltas into terraces up to
4500-439: The outlet of fjords where submerged glacially formed valleys perpendicular to the coast join with other cross valleys in a complex array. The island fringe of Norway is such a group of skerries (called a skjærgård ); many of the cross fjords are so arranged that they parallel the coast and provide a protected channel behind an almost unbroken succession of mountainous islands and skerries. By this channel, one can travel through
4575-460: The place name Fiordland . The use of the word fjord in Norwegian, Danish and Swedish is more general than in English and in international scientific terminology. In Scandinavia, fjord is used for a narrow inlet of the sea in Norway, Denmark and western Sweden, but this is not its only application. In Norway and Iceland, the usage is closest to the Old Norse, with fjord used for both a firth and for
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#17330856959874650-449: The previous glacier's reduced erosion rate and terminal moraine . In many cases this sill causes extreme currents and large saltwater rapids (see skookumchuck ). Saltstraumen in Norway is often described as the world's strongest tidal current . These characteristics distinguish fjords from rias (such as the Bay of Kotor ), which are drowned valleys flooded by the rising sea. Drammensfjorden
4725-569: The same regions typically are named Sund , in Scandinavian languages as well as in German. The word is related to "to sunder" in the meaning of "to separate". So the use of Sound to name fjords in North America and New Zealand differs from the European meaning of that word. The name of Wexford in Ireland is originally derived from Veisafjǫrðr ("inlet of the mud flats") in Old Norse, as used by
4800-482: The seaward margins of areas with fjords, the ice-scoured channels are so numerous and varied in direction that the rocky coast is divided into thousands of island blocks, some large and mountainous while others are merely rocky points or rock reefs , menacing navigation. These are called skerries . The term skerry is derived from the Old Norse sker , which means a rock in the sea. Skerries most commonly formed at
4875-413: 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. 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
4950-473: The sites of the historic Alpha and Golden Mines. In October 2019, the name of the inlet was officially altered to Rakituma / Preservation Inlet. After a massive exploitation for over years, southern right whales finally started returning into the inlet along with Chalky Inlet . There are anecdotal sightings of Hector's dolphins . while bottlenose dolphins are more regularly observed. Southern elephant seals are occasionally observed resting on shore around
5025-419: The steady cooling of the surface and wind. In the deep fjords, there is still fresh water from the summer with less density than the saltier water along the coast. Offshore wind, common in the fjord areas during winter, sets up a current on the surface from the inner to the outer parts. This current on the surface in turn pulls dense salt water from the coast across the fjord threshold and into the deepest parts of
5100-455: The water column, increasing turbidity and reducing light penetration into greater depths of the fjord. This effect can limit the available light for photosynthesis in deeper areas of the water mass, reducing phytoplankton abundance beneath the surface. Overall, phytoplankton abundance and species composition within fjords is highly seasonal, varying as a result of seasonal light availability and water properties that depend on glacial melt and
5175-487: The world are: Deep fjords include: Tuatapere Tuatapere is a small rural town in Southland , New Zealand. It is the self declared "Sausage Capital of New Zealand". Tuatapere is located eight kilometres from the southern coast. The Waiau River flows through the town before reaching Te Waewae Bay , where it has its outflow into Foveaux Strait . The main local industries are forestry and farming. Tuatapere has
5250-564: Was $ 31,500, compared with $ 31,800 nationally. 171 people (10.8%) earned over $ 70,000 compared to 17.2% nationally. The employment status of those at least 15 was that 879 (55.7%) people were employed full-time, 255 (16.2%) were part-time, and 48 (3.0%) were unemployed. Waiau Area School is a composite school for years 1 to 13 with a roll of 142 as of August 2024. The school first opened in 1910 as Tuatapere School providing primary education. It added secondary education in 1945, becoming Tuatapere District High, and later Waiau District High. In 1953
5325-467: Was 10.4, compared with 27.1% nationally. Although some people chose not to answer the census's question about religious affiliation, 55.2% had no religion, 32.8% were Christian , 0.3% had Māori religious beliefs , 0.3% were Hindu , 0.5% were Muslim , 0.6% were Buddhist and 1.1% had other religions. Of those at least 15 years old, 180 (11.4%) people had a bachelor's or higher degree, and 420 (26.6%) people had no formal qualifications. The median income
5400-585: Was adopted in German as Förde , used for the narrow long bays of Schleswig-Holstein , and in English as firth "fjord, river mouth". The English word ford (compare German Furt , Low German Ford or Vörde , in Dutch names voorde such as Vilvoorde, Ancient Greek πόρος , poros , and Latin portus ) is assumed to originate from Germanic * ferþu- and Indo-European root * pertu- meaning "crossing point". Fjord/firth/Förde as well as ford/Furt/Vörde/voorde refer to
5475-532: Was established here in 1828 or 1829 by Captain Peter Williams, exploiting southern right whales in the area. In the 1890s gold deposits were found. Two settlements, known as Cromarty and Te Oneroa, were established in Kisbee Bay for miners. However by 1904 only a few miners were left, and few traces of the settlements remain though in places large pieces of rusting equipment can be seen in the regenerating bush at
5550-420: Was one of the closest settlements to the 7.8 magnitude earthquake which occurred on 15 July 2009, the largest in New Zealand since 1931. Despite the earthquake's huge force, little damage was sustained and no injuries were reported. Tuatapere is described as a rural settlement by Statistics New Zealand. It covers 2.00 km (0.77 sq mi), and had an estimated population of 540 as of June 2024, with
5625-427: Was that 201 (44.7%) people were employed full-time, 57 (12.7%) were part-time, and 15 (3.3%) were unemployed. Longwood Forest statistical area covers 2,198.54 km (848.86 sq mi) and also includes Clifden . It had an estimated population of 2,140 as of June 2024, with a population density of 1.0 people per km . Longwood Forest had a population of 1,995 at the 2018 New Zealand census , unchanged since
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