1.
Loran-C
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Loran-C was a hyperbolic radio navigation system which allowed a receiver to determine its position by listening to low frequency radio signals transmitted by fixed land-based radio beacons. Loran-C combined two different techniques to provide a signal that was both long-range and highly accurate, traits that had formerly been at odds. The downside was the expense of the equipment needed to interpret the signals, Loran-C became one of the most common and widely used navigation systems for large areas of North America, Europe, Japan and the entire Atlantic and Pacific areas. The Soviet Union operated a nearly identical system, CHAYKA, the introduction of civilian satellite navigation in the 1990s led to a very rapid drop-off in Loran-C use. Discussions about the future of Loran-C began in the 1990s, and several dates were announced. In 2010 the US and Canadian systems were shut down, along with shared Loran-C/CHAYKA stations with Russia, several other chains remained active, and some had been upgraded for continued use. At the end of 2015, navigation chains in most of Europe were turned off, the original LORAN was proposed by Alfred Lee Loomis at a meeting of the Microwave Committee. The Microwave Committee, by this time organized into what would become the Radiation Laboratory, took up development as Project 3. During the initial meetings a member of the UK liaison team, Taffy Bowen, mentioned that he was aware the British were also working on a similar concept, but had no information on its performance. The development team, led by Loomis, made progress on the transmitter design. Extensive signal-strength measurements were made by mounting a conventional radio receiver in a station wagon, however, the custom receiver design and its associated cathode ray tube displays proved to be a bigger problem. In spite of efforts to design around the problem, instability in the display prevented accurate timing measurements. They met with the Gee team in 1941, and immediately adopted this solution and they also found that Project 3 and Gee called for almost identical systems, with similar performance, range and accuracy. But Gee had already completed basic development and was entering into initial production, in response, the Project 3 team told the Army Air Force to adopt Gee, and realigned their own efforts to provide long-range navigation on the oceans. Rapid development followed, and a system covering the western Atlantic was operational in 1943, additional stations followed, covering the European side, and then a massive expansion in the Pacific. By the end of the war there were 72 operational LORAN stations, in 1958 the operation of the LORAN system was handed over to the US Coast Guard, which renamed the system Loran-A, the lower-case name being introduced at that time. There are two ways to implement the timing measurements needed for a navigation system, pulse timing systems like Gee and LORAN. The former requires sharp pulses of signal, and their accuracy is limited to how rapidly the pulses can be turned on and off, which is, in turn
2.
Norwegian language
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Norwegian is a North Germanic language spoken mainly in Norway, where it is the official language. Along with Swedish and Danish, Norwegian forms a continuum of more or less mutually intelligible local and regional variants. These Scandinavian languages, together with Faroese and Icelandic as well as extinct languages. Faroese and Icelandic are hardly mutually intelligible with Norwegian in their spoken form because continental Scandinavian has diverged from them, as established by law and governmental policy, the two official forms of written Norwegian are Bokmål and Nynorsk. The official Norwegian Language Council is responsible for regulating the two forms, and recommends the terms Norwegian Bokmål and Norwegian Nynorsk in English. Two other written forms without official status also exist, one and it is regulated by the unofficial Norwegian Academy, which translates the name as Standard Norwegian. Nynorsk and Bokmål provide standards for how to write Norwegian, no standard of spoken Norwegian is officially sanctioned, and most Norwegians speak their own dialects in all circumstances. Thus, unlike in other countries, the use of any Norwegian dialect. Outside Eastern Norway, this variation is not used. From the 16th to the 19th centuries, Danish was the written language of Norway. As a result, the development of modern written Norwegian has been subject to strong controversy related to nationalism, rural versus urban discourse, historically, Bokmål is a Norwegianised variety of Danish, while Nynorsk is a language form based on Norwegian dialects and puristic opposition to Danish. The unofficial form known as Riksmål is considered more conservative than Bokmål, Norwegians are educated in both Bokmål and Nynorsk. A2005 poll indicates that 86. 3% use primarily Bokmål as their written language,5. 5% use both Bokmål and Nynorsk, and 7. 5% use primarily Nynorsk. Thus, 13% are frequently writing Nynorsk, though the majority speak dialects that resemble Nynorsk more closely than Bokmål. Broadly speaking, Nynorsk writing is widespread in western Norway, though not in major urban areas, examples are Setesdal, the western part of Telemark county and several municipalities in Hallingdal, Valdres, and Gudbrandsdalen. It is little used elsewhere, but 30–40 years ago, it also had strongholds in rural parts of Trøndelag. Today, not only is Nynorsk the official language of four of the 19 Norwegian counties, NRK, the Norwegian broadcasting corporation, broadcasts in both Bokmål and Nynorsk, and all governmental agencies are required to support both written languages. Bokmål is used in 92% of all publications, and Nynorsk in 8%
3.
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
4.
Island
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An island or isle is any piece of sub-continental land that is surrounded by water. Very small islands such as emergent land features on atolls can be called islets, skerries, an island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. A grouping of geographically or geologically related islands is called an archipelago, an island may be described as such, despite the presence of an artificial land bridge. Example, Singapore and its causeway, or the various Dutch delta islands, there are two main types of islands in the sea, continental and oceanic. The word island derives from Middle English iland, from Old English igland, Old English ieg is actually a cognate of Swedish ö and German Aue, and related to Latin aqua. There is a difference between islands and continents in terms of geology, continents sit on continental lithosphere which is part of tectonic plates floating high on Earths mantle. Oceanic crust is also part of tectonic plates, but it is denser than continental lithosphere, Islands are either extensions of the oceanic crust or geologically they are part of some continent sitting on continental lithosphere. This holds true for Australia, which sits on its own continental lithosphere, continental islands are bodies of land that lie on the continental shelf of a continent. A special type of island is the microcontinental island, which is created when a continent is rifted. Examples are Madagascar and Socotra off Africa, the Kerguelen Islands, New Caledonia, New Zealand, another subtype is an island or bar formed by deposition of tiny rocks where water current loses some of its carrying capacity. While some are transitory and may disappear if the volume or speed of the current changes, others are stable, oceanic islands are islands that do not sit on continental shelves. The vast majority are volcanic in origin, such as Saint Helena in the South Atlantic Ocean, the few oceanic islands that are not volcanic are tectonic in origin and arise where plate movements have lifted up the ocean floor above the surface. Examples are Saint Peter and Paul Rocks in the Atlantic Ocean, one type of volcanic oceanic island is found in a volcanic island arc. These islands arise from volcanoes where the subduction of one plate under another is occurring, examples are the Aleutian Islands, the Mariana Islands, and most of Tonga in the Pacific Ocean. The only examples in the Atlantic Ocean are some of the Lesser Antilles, another type of volcanic oceanic island occurs where an oceanic rift reaches the surface. There are two examples, Iceland, which is the second largest volcanic island, and Jan Mayen. A third type of oceanic island is formed over volcanic hotspots. A hotspot is more or less stationary relative to the tectonic plate above it
5.
Jan Mayen
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Jan Mayen is a Norwegian volcanic island situated in the North Arctic Ocean. It is 55 km long and 373 km2 in area, partly covered by glaciers and it has two parts, larger northeast Nord-Jan and smaller Sør-Jan, linked by a 2.5 km wide isthmus. It lies 600 km northeast of Iceland,500 km east of central Greenland and 1,000 km west of the North Cape, the island is mountainous, the highest summit being the Beerenberg volcano in the north. The isthmus is the location of the two largest lakes of the island, Sørlaguna, and Nordlaguna, a third lake is called Ullerenglaguna. Jan Mayen was formed by the Jan Mayen hotspot, although administered separately, Svalbard and Jan Mayen are collectively assigned the ISO 3166-1 alpha-2 country code SJ. Jan Mayen Island has one exploitable natural resource, gravel, from the site at Trongskaret, other than this, economic activity is limited to providing services for employees of Norways radio communications and meteorological stations located on the island. Jan Mayen has one unpaved airstrip, Jan Mayensfield, which is about 1,585 m long, the 124.1 km coast has no ports or harbours, only offshore anchorages. There are important fishing resources, and the existence of Jan Mayen establishes a large Exclusive Economic Zone around it, a dispute between Norway and Denmark regarding the fishing exclusion zone between Jan Mayen and Greenland was settled in 1988 granting Denmark the greater area of sovereignty. Significant deposits of petroleum and natural gas are suspected by geologists to lie below Jan Mayens surrounding seafloors, Jan Mayen Island is an integral part of the Kingdom of Norway. Since 1995, Jan Mayen has been administered by the County Governor of the northern Norwegian county of Nordland to which it is closest. However, some authority over Jan Mayen has been assigned to the commander of the Norwegian Defence Logistics Organisation. The only inhabitants on the island are personnel working for the Norwegian Armed Forces, eighteen people spend the winter on the island, but the population may double during the summer, when heavy maintenance is performed. Personnel serve either six months or one year, and are exchanged twice a year in April, the main purpose of the military personnel is to operate a Loran-C base. The support crew, including mechanics, cooks, and a nurse, are among the military personnel, both the LORAN transmitter and the meteorological station are located a few kilometres away from the settlement Olonkinbyen, where all personnel live. Transport to the island is provided by C-130 Hercules military transport planes operated by the Royal Norwegian Air Force that land at Jan Mayensfields gravel runway, the planes fly in from Bodø Main Air Station eight times a year. Since the airport does not have any instrument landing capabilities, good visibility is required, for heavy goods, freight ships visit during the summer, but since there are no harbours, the ships must anchor. The island has no population, but is assigned the ISO 3166-1 alpha-2 country code SJ. It uses the Internet country code top-level domain. no and data code JN, Jan Mayen has telephone and internet connection over satellite, using Norwegian telephone numbers
6.
Gennady Olonkin
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Gennady Nikitich Olonkin was a Russian-Norwegian polar explorer and radio operator. Olonkin was the only son among twelve children of a Norwegian mother, from 1918 to 1925, he was a radio operator and mechanic on the polar ship Maud, led by Roald Amundsen. In 1926 he was honored as a Knight of the Order of St. Olav, Olonkin acquired Norwegian citizenship and worked at the Norwegian Meteorological Institute. He served on Jan Mayen in the years 1928–1929, 1930–1931, 1933–1934, from 1958 he worked in conjunction with an expansion of a LORAN station on Jan Mayen. Gennadij Olonkin was married and had one son and two daughters, cape Olonkin and Olonkinbyen at Jan Mayen have been named in his honor. Gendij Olonkin at Norsk Polarhistorie Norwegian Polar Institute Place names at Svalbard and Jan Mayen
7.
Norwegian Armed Forces
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The Norwegian Armed Forces is the military organisation responsible for the defence of Norway. It consists of four branches, the Norwegian Army, the Royal Norwegian Navy, which includes the Coast Guard, the Royal Norwegian Air Force, the armed forces number 23,000 personnel, including civilian employees, and have a full-mobilisation combat strength of 83,000. The armed forces are subordinate to the Ministry of Defence, led by Ine Marie Eriksen Søreide, the formal commander-in-chief is King Harald V, however, the de facto commander-in-chief is Chief of Defence Haakon Bruun-Hanssen. His staff is located at Akershus Fortress in Oslo, while the Norwegian Joint Headquarters, the main naval base is Haakonsvern in Bergen, the main army camps are in Bardu, Målselv and Rena, and the main air station is Ørland. An organised military was first assembled in Norway in the 9th century and was focused around naval warfare. The army was created in 1628 as part of Denmark–Norway, followed by two centuries of regular wars, a Norwegian military was established in 1814, but the military did not see combat until the German occupation of Norway in 1940. Norway abandoned its position as a country in 1949 to become a founding member of the North Atlantic Treaty Organisation. The Cold War saw a large build-up of air stations and military bases, since the 2000s, the military has transformed from a focus on defence from an invasion to a mobile force for international missions. Among European NATO members, the expenditure of US$7.2 billion is the highest per capita. The Chief of Defence heads the armed forces, and is the military adviser to the Minister of Defence. It is headed by a general or admiral. DEFSTNOR assigns priorities, manages resources, provides force generation and support activities, each of the four branches of defence is headed by a two-star general/admiral who are subordinate to DEFSTNOR. National Joint Headquarters located at Reitan, close to Bodø has operational control of Norwegian armed forces worldwide 24/7 and it is headed by the Supreme Commander Norwegian Forces - a three-star general or admiral. Norwegian Defence Logistics Organisation at Kolsås outside Oslo is responsible for engineering, procurement, investment, supply, information and it is also responsible for maintenance, repair and storage of material. Norway employs a form of mandatory military service for men and women. While 63,841 men and women were called in for the examination of persons liable for service in 2012,9265 were conscripted. In 2015 conscription was extended to women making Norway the first NATO member, there is a right of conscientious objection. The press statements read, that serves as a means to “fight climate change”
8.
Norwegian Meteorological Institute
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The Norwegian Meteorological Institute, also known as MET Norway, is Norways national institute which provides weather forecasts. Its three main offices are located in Oslo, Bergen and Tromsø, MET Norway has around 500 employees and some 650 part-time observers around the country. The institute was founded in 1866 with the help of Norwegian astronomer and he is credited with founding meteorological research in Norway. The institute represents Norway in international organizations like the World Meteorological Organization, the European Centre for Medium-Range Weather Forecasts, the Institute is also partner to a number of international research and monitoring projects including EMEP, MyOcean, MyWave and the North West Shelf Operational Oceanographic System. Marine forecasts of sea state parameters are issued both commercially to oil companies and more generally for the public, the institute also provides data for the free online service yr. no, launched in 2007, which provides weather forecasts for some 7 million places in the world. The institute is responsible for maintaining, quality checking, archiving and updating the network consisting of automated weather stations, radiosondes. The marine observations of wave height and other oceanographic parameters gathered by petroleum platforms in Norwegian waters are also archived by the institute, the institute produces operational weather forecasts using different numerical weather prediction models including the Unified Model and HIRLAM. The forecasts are subject to modifications introduced by human forecasters before being issued, the institute also runs a suite of operational ocean models ranging in resolution from 20 km to less than 1 km. The model suite currently comprises both the Princeton Ocean Model as well as the more recent Regional Ocean Modeling System, Henrik Mohn Aksel Steen Hans Theodor Hesselberg Ragnar Fjørtoft Kaare Langlo Arne Grammeltvedt Anton Eliassen yr. no Official website Information about yr. no
9.
Radiosonde
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Modern radiosondes measure or calculate the following variables, altitude, pressure, temperature, relative humidity, wind, cosmic ray readings at high altitude and geographical position. Radiosondes measuring ozone concentration are known as ozonesondes, radiosondes may operate at a radio frequency of 403 MHz or 1680 MHz. A radiosonde whose position is tracked as it ascends to give wind speed, most radiosondes have radar reflectors and are technically rawinsondes. A radiosonde that is dropped from an airplane and falls, rather than being carried by a balloon is called a dropsonde, radiosondes are an essential source of meteorological data, and hundreds are launched all over the world daily. This proved to be difficult because the kites were linked to the ground and were difficult to manoeuvre in gusty conditions. Furthermore, the sounding was limited to low altitudes because of the link to the ground, gustave Hermite and Georges Besançon, from France, were the first in 1892 to use a balloon to fly the meteograph. In 1898, Léon Teisserenc de Bort organized at the Observatoire de Météorologie Dynamique de Trappes the first regular use of these balloons. Data from these launches showed that the temperature lowered with height up to an altitude, which varied with the season. De Borts discovery of the tropopause and stratosphere was announced in 1902 at the French Academy of Sciences, other researchers, like Richard Aßmann and William Henry Dines, were working at the same times with similar instruments. In 1924, Colonel William Blaire in the U. S. Signal Corps did the first primitive experiments with weather measurements from balloon, the first true radiosonde that sent precise encoded telemetry from weather sensors was invented in France by Robert Bureau. Bureau coined the name radiosonde and flew the first instrument on January 7,1929, developed independently a year later, Pavel Molchanov flew a radiosonde on January 30,1930. Molchanovs design became a popular standard because of its simplicity and because it converted sensor readings to Morse code, working with a modified Molchanov sonde, Sergey Vernov was the first to use radiosondes to perform cosmic ray readings at high altitude. On April 1,1935, he took measurements up to 13.6 km using a pair of Geiger counters in a circuit to avoid counting secondary ray showers. The sondes were tracked for two days, a rubber or latex balloon filled with either helium or hydrogen lifts the device up through the atmosphere. The maximum altitude to which the balloon ascends is determined by the diameter, balloon sizes can range from 100 to 3,000 g. As the balloon ascends through the atmosphere, the pressure decreases, eventually, the balloon will expand to the extent that its skin will break, terminating the ascent. An 800 g balloon will burst at about 21 km, after bursting, a small parachute on the radiosondes support line carries it to Earth. A typical radiosonde flight lasts 60 to 90 minutes, one radiosonde from Clark Air Base, Philippines, reached an altitude of 155,092 ft
10.
Electric generator
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In electricity generation, a generator is a device that converts mechanical energy to electrical energy for use in an external circuit. Sources of mechanical energy include steam turbines, gas turbines, water turbines, internal combustion engines, the first electromagnetic generator, the Faraday disk, was built in 1831 by British scientist Michael Faraday. Generators provide nearly all of the power for electric power grids, the reverse conversion of electrical energy into mechanical energy is done by an electric motor, and motors and generators have many similarities. Many motors can be driven to generate electricity and frequently make acceptable manual generators. Electromagnetic generators fall into one of two categories, dynamos and alternators. The magnetic field of the dynamo or alternator can be provided by either wire windings called field coils or permanent magnets, a generator using permanent magnets is sometimes called a magneto. Armature, The power-producing component of an electrical machine, in a generator, alternator, or dynamo the armature windings generate the electric current, which provides power to an external circuit. The armature can be on either the rotor or the stator, depending on the design, before the connection between magnetism and electricity was discovered, electrostatic generators were invented. They operated on electrostatic principles, by using moving electrically charged belts, plates, the charge was generated using either of two mechanisms, electrostatic induction or the triboelectric effect. Such generators generated very high voltage and low current and their only practical applications were to power early X-ray tubes, and later in some atomic particle accelerators. The operating principle of electromagnetic generators was discovered in the years of 1831–1832 by Michael Faraday, the principle later called Faradays law, is that an electromotive force is generated in an electrical conductor which encircles a varying magnetic flux. He also built the first electromagnetic generator, called the Faraday disk and it produced a small DC voltage. This design was inefficient, due to self-cancelling counterflows of current in regions of the disk that were not under the influence of the magnetic field. While current was induced directly underneath the magnet, the current would circulate backwards in regions that were outside the influence of the magnetic field and this counterflow limited the power output to the pickup wires, and induced waste heating of the copper disc. Later homopolar generators would solve this problem by using an array of magnets arranged around the perimeter to maintain a steady field effect in one current-flow direction. Another disadvantage was that the voltage was very low, due to the single current path through the magnetic flux. Experimenters found that using multiple turns of wire in a coil could produce higher, since the output voltage is proportional to the number of turns, generators could be easily designed to produce any desired voltage by varying the number of turns. Wire windings became a feature of all subsequent generator designs
11.
Precipitation
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In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, rain, sleet, snow, graupel, Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and precipitates. Thus, fog and mist are not precipitation but suspensions, because the vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated, Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers, moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain is occurring. A stationary front is often present near the area of freezing rain, provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. Eventually, the droplets will grow large enough to form raindrops. Lake-effect snowfall can be locally heavy, thundersnow is possible within a cyclones comma head and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation, on the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. The movement of the trough, or intertropical convergence zone. Precipitation is a component of the water cycle, and is responsible for depositing the fresh water on the planet. Approximately 505,000 cubic kilometres of water falls as precipitation each year,398,000 cubic kilometres of it over the oceans and 107,000 cubic kilometres over land. Given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres, Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on celestial bodies, e. g. when it gets cold, Mars has precipitation which most likely takes the form of frost. Precipitation is a component of the water cycle, and is responsible for depositing most of the fresh water on the planet. Approximately 505,000 km3 of water falls as precipitation each year,398,000 km3 of it over the oceans, given the Earths surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective, stratiform, and orographic rainfall, Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice
12.
Wayback Machine
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The Internet Archive launched the Wayback Machine in October 2001. It was set up by Brewster Kahle and Bruce Gilliat, and is maintained with content from Alexa Internet, the service enables users to see archived versions of web pages across time, which the archive calls a three dimensional index. Since 1996, the Wayback Machine has been archiving cached pages of websites onto its large cluster of Linux nodes and it revisits sites every few weeks or months and archives a new version. Sites can also be captured on the fly by visitors who enter the sites URL into a search box, the intent is to capture and archive content that otherwise would be lost whenever a site is changed or closed down. The overall vision of the machines creators is to archive the entire Internet, the name Wayback Machine was chosen as a reference to the WABAC machine, a time-traveling device used by the characters Mr. Peabody and Sherman in The Rocky and Bullwinkle Show, an animated cartoon. These crawlers also respect the robots exclusion standard for websites whose owners opt for them not to appear in search results or be cached, to overcome inconsistencies in partially cached websites, Archive-It. Information had been kept on digital tape for five years, with Kahle occasionally allowing researchers, when the archive reached its fifth anniversary, it was unveiled and opened to the public in a ceremony at the University of California, Berkeley. Snapshots usually become more than six months after they are archived or, in some cases, even later. The frequency of snapshots is variable, so not all tracked website updates are recorded, Sometimes there are intervals of several weeks or years between snapshots. After August 2008 sites had to be listed on the Open Directory in order to be included. As of 2009, the Wayback Machine contained approximately three petabytes of data and was growing at a rate of 100 terabytes each month, the growth rate reported in 2003 was 12 terabytes/month, the data is stored on PetaBox rack systems manufactured by Capricorn Technologies. In 2009, the Internet Archive migrated its customized storage architecture to Sun Open Storage, in 2011 a new, improved version of the Wayback Machine, with an updated interface and fresher index of archived content, was made available for public testing. The index driving the classic Wayback Machine only has a bit of material past 2008. In January 2013, the company announced a ground-breaking milestone of 240 billion URLs, in October 2013, the company announced the Save a Page feature which allows any Internet user to archive the contents of a URL. This became a threat of abuse by the service for hosting malicious binaries, as of December 2014, the Wayback Machine contained almost nine petabytes of data and was growing at a rate of about 20 terabytes each week. Between October 2013 and March 2015 the websites global Alexa rank changed from 162 to 208, in a 2009 case, Netbula, LLC v. Chordiant Software Inc. defendant Chordiant filed a motion to compel Netbula to disable the robots. Netbula objected to the motion on the ground that defendants were asking to alter Netbulas website, in an October 2004 case, Telewizja Polska USA, Inc. v. Echostar Satellite, No.02 C3293,65 Fed. 673, a litigant attempted to use the Wayback Machine archives as a source of admissible evidence, Telewizja Polska is the provider of TVP Polonia and EchoStar operates the Dish Network
13.
.sj
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. sj is the Internet country code top-level domain reserved for the designation Svalbard and Jan Mayen. The domain name registry is Norid, but. sj is not open for registration. sj was designated on 21 August 1997, both were placed under the. no registry Norid, which is also the sponsor. Norwegian policy states that. no is sufficient for those connected to both Svalbard and Jan Mayen, and therefore the domain is not open to registration. It is Norwegian policy not to commercialize domain resources, so there are no plans to sell. sj, should the domain later come into use, it will be under regulation of the Norwegian Post and Telecommunications Authority and follow the same policy as. no. There are two second-level domains reserved for the two areas, svalbard. no and jan-mayen. no, but other web addresses are also used, Svalbard and Jan Mayen are two integrated territories of Norway with special status. Jan Mayen is a nearly unpopulated volcanic island in the Atlantic Ocean and is an integrated part of Norway. During the establishment of the ISO3166 codes, it was proposed that Svalbard have its own code, following the ISO codes. sj was allocated on 21 August 1997, at the same time. bv was allocated. In June 2015, Norwegian computer scientist Håkon Wium Lie and the Socialist Left Party proposed using the. sj domain, along with. bv, the proposal aims at protecting both the Norwegian authorities and foreign dissidents from surveillance. Management of. sj lies with the Trondheim-based Norid, which is also the name registry for. no. Norid is a company owned by Uninett, which is again owned by the Norwegian Ministry of Education. The policy for use of. sj is regulated by the Regulation Concerning Domain Names Under Norwegian Country Code Top-level Domains and this regulation also regulates Norways other two ccTLDs. bv and. no. Should. sj later come unto use, the rules and procedures currently regarding. no would be used for. sj. The domain remains reserved for future use. Sale of the two unused ccTLDs has not been an item to consider for policymakers, as commercialization of the resources is in direct contradiction to Norwegian policy. no eller aldri
14.
Jan Mayen Microcontinent
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The Jan Mayen Microcontinent is a fragment of continental crust within the oceanic part of the western Eurasian Plate lying northeast of Iceland. At the onset of separation between the Greenland and Eurasian plates 55 million years ago, it formed part of the margin of the Greenland Plate. Propagation of a new spreading center from the Reykjanes Ridge separated this microcontinent from the Greenland Plate, for a short period it formed a microplate, until the Aegir Ridge became inactive, after which it formed part of the Eurasian Plate. The island of Jan Mayen is a younger feature, formed of volcanic rock. The microcontinent extends about 500 km southwards from the Jan Mayen fracture zone, the Jan Mayen Ridge separates the Norwegian Sea from the Greenland Sea. This interpretation has been confirmed using wide-angle seismic reflection and refraction data, the microcontinent consists of the prominent bathymetric high, the Jan Mayen Ridge and several subsidiary ridges and intervening basins towards the south and west. Investigations using seismic reflection and refraction data have identified two passive margin sequences on the two sides of the microcontinent, faults mapped on seismic reflection data are roughly N-S trending in the northern part becoming SW-NE trending to the south. The crustal thickness reaches a maximum of 16 km on the side of the main ridge. At the time of the initial break-up along the North Atlantic margin, towards the end of the Eocene period, at about the time marked by chron 17 a new spreading centre began to propagate northeastwards from the Reykjanes Ridge, forming the Kolbeinsey Ridge. During the period both the Kolbeinsey and Aegir ridges were active, the microcontinent underwent a 30°–50° anti-clockwise rotation. This was caused by the propagation of the Kolbeinsey Ridge. An alternative but challenged model involves no rotation but the development of several short-lived fracture zones cutting through the microcontinent, with both ridges active the microcontinent was also temporarily a microplate. The Kolbeinsey Ridge reached the Jan Mayen Fracture Zone and therefore linked up to the Mohns Ridge, at this time activity on the Aegir Ridge died away and the microcontinent became part of the Eurasian Plate. The northern end of the microcontinent was affected by renewed displacement on the Jan Mayen Fracture Zone. The volcanic island of Jan Mayen only formed in the Pleistocene, possibly related to a hotspot, known as the Jan Mayen hotspot, the area around the microcontinent has recently become open for licensing for hydrocarbon exploration
15.
Svalbard and Jan Mayen
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Svalbard and Jan Mayen is a statistical designation defined by ISO 3166-1 of two parts of Norway under separate jurisdictions—Svalbard and Jan Mayen. While the two are combined for the purposes of the International Organization for Standardization category, they are not administratively related and this has further resulted in the country code top-level domain. sj being issued for Svalbard and Jan Mayen, and ISO 3166-2, SJ. The United Nations Statistics Division also uses this code, but has named it Svalbard, Svalbard is an archipelago in the Arctic Ocean under the full sovereignty of Norway, but is subject to the special status granted by the Svalbard Treaty. Jan Mayen is an island in the Arctic Ocean, it has no permanent population and is administrated by the County Governor of Nordland. Svalbard and Jan Mayen have in common that they are the integrated parts of Norway not allocated to counties. While a separate ISO code for Svalbard was proposed by the United Nations, Svalbard is an archipelago in the Arctic about midway between mainland Norway and the North Pole. The group of range from 74° to 81° north latitude. The area is 61,022 square kilometres and there were 2,572 residents in 2009, spitsbergen is the largest island, followed by Nordaustlandet and Edgeøya. The Svalbard Treaty of 1920 recognizes Norwegian sovereignty, and the 1925 Svalbard Act made Svalbard a full part of the Kingdom of Norway, the archipelago is administrated by the Governor of Svalbard, which is subordinate to the Norwegian Ministry of Justice and the Police. Unlike the rest of Norway, Svalbard is an economic zone and a demilitarized zone. Jan Mayen is an island in the Arctic Ocean located at the border of the Norwegian Sea. The single island covers an area of 377 square kilometres and is dominated by the 2, the islands only population is a combined military and meteorological outpost that operates a LORAN-C transmitter at Olonkinbyen. The Norwegian Meteorological Institute annexed the island for Norway in 1922, on 27 February 1930, the island was made de jure a part of the Kingdom of Norway. Since 1994, the island has been administrated by the County Governor of Nordland, neither Svalbard nor Jan Mayen have their own flag or coat of arms, and the flag of Norway is used for both of them, both alone and as a group. An attempt to change the ISO code to just Svalbard has previously failed because of opposition from the Norwegian Ministry of Foreign Affairs, however, for statistics use within population and trade, Svalbard and Jan Mayen essentially means just Svalbard. ISO 3166-2, SJ is the entry for Svalbard and Jan Mayen in ISO 3166-2, by virtue of the ISO 3166-1 alpha-2 code SJ, Svalbard and Jan Mayen were grouped together and allocated the Internet country code top-level domain. sj. Norid, who administrated the Norways. no ccTLD, was given the responsibility for the. sj. Policy prohibits any registration with either of the domains, as connected to Svalbard can use the. no domain
16.
Beerenberg
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Beerenberg is a 2,277 m stratovolcano which forms the northeastern end of the Norwegian island of Jan Mayen. It is the worlds northernmost subaerial active volcano, the volcano is topped by a mostly ice-filled crater about 1 km wide, with numerous peaks along its rim including the highest summit, Haakon VII Toppen, on its western side. The upper slopes of the volcano are largely ice-covered, with several major glaciers including five which reach the sea. The longest of the glaciers is the Weyprecht Glacier, which flows from the summit crater via a breach through the portion of the crater rim. Beerenberg is composed primarily of basaltic lava flows with minor amounts of tephra, numerous cinder cones have been formed along flank fissures. Its most recent eruptions took place in 1985 and 1970 both of which were flank eruptions from fissures on the northeast side of the mountain, other eruptions with historical records occurred in 1732,1818, and 1851. Its name means Bear Mountain in Dutch, and it takes its name from the polar bears seen there by Dutch whalers in the early 17th century
17.
Engelskbukta (Jan Mayen)
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Engelskbukta is a broad, open bay mid-way up the west coast of the island of Jan Mayen. It lies between Kapp Rudsen and Kvalrossen, comprising Kvalrossbukta and Tømmerbukta, presumably this is where the English resorted to in 1616, when they sent their first whaling ships to the island. The Dutch also called it Noordbaai, the bay was the location of one of the two main Dutch whaling stations in the 17th century. In 1632 two Basque ships landed and plundered the station, causing the Dutch to send a party of seven men in 1633-34. Early Dutch and English Voyages to Spitsbergen in the Seventeenth Century, norwegian Polar Institute Place Names of Svalbard Database
18.
Hoepstockbukta
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Hoepstockbukta is a small cove on the western coast of the island of Jan Mayen and is named after Mathijs Jansz. Hoepstock, a Rotterdam whaler, who was the first to use the bay in 1616, the cove is shown on Joan Blaeus 1662 map of the island. Dansk-Norsk Hvalfangst 1615-1660, En Studie over Danmark-Norges Stilling i Europæisk Merkantil Expansion, norwegian Polar Institute Place Names of Svalbard Database
19.
Nansenflua
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Nansenflua is an undersea rock in the northern part of Rekvedbukta off the southeastern coast of Jan Mayen in the Arctic Ocean. The shoal is named after the ship HNoMS Fridtjof Nansen, which sank after striking the previously uncharted rock in November 1940, Nansenflua is the only obstruction in Rekvedbukta. The name Nansenflua was introduced in charts published by the Norwegian Polar Institute in 1955 and it follows a convention based on two then in force Orders in Council, dated 28 April 1933 and 31 May 1957, of using the Nynorsk grammatical form. The suffix -a in the definite form was chosen, as no local dialect existed on Jan Mayen. The last part of the name, flu, means rock awash, the geographical location is given by Orvin as 70°57′N 08°28′W, with an exactitude of 1. The rock, located two meters under the surface, has a top area and vertical sides of about twenty meters. It is located one nautical mile from Eggøykalven and 1.7 nautical miles west-southwest of the peninsula Eggøya. In anything but completely calm weather conditions, Nansenflua is visible by waves being broken against it, the rock is part of the remains of a crater. The ship returned in November of the year to disrupt German plans to re-establish a weather station on the island. Entering the bay of Rekvedbukta on 8 November 1940 in calm weather, the whole crew of 66 entered the lifeboats. The boats reached the shore during darkness, and by the morning the ship had sunk. Four days later the crew was rescued by the naval trawler HNoMS Honningsvåg. The wreck of Fridtjof Nansen, which had a length of 72.8 m and a displacement of 1,275 short tons, is probably still located near the rock
20.
Amsterdam
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Amsterdam is the capital and most populous municipality of the Kingdom of the Netherlands. Its status as the capital is mandated by the Constitution of the Netherlands, although it is not the seat of the government, which is The Hague. Amsterdam has a population of 851,373 within the city proper,1,351,587 in the urban area, the city is located in the province of North Holland in the west of the country. The metropolitan area comprises much of the part of the Randstad, one of the larger conurbations in Europe. Amsterdams name derives from Amstelredamme, indicative of the citys origin around a dam in the river Amstel, during that time, the city was the leading centre for finance and diamonds. In the 19th and 20th centuries the city expanded, and many new neighborhoods and suburbs were planned, the 17th-century canals of Amsterdam and the 19–20th century Defence Line of Amsterdam are on the UNESCO World Heritage List. As the commercial capital of the Netherlands and one of the top financial centres in Europe, Amsterdam is considered a world city by the Globalization. The city is also the capital of the Netherlands. Many large Dutch institutions have their headquarters there, and seven of the worlds 500 largest companies, including Philips and ING, are based in the city. In 2012, Amsterdam was ranked the second best city to live in by the Economist Intelligence Unit and 12th globally on quality of living for environment, the city was ranked 3rd in innovation by Australian innovation agency 2thinknow in their Innovation Cities Index 2009. The Amsterdam seaport to this day remains the second in the country, famous Amsterdam residents include the diarist Anne Frank, artists Rembrandt van Rijn and Vincent van Gogh, and philosopher Baruch Spinoza. The Amsterdam Stock Exchange, the oldest stock exchange in the world, is located in the city center. After the floods of 1170 and 1173, locals near the river Amstel built a bridge over the river, the earliest recorded use of that name is in a document dated October 27,1275, which exempted inhabitants of the village from paying bridge tolls to Count Floris V. This allowed the inhabitants of the village of Aemstelredamme to travel freely through the County of Holland, paying no tolls at bridges, locks, the certificate describes the inhabitants as homines manentes apud Amestelledamme. By 1327, the name had developed into Aemsterdam, Amsterdam is much younger than Dutch cities such as Nijmegen, Rotterdam, and Utrecht. In October 2008, historical geographer Chris de Bont suggested that the land around Amsterdam was being reclaimed as early as the late 10th century. This does not necessarily mean there was already a settlement then, since reclamation of land may not have been for farming—it may have been for peat. Amsterdam was granted city rights in either 1300 or 1306, from the 14th century on, Amsterdam flourished, largely from trade with the Hanseatic League
21.
Andorra la Vella
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Andorra la Vella is the capital of the Principality of Andorra, and is located high in the east Pyrenees between France and Spain. It is also the name of the parish that surrounds the capital, as of 2015, the city has a population of 22,886, and the urban area, which includes Escaldes-Engordany plus satellite villages, has over 40,000 inhabitants. The principal industry is tourism, although the country also earns income from being a tax haven. Furniture and brandies are local products, being at an elevation of 1,023 metres, it is the highest capital city in Europe and a popular ski resort. The site of Andorra la Vella has been settled prior to the Christian era—notably by the Andosin tribe from the late Neolithic. The state is one of the Marca Hispanica created and protected by Charlemagne in the century as a buffer from the Moorish settlers in the Iberian Peninsula. The settlement of Andorra la Vella has been the city of Andorra since 1278 when the French. Andorra la Vellas old town—the Barri Antic—includes streets and buildings dating from this time and its most notable building is the Casa de la Vall—constructed in the early sixteenth century—which has been the states parliamentary house since 1702. Andorra la Vella was, during this period, the capital of an isolated and feudal state. Well into the century, the area around Andorra la Vella remained largely forgotten, indeed the state was not part of the Treaty of Versailles. After political turmoil in the 1930s and a coup by Boris Skossyreff. In 1993, the countrys first constitution formalised this parliamentary democracy with executive, legislative, during this period, Andorra also developed as a tax haven, resulting in the construction of modern banking offices in Andorra La Vella. The city also developed its facilities, to the extent that Andorra la Vella was Andorras applicant city for the XXI Olympic Winter Games. However, Andorra la Vella was not selected by the IOC as a candidate city and it also hosted both the 1991 and 2005 Games of the Small States of Europe. It adjoins the area of Escaldes-Engordany. The city is at 1,023 metres above sea level, Andorra la Vella has an oceanic climate, with mild summers and chilly to cold, snowy winters. The average annual precipitation is 812.3 mm, temperatures are lowered by the altitude compared with lowland areas. The parish of Andorra la Vella is divided into the villages of Andorra la Vella itself, La Margineda, Andorra la Vella has direct access to air transportation with commercial helicopter flights from Andorra la Vella Heliport, located in the city centre
22.
Bern
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The city of Bern or Berne is the de facto capital of Switzerland, referred to by the Swiss as their Bundesstadt, or federal city. With a population of 141,762, Bern is the fourth-most populous city in Switzerland, the Bern agglomeration, which includes 36 municipalities, had a population of 406,900 in 2014. The metropolitan area had a population of 660,000 in 2000, Bern is also the capital of the canton of Bern, the second-most populous of Switzerlands cantons. The official language in Bern is German, but the language is an Alemannic Swiss German dialect. In 1983, the old town in the centre of Bern became a UNESCO World Heritage Site. Bern is ranked among the top ten cities for the best quality of life. The etymology of the name Bern is uncertain and it has long been considered likely that the city was named after the Italian city of Verona, which at the time was known as Bern in Middle High German. As a result of the find of the Bern zinc tablet in the 1980s, it is now common to assume that the city was named after a pre-existing toponym of Celtic origin. The bear was the animal of the seal and coat of arms of Bern from at least the 1220s. The earliest reference to the keeping of bears in the Bärengraben dates to the 1440s. No archaeological evidence that indicates a settlement on the site of city centre prior to the 12th century has been found so far. In antiquity, a Celtic oppidum stood on the Engehalbinsel north of Bern, fortified since the second century BC, during the Roman era, a Gallo-Roman vicus was on the same site. The Bern zinc tablet has the name Brenodor, in the Early Middle Ages, a settlement in Bümpliz, now a city district of Bern, was some 4 km from the medieval city. The medieval city is a foundation of the Zähringer ruling family, according to 14th-century historiography, Bern was founded in 1191 by Berthold V, Duke of Zähringen. In 1218, after Berthold died without an heir, Bern was made an imperial city by the Goldene Handfeste of Holy Roman Emperor Frederick II. In 1353, Bern joined the Swiss Confederacy, becoming one of the eight cantons of the period of 1353 to 1481. The city grew out towards the west of the boundaries of the peninsula formed by the river Aare, the Zytglogge tower marked the western boundary of the city from 1191 until 1256, when the Käfigturm took over this role until 1345. It was, in turn, succeeded by the Christoffelturm until 1622, during the time of the Thirty Years War, two new fortifications – the so-called big and small Schanze – were built to protect the whole area of the peninsula
23.
Brussels
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Brussels, officially the Brussels-Capital Region, is a region of Belgium comprising 19 municipalities, including the City of Brussels which is the capital of Belgium. The Brussels-Capital Region is a part of both the French Community of Belgium and the Flemish Community, but is separate from the region of Flanders or Wallonia. The region has a population of 1.2 million and an area with a population of over 1.8 million. Brussels is the de facto capital of the European Union as it hosts a number of principal EU institutions, the secretariat of the Benelux and the headquarters of the North Atlantic Treaty Organization are also located in Brussels. Today, it is considered an Alpha global city, historically a Dutch-speaking city, Brussels has seen a language shift to French from the late 19th century onwards. Today, the majority language is French, and the Brussels-Capital Region is a bilingual enclave within the Flemish Region. All road signs, street names, and many advertisements and services are shown in both languages, Brussels is increasingly becoming multilingual with increasing numbers of migrants, expatriates and minority groups speaking their own languages. The most common theory of the origin of Brussels name is that it derives from the Old Dutch Broekzele or Broeksel, meaning marsh, Saint Vindicianus, the bishop of Cambrai made the first recorded reference to the place Brosella in 695 when it was still a hamlet. The origin of the settlement that was to become Brussels lies in Saint Gaugericus construction of a chapel on an island in the river Senne around 580. The official founding of Brussels is usually situated around 979, when Duke Charles of Lower Lotharingia transferred the relics of Saint Gudula from Moorsel to the Saint Gaugericus chapel, Charles would construct the first permanent fortification in the city, doing so on that same island. Lambert I of Leuven, Count of Leuven gained the County of Brussels around 1000 by marrying Charles daughter, as it grew to a population of around 30,000, the surrounding marshes were drained to allow for further expansion. The Counts of Leuven became Dukes of Brabant at about this time, in the 13th century, the city got its first walls. After the construction of the city walls in the early 13th century, to let the city expand, a second set of walls was erected between 1356 and 1383. Today, traces of it can still be seen, mostly because the small ring, Brabant had lost its independence, but Brussels became the Princely Capital of the prosperous Low Countries, and flourished. In 1516 Charles V, who had been heir of the Low Countries since 1506, was declared King of Spain in St. Michael and St. Gudula Cathedral in Brussels. Upon the death of his grandfather, Maximilian I, Holy Roman Emperor in 1519 and it was in the Palace complex at Coudenberg that Charles V abdicated in 1555. This impressive palace, famous all over Europe, had expanded since it had first become the seat of the Dukes of Brabant. In 1695, during the Nine Years War, King Louis XIV of France sent troops to bombard Brussels with artillery, together with the resulting fire, it was the most destructive event in the entire history of Brussels
24.
Douglas, Isle of Man
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Douglas is the capital and largest town of the Isle of Man, with a population of 27,938. It is located at the mouth of the River Douglas, the River Douglas forms part of the towns harbour and main commercial port. Douglas was a settlement until it grew rapidly as a result of links with the English port of Liverpool in the 18th century. The town is the Islands main hub for business, finance, legal services, shipping, transport, shopping, the annual Isle of Man TT motorcycle races start and finish in Douglas. In the absence of any data, the origins of the town may be revealed by analysis of the original street. Scholars agree that the name of the town derives from Early Celtic Duboglassio meaning black river and these may be references to the site of the later Nunnery, a little upstream from the port. This suggests that the origins of the nucleus were as a non-urban port. Current speculation links the buildings with the Irish Sea Herring fishery. Other forms of trade grew, and following the Revestment Act 1765, Douglas began to reap the benefits of trans-Atlantic trade. Legitimate merchants who rose to prominence over the period included the Murreys, the Moores, the towns later prosperity was facilitated by the low cost of living, and the favourable legal status enjoyed by English debtors and half-pay officers. The initial growth and development of the town owed much to its natural harbour, over the 18th century, the towns population rose from about 800 in 1710 to nearly 2,500 in 1784. Throughout the 19th century, the towns demographics followed the trends as the United Kingdom. The number of visitors grew from the early 19th century, and from around 1870 onwards. But there were increasingly unsanitary conditions, and poor quality housing, the open sewage, middens, and smell from the harbour at low tide all contributed to the towns uncleanliness. Douglas in the first half of the 19th century often suffered from the destitution of its population and the many epidemics, in particular cholera. However, an Act passed later that decade, which did not include opt-out clauses, was accepted, and in 1860, Douglas elected its first town council, which was predominantly middle class in its makeup. The Town Commissioners could tackle the problems with greater efficiency. The Commissioners also designed to alter the anachronistic architecture of Douglas, built during the era of fishing and trading, the proportion of the Manx population living in Douglas was also expanding, with 35% living there by 1891
25.
Dublin
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Dublin is the capital and largest city of Ireland. Dublin is in the province of Leinster on Irelands east coast, the city has an urban area population of 1,345,402. The population of the Greater Dublin Area, as of 2016, was 1,904,806 people, founded as a Viking settlement, the Kingdom of Dublin became Irelands principal city following the Norman invasion. The city expanded rapidly from the 17th century and was briefly the second largest city in the British Empire before the Acts of Union in 1800, following the partition of Ireland in 1922, Dublin became the capital of the Irish Free State, later renamed Ireland. Dublin is administered by a City Council, the city is listed by the Globalization and World Cities Research Network as a global city, with a ranking of Alpha-, which places it amongst the top thirty cities in the world. It is a historical and contemporary centre for education, the arts, administration, economy, the name Dublin comes from the Irish word Dubhlinn, early Classical Irish Dubhlind/Duibhlind, dubh /d̪uβ/, alt. /d̪uw/, alt /d̪u, / meaning black, dark, and lind /lʲiɲ pool and this tidal pool was located where the River Poddle entered the Liffey, on the site of the castle gardens at the rear of Dublin Castle. In Modern Irish the name is Duibhlinn, and Irish rhymes from Dublin County show that in Dublin Leinster Irish it was pronounced Duílinn /d̪ˠi, other localities in Ireland also bear the name Duibhlinn, variously anglicized as Devlin, Divlin and Difflin. Historically, scribes using the Gaelic script wrote bh with a dot over the b and those without knowledge of Irish omitted the dot, spelling the name as Dublin. Variations on the name are found in traditionally Irish-speaking areas of Scotland, such as An Linne Dhubh. It is now thought that the Viking settlement was preceded by a Christian ecclesiastical settlement known as Duibhlinn, beginning in the 9th and 10th century, there were two settlements where the modern city stands. Baile Átha Cliath, meaning town of the ford, is the common name for the city in modern Irish. Áth Cliath is a name referring to a fording point of the River Liffey near Father Mathew Bridge. Baile Átha Cliath was an early Christian monastery, believed to have been in the area of Aungier Street, there are other towns of the same name, such as Àth Cliath in East Ayrshire, Scotland, which is Anglicised as Hurlford. Although the area of Dublin Bay has been inhabited by humans since prehistoric times and he called the settlement Eblana polis. It is now thought that the Viking settlement was preceded by a Christian ecclesiastical settlement known as Duibhlinn, beginning in the 9th and 10th century, there were two settlements where the modern city stands. The subsequent Scandinavian settlement centred on the River Poddle, a tributary of the Liffey in an area now known as Wood Quay, the Dubhlinn was a small lake used to moor ships, the Poddle connected the lake with the Liffey. This lake was covered during the early 18th century as the city grew, the Dubhlinn lay where the Castle Garden is now located, opposite the Chester Beatty Library in Dublin Castle
26.
London
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London /ˈlʌndən/ is the capital and most populous city of England and the United Kingdom. Standing on the River Thames in the south east of the island of Great Britain and it was founded by the Romans, who named it Londinium. Londons ancient core, the City of London, largely retains its 1. 12-square-mile medieval boundaries. London is a global city in the arts, commerce, education, entertainment, fashion, finance, healthcare, media, professional services, research and development, tourism. It is crowned as the worlds largest financial centre and has the fifth- or sixth-largest metropolitan area GDP in the world, London is a world cultural capital. It is the worlds most-visited city as measured by international arrivals and has the worlds largest city airport system measured by passenger traffic, London is the worlds leading investment destination, hosting more international retailers and ultra high-net-worth individuals than any other city. Londons universities form the largest concentration of education institutes in Europe. In 2012, London became the first city to have hosted the modern Summer Olympic Games three times, London has a diverse range of people and cultures, and more than 300 languages are spoken in the region. Its estimated mid-2015 municipal population was 8,673,713, the largest of any city in the European Union, Londons urban area is the second most populous in the EU, after Paris, with 9,787,426 inhabitants at the 2011 census. The citys metropolitan area is the most populous in the EU with 13,879,757 inhabitants, the city-region therefore has a similar land area and population to that of the New York metropolitan area. London was the worlds most populous city from around 1831 to 1925, Other famous landmarks include Buckingham Palace, the London Eye, Piccadilly Circus, St Pauls Cathedral, Tower Bridge, Trafalgar Square, and The Shard. The London Underground is the oldest underground railway network in the world, the etymology of London is uncertain. It is an ancient name, found in sources from the 2nd century and it is recorded c.121 as Londinium, which points to Romano-British origin, and hand-written Roman tablets recovered in the city originating from AD 65/70-80 include the word Londinio. The earliest attempted explanation, now disregarded, is attributed to Geoffrey of Monmouth in Historia Regum Britanniae and this had it that the name originated from a supposed King Lud, who had allegedly taken over the city and named it Kaerlud. From 1898, it was accepted that the name was of Celtic origin and meant place belonging to a man called *Londinos. The ultimate difficulty lies in reconciling the Latin form Londinium with the modern Welsh Llundain, which should demand a form *lōndinion, from earlier *loundiniom. The possibility cannot be ruled out that the Welsh name was borrowed back in from English at a later date, and thus cannot be used as a basis from which to reconstruct the original name. Until 1889, the name London officially applied only to the City of London, two recent discoveries indicate probable very early settlements near the Thames in the London area
