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Trångsund

Trångsund

Trångsund is a part of Huddinge to the south of Stockholm located between thw two lakes Magelungen and Drevviken. The region Trångsund/Skogås has about 21 500 inhabitants. From Trångsund it's a 20 minute travel to Stockholm central by train. Category:Metropolitan Stockholm

Huddinge

Huddinge Municipality is a Swedish municipality in Stockholm County, in central Sweden, within Metropolitan Stockholm. It is the most populated municipality in Stockholm County after Stockholm itself.

Geography

The municipality covers the entire central part of the Södertörn peninsula. More than half of the land area consists of agriculture, forests, hills or lakes, and it contains five nature reserves. Huddinge borders to Stockholm City, Ekerö (by water), Botkyrka, Haninge and Tyresö (by water).

Demography

Huddinge houses a total population of roughly 88,000, or 4,5 % of the population in Stockholm County. The average age is 36,7 years, but one third of the population is under 25 years of age. This means that Huddinge has a slightly younger population than both Stockholm County (38,9 yrs.) and the whole kingdom (40,6 yrs.). The population density of the municipality is increasing significantly. Since the 1960's the population has doubled in size and is currently among the 20 largest municipalities of Sweden.

History

It is believed that the history of Huddinge goes back at least 1,000 years, to before the Viking Age. When hostile ships approached the community, the inhabitants in Huddinge would climb to a high locations and light beacons, as the did in the movie Lord of the Rings. There were beacons located around the entire lake Mälaren. This procedure has formed the city arms of Huddinge.

Subdivisions

Huddinge municipality is sub-divided into six districts:
- Skogås/Trångsund (pop. 22,223)
- Sjödalen/Fullersta (pop. 18,439)
- Stuvsta/Snättringe (pop. 14,879)
- Flemingsberg (pop. 12,682)
- Segeltorp (pop. 10,507)
- Vårby (pop. 9,271). These areas occupy four congregations: Huddinge, Trångsund, Flemingsberg and S:t Mikael.

Culture

The municipality contains six public libraries and Södertörn University College. Kungens Kurva is one of Sweden's largest places of merchancy. It hosts, among other things, the largest IKEA store in the world, the largest cinema in the country, and a large shopping centre. In total, it generates a turnover of 6 billion crowns and has 15 million visitors per year.

External links

- [http://www.huddinge.se/ Huddinge] - Official site
- [http://zeal.com/category/preview.jhtml?cid=10215924 Huddinge Municipality] - Links at Zeal.com Category:Municipalities of Sweden Category:Municipalities of Stockholm County Category:Metropolitan Stockholm

Lake

A Lake is a body of water surrounded by land. The majority of lakes are fresh water, and most lie in the northern hemisphere at higher latitudes. Large lakes are sometimes referred to as "inland seas" and small seas are sometimes referred to as lakes. The term lake is also used to describe a feature such as Lake Eyre, which is dry most of the time but becomes filled under seasonal conditions of heavy rainfall. Many lakes are artificial and are constructed for hydro-electric power supply, recreation (swimming, wind surfing,...), water supply, etc. Finland is known as The Land of the Thousands Lakes (actually there are 187,888 lakes in Finland, 60,000 of them are big ones) and Minnesota is known as The Land of Ten Thousand Lakes. The Great Lakes of North America originated in the ice age. Over 60% of the world's lakes are in Canada; this is because of the deranged drainage system that dominates the country.

Origin of natural lakes

Most lakes are young, as the natural results of erosion will tend to wear away one of the basin sides containing the lake. There are a number of natural processes that can form lakes. A recent tectonic uplift of a mountain range can create bowl-shaped depressions that accumulate water and form lakes. The advance and retreat of glaciers can scrape depressions in the surface where lakes accumulate. Such lakes are common in Scandinavia, Siberia and Canada. Lakes can also form by means of landslides or by glacial blockages. An example of the latter occurred during the last ice age in the state of Washington, when a huge lake formed behind a glacial flow. When the ice retreated, the result was an immense flood that created the Dry Falls Monument at Sun Lakes, Washington. Saline lakes can form where there is no natural outlet or the water evaporates rapidly, and the drainage surface of the water table has a higher than normal salt content. Examples of salt lakes include the Great Salt Lake, the Caspian Sea and the Dead Sea. Small, crescent-shaped lakes called oxbow lakes can form in river valleys as the result of meandering. The slow-moving river forms a sinuous shape as the outer side of bends is torn away more rapidly than the inner side. Eventually a horseshoe bend is formed and the river cuts through the narrow neck. This gap now forms the main passage for the river and the ends of the bend become silted up. Lake Vostok is an under-ice lake in Antarctica, possibly the largest in the world. The pressure from ice and the internal chemical composition means that if the lake were drilled into, it may result in a fissure and spraying in the same manner as a shaken can of soda. Some lakes, like Lake Baikal and Lake Tanganyika are volcanic in origin, and lie on geological fault lines. The Crater Lake in Oregon is a lake located within the caldera of an extinct volcano. Some lakes come into existence as a result of sinkhole activity.

Characteristics

The change in level of a lake is controlled by the difference between the sources of inflow and outflow, compared to the total volume of the lake. The significant input sources are precipitation onto the lake; runoff carried by streams and channels from the lake's catchment area; groundwater channels and aquifers, and man-made sources from outside the catchment area. Output sources are evaporation from the lake; surface and groundwater flows, and any extraction of lake water by humans. As climate conditions and human water requirements vary, these will create fluctuations in the lake level. Lakes can be categorized on the basis of their richness of nutrients, which typically effects plant growth. Nutrient poor lakes are said to be oligotrophic, and are generally clear, having a low concentration of plant life. Mesotropic lakes have good clarity and an average level of nutrients. Eutrophic lakes are enriched with nutrients, resulting in good plant growth and possible algal blooms. A hypertrophic lake is a water body that has been highly enriched with nutrients. These lakes typically have poor clarity and are subject to algal blooms. Lakes typically reach this condition due to human activities, such as heavy use of fertilizers in the lake catchment area. Such lakes are of little use, and have a poor ecosystem.

Types of lakes

A periglacial lake is one in which part of its margin is formed by an ice sheet, ice cap or glacier, the ice having obstructed the natural drainage of the land. A subglacial lake is one which is permanently covered by ice. They can occur under glaciers and ice caps or ice sheets. There are many such lakes, but Lake Vostok in Antarctica is by far the largest. The are kept liquid because the overlying ice acts as a thermal insulator retaining energy introduced to its underside by friction, water percolating through crevasses, by the pressure from the mass of the ice sheet above or by geothermal heating below. Because of the unusual relationship between water's temperature and its density, the water in lakes in temperate climates mixes twice a year. Fresh water is most dense at about 4 degrees Celsius. When the temperature of the water at the surface of a lake reaches the temperature at which water is most dense all the water in the lake can mix, bringing oxygen starved water up from the depths, and bringing oxygen down to decomposing sediments. When the density of surface water differs from that of the deeper water there is a marked barrier layer, the thermocline, that prevents mixing. Deep Temperate lakes can maintain a reservoir of cold water year-round. The reservoir of deep, cold water allows cities to tap that reservoir for deep lake water cooling. Since the water of deep tropical lakes never reaches the temperature where water reaches its maximum density, there is no process that makes the water mix. The deeper layer becomes oxygen starved, and can become saturated with carbon dioxide, and possibly other gases, like sulfur dioxide, if there is even a trace of volcanic activity. Exceptional events, like earthquakes or landslides, which do cause mixing, that brings up the deep layers, can release a vast cloud of toxic gas. The amount of gas that can be dissolved in water is pressure related. As the water surfaces, and the pressure drops, a vast amount of gas cab comes out of solution. Under these circumstances even carbon dioxide is toxic. Carbon dioxide is heavier than air, and the released carbon dioxide flows down the river valley.

Artificial lakes

A reservoir (French: réservoir) is an artificial lake created by flooding land behind a dam. Some of the world's largest lakes are reservoirs. Artificial lakes can also be made deliberately by digging one or by flooding an open-pit mine.

Abiotic and biotic limnology

mine Limnology divides lakes in three zones: littoral zone, which is a sloped area that is close to land; open-water zone, where sunlight is abundant; and deep-water zone, where little sunlight can reach. The depth which light can reach in lakes depends on the density and motion of particles. These particles can be sedimentary or biological in origin and are responsible for the color of the water. Decaying plant matter for instance is responsible for a yellow or brown color, while algae result in greenish water. In very shallow water bodies, iron oxides make water reddish brown. Biological particles are algae and detritus. A sediment particle is in suspension if its weight is less than the random turbidity forces acting upon it. The turbidity is a decisive factor in the transparency of the water. Bottom-dwelling detritivorous fish are responsible for turbid waters, because they stir the mud in search for food. Piscivorous fish eat plant-eating (planktonivorous) fish, thus increasing the number of algae (see aquatic trophic cascade). The light depth or transparency is measured by using a Secchi disk. This is a 20 cm disk with alternating white and black quadrants. The depth at which the disk is no longer visible, is the Secchi depth, and is a measure for transparency. It is commonly used to test eutrophication. A lake moderates the surrounding region's temperature and climate because water has a very high specific heat capacity (4186). In the daytime, the lake can cool the land beside it with local winds, resulting in a sea breeze; in the night, it can warm it, forming a land breeze.

How lakes disappear

A lake may be infilled with deposited sediment, and gradually, the lake becomes a wetland, such as a swamp or marsh. An important difference exists between lowland and highland lakes: lowland lakes are more placid, are less rocky/more sedimentary, have a less sloping bottom, and generally contain more plant life. Large water plants (typically reeds) accelerate this closing process significantly because they trap sediment. Turbid lakes, and lakes with much plant-eating fish, tend to disappear slower. A "disappearing" lake (barely noticeable on a human timescale) typically has a water's edge with extensive plant mats. They become a new habitat for other plants (like peat moss, when conditions are right) and animals, many of which are very rare. Gradually, the lake closes, and young peat may form, forming a fen. In lowland river valleys (allowing the river to meander), the presence of peat is explained by the closing of historical oxbow lakes. In the very last stages of succession, more trees would grow in, eventually turning the wetland into a forest. Some lakes can also disappear seasonally; they are called Intermittent lakes and are typical of karstic terrain. A prime example of this is Lake Cerknica in Slovenia. On June 3, 2005 in Bolotnikovo, Russia, a lake called White Lake vanished in a short period of time (minutes). News sources reported government officials theorized that this strange phenomena may have been caused by a shift on soil underneath the lake which drained water to channels leading to Oka River. Neusiedler See, located in Austria and Hungary, dried up several times for a of number years during the past centuries. As of 2005, it is again rapidly losing water, giving rise to the fear that it will be completely dried up by 2010.

Extraterrestrial lakes

At present the surface of the planet Mars is too cold to permit pooling of liquid water on the surface. However geologic evidence appears to confirm that ancient lakes once formed on the surface. It is also possible that volcanic activity on Mars will occasionally melt the subsurface ice, forming large lakes. Under current conditions this water will quickly evaporate or freeze unless insulated in some manner, such as by a coating of volcanic ash. Jupiter's small moon Io is volcanically active due to tidal stresses, and as a result sulfur deposits have accumulated on the surface. Some photographs taken during the Galileo mission appear to show lakes of liquid sulfur on the surface. There are dark basaltic plains on the Moon, similar to lunar maria but smaller, that are called lacus (singular lacus, Latin for "lake"). They were once thought by early astronomers to be literal lakes.

Notable lakes

- The largest lake in the world by surface area is the Caspian Sea. With a surface area of 394,299 sq. km., it has a surface area greater than the next six largest lakes combined.
- The largest freshwater lake, and second largest lake altogether is Lake Superior with a surface area of 82,414 sq. km. It is also the largest lake in North America and is a part of the Great Lakes.
- The deepest lake is Lake Baikal in Siberia, with a bottom at 1,741 m (5,712 ft.) and is the world's largest freshwater lake by volume.
- The highest navigable lake is lake Titicaca, at 3821 m above sea level. It is also the second largest lake in South America.
- The world's highest lake is Lhagba Pool in Tibet at 6,368 m.
- The world's lowest lake is the Dead Sea, at 396 m (1,302 ft.) below sea level. It is also the lake with the highest salt concentration.
- The largest freshwater-lake island is Manitoulin Island on Lake Huron, with a surface area of 2,766 square km.
- The largest lake located on an island is Nettilling Lake on Baffin Island.
- Lake Toba on the island of Sumatra is located in what is probably the largest resurgent caldera on Earth.
- The largest freshwater lake in Europe is Lake Balaton, followed by Lake Geneva.
- Lake Victoria is the largest lake in Africa. It is a part of the Great Lakes of Africa.
- Lake Maracaibo is the largest lake in South America. Lake Titicaca is the largest freshwater lake in South America.
- The largest lake located completely within the boundaries of a single city is Lake Wanapitei in the city of Greater Sudbury, Ontario, Canada. Before the current city boundaries came into effect in 2001, this status was held by Lake Ramsey, also in Sudbury.
- Saimaa is the largest lake in Finland (the land of 187,888 lakes).

External links

- [http://www.highestlake.com/ Lists of the highest lakes in the US and the world]
- [http://www.mlswa.org/lkclassif1.htm Lake Classification Systems]
- [http://www.uklakes.net/ UKLakes Database]
- [http://www.midwestlakes.org/ Midwest Lakes Policy Center] Category:Bodies of water Category:Landforms ko:호수 ja:湖 simple:Lake th:ทะเลสาบ

Train

:For other types of train see train (disambiguation) In rail transport, a train consists of a single or several connected rail vehicles that are capable of being moved together along a guideway to transport freight or passengers from one place to another along a planned route. The guideway (permanent way) usually consists of conventional rail tracks, but might also be monorail or maglev. Propulsion for the train is typically provided by a separate locomotive, or from individual motors in self-propelled multiple units. Power is usually derived from diesel engines or from electricity supplied by trackside systems. Historically the steam engine was the dominant form of locomotive power, and other sources of power (such as horses, pneumatics, or gas turbines) are possible as well. In American railway terminology, a consist is used to describe the group of rail vehicles which make up a train.

Types of trains

railway terminology, Perth ]] There are various types of trains designed for particular purposes, see rail transport operations. A train can consist of a combination of a locomotive and attached railroad cars, or a self-propelled multiple unit (or occasionally a single powered coach, called a railcar). Trains can also be hauled by horses, pulled by a cable, or run downhill by gravity. Special kinds of trains running on corresponding special 'railways' are atmospheric railways, monorails, high-speed railways, Dinky Trains, maglev, rubber-tired underground, funicular and cog railways. cog railway A passenger train may consist of one or several locomotives, and one or more coaches. Alternatively, a train may consist entirely of passenger carrying coaches, some or all of which are powered as a "multiple unit". In many parts of the world, particularly Japan and Europe, high-speed rail is utilized extensively for passenger travel. Freight trains comprise wagons or trucks rather than carriages, though some parcel and mail trains (especially Travelling Post Offices) are outwardly more like passenger trains. In the United Kingdom, a train hauled by two locomotives is said to be "double-headed", and in Canada and the United States it is quite common for a long freight train to be headed by three, four, or even five locomotives. Trains can also be mixed, hauling both passengers and freight, see e.g. Transportation in Mauritania. Such mixed trains became rare in many countries, but were commonplace on the first 19th-century railroads. Special trains are also used for track maintenance; in some places, this is called maintenance of way. A single uncoupled rail vehicle is not technically a train, but is usually referred to as such for signaling reasons.

Motive power

maintenance of way] The first trains were rope-hauled or pulled by horses, but from the early 19th century almost all were powered by steam locomotives. From the 1920s onwards they began to be replaced by less labor intensive and cleaner (but more expensive) diesel locomotives and electric locomotives, while at about the same time self-propelled multiple unit vehicles of either power system became much more common in passenger service. Most countries had replaced steam locomotives for day-to-day use by the 1970s. A few countries, most notably the People's Republic of China where coal is in cheap and plentiful supply, still use steam locomotives, but this is being gradually phased out. Historic steam trains still run in many other countries, for the leisure and enthusiast market. coal Electric traction offers a lower cost per mile of train operation but at a very high initial cost, which can only be justified on high traffic lines. Since the cost per mile of construction is much higher, electric traction is less favored on long-distance lines. Electric trains receive their current via overhead lines or through a third rail electric system.

Passenger trains

Passenger trains have Passenger cars. Passenger trains travel between stations; the distance between stations may vary from under 1 km to much more. Long-distance trains, sometimes crossing several countries, may have a dining or restaurant car; they may also have sleeping cars, but not in the case of high-speed rail, these arrive at their destination before the night falls and are in competition with airplanes in speed. Very long distance trains such as those on the Trans-Siberian railway are usually not high-speed. Very fast trains sometimes tilt, like the Pendolino or Talgo. Tilting is a system where the passenger cars automatically lean into curves, reducing the centrifugal forces acting on passengers and permitting higher speeds on curves in the track with greater passenger comfort. For trains connecting cities, we can distinguish inter-city trains, which do not halt at small stations, and trains that serve all stations, usually known as local trains or "stoppers" (and sometimes an intermediate kind, see also limited-stop). limited-stop For shorter distances many cities have networks of commuter trains, serving the city and its suburbs. Some carriages may be laid out to have more standing room than seats, or to facilitate the carrying of prams, cycles or wheelchairs. Some countries have some double-decked passenger trains for use in conurbations. Double deck high speed and sleeper trains are becoming more common in Europe. Passenger trains usually have emergency brake handles (or a "communication cord") that the public can operate. Abuse is punished by a fine. fine Large cities often have a metro system, also called underground, subway or tube. The trains are electrically powered, usually by third rail, and their railroads are separate from other traffic, without level crossings. Usually they run in tunnels in the city center and sometimes on elevated structures in the outer parts of the city. They can accelerate and decelerate faster than heavier, long-distance trains. A light one- or two-car rail vehicle running through the streets is not called a train but a tram, trolley, light rail vehicle or streetcar, but the distinction is not strict. The term light rail is sometimes used for a modern tram, but it may also mean an intermediate form between a tram and a train, similar to metro except that it may have level crossings. These are often protected with crossing gates. They may also be called a trolley. Maglev trains and monorails represent minor technologies in the train field. The term rapid transit is used for public transport such as commuter trains, metro and light rail. However, in New York City, lines on the New York City Subway have been referred to as "trains".

Freight trains

Passenger train human waste disposal Freight trains have freight cars. Much of the world's freight is transported by train. In the USA the rail system is used mostly for transporting freight (or cargo). Under the right circumstances, transporting freight by train is highly economic, and also more energy efficient than transporting freight by road. Rail freight is most economic when freight is being carried in bulk and over long distances, but is less suited to short distances and small loads. The main disadvantage of rail freight is its lack of flexibility. For this reason, rail has lost much of the freight business to road competition. Many governments are now trying to encourage more freight onto trains, because of the environmental benefits that it would bring. road competition]] There are many different types of freight train, which are used to carry many different kinds of freight, with many different types of wagon. One of the most common types on modern railways are container trains, whereby the containers can be lifted on and off the train by cranes and loaded off or onto trucks or ships. ship in 1992.]] This type of freight train has largely superseded the traditional "box wagon" type of freight train, whereby the cargo had to be loaded or unloaded manually. In some countries "piggy back" trains are used whereby trucks can drive straight onto the train and drive off again when the end destination is reached. A system like this is used on the Channel Tunnel between England and France. Piggy back trains are the fastest growing type of freight trains in the United States, where they are also known as 'trailer on flat car' or TOFC trains. There are also some "inter-modal" vehicles, which have two sets of wheels, for use in a train, or as the trailer of a road vehicle. There are also many other types of wagon, such as "low loader" wagons for transporting road vehicles. There are refrigerator wagons for transporting food. There are simple types of open-topped wagons for transporting minerals and bulk material such as coal and tankers for tranporting liquids and gases. Freight trains are sometimes illegally boarded by passengers who do not wish, or do not have the money, to travel by ordinary means. This is referred to as "Hopping" and is considered by some communities to be a viable form of transport. Most hoppers sneak into train yards and stow away in boxcars. More bold hoppers will catch a train "on the fly", that is, as it is moving, leading to occasional fatalities, some of which go unrecorded.

Famous train routes

Main article: Famous trains Famous historical train services include the:
- Orient Express in Europe.
- Trans-Siberian in Russia.
- Blue Train in South Africa.
- Train-de-Luxe from Johannesburg to Victoria Falls.
- Chihuahua al Pacifico in Mexico.
- Palace on Wheels in Rajasthan, India.
- Frontier Mail and Grand Trunk Express, India.
- The Canadian in Canada.
- 20th Century Limited in the USA.
- City of New Orleans in the USA.
- California Zephyr in the USA.
- The Indian-Pacific and The Ghan in Australia (long-distance rail).
- Puffing Billy and The Gulflander in Australia (heritage and touring).
- Rheingold Express in The Netherlands, Germany and Switzerland, following the course of the Rhine.

Fictional trains

See also: Rail transport in fiction
- Hogwarts Express — Takes Harry Potter to Hogwarts Academy.
- Taggart Comet (Atlas Shrugged)
- The Great Train Robbery — feature film based on a true story, also title of a modern film.
- Starlight Express (Andrew Lloyd Webber) — Musical about an old steam engine being replaced by an electrical engine.
- Galaxy Express 999 — From the manga and anime of the same name by Leiji Matsumoto, this train travels the galaxy from planet to planet.
- The Polar Express — From the book of the same name, this train takes children to the North Pole.
- Runaway Train — Film about escaped inmates on a runaway train.
- Atomic Train — TV movie (1999) A runaway train carrying an atomic bomb into a town.
- Thomas the Tank Engine and Friends TV Series originated from The Railway Series by the Rev.W.Awdry For a list of railway movies, see [http://www.spikesys.com/Trains/rly_movs.html] (website last updated December 5, 1995).

External links

- [http://www.raileurope.co.uk Book European rail travel online]
- [http://www.railfaneurope.net High Speed Train]
- Official [http://ojp.nationalrail.co.uk/planmyjourney/time_table/journey_requirements.asp train times] in the UK (from [http://www.nationalrail.co.uk/ National Rail]).
- [http://www.railserve.com/ RailServe.com: The Internet Railroad Directory] - directory of 10,000 train sites
- [http://www.trainfoamers.com Trainfoamers.com] - It's Free To Talk Trains Again!
- [http://www.trainorders.com Trainorders.com] - Focus on trains of North America Category:Vehicles Category:Rail transport ms:Keretapi ja:列車

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Trångsund

Huddinge

Geography

Demography

History

Subdivisions

Culture

External links

Lake

Origin of natural lakes

Characteristics

Types of lakes

Artificial lakes

Abiotic and biotic limnology

How lakes disappear

Extraterrestrial lakes

Notable lakes

See also

External links

Train

Types of trains

Motive power

Passenger trains

See also

Freight trains

Famous train routes

Fictional trains

See also

Further reading

External links

Mount Aso

Beliefs

Core beliefs and central tenets of Scientology

Definition