1.
Great Plains
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The region is known for supporting extensive cattle ranching and dry farming. The Canadian portion of the Plains is known as the Prairies, some geographers include some territory of northern Mexico in the Plains, but many stop at the Rio Grande. The term Great Plains is used in the United States to describe a sub-section of the even more vast Interior Plains physiographic division and it also has currency as a region of human geography, referring to the Plains Indians or the Plains States. There is no region referred to as the Great Plains in The Atlas of Canada, in terms of human geography, the term prairie is more commonly used in Canada, and the region is known as the Prairie Provinces or simply the Prairies. The region is about 500 mi east to west and 2,000 mi north to south, much of the region was home to American bison herds until they were hunted to near extinction during the mid/late 19th century. It has an area of approximately 500,000 sq mi, current thinking regarding the geographic boundaries of the Great Plains is shown by this map at the Center for Great Plains Studies, University of Nebraska–Lincoln. The term Great Plains, for the region west of about the 96th or 98th meridian, nevin Fennemans 1916 study, Physiographic Subdivision of the United States, brought the term Great Plains into more widespread usage. Before that the region was almost invariably called the High Plains, today the term High Plains is used for a subregion of the Great Plains. The Great Plains are the westernmost portion of the vast North American Interior Plains, during the Cretaceous Period, the Great Plains were covered by a shallow inland sea called the Western Interior Seaway. However, during the Late Cretaceous to the Paleocene, the seaway had begun to recede, leaving thick marine deposits. During the Cenozoic era, specifically about 25 million years ago during the Miocene and Pliocene epochs, existing forest biomes declined and grasslands became much more widespread. The grasslands provided a new niche for mammals, including many ungulates and glires, traditionally, the spread of grasslands and the development of grazers have been strongly linked. The vast majority of animals became extinct in North America at the end of the Pleistocene. In general, the Great Plains have a variety of weather through the year, with very cold and harsh winters and very hot. Wind speeds are very high, especially in winter. Grasslands are among the least protected biomes, humans have converted much of the prairies for agricultural purposes or to create pastures. The Great Plains have dust storms mostly every year or so, the 100th meridian roughly corresponds with the line that divides the Great Plains into an area that receive 20 in or more of rainfall per year and an area that receives less than 20 in. The region is subjected to extended periods of drought, high winds in the region may then generate devastating dust storms
2.
Hungarian language
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Hungarian is the official language of Hungary and one of the 24 official languages of the European Union. Outside Hungary it is spoken by communities of Hungarian people in neighbouring countries. Like Finnish and Estonian, it belongs to the Uralic language family, its closest relatives being Mansi and it is one of several European languages not part of the Indo-European languages, and the most widely-spoken European language that does not belong to the Indo-European family. The Hungarian name for the language is magyar or magyar nyelv, the word Magyar is used as an English and Hungarian word to refer to Hungarian people as an ethnic group. Hungarian is a member of the Uralic language family, the name of Hungary could be a result of regular sound changes of Ungrian/Ugrian, and the fact that the Eastern Slavs referred to Hungarians as Ǫgry/Ǫgrove seemed to confirm that. Current literature favors the hypothesis that it comes from the name of the Turkic tribe Onogur, there are numerous regular sound correspondences between Hungarian and the other Ugric languages. For example, Hungarian /aː/ corresponds to Khanty /o/ in certain positions, for example, Hungarian ház house vs. Khanty xot house, and Hungarian száz hundred vs. Khanty sot hundred. The distance between the Ugric and Finnic languages is greater, but the correspondences are also regular, during the later half of the 19th century, a competing hypothesis proposed a Turkic affinity of Hungarian. Following an academic debate known as Az ugor-török háború, the Finno-Ugric hypothesis was concluded the sounder of the two, foremost based on work by the German linguist Josef Budenz. The traditional view argues that the Hungarian language separated from its Ugric relatives in the first half of the 1st millennium b. c. e. in western Siberia, east of the southern Urals. The Hungarians gradually changed their lifestyle from settled hunters to nomadic pastoralists, in Hungarian, Iranian loans date back to the time immediately following the breakup of Ugric and probably span well over a millennium. Among these include tehén ‘cow’, tíz ‘ten’, tej ‘milk’, increasing archaeological evidence from present-day southern Bashkortostan found in the previous decades confirms the existence of Hungarian settlements between the Volga River and Ural Mountains. The Onogurs later had a influence on the language, especially between the 5th-9th centuries. This layer of Turkic loans is large and varied, and includes words borrowed from Oghur Turkic, e. g. borjú ‘calf’, dél ‘noon, many words related to agriculture, to state administration or even to family relations have such backgrounds. Hungarian syntax and grammar were not influenced in a dramatic way during these 300 years. After the arrival of the Hungarians into the Carpathian Basin the language came into contact with different speech communities, Turkic loans from this period come mainly from the Pechenegs and Cumanians who settled in Hungary during the 12th-13th centuries, e. g. koboz ‘cobza’, komondor ‘mop dog’. Hungarian borrowed many words from especially the neighbouring Slavic languages, in exchange, these languages also borrowed words from Hungarian, e. g. Serbo-Croatian ašov from Hung ásó ‘spade’. Approximately 1. 6% of the Romanian lexicon is of Hungarian origin, on the basis of the growing genetic evidence, the accepted origin theory is contested by geneticists too
3.
Hungary
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Hungary is a unitary parliamentary republic in Central Europe. With about 10 million inhabitants, Hungary is a member state of the European Union. The official language is Hungarian, which is the most widely spoken language in Europe. Hungarys capital and largest metropolis is Budapest, a significant economic hub, major urban areas include Debrecen, Szeged, Miskolc, Pécs and Győr. His great-grandson Stephen I ascended to the throne in 1000, converting the country to a Christian kingdom, by the 12th century, Hungary became a middle power within the Western world, reaching a golden age by the 15th century. Hungarys current borders were established in 1920 by the Treaty of Trianon after World War I, when the country lost 71% of its territory, 58% of its population, following the interwar period, Hungary joined the Axis Powers in World War II, suffering significant damage and casualties. Hungary became a state of the Soviet Union, which contributed to the establishment of a four-decade-long communist dictatorship. On 23 October 1989, Hungary became again a democratic parliamentary republic, in the 21st century, Hungary is a middle power and has the worlds 57th largest economy by nominal GDP, as well as the 58th largest by PPP, out of 188 countries measured by the IMF. As a substantial actor in several industrial and technological sectors, it is both the worlds 36th largest exporter and importer of goods, Hungary is a high-income economy with a very high standard of living. It keeps up a security and universal health care system. Hungary joined the European Union in 2004 and part of the Schengen Area since 2007, Hungary is a member of the United Nations, NATO, WTO, World Bank, the AIIB, the Council of Europe and Visegrád Group. Well known for its cultural history, Hungary has been contributed significantly to arts, music, literature, sports and science. Hungary is the 11th most popular country as a tourist destination in Europe and it is home to the largest thermal water cave system, the second largest thermal lake in the world, the largest lake in Central Europe, and the largest natural grasslands in Europe. The H in the name of Hungary is most likely due to historical associations with the Huns. The rest of the word comes from the Latinized form of Medieval Greek Oungroi, according to an explanation the Greek name was borrowed from Proto-Slavic Ǫgǔri, in turn borrowed from Oghur-Turkic Onogur. Onogur was the name for the tribes who later joined the Bulgar tribal confederacy that ruled the eastern parts of Hungary after the Avars. The Hungarians likely belonged to the Onogur tribal alliance and it is possible they became its ethnic majority. The Hungarian endonym is Magyarország, composed of magyar and ország, the word magyar is taken from the name of one of the seven major semi-nomadic Hungarian tribes, magyeri
4.
Pannonian Basin
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The Pannonian Basin or Carpathian Basin is a large basin in Central Europe. It is a subsystem of the Alps-Himalaya system. Most of the consists of the Great Hungarian Plain and the Little Hungarian Plain. The Pannonian Basin lies in the part of Central Europe. It forms a discrete unit set in the European landscape, surrounded by imposing geographic boundaries - the Carpathian Mountains, the Alps, the Dinarides. The Rivers Danube and Tisza divide the basin roughly in half and it extends roughly between Vienna in the northwest, Zagreb in the southwest, Belgrade in the southeast and Satu Mare in the northeast. The name Pannonian comes from Pannonia, a province of the Roman Empire, in English, the terms Pannonian Basin and Carpathian Basin are used synonymously. The name Pannonian is taken from that of Pannonia, a province of the Roman Empire, the historical province overlapped but was not coterminous with the geographical plain or basin. Pannonia Inferior covered much of the half of the basin. Pannonia Superior included the western fringe of the basin as well as part of the Eastern Alps, the southern fringe of the basin was in Dalmatia and Moesia. The eastern half of the basin was not conquered by the Romans, likewise, the parts north of the Danube were not in the empire, they were considered part of Germania, inhabited by the Quadi. The term Pannonian Plain refers to the parts of the Pannonian Basin as well as those of some adjoining regions like Lower Austria, Moravia, Bosnia. The lands adjoining the plain proper are also called peri-Pannonian. In Hungarian geographical literature various subdivisions of the Carpathian Mountains are also considered parts of the Carpathian Basin on the basis of traditional geopolitical divisions, julius Pokorny derived the name Pannonia from Illyrian, from the Proto-Indo-European root *pen-, swamp, water, wet. For its early settlers, the plain offered few sources of metals or stone, thus when archaeologists come upon objects of obsidian or chert, copper or gold, they have almost unparalleled opportunities to interpret ancient pathways of trade. The Pannonian plain is divided into two parts along the Transdanubian Mountains, the northwestern part is called Western Pannonian plain and the southeastern part Eastern Pannonian plain. The plain was named after the Pannon named Medes, various different peoples inhabited the plain during its history. In the first century BC, the parts of the plain belonged to the Dacian state
5.
Carpathian Mountains
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The Carpathian Mountains or Carpathians are a mountain range system forming an arc roughly 1,500 km long across Central and Eastern Europe, making them the second-longest mountain range in Europe. The Carpathians and their foothills also have many thermal and mineral waters, the Carpathians consist of a chain of mountain ranges that stretch in an arc from the Czech Republic in the northwest through Slovakia, Poland, Hungary and Ukraine to Romania and Serbia. The highest range within the Carpathians is the Tatras, on the border of Slovakia and Poland, the second-highest range is the Southern Carpathians in Romania, where the highest peaks exceed 2,500 m. The divisions of the Carpathians are usually in three sections, Western Carpathians — Czech Republic, Poland, and Slovakia. Eastern Carpathians — southeastern Poland, eastern Slovakia, Ukraine, Romania, the term Outer Carpathians is frequently used to describe the northern rim of the Western and Eastern Carpathians. The most important cities in or near the Carpathians are, Bratislava and Košice in Slovakia, Kraków in Poland, Cluj-Napoca, Sibiu and Braşov in Romania, and Uzhhorod in Ukraine. In modern times, the range is called Karpaty in Czech, Polish, Slovak and Карпати in Ukrainian, Carpați in Romanian, Karpaten in German, Kárpátok in Hungarian and Karpati or Карпати in Serbian. Although the toponym was recorded already by Ptolemy in the 2nd century CE, for instance, Havasok was its medieval Hungarian name, Rus and Romanian chronicles referred to it as Hungarian Mountains. The archaic Polish word karpa meant rugged irregularities, underwater obstacles/rocks, the more common word skarpa means a sharp cliff or other vertical terrain. In late Roman documents, the Eastern Carpathian Mountains were referred to as Montes Sarmatici, the Western Carpathians were called Carpates, a name that is first recorded in Ptolemys Geographia. In the Scandinavian Hervarar saga, which relates ancient Germanic legends about battles between Goths and Huns, the name Karpates appears in the predictable Germanic form as Harvaða fjöllum, inter Alpes Huniae et Oceanum est Polonia by Gervase of Tilbury, has described in his Otia Imperialia in 1211. Thirteenth- to fifteenth-century Hungarian documents named the mountains Thorchal, Tarczal or less frequently Montes Nivium, the northwestern Carpathians begin in Slovakia and southern Poland. They surround Transcarpathia and Transylvania in a semicircle, sweeping towards the southeast. The total length of the Carpathians is over 1,500 km, the highest altitudes of the Carpathians occur where they are widest. The Carpathians cover an area of 190,000 km2 and, after the Alps, although commonly referred to as a mountain chain, the Carpathians do not actually form an uninterrupted chain of mountains. Rather, they consist of several orographically and geologically distinctive groups, the Carpathians at their highest altitude are only as high as the middle region of the Alps, with which they share a common appearance, climate, and flora. The Carpathians are separated from the Alps by the Danube, the two ranges meet at only one point, the Leitha Mountains at Bratislava. The river also separates them from the Balkan Mountains at Orşova in Romania, the valley of the March and Oder separates the Carpathians from the Silesian and Moravian chains, which belong to the middle wing of the great Central Mountain System of Europe
6.
Sava
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The Sava is a river in Central and Southeastern Europe, a right tributary of the Danube. It flows through Slovenia, Croatia, along the border of Bosnia and Herzegovina. Its central part is a border of Bosnia-Herzegovina and Croatia. The Sava forms the border of the Balkan Peninsula. The Sava is 990 kilometres long, including the 45-kilometre Sava Dolinka headwater rising in Zelenci and it is the greatest tributary of the Danube by volume of water, and second-largest after Tisza in terms of catchment area and length. It drains a significant portion of the Dinaric Alps region, through the tributaries of Drina, Bosna, Kupa, Una, Vrbas, Lonja, Kolubara, Bosut. The Sava is one of the longest rivers in Europe and among a handful of European rivers of that length that do not drain directly into a sea. The population in the Sava River basin is estimated at 8,176,000, the Sava is navigable for larger vessels from the confluence of the Kupa River in Sisak, Croatia, approximately two-thirds of its length. The Sava River is formed from the Sava Dolinka and the Sava Bohinjka headwaters in northwest Slovenia, the Sava Dolinka rises at the Zelenci Pools near Kranjska Gora, Slovenia, in a valley separating the Julian Alps from the Karavanke mountain range. The spring is located near the Slovene-Italian border at 833 metres above sea level, the Sava Dolinka spring is fed by groundwater possibly exhibiting bifurcation of source karst aquifer to the Sava and Soča basins. Nadiža creek, a losing stream flowing nearby, is the source of Zelenci Pools water. The Sava Dolinka is considered the Savas initial, 45-kilometre segment, the Sava Bohinjka originates in Ribčev Laz, at the confluence of the Jezernica, a short watercourse flowing out from Lake Bohinj and the Mostnica River. The watercourse flows 41 kilometres —including the length of the Savica—east to Radovljica, downstream from the confluence, the river is referred to as the Sava. The Sava is located in Southeast Europe, flowing through Slovenia, Croatia, Serbia and its total length is 990 kilometres, including the 45-kilometre Sava Dolinka and the 945-kilometre Sava proper. As a right tributary of the Danube, the river belongs to the Black Sea drainage basin and it is also the largest tributary of the Danube by discharge. The river course is used to describe the northern boundary of the Balkans. Before the breakup of Yugoslavia in 1991, the river was located completely inside Yugoslav borders, downstream of Radovljica, the Sava proceeds southeast towards Kranj. Between Kranj and Medvode, its course comprises the Lake Trboje and the Lake Zbilje reservoirs, built for the Mavčiče, the Sava then flows through the capital of Slovenia, Ljubljana, where another reservoir is located on the river, adjacent to the Tacen Whitewater Course
7.
Tisza
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The Tisza or Tisa is one of the main rivers of Central Europe. Once, it was called the most Hungarian river because it flowed entirely within the Kingdom of Hungary, today, it crosses several national borders. The Tisza begins near Rakhiv in Ukraine, at the confluence of the White Tisa, from there, the Tisza flows west, roughly following Ukraines borders with Romania, then Hungary, and finally Serbia. It traverses Hungary from north to south, a few kilometers south of the Hungarian city of Szeged, it enters Serbia. Finally, it joins the Danube near the village of Novi Slankamen in Vojvodina, the Tisza drains an area of about 156,087 km2 and has a length of 965 km —the largest catchment and greatest length of any of the Danubes tributaries. Its mean annual discharge is 792 m3/s and it contributes about 13% of the Danubes total runoff. Attila the Hun is said to have been buried under a section of the river Tisza. The river was known as the Tisia in antiquity, other ancient names for it included Tissus and Pathissus and it may be referred to as the Theiss in older English references, after the German name for the river, Theiß. It is known as the Tibisco in Italian, and in older French references it is referred to as the Tibisque. Modern names for the Tisza in the languages of the countries it flows through include, Romanian, Tisa, Ukrainian, Тиса, Slovak, Tisa, Hungarian, Tisza, Serbian, Тиса, the length of the Tisza in Hungary used to be 1419 km. It flowed through the Great Hungarian Plain, which is one of the largest flat areas in central Europe. Since plains can cause a river to flow very slowly, the Tisza used to follow a path with curves and turns. After several small-scale attempts, István Széchenyi organised the regulation of the Tisza which started on August 27,1846, and substantially ended in 1880. The new length of the river in Hungary was 966 km, in the 1970s, the building of the Tisza Dam at Kisköre started with the purpose of helping to control floods as well as storing water for drought seasons. However, the resulting Lake Tisza became one of the most popular tourist destinations in Hungary since it had similar features to Lake Balaton at drastically cheaper prices and was not crowded, the Tisza is navigable over much of its course. The river opened up for international navigation only recently, before, Hungary distinguished national rivers and international rivers, after Hungary joined the European Union, this distinction was lifted and vessels were allowed on the Tisza. Conditions of navigation differ with the circumstances, when the river is in flood, it is often unnavigable, the Tisza has a rich and varied wildlife. Over 200 species of birds reside in the reserve of Tiszafűred
Great Hungarian Plain travel guide from Wikivoyage
