Hungarians known as Magyars, are a nation and ethnic group native to Hungary and historical Hungarian lands who share a common culture and language. Hungarians belong to the Uralic-speaking peoples. There are an estimated 14.2–14.5 million ethnic Hungarians and their descendants worldwide, of whom 9.6 million live in today's Hungary. About 2.2 million Hungarians live in areas that were part of the Kingdom of Hungary before the Treaty of Trianon and are now parts of Hungary's seven neighbouring countries Slovakia, Romania, Croatia and Austria. Significant groups of people with Hungarian ancestry live in various other parts of the world, most of them in the United States, Germany, the United Kingdom, Brazil and Argentina. Hungarians can be classified into several subgroups according to local linguistic and cultural characteristics; the Hungarians' own ethnonym to denote themselves in the Early Middle Ages is uncertain. The exonym "Hungarian" is thought to be derived from Oghur-Turkic On-Ogur. Another possible explanation comes from the Old Russian "Yugra".
It may refer to the Hungarians during a time when they dwelt east of the Ural Mountains along the natural borders of Europe and Asia before their conquest of the Carpathian Basin. Prior to the Hungarian conquest of the Carpathian Basin in 895/6 and while they lived on the steppes of Eastern Europe east of the Carpathian Mountains, written sources called the Magyars "Hungarians", specifically: "Ungri" by Georgius Monachus in 837, "Ungri" by Annales Bertiniani in 862, "Ungari" by the Annales ex Annalibus Iuvavensibus in 881; the Magyars/Hungarians belonged to the Onogur tribal alliance, it is possible that they became its ethnic majority. In the Early Middle Ages, the Hungarians had many names, including "Węgrzy", "Ungherese", "Ungar", "Hungarus"; the "H-" prefix is a addition of Medieval Latin. The Hungarian people refer to themselves by the demonym "Magyar" rather than "Hungarian". "Magyar" is Finno-Ugric from the Old Hungarian "mogyër". "Magyar" derived from the name of the most prominent Hungarian tribe, the "Megyer".
The tribal name "Megyer" became "Magyar" in reference to the Hungarian people as a whole. "Magyar" may derive from the Hunnic "Muageris" or "Mugel". The Greek cognate of "Tourkia" was used by the scholar and Byzantine Emperor Constantine VII "Porphyrogenitus" in his De Administrando Imperio of c. AD 950, though in his use, "Turks" always referred to Magyars; this was a misnomer, as while the Magyars had adopted some Turkic cultural traits, they are not a Turkic people. The historical Latin phrase "Natio Hungarica" had a wider and political meaning because it once referred to all nobles of the Kingdom of Hungary, regardless of their ethnicity or mother tongue. During the 4th millennium BC, the Uralic-speaking peoples who were living in the central and southern regions of the Urals split up; some dispersed towards the west and northwest and came into contact with Iranian speakers who were spreading northwards. From at least 2000 BC onwards, the Ugrian speakers became distinguished from the rest of the Uralic community, of which the ancestors of the Magyars, being located farther south, were the most numerous.
Judging by evidence from burial mounds and settlement sites, they interacted with the Indo-Iranian Andronovo culture. In the 4th and 5th centuries AD, the Hungarians moved from the west of the Ural Mountains to the area between the southern Ural Mountains and the Volga River known as Bashkiria and Perm Krai. In the early 8th century, some of the Hungarians moved to the Don River to an area between the Volga and the Seversky Donets rivers. Meanwhile, the descendants of those Hungarians who stayed in Bashkiria remained there as late as 1241; the Hungarians around the Don River were subordinates of the Khazar khaganate. Their neighbours were the archaeological Saltov Culture, i.e. Bulgars and the Alans, from whom they learned gardening, elements of cattle breeding and of agriculture. Tradition holds; the names of the seven tribes were: Jenő, Kér, Keszi, Kürt-Gyarmat, Megyer, Nyék, Tarján. Around 830, a rebellion broke out in the Khazar khaganate; as a result, three Kabar tribes of the Khazars joined the Hungarians and moved to what the Hungarians call the Etelköz, the territory between the Carpathians and the Dnieper River.
The Hungarians faced their first attack by the Pechenegs around 854, though other sources state that an attack by Pechenegs was the reason for their departure to Etelköz. The new neighbours of the Hungarians were the eastern Slavs. From 862 onwards, the Hungarians along with their allies, the Kabars, started a series of looting raids from the Etelköz into the Carpathian Basin against the Eastern Frankish Empire and Great Moravia, but against the Balaton principality and Bulgaria. In 895/896, under the leadership of Árpád, some Hungarians crossed the Carpathians and entered the Carpathian Basin; the tribe called Magyar was the leading tribe of the Hungarian alliance that conquered the centre of the basin. At the same time, due to their involvement in the 894–896 Bulgaro-Byzantine war, Hungarians in Etelköz were attacked by Bulgaria and by their old enemies the Pechenegs; the Bulgarians won the decisive b
A municipality is a single administrative division having corporate status and powers of self-government or jurisdiction as granted by national and regional laws to which it is subordinate. It is to be distinguished from the county, which may encompass rural territory or numerous small communities such as towns and hamlets; the term municipality may mean the governing or ruling body of a given municipality. A municipality is a general-purpose administrative subdivision, as opposed to a special-purpose district; the term is derived from French Latin municipalis. The English word municipality derives from the Latin social contract municipium, referring to the Latin communities that supplied Rome with troops in exchange for their own incorporation into the Roman state while permitting the communities to retain their own local governments. A municipality can be any political jurisdiction from a sovereign state, such as the Principality of Monaco, to a small village, such as West Hampton Dunes, New York.
The territory over which a municipality has jurisdiction may encompass only one populated place such as a city, town, or village several of such places only parts of such places, sometimes boroughs of a city such as the 34 municipalities of Santiago, Chile. Powers of municipalities range from virtual autonomy to complete subordination to the state. Municipalities may have the right to tax individuals and corporations with income tax, property tax, corporate income tax, but may receive substantial funding from the state. In various countries, municipalities are referred to as "communes", notably in Romance languages such as French commune, Italian comune, Romanian comună, Spanish comuna, in Germanic languages such as German Kommune, Swedish kommun, Faroese kommuna, Norwegian, Danish kommune. However, in Moldova and Romania exist both municipalities and communes, a commune may be part of a municipality. Similar terms include Spanish ayuntamiento called municipalidad, Polish gmina, Dutch/Flemish Gemeente and Luxembourgish Gemeng.
In Australia, the term local government area is used in place of the generic municipality. Here, the "LGA Structure covers only incorporated areas of Australia. Incorporated areas are designated parts of states and territories over which incorporated local governing bodies have responsibility." In Canada, municipalities are local governments established through provincial and territorial legislation within general municipal statutes. Types of municipalities within Canada include cities, district municipalities, municipal districts, parishes, rural municipalities, townships and villes among others; the Province of Ontario has different tiers of municipalities, including lower and single tiers. Types of upper tier municipalities in Ontario include regional municipalities. Nova Scotia has regional municipalities, which include cities, districts, or towns as municipal units. In India, a Municipality or Nagar Palika is an urban local body that administers a city of population 100,000 or more. However, there are exceptions to that, as Municipality were constituted in urban centers with population over 20,000, so all the urban bodies which were classified as Municipality were reclassified as Municipality if their population was under 100,000.
Under the Panchayati Raj system, it interacts directly with the state government, though it is administratively part of the district it is located in. Smaller district cities and bigger towns have a Municipality. Municipality are a form of local self-government entrusted with some duties and responsibilities, as enshrined in the Constitutional Act,1992. In the United Kingdom, the term was used until the 1972 Local Government Act came into effect in 1974 in England and Wales, until 1975 in Scotland and 1976 in Northern Ireland, "both for a city or town, organized for self-government under a municipal corporation, for the governing body itself; such a corporation in Great Britain consists of a head as a mayor or provost, of superior members, as aldermen and councillors". Since local government reorganisation, the unit in England, Northern Ireland and Wales is known as a district, in Scotland as a council area. A district can retain its district title. In Jersey, a municipality refers to the honorary officials elected to run each of the 12 parishes into which it is subdivided.
This is the highest level of regional government in this jurisdiction. In Trinidad and Tobago, "municipality" is understood as a city, town, or other local government unit, formed by municipal charter from the state as a municipal corporation. A town may be awarded borough status and on may be upgraded to city status. Chaguanas, San Fernando, Port of Spain and Point Fortin are the 5 current municipalities in Trinidad and Tobago. In the United States, "municipality" is understood as a city, village, or other local government unit, formed by municipal charter from the state as a municipal corporation. In a state law contex
Sandstone is a clastic sedimentary rock composed of sand-sized mineral particles or rock fragments. Most sandstone is composed of quartz or feldspar because they are the most resistant minerals to weathering processes at the Earth's surface, as seen in Bowen's reaction series. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, yellow, grey, pink and black. Since sandstone beds form visible cliffs and other topographic features, certain colors of sandstone have been identified with certain regions. Rock formations that are composed of sandstone allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Fine-grained aquifers, such as sandstones, are better able to filter out pollutants from the surface than are rocks with cracks and crevices, such as limestone or other rocks fractured by seismic activity. Quartz-bearing sandstone can be changed into quartzite through metamorphism related to tectonic compression within orogenic belts.
Sandstones are clastic in origin. They are formed from cemented grains that may either be fragments of a pre-existing rock or be mono-minerallic crystals; the cements binding these grains together are calcite and silica. Grain sizes in sands are defined within the range of 0.0625 mm to 2 mm. Clays and sediments with smaller grain sizes not visible with the naked eye, including siltstones and shales, are called argillaceous sediments; the formation of sandstone involves two principal stages. First, a layer or layers of sand accumulates as the result of sedimentation, either from water or from air. Sedimentation occurs by the sand settling out from suspension. Once it has accumulated, the sand becomes sandstone when it is compacted by the pressure of overlying deposits and cemented by the precipitation of minerals within the pore spaces between sand grains; the most common cementing materials are silica and calcium carbonate, which are derived either from dissolution or from alteration of the sand after it was buried.
Colors will be tan or yellow. A predominant additional colourant in the southwestern United States is iron oxide, which imparts reddish tints ranging from pink to dark red, with additional manganese imparting a purplish hue. Red sandstones are seen in the Southwest and West of Britain, as well as central Europe and Mongolia; the regularity of the latter favours use as a source for masonry, either as a primary building material or as a facing stone, over other forms of construction. The environment where it is deposited is crucial in determining the characteristics of the resulting sandstone, which, in finer detail, include its grain size and composition and, in more general detail, include the rock geometry and sedimentary structures. Principal environments of deposition may be split between terrestrial and marine, as illustrated by the following broad groupings: Terrestrial environmentsRivers Alluvial fans Glacial outwash Lakes Deserts Marine environmentsDeltas Beach and shoreface sands Tidal flats Offshore bars and sand waves Storm deposits Turbidites Framework grains are sand-sized detrital fragments that make up the bulk of a sandstone.
These grains can be classified into several different categories based on their mineral composition: Quartz framework grains are the dominant minerals in most clastic sedimentary rocks. These physical properties allow the quartz grains to survive multiple recycling events, while allowing the grains to display some degree of rounding. Quartz grains evolve from plutonic rock, which are felsic in origin and from older sandstones that have been recycled. Feldspathic framework grains are the second most abundant mineral in sandstones. Feldspar can be divided into two smaller subdivisions: plagioclase feldspars; the different types of feldspar can be distinguished under a petrographic microscope. Below is a description of the different types of feldspar. Alkali feldspar is a group of minerals in which the chemical composition of the mineral can range from KAlSi3O8 to NaAlSi3O8, this represents a complete solid solution. Plagioclase feldspar is a complex group of solid solution minerals that range in composition from NaAlSi3O8 to CaAl2Si2O8.
Lithic framework grains are pieces of ancient source rock that have yet to weather away to individual mineral grains, called lithic fragments or clasts. Lithic fragments can be any fine-grained or coarse-grained igneous, metamorphic, or sedimentary rock, although the most common lithic fragments found in sedimentary rocks are clasts of volcanic rocks. Accessory minerals are all other mineral grains in a sandstone. Common accessory minerals include micas, olivine and corundum. Many of these accessory grains are more dense than the silicates that
Silesian Beskids is one of the Beskids mountain ranges in Outer Western Carpathians in southern Silesian Voivodeship and the eastern Moravian-Silesian Region, Czech Republic. Most of the range lies in Poland, it is separated from the Moravian-Silesian Beskids by the Jablunkov Pass. The Polish part of the range includes. Silesian Beskids have 20 mountains with a highest point above 1000 m, including three above 1200 m and nine above 1100 m. Skrzyczne - the highest mountain Barania Góra - the highest mountain of the Polish part of Upper Silesia Małe Skrzyczne Wierch Wisełka Równiański Wierch Zielony Kopiec Malinowska Skała Magurka Wiślańska Klimczok Malinów Magura Magurka Radziechowska Trzy Kopce Stołów Glinne Przysłop Szyndzielnia Muronka Jaworzyna Kościelec Czantoria Wielka - the highest mountain of the Czech part of the range Kiczory Stożek Wielki Cieszyn Silesia Polish minority in the Czech Republic Cicha, Irena. Beskidzkie gronie nad Olzą i Wisłą. Czeski Cieszyn: Vydavatelství Regio. ISBN 978-80-254-0261-0.
Regional Tourist Service
The Moravian–Silesian Beskids is a mountain range in the Czech Republic with a small part reaching to Slovakia. It lies on the historical division between Silesia, hence the name, it is part of the Western Beskids, in turn part of the Outer Western Carpathians. The mountains were created during the Alpine Orogeny in the Cenozoic. Geologically, they consist of flysch deposits. In the north, they steeply rise nearly 1,000 m over a rather flat landscape. In the south-west, they are separated from the Vsetínské vrchy by the Rožnovská Bečva valley; the highest point is Lysá hora mountain at 1,323 m, one of the rainiest places in the Czech Republic with around 1,500 mm of precipitation a year. Many legends are bound to Radhošť Mountain, 1,129 m, one of the most visited places in the mountains together with the nearby Pustevny resort. Smrk, with a height of 1,276 m, is the second highest summit of the range, its northern slope steeply rises from the surrounding lowlands and is separated from the rest of the mountains by the deep Ostravice River and Čeladenka river valleys.
The Moravian-Silesian Beskids create the largest part of the Beskydy Landscape Protected Area. The mountains are 80% forested, though by plantations of spruce which were in some parts damaged by emissions from the Ostrava industrial region; the mountains were covered by mixed forest with dominant beech which are preserved in many places. Permanent occurrence of all three large Central European carnivores – lynx and wolf – have been confirmed in the area. There are many popular holiday resorts for both winter and summer activities, with centers in the towns under the mountains and in smaller resorts and chalets throughout the mountains on the ridges. Parts of two euroregions, the Beskydy/Beskidy and Těšínské Slezsko/Śląsk Cieszyński, reach into the Moravian-Silesian Beskids. Ludvík, Marcel. Beskydy, Turistický průvodce ČSSR. Praha: Olympia. 27-031-87. Rohlík, Jiří. Moravskoslezské Beskydy, Soubor turistických map 1:50 000. Praha: TRASA, s.r.o. ISBN 80-85999-29-3. CHKO Beskydy Management. "CHKO Beskydy".
World War II
World War II known as the Second World War, was a global war that lasted from 1939 to 1945. The vast majority of the world's countries—including all the great powers—eventually formed two opposing military alliances: the Allies and the Axis. A state of total war emerged, directly involving more than 100 million people from over 30 countries; the major participants threw their entire economic and scientific capabilities behind the war effort, blurring the distinction between civilian and military resources. World War II was the deadliest conflict in human history, marked by 50 to 85 million fatalities, most of whom were civilians in the Soviet Union and China, it included massacres, the genocide of the Holocaust, strategic bombing, premeditated death from starvation and disease, the only use of nuclear weapons in war. Japan, which aimed to dominate Asia and the Pacific, was at war with China by 1937, though neither side had declared war on the other. World War II is said to have begun on 1 September 1939, with the invasion of Poland by Germany and subsequent declarations of war on Germany by France and the United Kingdom.
From late 1939 to early 1941, in a series of campaigns and treaties, Germany conquered or controlled much of continental Europe, formed the Axis alliance with Italy and Japan. Under the Molotov–Ribbentrop Pact of August 1939, Germany and the Soviet Union partitioned and annexed territories of their European neighbours, Finland and the Baltic states. Following the onset of campaigns in North Africa and East Africa, the fall of France in mid 1940, the war continued between the European Axis powers and the British Empire. War in the Balkans, the aerial Battle of Britain, the Blitz, the long Battle of the Atlantic followed. On 22 June 1941, the European Axis powers launched an invasion of the Soviet Union, opening the largest land theatre of war in history; this Eastern Front trapped most crucially the German Wehrmacht, into a war of attrition. In December 1941, Japan launched a surprise attack on the United States as well as European colonies in the Pacific. Following an immediate U. S. declaration of war against Japan, supported by one from Great Britain, the European Axis powers declared war on the U.
S. in solidarity with their Japanese ally. Rapid Japanese conquests over much of the Western Pacific ensued, perceived by many in Asia as liberation from Western dominance and resulting in the support of several armies from defeated territories; the Axis advance in the Pacific halted in 1942. Key setbacks in 1943, which included a series of German defeats on the Eastern Front, the Allied invasions of Sicily and Italy, Allied victories in the Pacific, cost the Axis its initiative and forced it into strategic retreat on all fronts. In 1944, the Western Allies invaded German-occupied France, while the Soviet Union regained its territorial losses and turned toward Germany and its allies. During 1944 and 1945 the Japanese suffered major reverses in mainland Asia in Central China, South China and Burma, while the Allies crippled the Japanese Navy and captured key Western Pacific islands; the war in Europe concluded with an invasion of Germany by the Western Allies and the Soviet Union, culminating in the capture of Berlin by Soviet troops, the suicide of Adolf Hitler and the German unconditional surrender on 8 May 1945.
Following the Potsdam Declaration by the Allies on 26 July 1945 and the refusal of Japan to surrender under its terms, the United States dropped atomic bombs on the Japanese cities of Hiroshima and Nagasaki on 6 and 9 August respectively. With an invasion of the Japanese archipelago imminent, the possibility of additional atomic bombings, the Soviet entry into the war against Japan and its invasion of Manchuria, Japan announced its intention to surrender on 15 August 1945, cementing total victory in Asia for the Allies. Tribunals were set up by fiat by the Allies and war crimes trials were conducted in the wake of the war both against the Germans and the Japanese. World War II changed the political social structure of the globe; the United Nations was established to foster international co-operation and prevent future conflicts. The Soviet Union and United States emerged as rival superpowers, setting the stage for the nearly half-century long Cold War. In the wake of European devastation, the influence of its great powers waned, triggering the decolonisation of Africa and Asia.
Most countries whose industries had been damaged moved towards economic expansion. Political integration in Europe, emerged as an effort to end pre-war enmities and create a common identity; the start of the war in Europe is held to be 1 September 1939, beginning with the German invasion of Poland. The dates for the beginning of war in the Pacific include the start of the Second Sino-Japanese War on 7 July 1937, or the Japanese invasion of Manchuria on 19 September 1931. Others follow the British historian A. J. P. Taylor, who held that the Sino-Japanese War and war in Europe and its colonies occurred and the two wars merged in 1941; this article uses the conventional dating. Other starting dates sometimes used for World War II include the Italian invasion of Abyssinia on 3 October 1935; the British historian Antony Beevor views the beginning of World War II as the Battles of Khalkhin Gol fought between Japan and the fo
Cieszyn Silesian dialect
Cieszyn Silesian dialect is one of the Silesian dialects. It has its roots in Polish and has strong influences from Czech and German and, to a lesser extent, from Vlach and Slovak, it is spoken in a region on both sides of the Polish-Czech border. It remains a spoken language; the dialect is better preserved today than dialects of many other West Slavic regions. Polish and Czech linguists differ in their views on the classification of the dialect. Most Czech linguists classify the dialect as it is spoken on the Czech side of the border as a "mixed Czech-Polish dialect". Polish linguists tend to classify the language on either side of the border under the Silesian dialects of the Polish language. Although the dialect has its roots in Polish, the diachronic development of the dialect is of a transitional nature. On the Czech side of the border it is spoken by the Polish minority, it is used in Zaolzie to reinforce a feeling of regional solidarity. Before World War II the dialect, like all Silesian dialects, was influenced by the German language, as a significant proportion of the urban population were Germans.
In 1920 Cieszyn Silesia was divided between Czechoslovakia. After that division the dialect in the Czech part of the region was and still is influenced by the Czech language, with most new vocabulary, aside from English loanwords, borrowed from Czech. On the other hand, in the Polish part it was and still is influenced by the Polish language. Writers and poets who wrote in Cieszyn Silesian dialect include Adolf Fierla, Paweł Kubisz, Władysław Młynek, Józef Ondrusz, Karol Piegza and Adam Wawrosz; the Lord's Prayer in the Cieszyn Silesian dialect, with Czech and Polish for comparison: Cieszyn Vlachs Tutejszy Dejna, Karol. Dialekty Polskie. Wrocław: Zakład Narodowy im. Ossolińskich. ISBN 83-04-04129-4. Hannan, Kevin. Borders of Language and Identity in Teschen Silesia. New York: Peter Lang. ISBN 0-8204-3365-9. Zahradnik, Stanisław. Korzenie Zaolzia. Warszawa - Praga - Trzyniec: PAI-press. OCLC 177389723. Basara, Jan. Słownictwo polskich gwar Śląska na terenie Czechosłowacji. Wrocław: Polska Akademia Nauk and Zakład Narodowy im.
Ossolińskich. OCLC 2531024. Cieszyn Silesian-Czech Dictionary