1.
Norwegian Maritime Museum
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The Norwegian Maritime Museum, previously known as the Norsk Sjøfartsmuseum, founded in 1914, is located at Bygdøynesveien on the Bygdøy peninsula, on the western side of Oslo, Norway. The museums building won an architectural award and its exhibits on coast culture and maritime history include boat models, fishing, marine archeology, marine paintings, ship building, and shipping. The video Maritime Norway by Ivo Caprino and a library are also a part of the museum experience, the Norwegian Maritime Museum is situated near several other museums, including the Fram Museum, the Kon-Tiki Museum, the Norwegian Museum of Cultural History, and the Viking Ship Museum. The Arctic ship Gjøa and the Stavanger are on display, Gjøa was the first vessel to transit the Northwest Passage in a 1903-06 expedition of Roald Amundsen. The Stavanger was designed by Colin Archer for the Norwegian Society for Sea Rescue, other boats are exhibited in the harbour. Gunnar Isachsen Kristian Kielland Svein Molaug Norwegian Maritime Museum - Official site
2.
Oslo
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Oslo is the capital and the most populous city in Norway. It constitutes both a county and a municipality, founded in the year 1040, and established as a kaupstad or trading place in 1048 by Harald Hardrada, the city was elevated to a bishopric in 1070 and a capital under Haakon V of Norway around 1300. Personal unions with Denmark from 1397 to 1523 and again from 1536 to 1814, after being destroyed by a fire in 1624, the city was moved closer to Akershus Fortress during the reign of Christian IV of Denmark and renamed Christiania in his honour. It was established as a municipality on 1 January 1838, following a spelling reform, it was known as Kristiania from 1877 to 1925, at which time its original Norwegian name was restored. Oslo is the economic and governmental centre of Norway, the city is also a hub of Norwegian trade, banking, industry and shipping. It is an important centre for industries and maritime trade in Europe. The city is home to companies within the maritime sector, some of which are among the worlds largest shipping companies, shipbrokers. Oslo is a city of the Council of Europe and the European Commission intercultural cities programme. Oslo is considered a city and ranked Beta World City in studies carried out by the Globalization and World Cities Study Group. It was ranked one in terms of quality of life among European large cities in the European Cities of the Future 2012 report by fDi magazine. A survey conducted by ECA International in 2011 placed Oslo as the second most expensive city in the world for living expenses after Tokyo. In 2013 Oslo tied with the Australian city of Melbourne as the fourth most expensive city in the world, as of January 1,2016, the municipality of Oslo has a population of 658,390, while the population of the citys urban area was 942,084. The metropolitan area had an population of 1.71 million. The population was during the early 2000 increasing at record rates and this growth stems for the most part from international immigration and related high birth rates, but also from intra-national migration. The immigrant population in the city is growing faster than the Norwegian population. As of January 1,2016, the municipality of Oslo has a population of 658,390, the urban area extends beyond the boundaries of the municipality into the surrounding county of Akershus, the total population of this agglomeration is 942,084. To the north and east, wide forested hills rise above the city giving the location the shape of a giant amphitheatre. The urban municipality of Oslo and county of Oslo are two parts of the entity, making Oslo the only city in Norway where two administrative levels are integrated
3.
Northwest Passage
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For centuries explorers sought a navigable passage as a possible trade route. Until 2009, the Arctic pack ice prevented regular marine shipping throughout most of the year, Arctic sea ice decline has rendered the waterways more navigable. If, as has been claimed, parts of the end of the Passage are barely 15 metres deep. Fully loaded, Nordic Orion was too large to sail through the Panama Canal, between the end of the 15th century and the 20th century, colonial powers from Europe dispatched explorers in an attempt to discover a commercial sea route north and west around North America. The Northwest Passage represented a new route to the trading nations of Asia. England called the northern route the Northwest Passage. The desire to establish such a route motivated much of the European exploration of both coasts of North America, when it became apparent that there was no route through the heart of the continent, attention turned to the possibility of a passage through northern waters. There was a lack of knowledge about conditions, for instance. Explorers thought that a water route close to the North Pole must exist. The belief that a route lay to the far north persisted for several centuries, many ended in disaster, including that by Sir John Franklin in 1845. While searching for him the McClure Arctic Expedition discovered the Northwest Passage in 1850, in 1906, the Norwegian explorer Roald Amundsen first successfully completed a passage from Greenland to Alaska in the sloop Gjøa. Since that date, several fortified ships have made the journey, from east to west, the direction of most early exploration attempts, expeditions entered the passage from the Atlantic Ocean via the Davis Strait and through Baffin Bay. Five to seven routes have taken through the Canadian Arctic Archipelago, via the McClure Strait, Dease Strait, and the Prince of Wales Strait. From there ships passed through waterways through the Beaufort Sea, Chukchi Sea, on August 21,2007, the Northwest Passage became open to ships without the need of an icebreaker. According to Nalan Koc of the Norwegian Polar Institute, this was the first time the Passage has been clear since they began keeping records in 1972, the Northwest Passage opened again on August 25,2008. Thawing ocean or melting ice simultaneously opened up the Northwest Passage, awaited by shipping companies, this historic event will cut thousands of miles off their routes. We are going to see more and more as the years go by. Due to Arctic shrinkage, the Beluga group of Bremen, Germany, however, Canadas Prime Minister Stephen Harper announced that ships entering the North-West passage should first report to his government
4.
Roald Amundsen
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Roald Engelbregt Gravning Amundsen was a Norwegian explorer of polar regions. He led the Antarctic expedition of 1910–12 which was the first to reach the South Pole, in 1926, he was the first expedition leader for the air expedition to the North Pole. Amundsen is recognized as the first person, without dispute, as having reached both poles and he is also known as having the first expedition to traverse the Northwest Passage in the Arctic. In June 1928, while taking part in a mission for the airship Italia. Amundsen was a key leader during the Heroic Age of Antarctic Exploration, in the class of Douglas Mawson, Robert Falcon Scott. Amundsen was born to a family of Norwegian shipowners and captains in Borge and his parents were Jens Amundsen and Hanna Sahlqvist. Roald was the son in the family. His mother wanted him to avoid the family trade and encouraged him to become a doctor. He promptly quit university for a life at sea, Amundsen had hidden a lifelong desire inspired by Fridtjof Nansens crossing of Greenland in 1888 and Franklins lost expedition. He decided on a life of exploration of wilderness places. Amundsen joined the Belgian Antarctic Expedition as first mate and this expedition, led by Adrien de Gerlache using the ship the RV Belgica, became the first expedition to winter in Antarctica. The Belgica, whether by mistake or design, became locked in the sea ice at 70°30′S off Alexander Island, the crew endured a winter for which they were poorly prepared. By Amundsens own estimation, the doctor for the expedition, the American Frederick Cook, probably saved the crew from scurvy by hunting for animals and feeding the crew fresh meat. In cases where citrus fruits are lacking, fresh meat from animals that make their own vitamin C contains enough of the vitamin to prevent scurvy and this was an important lesson for Amundsens future expeditions. In 1903, Amundsen led the first expedition to successfully traverse Canadas Northwest Passage between the Atlantic and Pacific oceans and he planned a small expedition of six men in a 45-ton fishing vessel, Gjøa, in order to have flexibility. His ship had relatively shallow draft and his technique was to use a small ship and hug the coast. Amundsen had the ship outfitted with a gasoline engine. They traveled via Baffin Bay, the Parry Channel and then south through Peel Sound, James Ross Strait, Simpson Strait and they spent two winters at King William Island in the harbor of what is today Gjoa Haven, Nunavut, Canada
5.
Sloop
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A sloop is a sailing boat with a single mast and a fore-and-aft rig. A sloop has only one head-sail, if a vessel has two or more head-sails, the cutter is used, and its mast may be set further aft than on a sloop. The most common rig of modern sailboats is the Bermuda-rigged sloop, typically, a modern sloop carries a mainsail on a boom aft of the mast, with a single loose-footed head-sail forward of the mast. Sloops are either masthead-rigged or fractional-rigged, on a masthead-rigged sloop, the forestay attaches at the top of the mast. The mainsail may be smaller than the headsail, which is called a genoa jib. On a fractional-rigged sloop, the forestay attaches to the mast at a point below the top, typically 3/4 of the way to top, or perhaps 7/8 or some other fraction. The mast of a fractional-rigged sloop may be placed forward, compared to a masthead-rigged sloop. After the cat rig, which has only a mainsail, the rig is one of the simpler sailing rig configurations. A sloop typically has two sails, a mainsail and a headsail, while the cutter has a mainsail and two or more headsails, next in complexity are the ketch, the yawl and the schooner, each of which has two masts and a minimum of three sails. A sloop has a system of mast rigging — a forestay. By having only two sails, the sails of a sloop are larger than those of an equivalent cutter. Until the advent of lightweight sailcloth and modern sail-handling systems, the sails of a sloop could be a handful. So, until the 1950s, sailboats over 10 metres Length Over All would typically use a rig or a two-mast rig. After the advent of modern winches and light sailcloth, the became the dominant sailing rig type for all. No rig type is perfect for all conditions, sloops, with their paucity of spars and control lines tend to impart less aerodynamic drag. Compared to other rigs, sloops tend to very well when sailing close hauled to windward. Cutters, ketches and yawls are often preferred to sloops when venturing far offshore, because it is easier to reef small sails as the wind increases, while still keeping the boat balanced. To maximize the amount of sail carried, the classic sloop may use a bowsprit, for downwind sailing, the typical foresail may be replaced by larger curved sails known as spinnakers or gennakers
6.
Rosendal, Norway
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Rosendal is the administrative centre of Kvinnherad municipality in Hordaland county, Norway. The village is known for the Barony Rosendal, a historic estate located in the village. Kvinnherad Church is also located in this village, the 1. 14-square-kilometre village has a population of 768, making it the third largest urban area in Kvinnherad. The village area has a density of 674 inhabitants per square kilometre. The economy of the village is centered on agriculture, ship building, the shipbuilder Skaalurens Skibsbyggeri was established in Rosendal in 1855
7.
Norway
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The Antarctic Peter I Island and the sub-Antarctic Bouvet Island are dependent territories and thus not considered part of the Kingdom. Norway also lays claim to a section of Antarctica known as Queen Maud Land, until 1814, the kingdom included the Faroe Islands, Greenland, and Iceland. It also included Isle of Man until 1266, Shetland and Orkney until 1468, Norway has a total area of 385,252 square kilometres and a population of 5,258,317. The country shares a long border with Sweden. Norway is bordered by Finland and Russia to the north-east, Norway has an extensive coastline, facing the North Atlantic Ocean and the Barents Sea. King Harald V of the Dano-German House of Glücksburg is the current King of Norway, erna Solberg became Prime Minister in 2013, replacing Jens Stoltenberg. A constitutional monarchy, Norway divides state power between the Parliament, the Cabinet and the Supreme Court, as determined by the 1814 Constitution, the kingdom is established as a merger of several petty kingdoms. By the traditional count from the year 872, the kingdom has existed continuously for 1,144 years, Norway has both administrative and political subdivisions on two levels, counties and municipalities. The Sámi people have an amount of self-determination and influence over traditional territories through the Sámi Parliament. Norway maintains close ties with the European Union and the United States, the country maintains a combination of market economy and a Nordic welfare model with universal health care and a comprehensive social security system. Norway has extensive reserves of petroleum, natural gas, minerals, lumber, seafood, the petroleum industry accounts for around a quarter of the countrys gross domestic product. On a per-capita basis, Norway is the worlds largest producer of oil, the country has the fourth-highest per capita income in the world on the World Bank and IMF lists. On the CIAs GDP per capita list which includes territories and some regions, from 2001 to 2006, and then again from 2009 to 2017, Norway had the highest Human Development Index ranking in the world. It also has the highest inequality-adjusted ranking, Norway ranks first on the World Happiness Report, the OECD Better Life Index, the Index of Public Integrity and the Democracy Index. Norway has two names, Noreg in Nynorsk and Norge in Bokmål. The name Norway comes from the Old English word Norðrveg mentioned in 880, meaning way or way leading to the north. In contrasting with suðrvegar southern way for Germany, and austrvegr eastern way for the Baltic, the Anglo-Saxon of Britain also referred to the kingdom of Norway in 880 as Norðmanna land. This was the area of Harald Fairhair, the first king of Norway, and because of him
8.
Old Norse
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Old Norse was a North Germanic language that was spoken by inhabitants of Scandinavia and inhabitants of their overseas settlements during about the 9th to 13th centuries. These dates, however, are not absolute, since written Old Norse is found well into the 15th century, Old Norse was divided into three dialects, Old West Norse, Old East Norse and Old Gutnish. Old West and East Norse formed a continuum, with no clear geographical boundary between them. For example, Old East Norse traits were found in eastern Norway, although Old Norwegian is classified as Old West Norse, most speakers spoke Old East Norse in what is present day Denmark and Sweden. Old Gutnish, the more obscure dialectal branch, is included in the Old East Norse dialect due to geographical associations. It developed its own features and shared in changes to both other branches. The 12th century Icelandic Gray Goose Laws state that Swedes, Norwegians, Icelanders and Danes spoke the same language, another term used, used especially commonly with reference to West Norse, was norrœnt mál. In some instances the term Old Norse refers specifically to Old West Norse, the Old East Norse dialect was spoken in Denmark, Sweden, settlements in Kievan Rus, eastern England, and Danish settlements in Normandy. The Old Gutnish dialect was spoken in Gotland and in settlements in the East. In the 11th century, Old Norse was the most widely spoken European language, in Kievan Rus, it survived the longest in Veliky Novgorod, probably lasting into the 13th century there. Norwegian is descended from Old West Norse, but over the centuries it has heavily influenced by East Norse. Old Norse also had an influence on English dialects and Lowland Scots and it also influenced the development of the Norman language, and through it and to a smaller extent, that of modern French. Various other languages, which are not closely related, have heavily influenced by Norse, particularly the Norman dialects, Scottish Gaelic. The current Finnish and Estonian words for Sweden are Ruotsi and Rootsi, of the modern languages, Icelandic is the closest to Old Norse. Written modern Icelandic derives from the Old Norse phonemic writing system, contemporary Icelandic-speakers can read Old Norse, which varies slightly in spelling as well as semantics and word order. However, pronunciation, particularly of the phonemes, has changed at least as much as in the other North Germanic languages. Faroese retains many similarities but is influenced by Danish, Norwegian, although Swedish, Danish and the Norwegian languages have diverged the most, they still retain asymmetric mutual intelligibility. Speakers of modern Swedish, Norwegian and Danish can mostly understand each other without studying their neighboring languages, the languages are also sufficiently similar in writing that they can mostly be understood across borders
9.
Herring
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Herring are forage fish, mostly belonging to the family Clupeidae. Herring often move in schools around fishing banks and near the coast. Three species of Clupea are recognised, and provide about 90% of all captured in fisheries. Most abundant of all is the Atlantic herring, providing half of all herring capture. Fishes called herring are found in India, in the Arabian Sea, Indian Ocean. Herring played a role in the history of marine fisheries in Europe. These oily fish also have a history as an important food fish. A number of different species, most belonging to the family Clupeidae, are referred to as herrings. The origins of the herring is somewhat unclear, though it may derive from the Old High German heri meaning a host, multitude. The type genus of the herring family Clupeidae is Clupea, Clupea contains three species, the Atlantic herring found in the north Atlantic, the Pacific herring found in the north Pacific, and the Araucanian herring found off the coast of Chile. Subspecific divisions have been suggested for both the Atlantic and Pacific herrings, but their biological basis remain unclear, in addition, a number of related species, all in the family Clupeidae, are commonly referred to as herrings. The table immediately below includes those members of the Clupeidae family referred to by FishBase as herrings which have been assessed by the International Union for Conservation of Nature. There are also a number of other species called herrings, which may be related to clupeids or just share some characteristics of herrings. Just which of these species are called herrings can vary with locality, some examples, The species of Clupea belong to the larger family Clupeidae, which comprises some 200 species that share similar features. These silvery-coloured fish have a dorsal fin, which is soft. They have no lateral line and have a lower jaw. At least one stock of Atlantic herring spawns in every month of the year, each spawns at a different time and place. Greenland populations spawn in 0–5 metres of water while North Sea herrings spawn at up to 200 metres in autumn
10.
Ullensvang
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Ullensvang is a municipality in Hordaland county, Norway. It is located in the district of Hardanger. The administrative centre is the village of Kinsarvik, other villages in the municipality include Lofthus, Utne, Vikebygd, and Alsåker. There are 3,369 inhabitants as of 1 January 2014, the number of inhabitants has shown a decrease of almost 700 people since 1980. This development can be seen in light of the depopulation of rural Norway. The main inhabited part of Ullensvang municipality lies just to the west of Hardangervidda National Park, most inhabitants live in the narrow coastal mountainsides and valleys along the Hardangerfjorden and Sørfjorden. The largest urban areas in Ullensvang are Kinsarvik and Lofthus, the Norwegian National Road 13 is one of the main roads through the municipality, and it crosses the Hardangerfjorden via the Hardanger Bridge in the far northern part of the municipality. In 2016 the chief of police formally suggested that the station in Ullensvang og Eidsfjord be closed down. The municipality is named after the old Ullensvang farm, since Ullensvang Church was built there, the first element is the genitive case of the name of the Norse god Ullin. The last element is vangr which means field or meadow, the coat-of-arms was granted on 8 November 1979. The arms are red with a gold stripe across the middle. The municipal arms are derived from the arms of nobleman from the area, Sigurd Brynjulvsson Galte, as it is the oldest gravestone in the church, the arms were well known in the village, hence the choice for the arms of this knight as municipal arms. The Church of Norway has three parishes within the municipality of Ullensvang and it is part of the Hardanger og Voss deanery in the Diocese of Bjørgvin. On 1 January 1838, the parish of Kinsarvik was established as a municipality. The large parish was made up of the parish and the annex of Ullensvang. On 1 January 1869, Ullensvang became the parish and Kinsarvik became an annex to Ullensvang. At this time the municipality changed its name to Ullensvang, on 1 January 1882, a small area of Ullensvang was transferred to the neighboring municipality of Vikør. This left Ullensvang with 1,941 residents, on 1 January 1964, a major municipal merger took place as a result of the recommendations by the Schei Committee
11.
Arctic Ocean
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The Arctic Ocean is the smallest and shallowest of the worlds five major oceans. Alternatively, the Arctic Ocean can be seen as the northernmost part of the all-encompassing World Ocean, located mostly in the Arctic north polar region in the middle of the Northern Hemisphere, the Arctic Ocean is almost completely surrounded by Eurasia and North America. It is partly covered by sea ice throughout the year and almost completely in winter, the summer shrinking of the ice has been quoted at 50%. The US National Snow and Ice Data Center uses satellite data to provide a record of Arctic sea ice cover. The Arctic may become ice free for the first time in human history within a few years or by 2040, for much of European history, the north polar regions remained largely unexplored and their geography conjectural. He was probably describing loose sea ice known today as growlers or bergy bits, his Thule was probably Norway, early cartographers were unsure whether to draw the region around the North Pole as land or water. The makers of navigational charts, more conservative than some of the more fanciful cartographers, tended to leave the region blank and this lack of knowledge of what lay north of the shifting barrier of ice gave rise to a number of conjectures. In England and other European nations, the myth of an Open Polar Sea was persistent, john Barrow, longtime Second Secretary of the British Admiralty, promoted exploration of the region from 1818 to 1845 in search of this. In the United States in the 1850s and 1860s, the explorers Elisha Kane, even quite late in the century, the eminent authority Matthew Fontaine Maury included a description of the Open Polar Sea in his textbook The Physical Geography of the Sea. Nevertheless, as all the explorers who travelled closer and closer to the reported, the polar ice cap is quite thick. Fridtjof Nansen was the first to make a crossing of the Arctic Ocean. The first surface crossing of the ocean was led by Wally Herbert in 1969, in a dog sled expedition from Alaska to Svalbard, with air support. The first nautical transit of the pole was made in 1958 by the submarine USS Nautilus. Since 1937, Soviet and Russian manned drifting ice stations have extensively monitored the Arctic Ocean, scientific settlements were established on the drift ice and carried thousands of kilometres by ice floes. In World War II, the European region of the Arctic Ocean was heavily contested, the Arctic Ocean occupies a roughly circular basin and covers an area of about 14,056,000 km2, almost the size of Antarctica. The coastline is 45,390 km long and it is surrounded by the land masses of Eurasia, North America, Greenland, and by several islands. It is connected to the Pacific Ocean by the Bering Strait and to the Atlantic Ocean through the Greenland Sea, countries bordering the Arctic Ocean are, Russia, Norway, Iceland, Greenland, Canada and the United States. There are several ports and harbours around the Arctic Ocean In Alaska, in Canada, ships may anchor at Churchill in Manitoba, Nanisivik in Nunavut, Tuktoyaktuk or Inuvik in the Northwest territories
12.
John Franklin
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Rear-Admiral Sir John Franklin KCH FRGS RN was an English Royal Navy officer and explorer of the Arctic. Franklin also served as Lieutenant-Governor of Van Diemens Land from 1837 to 1843 and he disappeared on his last expedition, attempting to chart and navigate a section of the Northwest Passage in the Canadian Arctic. The icebound ships were abandoned and the crew perished from starvation, hypothermia, tuberculosis, lead poisoning. Franklin was born in Spilsby, Lincolnshire, in 1786 and educated at King Edward VI Grammar School and he was the ninth of twelve children born to Hannah Weekes and Willingham Franklin, the descendant of a long line of country gentlemen. One of Johns sisters, Sarah, was the mother of Emily Tennyson and his father initially opposed Franklins interest in a career at sea and reluctantly allowed him to go on a trial voyage with a merchant ship. This confirmed his decision, so when he was 14, his father secured him a Royal Navy appointment on HMS Polyphemus. He also accompanied Captain Dance on the East India Companys ship the Earl Camden, in 1819, Franklin was chosen to lead an expedition overland from Hudson Bay to chart the north coast of Canada eastwards from the mouth of the Coppermine River. On his 1819 expedition, Franklin fell into the Hayes River at Robinson Falls and was rescued by a member of his expedition about 90 metres downstream, between 1819 and 1822, he lost 11 of the 20 men in his party. Most died of starvation, but there were also at least one murder, the survivors were forced to eat lichen and even attempted to eat their own leather boots. This gained Franklin the nickname of the man who ate his boots, in 1823, after returning to England, Sir John Franklin married the poet Eleanor Anne Porden. Their daughter, Eleanor Isabella, was born the following year, Eleanor died of tuberculosis in 1825. In 1825 he left for his second Canadian and third Arctic expedition, with him was John Richardson who would follow the coast east from the Mackenzie to the mouth of the Coppermine River. At the same time, William Edward Parry would try to sail west from the Atlantic, supplies were better organized this time, in part because they were managed by Peter Warren Dease of the Hudsons Bay Company. He erected a flagpole with buried letters for Parry and he returned to winter at Fort Franklin on the Great Bear Lake. Next summer he went downriver and found the ocean frozen and he worked his way west for several hundred miles and gave up on 16 August 1826 at Return Reef when he was about 150 miles east of Beecheys Point Barrow. He reached safety at Fort Franklin on 21 September and he left Fort Franklin on 20 February 1827 and spent the rest of the winter and spring at Fort Chipewyan, Alberta. He reached Liverpool on the first of September 1827, richardsons eastward journey was more successful. On 5 November 1828, he married Jane Griffin, a friend of his first wife, on 29 April 1829, he was knighted by George IV and the same year awarded the first Gold Medal of the Société de Géographie of France
13.
Arctic
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The Arctic is a polar region located at the northernmost part of Earth. The Arctic consists of the Arctic Ocean, adjacent seas, and parts of Alaska, Canada, Finland, Greenland, Iceland, Norway, Russia, land within the Arctic region has seasonally varying snow and ice cover, with predominantly treeless permafrost-containing tundra. Arctic seas contain seasonal sea ice in many places, the Arctic region is a unique area among Earths ecosystems. For example, the cultures in the region and the Arctic indigenous peoples have adapted to its cold, in recent years, Arctic sea ice decline has been caused by global warming. Life in the Arctic includes organisms living in the ice, zooplankton and phytoplankton, fish and marine mammals, birds, land animals, plants, Arctic land is bordered by the subarctic. The word Arctic comes from the Greek word ἀρκτικός, near the Bear, northern, there are a number of definitions of what area is contained within the Arctic. The area can be defined as north of the Arctic Circle, the southern limit of the midnight sun. The Arctics climate is characterized by cold winters and cool summers and its precipitation mostly comes in the form of snow and is low, with most of the area receiving less than 50 cm. High winds often stir up snow, creating the illusion of continuous snowfall, average winter temperatures can be as low as −40 °C, and the coldest recorded temperature is approximately −68 °C. Coastal Arctic climates are moderated by oceanic influences, having generally warmer temperatures, the Arctic is affected by current global warming, leading to Arctic sea ice shrinkage, diminished ice in the Greenland ice sheet, and Arctic methane release as the permafrost thaws. Due to the migration of the planets isotherms, the Arctic region is currently shrinking. Perhaps the most spectacular result of Arctic shrinkage is sea ice loss, there is a large variance in predictions of Arctic sea ice loss, with models showing near-complete to complete loss in September from 2040 to some time well beyond 2100. About half of the models show near-complete to complete sea ice loss in September by the year 2100. Arctic life is characterized by adaptation to short growing seasons with long periods of sunlight, Arctic vegetation is composed of plants such as dwarf shrubs, graminoids, herbs, lichens and mosses, which all grow relatively close to the ground, forming tundra. As one moves northward, the amount of available for plant growth decreases considerably. Colder summer temperatures cause the size, abundance, productivity and variety of plants to decrease, trees cannot grow in the Arctic, but in its warmest parts, shrubs are common and can reach 2 m in height, sedges, mosses and lichens can form thick layers. In the coldest parts of the Arctic, much of the ground is bare, non-vascular plants such as lichens and mosses predominate, along with a few scattered grasses, herbivores on the tundra include the Arctic hare, lemming, muskox, and caribou. They are preyed on by the owl, Arctic fox, Grizzly bear
14.
Barents Sea
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The Barents Sea is a marginal sea of the Arctic Ocean, located off the northern coasts of Norway and Russia divided between Norwegian and Russian territorial waters. Known among Russians in the Middle Ages as the Murman Sea and it is a rather shallow shelf sea, with an average depth of 230 metres, and is an important site for both fishing and hydrocarbon exploration. Novaya Zemlya, an extension of the part of the Ural Mountains. The southern half of the Barents Sea, including the ports of Murmansk, in September, the entire Barents Sea is more or less completely ice-free. Until the Winter War, Finlands territory also reached to the Barents Sea, with the harbor at Petsamo being Finlands only ice-free winter harbor. There are three types of water masses in the Barents Sea, Warm, salty Atlantic water from the North Atlantic drift, cold Arctic water from the north, and warm. Between the Atlantic and Polar waters, a front called the Polar Front is formed, the lands of Novaya Zemlya attained most of their early Holocene coastal deglaciation approximately 10,000 years before present. The International Hydrographic Organization defines the limits of the Barentsz Sea as follows, On the west, on the northwest, The eastern shore of West Spitzbergen, Hinlopen Strait up to 80° latitude north, south and east coasts of North-East Land to Cape Leigh Smith. On the north, Cape Leigh Smith across the Islands Bolshoy Ostrov, Gilles and Victoria, on the east, Cape Kohlsaat to Cape Zhelaniya, west and southwest coast of Novaya Zemlya to Cape Kussov Noss and thence to western entrance Cape, Dolgaya Bay on Vaigach Island. Through Vaigach Island to Cape Greben, thence to Cape Belyi Noss on the mainland, on the south, The northern limit of the White Sea. Other islands in the Barents Sea include Chaichy and Timanets, most of its geological history is dominated by extensional tectonics, caused by the collapse of the Caledonian and Uralian orogenic belts and the break-up of Pangaea. These events created the rift basins that dominate the Barents Shelf, along with various platforms. Due to the North Atlantic drift, the Barents Sea has a high biological production compared to other oceans of similar latitude. The spring bloom of phytoplankton can start quite early close to the ice edge, the phytoplankton bloom feeds zooplankton such as Calanus finmarchicus, Calanus glacialis, Calanus hyperboreus, Oithona spp. and krill. The zooplankton feeders include young cod, capelin, polar cod, whales, the capelin is a key food for top predators such as the north-east Arctic cod, harp seals, and seabirds such as common guillemot and Brunnichs guillemot. The fisheries of the Barents Sea, in particular the cod fisheries, are of importance for both Norway and Russia. There is a genetically distinct polar bear population associated with the Barents Sea and its eastern corner, in the region of the Pechora Rivers estuary, has been known as Pechorskoye Morye, that is, Pechora Sea. This sea was given its present name in honor of Willem Barentsz, Barentsz was the leader of early expeditions to the far north, at the end of the sixteenth century
15.
Horsepower
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Horsepower is a unit of measurement of power. There are many different standards and types of horsepower, two common definitions being used today are the mechanical horsepower, which is approximately 746 watts, and the metric horsepower, which is approximately 735.5 watts. The term was adopted in the late 18th century by Scottish engineer James Watt to compare the output of engines with the power of draft horses. It was later expanded to include the power of other types of piston engines, as well as turbines, electric motors. The definition of the unit varied among geographical regions, most countries now use the SI unit watt for measurement of power. With the implementation of the EU Directive 80/181/EEC on January 1,2010, units called horsepower have differing definitions, The mechanical horsepower, also known as imperial horsepower equals approximately 745.7 watts. It was defined originally as exactly 550 foot-pounds per second [745.7 N. m/s), the metric horsepower equals approximately 735.5 watts. It was defined originally as 75 kgf-m per second is approximately equivalent to 735.5 watts, the Pferdestärke PS is a name for a group of similar power measurements used in Germany around the end of the 19th century, all of about one metric horsepower in size. The boiler horsepower equals 9809.5 watts and it was used for rating steam boilers and is equivalent to 34.5 pounds of water evaporated per hour at 212 degrees Fahrenheit. One horsepower for rating electric motors is equal to 746 watts, one horsepower for rating Continental European electric motors is equal to 735 watts. Continental European electric motors used to have dual ratings, one British Royal Automobile Club horsepower can equal a range of values based on estimates of several engine dimensions. It is one of the tax horsepower systems adopted around Europe, the development of the steam engine provided a reason to compare the output of horses with that of the engines that could replace them. He had previously agreed to take royalties of one third of the savings in coal from the older Newcomen steam engines and this royalty scheme did not work with customers who did not have existing steam engines but used horses instead. Watt determined that a horse could turn a mill wheel 144 times in an hour, the wheel was 12 feet in radius, therefore, the horse travelled 2.4 × 2π ×12 feet in one minute. Watt judged that the horse could pull with a force of 180 pounds-force. So, P = W t = F d t =180 l b f ×2.4 ×2 π ×12 f t 1 m i n =32,572 f t ⋅ l b f m i n. Watt defined and calculated the horsepower as 32,572 ft·lbf/min, Watt determined that a pony could lift an average 220 lbf 100 ft per minute over a four-hour working shift. Watt then judged a horse was 50% more powerful than a pony, engineering in History recounts that John Smeaton initially estimated that a horse could produce 22,916 foot-pounds per minute
16.
Kerosene
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Kerosene, also known as paraffin, lamp oil and coal oil, is a combustible hydrocarbon liquid which is derived from petroleum, widely used as a fuel in industry as well as households. Its name derives from Greek, κηρός meaning wax, and was registered as a trademark by Abraham Gesner in 1854 before evolving into a genericized trademark and it is sometimes spelled kerosine in scientific and industrial usage. Liquid paraffin is a more viscous and highly refined product which is used as a laxative, paraffin wax is a waxy solid extracted from petroleum. Kerosene is widely used to power jet engines of aircraft and some rocket engines, in parts of Asia, where the price of kerosene is subsidized, it fuels outboard motors on small fishing boats. World total kerosene consumption for all purposes is equivalent to about 1.2 million barrels per day, to prevent confusion between kerosene and the much more flammable and volatile gasoline, some jurisdictions regulate markings or colorings for containers used to store or dispense kerosene. For example, in the United States, the Commonwealth of Pennsylvania requires that portable containers used at retail service stations be colored blue and it is miscible in petroleum solvents but immiscible in water. The American Society for Testing and Materials standard specification D-3699-78 recognizes two grades of kerosene, grades 1-K and 2-K, regardless of crude oil source or processing history, kerosenes major components are branched and straight chain alkanes and naphthenes, which normally account for at least 70% by volume. Aromatic hydrocarbons in this range, such as alkylbenzenes and alkylnaphthalenes. Olefins are usually not present at more than 5% by volume, the flash point of kerosene is between 37 and 65 °C, and its autoignition temperature is 220 °C. The pour point of kerosene depends on grade, with aviation fuel standardized at −47 °C. 1-K grade kerosene freezes around -40 °C, heat of combustion of kerosene is similar to that of diesel fuel, its lower heating value is 43.1 MJ/kg, and its higher heating value is 46.2 MJ/kg. In the United Kingdom, two grades of heating oil are defined, BS2869 Class C1 is the lightest grade used for lanterns, camping stoves, wick heaters, and mixed with gasoline in some vintage combustion engines as a substitute for tractor vaporising oil. BS2869 Class C2 is a heavier distillate, which is used as heating oil. Premium kerosene is sold in 5 or 20 liter containers from hardware, camping. Standard kerosene is usually dispensed in bulk by a tanker and is undyed, National and international standards define the properties of several grades of kerosene used for jet fuel. Flash point and freezing point properties are of particular interest for operation and safety, the process of distilling crude oil/petroleum into kerosene, as well as other hydrocarbon compounds, was first written about in the 9th century by the Persian scholar Rāzi. In his Kitab al-Asrar, the physician and chemist Razi described two methods for the production of kerosene, termed naft abyad, using an apparatus called an alembic, one method used clay as an absorbent, whereas the other method used ammonium chloride. The distillation process was repeated until all most of the volatile hydrocarbon fractions had been removed, Kerosene was also produced during the same period from oil shale and bitumen by heating the rock to extract the oil, which was then distilled
17.
Sail
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A sail derives power from the wind to provide motive power for sailing craft, including sailing ships, sailboats, windsurfers, ice boats, and sail-powered land vehicles. Sails mobilize lift and drag properties as air passes along the surface, in most cases sails are supported directly by a mast rigidly attached to the sailing craft or on a wire stay attached to the mast, however some craft employ a flexible mount for a mast. Sails also employ spars and battens to help determine their shape, as a result, sails come in a variety of shapes that include both triangular and quadrilateral configurations, usually with curved edges that promote three-dimensional curvature of the sail. Kites also power certain sailing craft, but do not employ a mast to support the airfoil and are beyond the scope of this article, sailing craft employ two types of rig, the square rig and the fore-and-aft rig. The square rig carries the primary driving sails are carried on horizontal spars and these spars are called yards and their tips, beyond the last stay, are called the yardarms. A ship mainly so rigged is called a square-rigger, the square rig is aerodynamically most efficient when running. A fore-and-aft rig consists of sails that are set along the line of the rather than perpendicular to it. Vessels so rigged are described as fore-and-aft rigged, archaeological studies of the Cucuteni-Trypillian culture ceramics show use of sailing boats from the sixth millennium onwards. Excavations of the Ubaid period in Mesopotamia provides direct evidence of sailing boats, Sails from ancient Egypt are depicted around 3200 BCE, where reed boats sailed upstream against the River Niles current. Ancient Sumerians used square rigged sailing boats at about the same time, the proto-Austronesian words for sail, lay, and other rigging parts date to about 3000 BCE when this group began their Pacific expansion. Greeks and Phoenicians began trading by ship by around 1,200 BCE, northern Europeans were resistant to adopting the fore-and-aft rig, despite having seen its use in the course of trade and during the Crusades. The lateen sail proved to have better performance for smaller vessels. Aerodynamic forces on sails depend on speed and direction and the speed. The direction that the craft is traveling with respect to the wind is called the point of sail. The speed of the craft at a point of sail contributes to the apparent wind —the wind speed. Depending on the alignment of the sail with the apparent wind, for apparent wind angles aligned with the entry point of the sail, the sail acts as an airfoil and lift is the predominant component of propulsion. For apparent wind angles behind the sail, lift diminishes and drag increases as the predominant component of propulsion, because of limitations on speed through the water, displacement sailboats generally derive power from sails generating lift on points of sail that include close-hauled through broad reach. Downwind sailing with a spinnaker Each rig is configured in a sail plan, a sail plan is a set of drawings, usually prepared by a naval architect which shows the various combinations of sail proposed for a sailing ship
18.
Sweden
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Sweden, officially the Kingdom of Sweden, is a Scandinavian country in Northern Europe. It borders Norway to the west and Finland to the east, at 450,295 square kilometres, Sweden is the third-largest country in the European Union by area, with a total population of 10.0 million. Sweden consequently has a low density of 22 inhabitants per square kilometre. Approximately 85% of the lives in urban areas. Germanic peoples have inhabited Sweden since prehistoric times, emerging into history as the Geats/Götar and Swedes/Svear, Southern Sweden is predominantly agricultural, while the north is heavily forested. Sweden is part of the area of Fennoscandia. The climate is in very mild for its northerly latitude due to significant maritime influence. Today, Sweden is a monarchy and parliamentary democracy, with a monarch as head of state. The capital city is Stockholm, which is also the most populous city in the country, legislative power is vested in the 349-member unicameral Riksdag. Executive power is exercised by the government chaired by the prime minister, Sweden is a unitary state, currently divided into 21 counties and 290 municipalities. Sweden emerged as an independent and unified country during the Middle Ages, in the 17th century, it expanded its territories to form the Swedish Empire, which became one of the great powers of Europe until the early 18th century. Swedish territories outside the Scandinavian Peninsula were gradually lost during the 18th and 19th centuries, the last war in which Sweden was directly involved was in 1814, when Norway was militarily forced into personal union. Since then, Sweden has been at peace, maintaining a policy of neutrality in foreign affairs. The union with Norway was peacefully dissolved in 1905, leading to Swedens current borders, though Sweden was formally neutral through both world wars, Sweden engaged in humanitarian efforts, such as taking in refugees from German-occupied Europe. After the end of the Cold War, Sweden joined the European Union on 1 January 1995 and it is also a member of the United Nations, the Nordic Council, Council of Europe, the World Trade Organization and the Organisation for Economic Co-operation and Development. Sweden maintains a Nordic social welfare system that provides health care. The modern name Sweden is derived through back-formation from Old English Swēoþēod and this word is derived from Sweon/Sweonas. The Swedish name Sverige literally means Realm of the Swedes, excluding the Geats in Götaland, the etymology of Swedes, and thus Sweden, is generally not agreed upon but may derive from Proto-Germanic Swihoniz meaning ones own, referring to ones own Germanic tribe
19.
Oscar II of Sweden
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Oscar II was King of Sweden from 1872 until his death and King of Norway from 1872 until his dethronement in 1905. He was the third of four sons of King Oscar I, as his eldest brother Charles XV was without heirs and his brother Prince Gustaf died in 1852, it was he who succeeded his brother as king. Oscar II was king during a period when Sweden was undergoing a period of industrialization, the declining Union of Sweden and Norway was finally dissolved in 1905 and Oscar became the last Bernadotte king of Norway. He died in 1907 and was succeed as King of Sweden by his son, at his birth in Stockholm, Oscar Fredrik was created Duke of Östergötland. He entered the navy at the age of eleven, and was appointed lieutenant in July 1845. Later he studied at Uppsala University, where he distinguished himself in mathematics, on 13 December 1848, he was made an honorary member of the Royal Swedish Academy of Sciences. On 6 June 1857 he married in Wiesbaden-Biebrich, Germany, Princess Sophia Wilhelmina, from 1859, when his father died, he was first in line to the Swedish throne after his oldest brother King Charles, who then had no male heirs. His middle brother Gustaf had died in 1852 and he succeeded his brother Charles XV / IV on 18 September 1872. At the accession he adopted as his motto Brödrafolkens väl / Broderfolkenes Vel, the political events which led up to the peaceful dissolution of the union between Norway and Sweden in 1905 could hardly have been attained but for the tact and patience of the king himself. He was dethroned on 7 June 1905 by the Norwegian Parliament and he declined, indeed, to permit any prince of his house to become king of Norway, but better relations between the two countries were restored before his death. He died in Stockholm on 8 December 1907 at 9,10 AM and his acute intelligence and his aloofness from the dynastic considerations affecting most European sovereigns gave the king considerable weight as an arbitrator in international questions. At the request of Great Britain, Germany and the United States in 1889 he appointed the justice of Samoa. He was the 1, 027th Knight of the Order of the Golden Fleece in Spain, the office of prime minister was instituted in 1876. Louis De Geer became the first head of government in Sweden to use this title, the most known and powerful first minister of the Crown during the reign of Oscar was the conservative estate owner Erik Gustaf Boström. Boström served as Prime Minister in 1891-1900 and 1902-1905 and he was trusted and respected by the king, who had much difficulty approving someone else as prime minister. Over a period of time, the king gave Boström a free hand to select his own ministers without much royal involvement and it was an arrangement that furthered the road to parliamentarism. Himself a distinguished writer and musical amateur, King Oscar proved a friend of learning. In 1858 a collection of his lyrical and narrative poems, Memorials of the Swedish Fleet, published anonymously, obtained the second prize of the Swedish Academy
20.
Denmark
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The term Danish Realm refers to the relationship between Denmark proper, the Faroe Islands and Greenland—three countries constituting the Kingdom of Denmark. The legal nature of the Kingdom of Denmark is fundamentally one of a sovereign state. The Faroe Islands and Greenland have been part of the Crown of Denmark since 1397 when the Kalmar Union was ratified, legal matters in The Danish Realm are subject to the Danish Constitution. Beginning in 1953, state law issues within The Danish Realm has been governed by The Unity of the Realm, a less formal name for The Unity of the Realm is the Commonwealth of the Realm. In 1978, The Unity of The Realm was for the first time referred to as rigsfællesskabet. The name caught on and since the 1990s, both The Unity of The Realm and The Danish Realm itself has increasingly been referred to as simply rigsfællesskabet in daily parlance. The Danish Constitution stipulates that the foreign and security interests for all parts of the Danish Realm are the responsibility of the Danish government, the Faroes received home rule in 1948 and Greenland did so in 1979. In 2005, the Faroes received a self-government arrangement, and in 2009 Greenland received self rule, the Danish Realms unique state of internal affairs is acted out in the principle of The Unity of the Realm. This principle is derived from Article 1 of the Danish Constitution which specifies that constitutional law applies equally to all areas of the Danish Realm, the Constitutional Act specifies that sovereignty is to continue to be exclusively with the authorities of the Realm. The language of Denmark is Danish, and the Danish state authorities are based in Denmark, the Kingdom of Denmarks parliament, with its 179 members, is located in the capital, Copenhagen. Two of the members are elected in each of Greenland and the Faroe Islands. The Government ministries are located in Copenhagen, as is the highest court, in principle, the Danish Realm constitutes a unified sovereign state, with equal status between its constituent parts. Devolution differs from federalism in that the powers of the subnational authority ultimately reside in central government. The Self-Government Arrangements devolves political competence and responsibility from the Danish political authorities to the Faroese, the Faroese and Greenlandic authorities administer the tasks taken over from the state, enact legislation in these specific fields and have the economic responsibility for solving these tasks. The Danish government provides a grant to the Faroese and the Greenlandic authorities to cover the costs of these devolved areas. The 1948 Home Rule Act of the Faroe Islands sets out the terms of Faroese home rule, the Act states. the Faroe Islands shall constitute a self-governing community within the State of Denmark. It establishes the government of the Faroe Islands and the Faroese parliament. The Faroe Islands were previously administered as a Danish county, the Home Rule Act abolished the post of Amtmand and these powers were expanded in a 2005 Act, which named the Faroese home government as an equal partner with the Danish government
21.
Helmer Hanssen
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Helmer Julius Hanssen was a Norwegian polar explorer, and one of the first five to reach the South Pole on the expedition of Roald Amundsen. Helmer Hanssen was born in Bjørnskinn, on the island of Andøya in the part of Norway. He was an experienced ice pilot, a skill he had learned while hunting seals around Spitsbergen, from 1903 to 1905 Helmer Hanssen participated in Roald Amundsens successful search for the Northwest Passage, as second mate on board the ship Gjøa. On the expedition he learned from the Inuit how to drive sled dogs, in 1910 he headed south with Amundsen to conquer the South Pole. This time as a dog driver. He was also in charge of navigation, carrying the master compass on his sledge and he was one of the first five people to reach the South Pole on 14 December 1911, along with Roald Amundsen, Olav Bjaaland, Oscar Wisting, and Sverre Hassel. During their stay at the South Pole, it is believed that Hanssen passed within 200 yards of the mathematical South Pole point. This was during one of his ski runs which Amundsen had ordered be performed to completely encircle or box the pole to ensure there was no doubt that the expedition had attained the pole. In 1919 he once again went north this time as captain on Maud in Roald Amundsens Northeast Passage expedition, in 1936 Hanssen published his autobiography The Voyages of a Modern Viking, London, Rutledge,1936. Helmer Julius Hanssen was awarded the Knight of St. Olav for exceptional seamanship on Roald Amundsens expeditions in the northern and southern parts of the world
22.
Royal Norwegian Navy
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The Royal Norwegian Navy is the branch of the Norwegian Armed Forces responsible for naval operations of the state of Norway. The navy also includes the Coast Guard, the Royal Norwegian Navy has a history dating back to 955. From 1509 to 1814, it formed part of the navy of Denmark-Norway, since 1814, the Royal Norwegian Navy has again existed as a separate navy. In Norwegian, Royal Norwegian Navy vessels have since 1946 been given the ship prefix KNM, in English, they are given the prefix HNoMS, short for His/Her Norwegian Majestys Ship. Coast Guard vessels are given the prefix KV for KystVakt in Norwegian, during the last part of the Middle Ages the system of levying of ships, equipment and manpower for the leidang was mainly used to levying tax and existed as such into the 1700th Century. During most of the union between Norway and Denmark the two countries had a common fleet and this fleet was established by King Hans in 1509 in Denmark. A large proportion of the crew and officers in this new Navy organisation were Norwegian, in 1709 there were about 15,000 personnel enrolled in the common fleet, of these 10,000 were Norwegian. When Tordenskjold carried out his famous raid at Dynekil in 1716 more than 80 percent of the sailors and 90 percent of the soldiers in his force were Norwegian, because of this the Royal Norwegian Navy shares its history from 1509 to 1814 with the Royal Danish Navy. The modern, separate Royal Norwegian Navy was founded on April 12,1814 by Prince Christian Fredrik on the remnants of the Dano-Norwegian Navy, at the time of separation, the Royal Dano-Norwegian Navy was in a poor state and Norway was left with the lesser share. All officers of Danish birth were ordered to return to Denmark and it then consisted of 39 officers, seven brigs, one schooner-brig, eight gun schooners,46 gun chalups and 51 gun barges. April 1,1815 the RNoNs leadership was reorganized into a navy ministry, Norway retained its independent armed forces, including the navy, during the union with Sweden. During most of the union the navy was subjected to low funding, in the late 19th century, the fleet was increased to defend a possible independent Norway from her Swedish neighbours. These were operated by 116 active duty officers and 700 petty officers, Norway was neutral during World War I, but the armed forces were mobilised to protect Norways neutrality. The neutrality was sorely tested – the nations merchant fleet suffered casualties to German U-Boats. World War II began for the Royal Norwegian Navy on April 8,1940, the artillery pieces inflicted heavy damage on the German heavy cruiser Blücher, which was subsequently sunk by torpedoes fired from Oscarsborgs land based torpedo battery. Blücher sank with over 1,000 casualties among its crew, the German invasion fleet – believing Blücher had struck a mine – retreated south and called for air strikes on the fortress. This delay allowed King Haakon VII of Norway and the Royal family, as well as the government, to escape captivity. On June 7,1940, thirteen vessels, five aircraft and 500 men from the Royal Norwegian Navy followed the King to the United Kingdom, the number of men was steadily increased as Norwegians living abroad, civilian sailors and men escaping from Norway joined the RNoN
23.
Oslofjord
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The Oslofjord is an inlet in the south-east of Norway, stretching from an imaginary line between the Torbjørnskjær and Færder lighthouses and down to Langesund in the south to Oslo in the north. It is part of the Skagerrak strait, connecting the North Sea and the Kattegat sea area, the Oslofjord is not a fjord in the geological sense - in Norwegian the term fjord can refer to a wide range of waterways. The bay is divided into the inner and outer Oslofjord at the point of the 17 by 1 kilometre Drøbak Sound, in the period 1624-1925 the name of the fjord was Kristianiafjorden - since this was the name of the capital in this period. The old Norse name of the fjord was Fold, giving names to the counties of Vestfold and Østfold -, each of the islands in the innermost part of the fjord has its own identity and distinguishing history. Among them are Hovedøya, Lindøya, Nakholmen, Bleikøya, Gressholmen and these islands can be reached with the Oslo-boats from Vippetangen. Hovedøya contains monastery ruins, Gressholmen for its rabbits, Nakholmen, Bleikøya, Lindøya for their cabins at the water’s edge. The inner part of the Oslofjord has steep and forest covered hill slopes down towards the fjord, the Oslofjord has Norway’s highest all year temperature,7.5 degrees Celsius. February is the coldest month in the fjord with -1.3 degrees Celsius, the islands in the middle of the fjord are among Norway’s warmest with high summer temperatures and moderate winters. Oslofjord’s relatively high temperatures enable various flora to flourish, the oldest settlements in the area surrounding the Oslofjord date from the Stone Age and the Bronze Age. It was here on the eastern and western shores that three of the best preserved Viking ships were unearthed, in historical times, this bay was known by the current name of the region, Viken. Oslofjord has been an important body of water due to its proximity to Oslo. During WWII, there were German installations at several points on its coastline, one installation in Hovedøya held 1,100 Wehrmacht soldiers and later women deemed Nazi collaborators at the National Internment Camp for Women in Hovedøya. Norwegian painter Edvard Munch had a cottage and studio in Åsgårdstrand on the fjord, the fjord was the scene of a key event in the German invasion of Norway in April 1940, the Battle of Drøbak Sound. The invasion included a landing of 1,000 troops transported by ship to Oslo. Colonel Eriksen, Commander of the Oscarsborg fortress near Drøbak, mainly maintained for historical purposes, the fortresss resistance blocked the route to Oslo, thus delaying the rest of the group long enough for the royal family, government, parliament, and national treasury to be evacuated. The entire population situated around the Oslofjord including Oslo is about 1.96 million, more than 40% of Norway’s population resides under 45 minutes of driving from the Oslofjord. The Oslofjord has Norway’s busiest traffic of ferries and cargo boats, even though the Oslofjord contains hundreds of populated islands, most of the population of the fjord resides on the mainland. In the summer there are boats of all sizes on the fjord, and it is possible to go kayaking, canoeing, fishing, the Oslofjord is one of the nine venues of the Class 1 World Powerboat Championship
24.
Labrador Sea
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The Labrador Sea is an arm of the North Atlantic Ocean between the Labrador Peninsula and Greenland. The sea is flanked by continental shelves to the southwest, northwest and it connects to the north with Baffin Bay through the Davis Strait. It has been described as a sea of the Atlantic. The sea formed upon separation of the North American Plate and Greenland Plate that started about 60 million years ago, the Labrador Sea formed upon separation of the North American Plate and Greenland Plate that started about 60 million years ago and stopped about 40 million years ago. A sedimentary basin, which is now buried under the continental shelves, onset of magmatic sea-floor spreading was accompanied by volcanic eruptions of picrites and basalts in the Paleocene at the Davis Strait and Baffin Bay. Between about 500 BC and 1300 AD, the southern coast of the sea contained Dorset, Beothuk and Inuit settlements, the International Hydrographic Organization defines the limits of the Labrador Sea as follows, On the North, the South limit of Davis Strait. On the East, a line from Cape St. Francis 47°45′N 52°27′W to Cape Farewell, thence a line joining this ledge with the East extreme of Cape St. Charles in Labrador. The Labrador Sea is about 3,400 m deep and 1,000 km wide where it joins the Atlantic Ocean and it becomes shallower, to less than 700 m towards Baffin Bay and passes into the 300 kilometres wide Davis Strait. A 100–200 m deep turbidity current channel system, which is about 2–5 km wide and 3,800 kilometres long, runs on the bottom of the sea and it is called the Northwest Atlantic Mid-Ocean Channel and is one of the worlds longest drainage systems of Pleistocene age. It appears as a river bed with numerous tributaries and is maintained by high-density turbidity currents flowing within the levees. The water temperature varies between −1 °C in winter and 5–6 °C in summer, the salinity is relatively low, at 31–34.9 parts per thousand. Two-thirds of the sea is covered in ice in winter, tides are semi-diurnal, reaching 4 m. There is a water circulation in the sea. It is initiated by the East Greenland Current and continued by the West Greenland Current, then, the Baffin Island Current and Labrador Current transport cold and less saline water southward along the Canadian coast. These currents carry numerous icebergs and therefore hinder navigation and exploration of the gas fields beneath the sea bed. The speed of the Labrador current is typically 0. 3–0.5 m/s, the Labrador Current maintains the water temperature at 0 °C and salinity between 30 and 34 parts per thousand. The NADW consists of three parts of different origin and salinity, and the top one, the Labrador Sea Water, is formed in the Labrador Sea. This part occurs at a depth and has a relatively low salinity, low temperature and high oxygen content compared to the layers above
25.
Greenland
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Greenland is an autonomous constituent country within the Danish Realm between the Arctic and Atlantic Oceans, east of the Canadian Arctic Archipelago. Though physiographically a part of the continent of North America, Greenland has been politically and culturally associated with Europe for more than a millennium. The majority of its residents are Inuit, whose ancestors began migrating from the Canadian mainland in the 13th century, Greenland is the worlds largest island. Three-quarters of Greenland is covered by the permanent ice sheet outside Antarctica. With a population of about 56,480, it is the least densely populated country in the world, the Arctic Umiaq Line ferry acts as a lifeline for western Greenland, connecting the various cities and settlements. Greenland has been inhabited off and on for at least the last 4,500 years by Arctic peoples whose forebears migrated there from what is now Canada, Norsemen settled the uninhabited southern part of Greenland beginning in the 10th century, and Inuit peoples arrived in the 13th century. The Norse colonies disappeared in the late 15th century, soon after their demise, beginning in 1499, the Portuguese briefly explored and claimed the island, naming it Terra do Lavrador. In the early 18th century, Scandinavian explorers reached Greenland again, to strengthen trading and power, Denmark-Norway affirmed sovereignty over the island. Greenland was settled by Vikings more than a thousand years ago, Vikings set sail from Greenland and Iceland, discovering North America nearly 500 years before Columbus reached Caribbean islands. Though under continuous influence of Norway and Norwegians, Greenland was not formally under the Norwegian crown until 1262, the Kingdom of Norway was extensive and a military power until the mid-14th century. Thus, the two kingdoms resources were directed at creating Copenhagen, Norway became the weaker part and lost sovereignty over Greenland in 1814 when the union was dissolved. Greenland became a Danish colony in 1814, and was made a part of the Danish Realm in 1953 under the Constitution of Denmark, in 1973, Greenland joined the European Economic Community with Denmark. However, in a referendum in 1982, a majority of the population voted for Greenland to withdraw from the EEC which was effected in 1985, Greenland contains the worlds largest and most northernly national park, Northeast Greenland National Park. Greenland is divided into four municipalities - Sermersooq, Kujalleq, Qaasuitsup and it also retains control of monetary policy, providing an initial annual subsidy of DKK3.4 billion, which is planned to diminish gradually over time. Greenland expects to grow its economy based on increased income from the extraction of natural resources, the capital, Nuuk, held the 2016 Arctic Winter Games. At 70%, Greenland has one of the highest shares of renewable energy in the world, the early Viking settlers named the island as Greenland. In the Icelandic sagas, the Norwegian-born Icelander Erik the Red was said to be exiled from Iceland for manslaughter, along with his extended family and his thralls, he set out in ships to explore an icy land known to lie to the northwest. After finding an area and settling there, he named it Grœnland
26.
Baffin Bay
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Baffin Bay, located between Baffin Island and the southwest coast of Greenland, is a marginal sea of the North Atlantic Ocean. It is connected to the Atlantic via Davis Strait and the Labrador Sea, the narrower Nares Strait connects Baffin Bay with the Arctic Ocean. The bay is not navigable most of the year because of the ice cover and high density of floating ice, however, a polynya of about 80,000 km2, known as the North Water, opens in summer on the north near Smith Sound. Most of the life of the bay is concentrated near that region. The International Hydrographic Organization defines the limits of Baffin Bay as follows, a line from Cape Sheridan, Grant Land to Cape Bryant, Greenland. The parallel of 70° North between Greenland and Baffin Land, the Eastern limits of the North-West Passages. The area of the bay has been inhabited since c. 500 BC, around AD1200, the initial Dorset settlers were replaced by the Thule peoples. Recent excavations also suggest that the Norse colonization of the Americas reached the shores of Baffin Bay sometime between the 10th and 14th centuries, the English explorer John Davis was the first recorded European to enter the bay, arriving in 1585. In 1612, a group of English merchants formed the Company of Merchants of London and their governor Thomas Smythe organized five expeditions to explore the northern coasts of Canada in search of a maritime passage to the Far East. Henry Hudson and Thomas Buttons explored Hudson Bay, William Gibbons Labrador, and Robert Bylot Hudson Strait, aboard the Discovery, Baffin charted the area and named Lancaster, Smith, and Jones Sounds after members of his company. By the completion of his 1616 voyage, Baffin held out no hope of an ice-free passage, over time, his account came to be doubted until it was confirmed by John Rosss 1818 voyage. More advanced scientific studies followed in 1928, in the 1930s and after World War II by Danish, currently, there are a few Inuit settlements on the Canadian coast of the bay, including Arctic Bay, Pond Inlet and Clyde River. Those settlements are accessed and supplied by air and annual sealifts, in 1975, a town was built at Nanisivik to support lead and zinc production at the Nanisivik Mine—the first Canadian mine in the Arctic. The mine was closed in 2002 due to declining resources and metal prices, whereas the town still has a functional seaport and an airport, as of the 2006 census, it has an official population of zero. Baffin Bay was the epicenter of a 7.3 magnitude earthquake in 1933 and this is the largest known earthquake north of the Arctic Circle. It caused no damage because of its location and the small number of the nearby onshore communities. The northwestern part of the bay remains one of the most seismically active regions in eastern Canada, five earthquakes of magnitude 6 have occurred here since 1933. The latest strong earthquake occurred on 15 April 2010 and had the magnitude of 5.1, Baffin Bay is an arm of the Atlantic Ocean bounded by the Baffin Island in the west, Greenland in the east, and Ellesmere Island in the north
27.
Canadian Arctic Archipelago
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The Canadian Arctic Archipelago, also known as the Arctic Archipelago, is a group of islands north of the Canadian mainland. The Canadian Arctic Archipelago is showing some effects of global warming, British claims on the islands were based on the explorations in the 1570s by Martin Frobisher. Canadian sovereignty was only over island portions that drained into Foxe Basin, Hudson Bay. Canadian sovereignty over all of the islands was not established until the 1880 transfer by Britain to Canada of the remaining islands, the District of Franklin – established in 1895 – comprised almost all of the archipelago, the district was dissolved upon the creation of Nunavut in 1999. Canada claims all the waterways of the Northwestern Passages as Canadian Internal Waters, however the United States, disagreement over the passages status has raised Canadian concerns about environmental enforcement, national security, and general sovereignty. Hans Island, in the Nares Strait east of Ellesmere Island, is a territory contested between Canada and Denmark. The archipelago extends some 2,400 km longitudinally and 1,900 km from the mainland to Cape Columbia, the northernmost point on Ellesmere Island. It is bounded on the west by the Beaufort Sea, on the northwest by the Arctic Ocean, on the east by Greenland, Baffin Bay and Davis Strait, and on the south by Hudson Bay and the Canadian mainland. The various islands are separated from other and the continental mainland by a series of waterways collectively known as the Northwestern Passages. Two large peninsulas, Boothia and Melville, extend northward from the mainland, the archipelago consists of 36,563 islands, of which 94 are classified as major islands, being larger than 130 km2, and cover a total area of 1,400,000 km2. The climate of the islands is arctic, and the terrain consists of tundra except in mountainous areas, most of the islands are uninhabited, human settlement is extremely thin and scattered, being mainly coastal Inuit settlements on the southern islands. Islands not on map British Arctic Territories List of Canadian islands by area List of islands of Canada
28.
Boothia Peninsula
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Boothia Peninsula is a large peninsula in Nunavuts northern Canadian Arctic, south of Somerset Island. The northern part, Murchison Promontory, is the northernmost point of mainland Canada, Bellot Strait separates the peninsula from Somerset Island to the north. Babbage Bay is on the east coast, as is Abernethy Bay, the community of Taloyoak lies in the far south and is its only significant population centre. Paisley Bay is on the west coast, as is Wrottesley Inlet, john Ross was forced by ice to stop for four years at its easternmost point starting in 1829. He named it after his patron Sir Felix Booth, Ross encountered a large Inuit community whom he described as living in snow cottages and immortalized in Rosss painting North Hendon. In 1831 his nephew James Clark Ross went overland and reached the north pole which was then on its western side. He also crossed west to King William Island, both Roald Amundsens first successful traverse of the Northwest Passage and Henry Larsens second successful traverse of the Northwest Passage passed through the Bellot Strait. Larsen thought the strait too shallow for vessels, and described how his vessel was almost crushed by ice floes when there was a change in the winds direction. On his return voyage Larsen passed north of Somerset Island
29.
King William Island
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King William Island is an island in the Kitikmeot Region of Nunavut, which is part of the Canadian Arctic Archipelago. In area it is between 12,516 km2 and 13,111 km2 making it the 61st-largest island in the world and its population, as of the 2011 census, was 1,279, all of whom live in the islands only community, Gjoa Haven. The island is separated from the Boothia Peninsula by the James Ross Strait to the northeast, to the west is the Victoria Strait and beyond it Victoria Island. Within the Simpson Strait, to the south of the island, is Todd Island, queen Maud Gulf lies to the southwest. The island is known for its populations of caribou, which summer there before migrating in the autumn by walking south over the sea ice. While searching for the Northwest Passage, a number of explorers visited, or spent their winters on. The island was occupied by Inuit people, who had a culture adapted to the extreme environment. The British explorer John Ross named it King William Land for the reigning British King William IV in 1830, in 1834, George Back, another Arctic explorer, viewed its south shore from Chantry Inlet but failed to recognize it as an island. The Franklin Expedition likely recognized it as an island on their retreat to Backs River via Chantry Inlet. John Franklin, another British explorer, made an Arctic expedition about a decade later, after abandoning the two ships, most of the crew died from exposure and starvation as they attempted to walk south near the western coastline. Two of Franklins men were buried at Hall Point on the south coast. The ships were believed lost forever, as subsequent expeditions were unable to find them, on 9 September 2014, Canadas Prime Minister Stephen Harper announced that the Victoria Strait Expedition had located one of Franklins two ships beneath shallow waters south of King William Island. It is preserved in good condition, the side-scan sonar could detect the deck planking. By the beginning of October, the wreck had been identified as HMS Erebus, the other expedition vessel, HMS Terror, was found in 2016 in Terror Bay, off the south-west coast of King William Island. In 1903, Norwegian explorer Roald Amundsen, looking for the Northwest Passage, sailed through the James Ross Strait, unable to proceed due to sea ice, he spent the winters of 1903–1904 and 1904–1905 there. During his stays, he learned Arctic living skills from the local Netsilik Inuit and he used his ship Gjøa as a base for explorations in the summer of 1904, during which he traveled by dogsled on the Boothia Peninsula and to the North Magnetic Pole. After 22 months on the island, Amundsen left in August 1905, the harbour where he lived has the islands only settlement, Gjoa Haven. Amundsen used skills learned from the Inuit when he made his expedition to the South Pole
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North Magnetic Pole
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Magnetic declination or variation is the angle on the horizontal plane between magnetic north and true north. This angle varies depending on position on the Earths surface, and changes over time. The angle between magnetic and grid meridians is called grid magnetic angle, grid variation, or grivation. ”By convention, declination is positive when magnetic north is east of true north, and negative when it is to the west. Isogonic lines are lines on the Earths surface along which the declination has the constant value. The lowercase Greek letter δ is frequently used as the symbol for magnetic declination, Magnetic declination varies both from place to place and with the passage of time. As a traveller cruises the east coast of the United States, for example, the declination at London, UK is one degree 7 minutes west, and as the country is quite small that figure is fairly good for the whole of the country. It is reducing, and scientists predict that in about 2050 it will be zero, similarly, secular changes to these flows result in slow changes to the field strength and direction at the same point on the Earth. The magnetic declination in an area may change slowly over time, possibly as little as 2–2.5 degrees every hundred years or so. For a location closer to the pole like Ivujivik, the declination may change by 1 degree every three years and this may be insignificant to most travellers, but can be important if using magnetic bearings from old charts or metes in old deeds for locating places with any precision. As an example of how variation changes over time, see the two charts of the area, below, surveyed 124 years apart. The 1884 chart shows a variation of 8 degrees,20 minutes West, the 2008 chart shows 13 degrees,15 minutes West. The instrument used to perform this measurement is known as a declinometer, the approximate position of the north celestial pole is indicated by Polaris. In the northern hemisphere, declination can therefore be determined as the difference between the magnetic bearing and a visual bearing on Polaris. Polaris currently traces a circle 0. 75° in radius around the celestial pole. At high latitudes a plumb-bob is helpful to sight Polaris against an object close to the horizon. A rough estimate of the local declination can be determined from a general isogonic chart of the world or a continent, isogonic lines are also shown on aeronautical and nautical charts. Larger-scale local maps may indicate current local declination, often with the aid of a schematic diagram, unless the area depicted is very small, declination may vary measurably over the extent of the map, so the data may be referred to a specific location on the map. The current rate and direction of change may also be shown, the same diagram may show the angle of grid north, which may differ from true north
31.
Inuit
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Inuit are a group of culturally similar indigenous peoples inhabiting the Arctic regions of Greenland, Canada and Alaska. Inuit is a noun, the singular is Inuk. The Inuit languages are part of the Eskimo-Aleut family, Inuit Sign Language is a critically endangered language isolate spoken in Nunavut. In the United States and Canada, the term Eskimo was commonly used to describe the Inuit and Alaskas Yupik, however, Inuit is not accepted as a term for the Yupik, and Eskimo is the only term that includes Yupik, Iñupiat and Inuit. However, aboriginal peoples in Canada and Greenlandic Inuit view Eskimo as pejorative, in Canada, sections 25 and 35 of the Constitution Act of 1982 classified the Inuit as a distinctive group of Aboriginal Canadians who are not included under either the First Nations or the Métis. These areas are known in Inuktitut as the Inuit Nunangat, in the United States, the Iñupiat live primarily on the Alaska North Slope and on Little Diomede Island. The Greenlandic Inuit are descendants of migrations from Canada. In the 21st century they are citizens of Denmark, although not of the European Union, Inuit are the descendants of what anthropologists call the Thule culture, who emerged from western Alaska around 1000 CE. They had split from the related Aleut group about 4,000 years ago and from northeastern Siberian migrants, possibly related to the Chukchi language group and they spread eastwards across the Arctic. They displaced the related Dorset culture, the last major Paleo-Eskimo culture, Inuit legends speak of the Tuniit as giants, people who were taller and stronger than the Inuit. Less frequently, the legends refer to the Dorset as dwarfs, researchers believe that the Dorset culture lacked the dogs, larger weapons and other technologies of the Inuit society, which gave the latter an advantage. By 1300, Inuit migrants had reached west Greenland, where they settled, faced with population pressures from the Thule and other surrounding groups, such as the Algonquian and Siouan to the south, the Tuniit gradually receded. They were thought to have become extinct as a people by about 1400 or 1500. But, in the mid-1950s, researcher Henry B. Collins determined that, based on the ruins found at Native Point, the Sadlermiut population survived up until winter 1902–03, when exposure to new infectious diseases brought by contact with Europeans led to their extinction as a people. In the early 21st century, mitochondrial DNA research has supported the theory of continuity between the Tuniit and the Sadlermiut peoples and it also provided evidence that a population displacement did not occur within the Aleutian Islands between the Dorset and Thule transition. In contrast to other Tuniit populations, the Aleut and Sadlermiut benefited from both geographical isolation and their ability to adopt certain Thule technologies, in Canada and Greenland, Inuit circulated almost exclusively north of the Arctic tree line, the effective southern border of Inuit society. The most southern officially recognized Inuit community in the world is Rigolet in Nunatsiavut, south of Nunatsiavut, the descendants of the southern Labrador Inuit in NunatuKavut continued their traditional transhumant semi-nomadic way of life until the mid-1900s. The Nunatukavummuit people usually moved among islands and bays on a seasonal basis and they did not establish stationary communities
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Inuktitut
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For example, being educated in Inuktitut does not mean just using the language. An Inukitut education is not done in classrooms and from books written in their language, parents still teach their children in Inuktitut away from schools. Inuit generally consider their culture and language to be parts of a single whole. The language of Inuktitut is one of the principal Inuit languages of Canada and it is one of the aboriginal languages written with Canadian Aboriginal syllabics. It is recognised as a language in Nunavut alongside Inuinnaqtun. It also has some recognition in Nunatsiavut—the Inuit area in Labrador—following the ratification of its agreement with the government of Canada, the Canadian census reports that there are roughly 35,000 Inuktitut speakers in Canada, including roughly 200 who live regularly outside of traditionally Inuit lands. The term Inuktitut is often used broadly to include Inuvialuktun. For more information on the relationship between Inuktitut and the Inuit languages spoken in Greenland and Alaska, see Inuit languages, the word Inuktitut is often used to describe both. A more proper term has been adopted using Inuit Languages when speaking of Inuinnaqtun, the demographic situation of Inuktitut is quite strong in Nunavut. Nunavut is the home of some 24,000 Inuit, most of whom – over 80% according to the 2001 census – speak Inuktitut, including some 3,500 people reported as monolinguals. 2001 census data shows that the use of Inuktitut, while lower among the young than the elderly, has stopped declining in Canada as a whole, the South Baffin dialect is spoken across the southern part of Baffin Island, including the territorial capital Iqaluit. This has in recent years made it a more widely heard dialect. Some linguists also distinguish an East Baffin dialect from either South Baffin or North Baffin, Quebec is home to roughly 12,000 Inuit, nearly all of whom live in Nunavik. According to the 2001 census, 90% of Quebec Inuit speak Inuktitut, the Nunavik dialect is relatively close to the South Baffin dialect, but not identical. In the Nunavik dialect, Inuktitut is called Inuttitut and this dialect is also sometimes called Tarramiutut or Taqramiutut. Subdialects of Inuktitut in this region include Tarrarmiut and Itivimuit, Itivimuit is associated with Inukjuak, Quebec, and there is a Itivimuit River near the town. The Nunatsiavut dialect was spoken across northern Labrador. It has a writing system, created by German missionaries from the Moravian Church in Greenland in the 1760s
33.
Gjoa Haven
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Gjoa Haven is a hamlet in Nunavut, above the Arctic Circle, located in the Kitikmeot Region,1,056 km northeast of Yellowknife, Northwest Territories. It is the settlement on King William Island. The name Gjoa Haven is from the Norwegian Gjøahavn or Gjøas Harbour and this was derived from the old Norse name Gyða, a compressed compound form of Guðfríðr. In 1903, the Norwegian explorer Roald Amundsen had entered the area on his ship Gjøa in an expedition intending to travel through the Northwest Passage, by October the straits through which he was travelling began to ice up. Amundsen put Gjøa into a harbour on the southeast coast of King William Island. He stayed there, in what Amundsen called the finest little harbor in the world and he and his crew spent much of that time with the local Netsilik Inuit, learning from them the skills to live off the land and travel efficiently in the Arctic environment. This knowledge proved to be vital for Amundsens later successful exploration to the South Pole and he explored the Boothia Peninsula, searching for the exact location of the North Magnetic Pole. Some Inuit people in Gjøa Haven with European ancestry have claimed to be descendants of Amundsen, accounts by members of the expedition told of their relations with Inuit women, and historians have speculated that Amundsen might also have taken a partner, although he wrote a warning against this. Specifically, half brothers Bob Konona and Paul Ikuallaq say that their father Luke Ikuallaq told them on his deathbed that he was the son of Amundsen. Konona said that their father Ikuallaq was left out on the ice to die after his birth, as his European ancestry made him illegitimate to the Inuit, threatening their community. In 2012, Y-DNA analysis, with the permission, showed that Ikuallaq was not a match to the direct male line of Amundsen. Not all descendants claiming European ancestry have been tested for a match to Amundsen, permanent European-style settlement at Gjoa Haven started in 1927 with a Hudsons Bay Company trading outpost. In 1941 Henry Larsen reached the post from the west, the settlement has attracted the traditionally nomadic Inuit people as they have adapted a more settled lifestyle. In 1961, the population was 110. By 2001, the population was 960 according to the Census, as the Inuit have moved from their camps to be close to the healthcare. At the 2016 census, the population was 1,324, the Population Centre of Gjoa Haven showed 1,197 people living in 0.78 km2, a decrease of 1. 4% from 2011. Gjoa Haven has expanded to such an extent that a newer subdivision has been developed near the airport at 68°37′56″N 095°52′04″W, the community is served by the Gjoa Haven Airport and by annual supply sealift. The area is home to CAM-B, a North Warning System site, quqshuun Ilihakvik Centre is a community heritage museum and cultural centre opened in 2013
34.
Nunavut
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Nunavut is the newest, largest, and northernmost territory of Canada. The creation of Nunavut resulted in the first major change to Canadas political map since the incorporation of the province of Newfoundland, Nunavut comprises a major portion of Northern Canada, and most of the Canadian Arctic Archipelago. Its vast territory makes it the fifth-largest country subdivision in the world, the capital Iqaluit, on Baffin Island in the east, was chosen by the 1995 capital plebiscite. Other major communities include the regional centres of Rankin Inlet and Cambridge Bay and it is Canadas only geo-political region that is not connected to the rest of North America by highway. Nunavut is the largest in area and the second least populous of Canadas provinces and territories. One of the worlds most remote, sparsely settled regions, it has a population of 35,944, mostly Inuit, spread over an area of just over 1,750,000 km2, Nunavut is also home to the worlds northernmost permanently inhabited place, Alert. A weather station farther down Ellesmere Island, Eureka, has the lowest average temperature of any Canadian weather station. Nunavut means our land in Inuktitut, Nunavut covers 1,877,787 km2 of land and 160,935 km2 of water in Northern Canada. This makes it the fifth largest subnational entity in the world, if Nunavut were a country, it would rank 15th in area. It also shares borders with Greenland and the provinces of Quebec, Ontario. Nunavuts highest point is Barbeau Peak on Ellesmere Island, the population density is 0.019 persons/km2, one of the lowest in the world. By comparison, Greenland has approximately the area and nearly twice the population. Nunavut experiences a climate in most regions, owing to its high latitude. In more southerly continental areas very cold climates can be found. The region now known as Nunavut has supported an indigenous population for approximately 4,000 years. Most historians identify the coast of Baffin Island with the Helluland described in Norse sagas, the materials were collected in five seasons of excavation at Cape Tanfield. Scholars determined that these provide evidence of European traders and possibly settlers on Baffin Island and they seem to indicate prolonged contact, possibly up to 1450. So you have to consider the possibility that as remote as it may seem, the ore turned out to be worthless, but Frobisher made the first recorded European contact with the Inuit
35.
Victoria Island (Canada)
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Victoria Island is a large island in the Canadian Arctic Archipelago that straddles the boundary between Nunavut and the Northwest Territories of Canada. It is the eighth largest island in the world, and at 217,291 km21 in area and it is nearly double the size of Newfoundland, and is slightly larger than the island of Great Britain. It contains the worlds largest island within an island within an island, the western third of the island belongs to the Inuvik Region in the Northwest Territories, the remainder is part of Nunavuts Kitikmeot Region. In 1826 John Richardson saw the southwest coast and called it Wollaston Land, in 1839 Peter Warren Dease and Thomas Simpson followed its southeast coast and called it Victoria Land. A map published by John Barrow in 1846 shows a complete blank from these two lands north to Banks Land which is the north coast of Banks Island, in 1851 John Rae charted its entire south coast and connected the two lands. In 1850 and 1851 Robert McClure circumnavigated most of Banks Island and his men also charted the northwest and west coasts of Victoria Island. Viscount Melville Soundmap1 lies to the north, and the MClintock Channelmap2, Victoria Island is an island of peninsulas, having a heavily indented coastline with many inlets. Another, broad peninsula is found in the north, Prince Albert Peninsula. map15 This ends at the Prince of Wales Strait, in the south, and pointing westwards, is the Wollaston Peninsula, map16 separated from the islands central areas by Prince Albert Sound. The island as a whole coincidentally resembles a stylized maple leaf, the highest point of Victoria Island is 655 m in the Shaler Mountainsmap17 in the north-central region. Located in the southeast, just north of Cambridge Bay is Ferguson Lakemap18 with an area of 562 km2 is the largest lake on the island, the island is named after Queen Victoria, the Canadian sovereign from 1867 to 1901. The features bearing the name Prince Albert are named after her consort, there is also a smaller Victoria Island in Nunavut, located in Amadjuak Lake on Baffin Island. They migrate across the Dolphin and Union Strait from their summer grazing on Victoria Island to their winter grazing area on the Nunavut-NWT mainland in Canada. It is unusual for North American caribou to cross sea ice. In the Canada 2006 Census the population of the island was 1,875,1,477 in Nunavut and 398 in the Northwest Territories, of the two settlements on the island the largest is Cambridge Bay, map19 which lies on the south-east coast and is in Nunavut. Ulukhaktokmap20 is on the west coast and is in the Northwest Territories, trading posts, such as Fort Collinsonmap21 on the northwest coast, have long since been abandoned. ^1 The United Nations Environment Programme says that Victoria Island has an area of 220,548 km2, however, the Atlas of Canada indicates the island is 217,291 km2. Parkers Notch Prince Albert Impact Crater Map of Victoria Island at the Atlas of Canada Victoria Island Expedition
36.
Beaufort Sea
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The Beaufort Sea is a marginal sea of the Arctic Ocean, located north of the Northwest Territories, the Yukon, and Alaska, west of Canadas Arctic islands. The sea is named after hydrographer Sir Francis Beaufort, the major Mackenzie River empties into the Canadian part of the sea, west of Tuktoyaktuk, which is one of the few permanent settlements on the sea shores. The sea, characterized by climate, is frozen over most of the year. Historically, only a narrow pass up to 100 km opened in August–September near its shores, claims that the seacoast was populated about 30,000 years ago have been largely discredited, present population density is very low. The sea contains significant resources of petroleum and natural gas under its shelf and they were discovered in the period between the 1950s and 1980s, and their exploration became the major human activity in the area since the 1980s. The traditional occupations of fishery and whale and seal hunting are practiced only locally, as a result, the sea hosts one of the largest colonies of beluga whales, and there is no sign of overfishing. To prevent overfishing in its waters, the US adopted precautionary commercial fisheries management plan in August 2009, in April 2011 the Canadian government signed a memorandum of understanding with the Inuvialuit as a first step in developing a larger ocean management plan. The Canadian government has set a new block of the Beaufort Sea off the Parry Peninsula in the Amundsen as a Marine Protected Area, the protected area is set to protect species and habits for the Inuvialuit community. The International Hydrographic Organization defines the limits of the Beaufort Sea as follows, a line from Point Barrow, Alaska, to Lands End, Prince Patrick Island. There is a dispute involving a wedge-shaped slice on the International Boundary in the Beaufort Sea. Canada claims the maritime boundary to be along the 141st meridian west out to a distance of 200 nmi, following the Alaska–Yukon land border. The position of the United States is that the line is perpendicular to the coast out to a distance of 200 nmi. This difference creates a wedge with an area of about 21,000 km2 that is claimed by both nations, Canadas position has its roots in the Treaty of Saint Petersburg between the United Kingdom and the Russian Empire that set the boundary between the two. They differ on what should be deemed equitable, Canada contends that an equidistance principle does not result in an equitable boundary, because distortion would occur. The coast of Yukon is concave, whereas the coast of Alaska is convex, because of this, Canada argues that special circumstances apply to this border, a position that the U. S. rejects. Before the end of 2004, the US leased eight plots of land below the water for oil exploration and exploitation, provoking a diplomatic protest from Canada. On 20 August 2009, United States Secretary of Commerce Gary Locke announced a moratorium on fishing of the Beaufort Sea north of Alaska. In July 2010, US–Canada negotiations have started in Ottawa with the meeting planned in 2011
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Herschel Island
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Herschel Island is an island in the Beaufort Sea, which lies 5 km off the coast of Yukon in Canada, of which it is administratively a part. The earliest evidence of human occupation unearthed so far by archaeological investigations is that of the Thule culture and these people are the ancestors of the present-day Inuvialuit. The Inuvialuktun word for Herschel Island is Qikiqtaruk, which means island. The first European to sight the island was explorer Sir John Franklin and it is not clear after whom the island was named. At the time of Franklins explorations there were three Inuvialuit settlements on Herschel Island, estimates of the number of people living on the island at that time ranged from 200 to 2000. The island was used as a base for hunting, fishing and whaling, in the late 19th century, whalers discovered that the Beaufort Sea was one of the last refuges of the depleted bowhead whale, which was prized for its baleen, blubber, and oil. Commercial bowhead hunting in the began in 1889. In order for the short Arctic whaling season to be profitable, Herschel Island was found to have a good harbour for large whaling ships. In 1890 a Euro-American settlement was established at Pauline Cove, at the height of the Beaufort Sea whaling period the number of residents on the island was estimated at 1,500, making it the largest Yukon community at that time. Though several frame buildings had been constructed, most residents continued to live on whaling ships, in 1893, the Pacific Steam Whaling Company constructed a building called the Community House at Pauline Cove. With a recreation room, an office for the manager and storekeeper, and storage facilities, in 1896 the company offered the house to the Anglican church, who used the building until 1906. In 1903, Francis Joseph Fitzgerald was the first North-West Mounted Police officer assigned to the area, in 1911, the Royal North-West Mounted Police purchased all Herschel Island assets of the PSW Co. for $1,500. The Community House still stands, and is believed to be the oldest frame building in Yukon and it remains in excellent condition, and is now used as a park office and visitor centre. The first court held in the Canadian Arctic took place at Pauline Cove in 1924 in a building known as the Bonehouse. Court officials traveled from Edmonton for the trial of two Inuvialuit men charged with murder, jury members were chosen in Fort McPherson, Arctic Red River and Herschel Island. The men were guilty, and were hanged from a tie beam in the Bonehouse. The tie beam was removed by the RCMP when they left the island in 1963, Anglican missionary Isaac Stringer first visited Herschel Island in 1893. He returned with his wife in 1896, and ministered to the people there until his departure in 1901, Stringer and other missionaries attempted to build a church on the island, but were not successful
38.
Yukon
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Yukon is the smallest and westernmost of Canadas three federal territories. The territory has the smallest population of any province or territory in Canada, Whitehorse is the territorial capital and Yukons only city. The territory was split from the Northwest Territories in 1898 and was named the Yukon Territory, though officially bilingual, the Yukon Government also recognizes First Nations languages. At 5,959 m, Yukons Mount Logan, in Kluane National Park and Reserve, is the highest mountain in Canada, most of Yukon has a subarctic climate, characterized by long cold winters and brief warm summers. The Arctic Ocean coast has a tundra climate, notable rivers include the Yukon River, after which the territory was named, as well as the Pelly, Stewart, Peel, White and Tatshenshini rivers. Long before the arrival of Europeans, central and southern Yukon was populated by First Nations people, sites of archeological significance in Yukon hold some of the earliest evidence of the presence of human occupation in North America. The sites safeguard the history of the first people and the earliest First Nations of the Yukon, the volcanic eruption of Mount Churchill in approximately 800 AD in what is now the U. S. Coastal and inland First Nations had extensive trading networks, European incursions into the area only began early in the 19th century with the fur trade, followed by missionaries. By the 1870s and 1880s gold miners began to arrive and this drove a population increase that justified the establishment of a police force, just in time for the start of the Klondike Gold Rush in 1897. The increased population coming with the gold led to the separation of the Yukon district from the Northwest Territories. Its northern coast is on the Beaufort Sea and its ragged eastern boundary mostly follows the divide between the Yukon Basin and the Mackenzie River drainage basin to the east in the Mackenzie mountains. Most of the territory is in the watershed of its namesake, the southern Yukon is dotted with a large number of large, long and narrow glacier-fed alpine lakes, most of which flow into the Yukon River system. The larger lakes include Teslin Lake, Atlin Lake, Tagish Lake, Marsh Lake, Lake Laberge, Kusawa Lake, bennett Lake on the Klondike Gold Rush trail is a lake flowing into Nares Lake, with the greater part of its area within Yukon. Canadas highest point, Mount Logan, is in the territorys southwest, Mount Logan and a large part of the Yukons southwest are in Kluane National Park and Reserve, a UNESCO World Heritage Site. Other national parks include Ivvavik National Park and Vuntut National Park in the north, other watersheds include the Mackenzie River, the Peel Watershed and the Alsek–Tatshenshini, and a number of rivers flowing directly into the Beaufort Sea. The two main Yukon rivers flowing into the Mackenzie in the Northwest Territories are the Liard River in the southeast, notable widespread tree species within Yukon are the black spruce and white spruce. Many trees are stunted because of the growing season and severe climate. The capital, Whitehorse, is also the largest city, with about three-quarters of the population, the second largest is Dawson City, which was the capital until 1952
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Eagle, Alaska
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Eagle is a city located along the south bank of the Yukon River near the Canada–US border in the Southeast Fairbanks Census Area, Alaska, United States. It includes the Eagle Historic District, a U. S. National Historic Landmark, the population was 86 at the 2010 census. Every February, Eagle hosts a checkpoint for the long-distance Yukon Quest sled dog race, Eagle is located at 64°47′10″N 141°12′0″W. Eagle is located on the bank of the Yukon River,8 miles west of the border between Alaska and the Yukon Territory of Canada at the end of the Taylor Highway. According to the United States Census Bureau, the city has an area of 1. 0-square-mile. Like most of Alaska, Eagle has a climate with long, cold winters occasionally moderated by chinook winds. When chinooks occur, winter temperatures can get above 32 °F or 0 °C, for thousands of years, the Eagle area was the home to indigenous peoples, including the historic Han people since long before the arrival of Europeans in Alaska. The first permanent structure by Europeans in present-day Eagle was a log trading post called Belle Isle, in the late 1800s, Eagle became a supply and trading center for miners working the upper Yukon River and its tributaries. By 1898, its population had exceeded 1,700, as people were coming into the area because of the Klondike Gold Rush, in 1901 Eagle became the first incorporated city in the Alaska Interior. It was named for the eagles that nested on nearby Eagle Bluff. A United States Army camp, Fort Egbert, was built at Eagle in 1900, a telegraph line between Eagle and Valdez was completed in 1903. In 1905, Roald Amundsen arrived in Eagle and telegraphed the news of the Northwest Passage to the rest of the world, the gold rushes in Nome and Fairbanks lured people away from Eagle. In 1903 Judge James Wickersham moved the Third Division court from Eagle to Fairbanks, by 1910, Eagles population had declined to its present-day level. Fort Egbert was abandoned in 1911, present-day Eagle is home to mostly people of European descent. Nearby Eagle Village has a population that is about 50 percent Han. The town enjoyed some notoriety as the setting of John McPhees book Coming into the Country, many of the buildings from the Gold Rush years are preserved as part of the Eagle Historic District, a National Historic Landmark district. As of the census of 2000, there were 129 people,58 households, the population density was 127. 9/sq mi. There were 137 housing units at a density of 135.8 per square mile
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Alaska
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Alaska is a U. S. state located in the northwest extremity of North America. To the north are the Chukchi and Beaufort seas–the southern parts of the Arctic Ocean, the Pacific Ocean lies to the south and southwest. Alaska is the largest state in the United States by area, the 3rd least populous, approximately half of Alaskas residents live within the Anchorage metropolitan area. Alaskas economy is dominated by the fishing, natural gas, military bases and tourism are also a significant part of the economy. The United States purchased Alaska from the Russian Empire on March 30,1867, the area went through several administrative changes before becoming organized as a territory on May 11,1912. It was admitted as the 49th state of the U. S. on January 3,1959, the name Alaska was introduced in the Russian colonial period when it was used to refer to the peninsula. It was derived from an Aleut, or Unangam idiom, which refers to the mainland of Alaska. Literally, it means object to which the action of the sea is directed, Alaska is the northernmost and westernmost state in the United States and has the most easterly longitude in the United States because the Aleutian Islands extend into the Eastern Hemisphere. Alaska is the only non-contiguous U. S. state on continental North America and it is technically part of the continental U. S. but is sometimes not included in colloquial use, Alaska is not part of the contiguous U. S. often called the Lower 48. The capital city, Juneau, is situated on the mainland of the North American continent but is not connected by road to the rest of the North American highway system. Alaskas territorial waters touch Russias territorial waters in the Bering Strait, as the Russian Big Diomede Island, Alaska has a longer coastline than all the other U. S. states combined. Alaska is the largest state in the United States by total area at 663,268 square miles, over twice the size of Texas, Alaska is larger than all but 18 sovereign countries. Counting territorial waters, Alaska is larger than the area of the next three largest states, Texas, California, and Montana. It is also larger than the area of the 22 smallest U. S. states. Also referred to as the Panhandle or Inside Passage, this is the region of Alaska closest to the rest of the United States, as such, this was where most of the initial non-indigenous settlement occurred in the years following the Alaska Purchase. The region is dominated by the Alexander Archipelago as well as the Tongass National Forest and it contains the state capital Juneau, the former capital Sitka, and Ketchikan, at one time Alaskas largest city. The Alaska Marine Highway provides a vital transportation link throughout the area. The Interior is the largest region of Alaska, much of it is uninhabited wilderness, Fairbanks is the only large city in the region
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Nome, Alaska
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Nome is a city in the Nome Census Area in the Unorganized Borough of the U. S. state of Alaska. The city is located on the southern Seward Peninsula coast on Norton Sound of the Bering Sea, according to the 2010 Census, the city population was 3,598. The 2014 population estimate was 3,788, suggesting a slight increase, Nome was incorporated on April 9,1901, and was once the most populous city in Alaska. Nome lies within the region of the Bering Straits Native Corporation, the city of Nome claims to be home to the worlds largest gold pan, although this claim has been disputed by the Canadian city of Quesnel, British Columbia. In the winter of 1925, a diphtheria epidemic raged among Alaska Natives in the Nome area, fierce territory-wide blizzard conditions prevented delivery of a life-saving serum by airplane from Anchorage. A relay of dog sled teams was organized to deliver the serum, the origin of the citys name Nome is debated, there are three theories. The first is that the name was given by Nomes founder, Jafet Lindeberg, within trekking distance of his home in Kvænangen, Norway. Name next to the unnamed cape, the mapmaker misread the annotation as C. Nome, or Cape Nome, and used that name on his own chart, the third proposed origin of the name is from a misunderstanding of the local Inupiaq word for Where at. The United States Post Office in Nome refused to accept the change, fearing a move of the post office to Nome City, a mining camp on the Nome River, the merchants unhappily agreed to change the name of Anvil City back to Nome. Nome is located at 64°30′14″N 165°23′58″W, according to the United States Census Bureau, the city has a total area of 21.6 square miles, of which 12.5 square miles is land and 9.1 square miles is water. Nome has a climate, with long, very cold winters. However, conditions in winter and summer are moderated by the citys coastal location, winters are less severe than in the Interior. For example, Fairbanks at a similar parallel quite far inland has much greater temperature swings with both very warm and cold temperatures throughout the year, the coldest month is January, averaging 5. Average highs stay below freezing from late October until late April, and the average first and last dates of freezing lows are August 30 and June 9, respectively, a freeze-free period of 81 days. The warmest month is July, with an average of 52.2 °F, Snow averages 76 inches per season, with the average first and last dates of measurable snowfall being October 4 and May 16, accumulating snow has not been officially observed in July or August. Precipitation is greatest in the months, and averages 16.8 inches per year. The annual average temperature is 27.35 °F, extreme temperatures range from −54 °F on January 27–28,1989 up to 86 °F on June 19,2013 and July 31,1977
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1906 San Francisco earthquake
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The 1906 San Francisco earthquake struck the coast of Northern California at 5,12 a. m. on April 18 with an estimated moment magnitude of 7.8 and a maximum Mercalli intensity of XI. Severe shaking was felt from Eureka on the North Coast to the Salinas Valley, devastating fires soon broke out in the city and lasted for several days. As a result, about 3,000 people died and over 80% of the city of San Francisco was destroyed, the events are remembered as one of the worst and deadliest natural disasters in the history of the United States. The death toll remains the greatest loss of life from a disaster in Californias history. The San Andreas Fault is a transform fault that forms part of the tectonic boundary between the Pacific Plate and the North American Plate. The strike-slip fault is characterized by mainly lateral motion in a dextral sense, the 1906 rupture propagated both northward and southward for a total of 296 miles. This fault runs the length of California from the Salton Sea in the south to Cape Mendocino in the north, the maximum observed surface displacement was about 20 feet, geodetic measurements show displacements of up to 28 feet. The 1906 earthquake preceded the development of the Richter magnitude scale by three decades. The most widely accepted estimate for the magnitude of the quake on the moment magnitude scale is 7.8. According to findings published in the Journal of Geophysical Research, severe deformations in the earths crust took place both before and after the earthquakes impact. Accumulated strain on the faults in the system was relieved during the earthquake, the main shock epicenter occurred offshore about 2 miles from the city, near Mussel Rock. Shaking was felt from Oregon to Los Angeles, and inland as far as central Nevada, a strong foreshock preceded the main shock by about 20 to 25 seconds. The strong shaking of the main shock lasted about 42 seconds, there were decades of minor earthquakes – more than at any other time in the historical record for northern California – before the 1906 quake. For years, the epicenter of the quake was assumed to be near the town of Olema, in the Point Reyes area of Marin County, because of evidence of the degree of local earth displacement. In the 1960s, a seismologist at UC Berkeley proposed that the epicenter was more likely offshore of San Francisco, at the time,375 deaths were reported, partly because hundreds of fatalities in Chinatown went ignored and unrecorded. The total number of deaths is uncertain today, and is estimated to be roughly 3,000 at minimum. Most of the deaths occurred in San Francisco itself, but 189 were reported elsewhere in the Bay Area, nearby cities, such as Santa Rosa and San Jose, in Monterey County, the earthquake permanently shifted the course of the Salinas River near its mouth. Where previously the river emptied into Monterey Bay between Moss Landing and Watsonville, it was diverted 6 miles south to a new channel just north of Marina
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San Francisco
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San Francisco, officially the City and County of San Francisco, is the cultural, commercial, and financial center of Northern California. It is the birthplace of the United Nations, the California Gold Rush of 1849 brought rapid growth, making it the largest city on the West Coast at the time. San Francisco became a consolidated city-county in 1856, after three-quarters of the city was destroyed by the 1906 earthquake and fire, San Francisco was quickly rebuilt, hosting the Panama-Pacific International Exposition nine years later. In World War II, San Francisco was a port of embarkation for service members shipping out to the Pacific Theater. Politically, the city votes strongly along liberal Democratic Party lines, San Francisco is also the headquarters of five major banking institutions and various other companies such as Levi Strauss & Co. Dolby, Airbnb, Weebly, Pacific Gas and Electric Company, Yelp, Pinterest, Twitter, Uber, Lyft, Mozilla, Wikimedia Foundation, as of 2016, San Francisco is ranked high on world liveability rankings. The earliest archaeological evidence of habitation of the territory of the city of San Francisco dates to 3000 BC. Upon independence from Spain in 1821, the became part of Mexico. Under Mexican rule, the system gradually ended, and its lands became privatized. In 1835, Englishman William Richardson erected the first independent homestead, together with Alcalde Francisco de Haro, he laid out a street plan for the expanded settlement, and the town, named Yerba Buena, began to attract American settlers. Commodore John D. Sloat claimed California for the United States on July 7,1846, during the Mexican–American War, montgomery arrived to claim Yerba Buena two days later. Yerba Buena was renamed San Francisco on January 30 of the next year, despite its attractive location as a port and naval base, San Francisco was still a small settlement with inhospitable geography. The California Gold Rush brought a flood of treasure seekers, with their sourdough bread in tow, prospectors accumulated in San Francisco over rival Benicia, raising the population from 1,000 in 1848 to 25,000 by December 1849. The promise of fabulous riches was so strong that crews on arriving vessels deserted and rushed off to the gold fields, leaving behind a forest of masts in San Francisco harbor. Some of these approximately 500 abandoned ships were used at times as storeships, saloons and hotels, many were left to rot, by 1851 the harbor was extended out into the bay by wharves while buildings were erected on piles among the ships. By 1870 Yerba Buena Cove had been filled to create new land, buried ships are occasionally exposed when foundations are dug for new buildings. California was quickly granted statehood in 1850 and the U. S. military built Fort Point at the Golden Gate, silver discoveries, including the Comstock Lode in Nevada in 1859, further drove rapid population growth. With hordes of fortune seekers streaming through the city, lawlessness was common, and the Barbary Coast section of town gained notoriety as a haven for criminals, prostitution, entrepreneurs sought to capitalize on the wealth generated by the Gold Rush
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California
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California is the most populous state in the United States and the third most extensive by area. Located on the western coast of the U. S, California is bordered by the other U. S. states of Oregon, Nevada, and Arizona and shares an international border with the Mexican state of Baja California. Los Angeles is Californias most populous city, and the second largest after New York City. The Los Angeles Area and the San Francisco Bay Area are the nations second- and fifth-most populous urban regions, California also has the nations most populous county, Los Angeles County, and its largest county by area, San Bernardino County. The Central Valley, an agricultural area, dominates the states center. What is now California was first settled by various Native American tribes before being explored by a number of European expeditions during the 16th and 17th centuries, the Spanish Empire then claimed it as part of Alta California in their New Spain colony. The area became a part of Mexico in 1821 following its war for independence. The western portion of Alta California then was organized as the State of California, the California Gold Rush starting in 1848 led to dramatic social and demographic changes, with large-scale emigration from the east and abroad with an accompanying economic boom. If it were a country, California would be the 6th largest economy in the world, fifty-eight percent of the states economy is centered on finance, government, real estate services, technology, and professional, scientific and technical business services. Although it accounts for only 1.5 percent of the states economy, the story of Calafia is recorded in a 1510 work The Adventures of Esplandián, written as a sequel to Amadis de Gaula by Spanish adventure writer Garci Rodríguez de Montalvo. The kingdom of Queen Calafia, according to Montalvo, was said to be a land inhabited by griffins and other strange beasts. This conventional wisdom that California was an island, with maps drawn to reflect this belief, shortened forms of the states name include CA, Cal. Calif. and US-CA. Settled by successive waves of arrivals during the last 10,000 years, various estimates of the native population range from 100,000 to 300,000. The Indigenous peoples of California included more than 70 distinct groups of Native Americans, ranging from large, settled populations living on the coast to groups in the interior. California groups also were diverse in their organization with bands, tribes, villages. Trade, intermarriage and military alliances fostered many social and economic relationships among the diverse groups, the first European effort to explore the coast as far north as the Russian River was a Spanish sailing expedition, led by Portuguese captain Juan Rodríguez Cabrillo, in 1542. Some 37 years later English explorer Francis Drake also explored and claimed a portion of the California coast in 1579. Spanish traders made unintended visits with the Manila galleons on their trips from the Philippines beginning in 1565
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Cape Horn
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Cabo de Hornos is a Chilean commune located in the south of Tierra del Fuego archipelago, in Antártica Province, Magallanes Region. The municipality of Cabo de Hornos, located in the town of Puerto Williams and it is named for Cape Horn. According to the 2002 census of the National Statistics Institute, Cabo de Hornos spans an area of 15,853.7 km2 and has 2,262 inhabitants, of these,1,952 lived in urban areas and 310 in rural areas. The population grew by 24. 7% between the 1992 and 2002 censuses, as a commune, Cabo de Hornos is a third-level administrative division of Chile administered by a municipal council, headed by an alcalde who is directly elected every four years. The 2016-2020 alcalde is Patricio Fernández, the commune is represented in the Senate by Carlos Bianchi Chelech and Carolina Goic as part of the 19th senatorial constituency. Murray Channel Cabo de Hornos commune,2006 Official website of the Municipality of Cabo de Hornos Official website of Puerto Williams Gobierno Regional Magallanes y Antártica Chilena Official website Cape Horn Biosphere Reserve
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Norwegian Americans
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Norwegian Americans comprise Americans with ancestral roots from Norway. Norwegian immigrants went to the United States primarily in the half of the 19th century. There are more than 4.5 million Norwegian Americans according to the most recent U. S. census, Norwegian Americans currently comprise the 10th largest European ancestry group in the United States. Norsemen from Greenland and Iceland were the first Europeans to reach North America, leif Ericson reached North America via Norse settlements in Greenland around the year 1000. Norse settlers from Greenland founded the settlement of LAnse aux Meadows and Point Rosee in Vinland, in what is now Newfoundland and these settlers failed to establish a permanent settlement because of conflicts with indigenous people and within the Norse community. There was a Norwegian presence in New Amsterdam in the part of 17th century. Hans Hansen Bergen, a native of Bergen, Norway, was one of the earliest settlers of the Dutch colony of New Amsterdam having immigrated in 1633, another of the first Norwegian settlers was Albert Andriessen Bradt who arrived in New Amsterdam in 1637. Pieter Van Brugh, Mayor of Albany, New York was the grandson of Norwegian immigrants, approximately 60 persons had settled in the Manhattan area before the British take-over in 1664. How many Norwegians that settled in New Netherland is not known, the Netherlands had strong commercial ties with the coastal lumber trade of Norway during the 17th century and many Norwegians immigrated to Amsterdam. Some of them settled in Dutch colonies, although never in large numbers, there were also Norwegian settlers in Pennsylvania in the first half of the 18th century, upstate New York in the latter half of the same century, and in New England during both halves. The earliest immigrants from Norway to America emigrated mostly because of religious motives, as Religious Society of Friends, organized Norwegian immigration to North America began in 1825, when several dozen Norwegians left Stavanger bound for North America on the sloop Restauration under the leadership of Cleng Peerson. To a great extent, this emigration from Norway was borne out of religious persecution, especially for Quakers and a local religious group. The ship landed in New York City, where it was at first impounded for exceeding its passenger limit. After intervention from President John Quincy Adams, the passengers moved on to settle in Kendall, New York with the help of Andreas Stangeland, many of these immigrants moved on from the Kendall Settlement, settling in Illinois and Wisconsin. In July of that year, a group of six dissenting families, seeking a haven from the official Norwegian state church, set sail from Stavanger in an undersized sloop, the Restaurationen. When it arrived in New York harbor after an arduous 14-week journey, the Restaurationen caused a sensation, local Quakers helped the destitute emigrants, who eventually established a community in upstate New York. Today, their descendants are known as sloopers. While about 65 Norwegians emigrated via Sweden and elsewhere in the years, no emigrant ships left Norway for the New World until the 1836 departures of the Den Norske Klippe
Media related to Gjøa (ship in museum) at Wikimedia Commons