1.
Polish language
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Polish is a West Slavic language spoken primarily in Poland and is the native language of the Poles. It belongs to the Lechitic subgroup of the West Slavic languages, Polish is the official language of Poland, but it is also used throughout the world by Polish minorities in other countries. It is one of the languages of the European Union. Its written standard is the Polish alphabet, which has 9 additions to the letters of the basic Latin script, Polish is closely related to Kashubian, Silesian, Upper Sorbian, Lower Sorbian, Czech and Slovak. It is also the second most widely spoken Slavic language, after Russian, in history, Polish is known to be an important language, both diplomatically and academically in Central and Eastern Europe. Today, Polish is spoken by over 38.5 million people as their first language in Poland. It is also spoken as a language in western parts of Belarus and Ukraine, west and central Lithuania, as well as the northern parts of the Czech Republic. There are 55 million Polish language speakers around the world, Polish began to emerge as a distinct language around the 10th century, the process largely triggered by the establishment and development of the Polish state. With Christianity, Poland also adopted the Latin alphabet, which made it possible to write down Polish, the precursor to modern Polish is the Old Polish language. Ultimately, Polish is thought to descend from the unattested Proto-Slavic language, Poland is the most linguistically homogeneous European country, nearly 97% of Polands citizens declare Polish as their first language. Elsewhere, Poles constitute large minorities in Lithuania, Belarus, Polish is the most widely used minority language in Lithuanias Vilnius County and is found elsewhere in southeastern Lithuania. There are significant numbers of Polish speakers among Polish emigrants and their descendants in many other countries, in the United States, Polish Americans number more than 11 million but most of them cannot speak Polish fluently. The largest concentrations of Polish speakers reported in the census were found in three states, Illinois, New York, and New Jersey. Enough people in these areas speak Polish that PNC Financial Services offer services available in Polish at all of their machines in addition to English and Spanish. According to the 2011 census there are now over 500,000 people in England, in Canada, there is a significant Polish Canadian population, There are 242,885 speakers of Polish according to the 2006 census, with a particular concentration in Toronto and Montreal. The geographical distribution of the Polish language was affected by the territorial changes of Poland immediately after World War II. Poles settled in the Recovered Territories in the west and north and this tendency toward a homogeneity also stems from the vertically integrated nature of the authoritarian Polish Peoples Republic. The inhabitants of different regions of Poland still speak standard Polish somewhat differently, first-language speakers of Polish have no trouble understanding each other, and non-native speakers may have difficulty distinguishing regional variations
2.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
3.
Lesser Poland Voivodeship
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Lesser Poland Voivodeship, also known as Małopolska Voivodeship or Małopolska Province, is a voivodeship, in southern Poland. It has an area of 15,108 square kilometres, the provinces name recalls the traditional name of a historic Polish region, Lesser Poland, or in Polish, Małopolska. Current Lesser Poland Voivodeship, however, covers only part of the broader ancient Małopolska region which, together with Greater Poland and Silesia. Historic Lesser Poland is much larger than the current province and it stretches far north, to Radom, and Siedlce, also including such cities, as Stalowa Wola, Lublin, Kielce, Częstochowa, and Sosnowiec. The province is bounded on the north by the Świętokrzyskie Mountains, on the west by Jura Krakowsko-Częstochowska, politically it is bordered by Silesian Voivodeship to the west, Świętokrzyskie Voivodeship to the north, Subcarpathian Voivodeship to the east, and Slovakia to the south. Almost all of Lesser Poland lies in the Vistula River catchment area, the city of Kraków was one of the European Cities of Culture in 2000. Kraków has railway and road connections with Katowice, Warsaw, Wrocław and it lies at the crossroads of major international routes linking Dresden with Kiev, and Gdańsk with Budapest. Located here is the second largest international airport in Poland, the John Paul II International Airport, the regions economy includes high technology, banking, chemical and metallurgical industries, coal, ore, food processing, and spirit and tobacco industries. The most industrialized city of the voivodeship is Kraków, the largest regional enterprise operates here, the Tadeusz Sendzimir Steelworks in Nowa Huta, employing 17,500 people. Another major industrial center is located in the west, in the neighborhood of Chrzanów, Kraków Park Technologiczny, a Special Economic Zone, has been established within the voivodeship. There are almost 210,000 registered economic entities operating in the voivodeship, mostly small and medium-sized, foreign investment, growing in the region, reached approximately US$18.3 billion by the end of 2006. 130,000 students attend fifteen Kraków institutions of higher learning, the Jagiellonian University, the largest university in the city, was founded in 1364 as Cracow Academy. Nicolaus Copernicus and Karol Wojtyła graduated from it, the AGH University of Science and Technology is considered to be the best technical university in Poland. The Academy of Economics, the Pedagogical University, the Kraków University of Technology, there are also the Fine Arts Academy, the State Theatre University and the Musical Academy. Nowy Sącz has become an educational center in the region thanks to its Higher School of Business and Administration, with an American curriculum. There are also two higher schools in Tarnów. The city of Tarnów, which is located in Lesser Poland, is the hottest place in Poland all year round and it all depends on the many various wind patters that affect Poland from different regions of the world. Błędów Desert the only desert in Poland is located in Lesser Poland, four national parks and numerous reserves have been established in the voivodeship to protect the environment of Lesser Poland
4.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
5.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
6.
Giewont
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Giewont is a mountain massif in the Tatra Mountains of Poland, and is 1,895 metres AMSL at its highest. It comprises three peaks, Small Giewont - Great Giewont - Long Giewont -, there is a mountain pass located between Great and Long Giewont, known as Szczerba. It is located between the valleys of Kondratowa, Małej Łąki and Strążyska, Long Giewont and Great Giewont are situated at a higher altitude than the nearby town of Zakopane, making them clearly visible from that city. On Great Giewont, there is a 15 m steel cross - the site of religious pilgrimages, the area is notorious for its hazardous nature during thunderstorms, so this should be taken into consideration when approaching the summit. Geologically, Giewont is composed of dolomite and limestone caves, as well as gneiss, the first recorded ascent to Giewonts summit was undertaken in 1830 by Franciszek Herbich and Aleksander Zawadzki. The first winter ascent of Giewont occurred in 1904 by a group of five led by Mariusz Zaruski. Nowadays the climbing on Giewont is strictly banned, on the other hand hiking on the hiking trials is allowed and the access is not difficult hence Giewont is a very popular destination among amblers and Sunday tourists. In the summer up to few thousands tourists a day ascend the top, Giewont lies in the area of the Polish Tatra National Park. In Polish folklore it is associated with a legend about oversleeping knights, the profile of the mountains is similar to a lying knight, wherein the Long Giewont is the knights torso, and the Great Giewont is the knights face as viewed from the side. The image of Giewont as viewed from the north makes the profile easy to discern, Giewont webcam - click Day at a Glance if night
7.
Tatra Mountains
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The Tatra Mountains, Tatras or Tatra, are a mountain range that form a natural border between Slovakia and Poland. They are the highest mountain range in the Carpathian Mountains, the Tatras should be distinguished from the Low Tatras which are located south of the Tatra Mountains in Slovakia. The Tatra Mountains occupy an area of 785 square kilometres, of which about 610 square kilometres lie within Slovakia, the highest peak, called Gerlach, at 2,655 m is located north of Poprad. The highest point in Poland, Rysy, at 2,499 m is located south of Zakopane. The Tatras length, measured from the foothills of the Kobyli Wierch to the southwestern foot of Ostry Wierch Kwaczański, in a straight line is 57 km. The range is only 19 km wide, the Tatras main ridge leads from Huciańska Pass in the west to Zdziarska Pass to the east. In 1992 the Polish and Slovak parks were designated a transboundary biosphere reserve by UNESCO in the World Network of Biosphere Reserves under its Man. It is the highest mountain range within Carpathians, by the end of the First Polish Republic and the Polish border between the Kingdom of Hungary in the Tatras was not strictly defined. The Tatras became an unoccupied borderland, two years later, the First Partition of Poland allocated the lands to Austria. In 1824, Zakopane good and Fish Creek Valley with Morskie Oko purchased from the authorities of the Austrian Hungarian Emanuel Homolacs. In 1867 formed the Austria-Hungary and the Tatra Mountains have become imaginary border between the two states of the monarchy, but the border still has not been exactly determined. In 1889, Count Władysław Zamoyski purchased at auction a good Zakopane, due to numerous disputes over lands belonging in the late nineteenth century, attempts were made to the delimitation of the border. They did not bring effect in 1897, and the case went to a court that on September 13,1902 determined the exact course of the Austria-Hungary border in the disputed area. The Tatras lie in the zone of Central Europe. They are an important barrier to the movements of air masses and their mountainous topography causes one of the most diverse climates in that region. Winds The average wind speed on the summits is 6 m/s. southerly winds on the northern side westerly winds at the base of Tatra foehn winds most often occur between October and May and they are warm and dry and can cause extensive damage. On 19 November 2004, large parts of the forests in the southern Slovak part of the High Tatras were damaged by a wind storm. Three million cubic metres of trees were uprooted, two died and several villages were totally cut off
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Media related to Western Tatras at Wikimedia Commons