1.
Upper Palatine Forest
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The Upper Palatine Forest is a mountain range in Central Europe that is divided between Germany and the Czech Republic. It is part of the larger Bohemian Massif and the German Central Uplands, the German side belongs to the Upper Palatinate region of Bavaria, it stretches about 100 km from the Bavarian Forest in the south up to the Fichtel Mountains and the Steinwald range in the north. However, the highest peaks of the range lie along the eastern Czech side in the Plzeň Region of western Bohemia, the southern rim runs from the Cham and Furth Basin across the border to the Všeruby mountain pass, which is part of the Main European Watershed. The other end is marked by Waldsassen, the northernmost town of the Upper Palatinate, the Mittelgebirge range is a mountainous solid mass, its highest point being at an altitude of 1,042 m. Prominent rocks include the Wolfenstein and the Parkstein hill, once a mining area for iron and gold, the uplands feature many steep valleys, medieval castle ruins and numerous hiking trails. It is a destination for recreation
2.
Bavarian Forest
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The Bavarian Forest is a wooded low-mountain region in Bavaria, Germany. It extends along the Czech border and is continued on the Czech side by the Šumava, geographically the Bavarian Forest and Bohemian Forest are sections of the same mountain range. A part of the Bavarian Forest belongs to the Bavarian Forest National Park, another 3,008 km² belong to the Bavarian Forest Nature Park, established 1967, and 1738 km² to the Eastern Bavarian Forest Nature Park, established 1965. The Bavarian Forest is a remnant of the Hercynian Forest that stretched across southern Germania in Roman times and it is the largest protected forest area in central Europe. The highest mountain in the region is the Großer Arber, the main river is the Regen, which is formed by the conjunction of White Regen and Black Regen and leaves the mountains towards the city of Regensburg
3.
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
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.
Central Europe
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Central Europe lies between Eastern Europe and Western Europe. The concept of Central Europe is based on a historical, social and cultural identity. Central Europe is going through a phase of strategic awakening, with such as the CEI, Centrope. While the regions economy shows high disparities with regard to income, elements of unity for Western and Central Europe were Roman Catholicism and Latin. According to Hungarian historian Jenő Szűcs, foundations of Central European history at the first millennium were in connection with Western European development. The keyword of Western social development after millennium was the spread of liberties and autonomies in Western Europe and these phenomena appeared in the middle of the 13th century in Central European countries. There were self-governments of towns, counties and parliaments, in 1335 under the rule of the King Charles I of Hungary, the castle of Visegrád, the seat of the Hungarian monarchs was the scene of the royal summit of the Kings of Poland, Bohemia and Hungary. They agreed to cooperate closely in the field of politics and commerce, in the Middle Ages, countries in Central Europe adopted Magdeburg rights. Before 1870, the industrialization that had developed in Western and Central Europe, even in Eastern Europe, industrialization lagged far behind. Russia, for example, remained rural and agricultural. The concept of Central Europe was already known at the beginning of the 19th century, an example of that-time vision of Central Europe may be seen in J. Partsch’s book of 1903. On 21 January 1904, Mitteleuropäischer Wirtschaftsverein was established in Berlin with economic integration of Germany, another time, the term Central Europe became connected to the German plans of political, economic and cultural domination. The bible of the concept was Friedrich Naumann’s book Mitteleuropa in which he called for a federation to be established after the war. The concept failed after the German defeat in World War I, the revival of the idea may be observed during the Hitler era. According to Emmanuel de Martonne, in 1927 the Central European countries included, Austria, Czechoslovakia, Germany, Hungary, Poland, Romania, italy and Yugoslavia are not considered by the author to be Central European because they are located mostly outside Central Europe. The author use both Human and Physical Geographical features to define Central Europe, the interwar period brought new geopolitical system and economic and political problems, and the concept of Central Europe took a different character. The centre of interest was moved to its eastern part – the countries that have appeared on the map of Europe, Czechoslovakia, Hungary, however, the conflict of interests was too big and neither Little Entente nor Intermarium ideas succeeded. The interwar period brought new elements to the concept of Central Europe, after the war, the Eastern part of Central Europe was placed at the centre of the concept
7.
South Bohemian Region
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South Bohemia is an administrative unit of the Czech Republic, located mostly in the southern part of its historical land of Bohemia, with a small part in southwestern Moravia. The western part of the South Bohemian Region is former Prachens, in 2011, there were 623 municipalities in the region, whereof 54 had a status of town. The region borders the regions Plzeň, Central Bohemia, Vysocina, to the south it borders Austria and Germany. Until 30 May 2001, the region was named as Budějovický kraj or Českobudějovický kraj, after its capital, thanks to its geographical location and natural conditions the region belongs to the areas where the first settlements began to appear in the distant past. In the past centuries, the South Bohemia was famous for fishpond cultivation, the region has been industrialized since the beginning of the twentieth century. Nowadays, it is a destination due to its natural. The travel industry has been recently the fastest growing industry in the region, the region was established based on the constitutional lax No. 347/97 of Collections concerning the formation of higher territorial administrative units, the region and its authorities are specified by Act No. 129-2000 of Collections concerning regions, which came into effect on the day of the regional authorities elections, as of September 2013, South Bohemias population is 636,459 and with only 63 people per 1 km² the region has the lowest population density in the whole country. 64. 2% of region’s population lives in towns or cities, one third of the inhabitants live in the five largest municipalities. Only 4% of region’s population lives in municipalities with less than 200 inhabitants, in 2011, the average age in the region is 41.2 years. Approximately 11% of inhabitants who were 15 years or older had a university degree, according to 2011 census,20. 6% of inhabitants in the region believe in god. The table below gives an overview of town and cities in the region that have more than 8,000 inhabitants, other significant towns are, Vimperk, Dačice, Kaplice, Soběslav, Sezimovo Ústí, Vodňany, Blatná, Veselí nad Lužnicí, Bechyně and Protivín. The following table provides details on the districts of the South Bohemia, South Bohemia consists of the South Bohemian Basin, České Budějovice Basin. The Bohemian Forest is a low range of mountains situated in the south-west, other highlands that can be found in the region are the Brdy Highlands, the Central-Bohemian Highlands, the Bohemian-Moravian Highlands and the Novohradské Mountains. The highest elevation in the region is the 1, 378-metre high Plechý in the Bohemian Forest, the region is located in the drainage basin of Vltava river. Other significant rivers are Malše, Lužnice, Otava, Nežárka, South Bohemia is famous for its countless ponds. In the past, more than seven thousand ponds were established across the region, with its 489 ha Rožmberk is the largest one, followed by Bezdrev and Horusice pond
8.
Czech Republic
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The Czech Republic, also known as Czechia, is a nation state in Central Europe bordered by Germany to the west, Austria to the south, Slovakia to the east and Poland to the northeast. The Czech Republic covers an area of 78,866 square kilometres with mostly temperate continental climate and it is a unitary parliamentary republic, has 10.5 million inhabitants and the capital and largest city is Prague, with over 1.2 million residents. The Czech Republic includes the territories of Bohemia, Moravia. The Czech state was formed in the late 9th century as the Duchy of Bohemia under the Great Moravian Empire, after the fall of the Empire in 907, the centre of power transferred from Moravia to Bohemia under the Přemyslid dynasty. In 1002, the duchy was formally recognized as part of the Holy Roman Empire, becoming the Kingdom of Bohemia in 1198 and reaching its greatest territorial extent in the 14th century. Following the Battle of Mohács in 1526, the whole Crown of Bohemia was gradually integrated into the Habsburg Monarchy alongside the Archduchy of Austria, the Protestant Bohemian Revolt against the Catholic Habsburgs led to the Thirty Years War. After the Battle of the White Mountain, the Habsburgs consolidated their rule, reimposed Roman Catholicism, the Czech part of Czechoslovakia was occupied by Germany in World War II, and was liberated in 1945 by the armies of the Soviet Union and the United States. The Czech country lost the majority of its German-speaking inhabitants after they were expelled following the war, the Communist Party of Czechoslovakia won the 1946 elections. Following the 1948 coup détat, Czechoslovakia became a one-party communist state under Soviet influence, in 1968, increasing dissatisfaction with the regime culminated in a reform movement known as the Prague Spring, which ended in a Soviet-led invasion. Czechoslovakia remained occupied until the 1989 Velvet Revolution, when the communist regime collapsed, on 6 March 1990, the Czech Socialistic Republic was renamed to the Czech Republic. On 1 January 1993, Czechoslovakia peacefully dissolved, with its constituent states becoming the independent states of the Czech Republic and the Slovak Republic. The Czech Republic joined NATO in 1999 and the European Union in 2004, it is a member of the United Nations, the OECD, the OSCE, and it is a developed country with an advanced, high income economy and high living standards. The UNDP ranks the country 14th in inequality-adjusted human development, the Czech Republic also ranks as the 6th most peaceful country, while achieving strong performance in democratic governance. It has the lowest unemployment rate in the European Union, the traditional English name Bohemia derives from Latin Boiohaemum, which means home of the Boii. The current name comes from the endonym Čech, spelled Cžech until the reform in 1842. The name comes from the Slavic tribe and, according to legend, their leader Čech, the etymology of the word Čech can be traced back to the Proto-Slavic root *čel-, meaning member of the people, kinsman, thus making it cognate to the Czech word člověk. The country has traditionally divided into three lands, namely Bohemia in the west, Moravia in the southeast, and Czech Silesia in the northeast. Following the dissolution of Czechoslovakia at the end of 1992, the Czech part of the former nation found itself without a common single-word geographical name in English, the name Czechia /ˈtʃɛkiə/ was recommended by the Czech Ministry of Foreign Affairs
9.
Austria
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Austria, officially the Republic of Austria, is a federal republic and a landlocked country of over 8.7 million people in Central Europe. It is bordered by the Czech Republic and Germany to the north, Hungary and Slovakia to the east, Slovenia and Italy to the south, the territory of Austria covers 83,879 km2. The terrain is mountainous, lying within the Alps, only 32% of the country is below 500 m. The majority of the population speaks local Bavarian dialects of German as their native language, other local official languages are Hungarian, Burgenland Croatian, and Slovene. The origins of modern-day Austria date back to the time of the Habsburg dynasty, from the time of the Reformation, many northern German princes, resenting the authority of the Emperor, used Protestantism as a flag of rebellion. Following Napoleons defeat, Prussia emerged as Austrias chief competitor for rule of a greater Germany, Austrias defeat by Prussia at the Battle of Königgrätz, during the Austro-Prussian War of 1866, cleared the way for Prussia to assert control over the rest of Germany. In 1867, the empire was reformed into Austria-Hungary, Austria was thus the first to go to war in the July Crisis, which would ultimately escalate into World War I. The First Austrian Republic was established in 1919, in 1938 Nazi Germany annexed Austria in the Anschluss. This lasted until the end of World War II in 1945, after which Germany was occupied by the Allies, in 1955, the Austrian State Treaty re-established Austria as a sovereign state, ending the occupation. In the same year, the Austrian Parliament created the Declaration of Neutrality which declared that the Second Austrian Republic would become permanently neutral, today, Austria is a parliamentary representative democracy comprising nine federal states. The capital and largest city, with a population exceeding 1.7 million, is Vienna, other major urban areas of Austria include Graz, Linz, Salzburg and Innsbruck. Austria is one of the richest countries in the world, with a nominal per capita GDP of $43,724, the country has developed a high standard of living and in 2014 was ranked 21st in the world for its Human Development Index. Austria has been a member of the United Nations since 1955, joined the European Union in 1995, Austria also signed the Schengen Agreement in 1995, and adopted the euro currency in 1999. The German name for Austria, Österreich, meant eastern realm in Old High German, and is cognate with the word Ostarrîchi and this word is probably a translation of Medieval Latin Marchia orientalis into a local dialect. Austria was a prefecture of Bavaria created in 976, the word Austria is a Latinisation of the German name and was first recorded in the 12th century. Accordingly, Norig would essentially mean the same as Ostarrîchi and Österreich, the Celtic name was eventually Latinised to Noricum after the Romans conquered the area that encloses most of modern-day Austria, around 15 BC. Noricum later became a Roman province in the mid-first century AD, heers hypothesis is not accepted by linguists. Settled in ancient times, the Central European land that is now Austria was occupied in pre-Roman times by various Celtic tribes, the Celtic kingdom of Noricum was later claimed by the Roman Empire and made a province
10.
Bavaria
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Bavaria is a free state and one of 16 federal states of Germany. Located in the German southeast with an area of 70,548 square kilometres and its territory comprises roughly a fifth of the total land area of Germany, and, with 12.9 million inhabitants, it is Germanys second most populous state. Munich, Bavarias capital and largest city, is the third largest city in Germany, the Duchy of Bavaria dates back to the year 555. In the 17th century CE, the Duke of Bavaria became a Prince-elector of the Holy Roman Empire, the Kingdom of Bavaria existed from 1806 to 1918, when Bavaria became a republic. In 1946, the Free State of Bavaria re-organised itself on democratic lines after the Second World War, Bavaria has a unique culture, largely because of the states Catholic majority and conservative traditions. Bavarians have traditionally been proud of their culture, which includes such as Oktoberfest. The state also has the second largest economy among the German states by GDP figures, modern Bavaria also includes parts of the historical regions of Franconia, Upper Palatinate and Swabia. The Bavarians emerged in a north of the Alps, previously inhabited by Celts. The Bavarians spoke Old High German but, unlike other Germanic groups, rather, they seem to have coalesced out of other groups left behind by Roman withdrawal late in the 5th century. These peoples may have included the Celtic Boii, some remaining Romans, Marcomanni, Allemanni, Quadi, Thuringians, Goths, Scirians, Rugians, the name Bavarian means Men of Baia which may indicate Bohemia, the homeland of the Celtic Boii and later of the Marcomanni. They first appear in written sources circa 520, a 17th century Jewish chronicler David Solomon Ganz, citing Cyriacus Spangenberg, claimed that the diocese was named after an ancient Bohemian king, Boiia, in the 14th century BCE. From about 554 to 788, the house of Agilolfing ruled the Duchy of Bavaria and their daughter, Theodelinde, became Queen of the Lombards in northern Italy and Garibald was forced to flee to her when he fell out with his Frankish overlords. Garibalds successor, Tassilo I, tried unsuccessfully to hold the frontier against the expansion of Slavs. Tassilos son Garibald II seems to have achieved a balance of power between 610 and 616, after Garibald II little is known of the Bavarians until Duke Theodo I, whose reign may have begun as early as 680. From 696 onwards he invited churchmen from the west to organize churches and his son, Theudebert, led a decisive Bavarian campaign to intervene in a succession dispute in the Lombard Kingdom in 714, and married his sister Guntrud to the Lombard King Liutprand. At Theodos death the duchy was divided among his sons, at Hugberts death the duchy passed to a distant relative named Odilo, from neighbouring Alemannia. He was defeated near Augsburg in 743 but continued to rule until his death in 748, saint Boniface completed the peoples conversion to Christianity in the early 8th century. Bavaria was in ways affected by the Protestant Reformation in the 16th century
11.
Germany
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Germany, officially the Federal Republic of Germany, is a federal parliamentary republic in central-western Europe. It includes 16 constituent states, covers an area of 357,021 square kilometres, with about 82 million inhabitants, Germany is the most populous member state of the European Union. After the United States, it is the second most popular destination in the world. Germanys capital and largest metropolis is Berlin, while its largest conurbation is the Ruhr, other major cities include Hamburg, Munich, Cologne, Frankfurt, Stuttgart, Düsseldorf and Leipzig. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity, a region named Germania was documented before 100 AD. During the Migration Period the Germanic tribes expanded southward, beginning in the 10th century, German territories formed a central part of the Holy Roman Empire. During the 16th century, northern German regions became the centre of the Protestant Reformation, in 1871, Germany became a nation state when most of the German states unified into the Prussian-dominated German Empire. After World War I and the German Revolution of 1918–1919, the Empire was replaced by the parliamentary Weimar Republic, the establishment of the national socialist dictatorship in 1933 led to World War II and the Holocaust. After a period of Allied occupation, two German states were founded, the Federal Republic of Germany and the German Democratic Republic, in 1990, the country was reunified. In the 21st century, Germany is a power and has the worlds fourth-largest economy by nominal GDP. As a global leader in industrial and technological sectors, it is both the worlds third-largest exporter and importer of goods. Germany is a country with a very high standard of living sustained by a skilled. It upholds a social security and universal health system, environmental protection. Germany was a member of the European Economic Community in 1957. It is part of the Schengen Area, and became a co-founder of the Eurozone in 1999, Germany is a member of the United Nations, NATO, the G8, the G20, and the OECD. The national military expenditure is the 9th highest in the world, the English word Germany derives from the Latin Germania, which came into use after Julius Caesar adopted it for the peoples east of the Rhine. This in turn descends from Proto-Germanic *þiudiskaz popular, derived from *þeudō, descended from Proto-Indo-European *tewtéh₂- people, the discovery of the Mauer 1 mandible shows that ancient humans were present in Germany at least 600,000 years ago. The oldest complete hunting weapons found anywhere in the world were discovered in a mine in Schöningen where three 380, 000-year-old wooden javelins were unearthed
12.
Bohemian Massif
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It is surrounded by four ranges, the Ore Mountains in the northwest, the Sudetes in the northeast, the Bohemian-Moravian Highlands in the southeast, and the Bohemian Forest in the southwest. The massif encompasses a number of mittelgebirges and consists of crystalline rocks, the landscapes in the Bohemian Massif are mostly dominated by rolling hills. North of the river Danube the topography is characterized by valleys and broad, flat ridges. The highest peaks on the Czech-Austrian borderline are Plechý-Plöckenstein and Sternstein, the bedrock of acid gneiss and granite is weathered to brown soil. In flat areas and valleys the groundwater had more influence on soil formation, as in the other Variscan mittelgebirges of Central Europe, the valleys are more irregular and less pronounced as in the relatively young fold and thrust belt of the Alps. The plateaus are more similar in morphology. Water gaps in the Bohemian Massif are the Wachau, the Strudengau and the valley of the Danube from Vilshofen over Passau, the internal tectonic structure of the Bohemian Massif was formed during the Variscan Orogeny. The Variscan Orogeny was a phase of building and accretion of terranes that resulted from the closing of the Rheic Ocean when the two paleocontinents Gondwana and Laurussia collided. Most of the Bohemian Massif is often supposed to belong to a terrane called Cadomia or Armorica and this supposedly formed a microcontinent that became sandwiched between the large continental masses north and south. The result of the Variscan Orogeny was that almost all continental mass became united in a supercontinent called Pangaea, from the Permian period onward the Variscan mountain belt eroded and became partly covered by younger sediments, with the exception of Variscan massifs like the Bohemian Massif. The basement rocks and terranes of the Bohemian Massif are tectonically part of three main zones, which differ in metamorphic degrees, lithologies and tectonic styles. This tectonic subdivision was formed during the Variscan Orogeny, the Saxothuringian Zone forms the northern parts of the massif. The northernmost part of the Saxothuringian Zone is the Mid-German Crystalline High, the northern boundary of this zone is assumed to be the Rheic suture which separates the former continental masses of Gondwana and Laurussia. The Moldanubian Zone forms the parts of the massif and has generally a higher grade than the Saxothuringian Zone. It includes the Teplá-Barrandian Terrane, which is assumed to have been a small microcontinent, the southeast of the massif forms a third unit, the Moravo-Silesian Zone. This zone includes the Brunovistulian Block, an allochthonous unit thrusted over the Moravo-Silesian crystalline rocks, contradictionary to most parts of the Bohemian Massif, the Brunovistulian was originally part of or close to the southern part of Laurussia. Unlike other Variscan massifs in Central Europe the Bohemian Massif is not very rich in ores, the Harz Mountains further north in Germany, which are geologically part of the Rhenohercynian Zone, have more ore deposits. On the other hand, the Bohemian massif has many quarries where granite, granodiorite and diorite are won for use as building stone
13.
Czech language
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Czech, historically also Bohemian, is a West Slavic language of the Czech–Slovak group. It is spoken by over 10 million people and is the language of the Czech Republic. Czech is closely related to Slovak, to the point of being intelligible to a very high degree. In the later 18th to mid-19th century, the written standard was codified in the context of the Czech National Revival. The main vernacular, known as Common Czech, is based on the vernacular of Prague, the Moravian dialects spoken in the eastern part of the country are mostly also counted as Czech, although some of their eastern variants are closer to Slovak. The Czech phoneme inventory is moderate in size, comprising five vowels, words may contain uncommon consonant clusters, including one consonant represented by the grapheme ř, or lack vowels altogether. Czech orthography is simple, and has used as a model by phonologists. Czech is classified as a member of the West Slavic sub-branch of the Slavic branch of the Indo-European language family and this branch includes Polish, Kashubian, Upper and Lower Sorbian and Slovak. Slovak is by far the closest genetic neighbor of Czech, the West Slavic languages are spoken in an area classified as part of Central Europe. Around the 7th century, the Slavic expansion reached Central Europe, the West Slavic polity of Great Moravia formed by the 9th century. The Christianization of Bohemia took place during the 9th and 10th centuries, the Bohemian language is first recorded in writing in glosses and short notes during the 12th to 13th centuries. Literary works written in Czech appear in the early 14th century, the first complete Bible translation also dates to this period. Old Czech texts, including poetry and cookbooks, were produced outside the university as well, literary activity becomes widespread in the early 15th century in the context of the Bohemian Reformation. There was no standardization distinguishing between Czech and Slovak prior to the 15th century, the publication of the Kralice Bible between 1579 and 1593 became very important for standardization of the Czech language in the following centuries. In 1615, the Bohemian diet tried to declare Czech to be the official language of the kingdom. After the Bohemian Revolt which was defeated by the Habsburgs in 1620 and this emigration together with other consequences of the Thirty Years War had a negative impact on the further use of the Czech language. In 1627, Czech and German became official languages of the Kingdom of Bohemia and in the 18th century German became dominant in Bohemia and Moravia, the modern standard Czech language originates in standardization efforts of the 18th century. Changes include the shift of í to ej and é to í and the merging of í
14.
German language
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German is a West Germanic language that is mainly spoken in Central Europe. It is the most widely spoken and official language in Germany, Austria, Switzerland, South Tyrol, the German-speaking Community of Belgium and it is also one of the three official languages of Luxembourg. Major languages which are most similar to German include other members of the West Germanic language branch, such as Afrikaans, Dutch, English, Luxembourgish and it is the second most widely spoken Germanic language, after English. One of the languages of the world, German is the first language of about 95 million people worldwide. The German speaking countries are ranked fifth in terms of publication of new books. German derives most of its vocabulary from the Germanic branch of the Indo-European language family, a portion of German words are derived from Latin and Greek, and fewer are borrowed from French and English. With slightly different standardized variants, German is a pluricentric language, like English, German is also notable for its broad spectrum of dialects, with many unique varieties existing in Europe and also other parts of the world. The history of the German language begins with the High German consonant shift during the migration period, when Martin Luther translated the Bible, he based his translation primarily on the standard bureaucratic language used in Saxony, also known as Meißner Deutsch. Copies of Luthers Bible featured a long list of glosses for each region that translated words which were unknown in the region into the regional dialect. Roman Catholics initially rejected Luthers translation, and tried to create their own Catholic standard of the German language – the difference in relation to Protestant German was minimal. It was not until the middle of the 18th century that a widely accepted standard was created, until about 1800, standard German was mainly a written language, in urban northern Germany, the local Low German dialects were spoken. Standard German, which was different, was often learned as a foreign language with uncertain pronunciation. Northern German pronunciation was considered the standard in prescriptive pronunciation guides though, however, German was the language of commerce and government in the Habsburg Empire, which encompassed a large area of Central and Eastern Europe. Until the mid-19th century, it was essentially the language of townspeople throughout most of the Empire and its use indicated that the speaker was a merchant or someone from an urban area, regardless of nationality. Some cities, such as Prague and Budapest, were gradually Germanized in the years after their incorporation into the Habsburg domain, others, such as Pozsony, were originally settled during the Habsburg period, and were primarily German at that time. Prague, Budapest and Bratislava as well as cities like Zagreb, the most comprehensive guide to the vocabulary of the German language is found within the Deutsches Wörterbuch. This dictionary was created by the Brothers Grimm and is composed of 16 parts which were issued between 1852 and 1860, in 1872, grammatical and orthographic rules first appeared in the Duden Handbook. In 1901, the 2nd Orthographical Conference ended with a standardization of the German language in its written form
15.
Bohemia
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Bohemia is the westernmost and largest historical region of the Czech lands in the present-day Czech Republic. Bohemia was a duchy of Great Moravia, later an independent principality, a kingdom in the Holy Roman Empire, and subsequently a part of the Habsburg Monarchy, after World War I and the establishment of an independent Czechoslovak state, Bohemia became a part of Czechoslovakia. Between 1938 and 1945, border regions with sizeable German-speaking minorities of all three Czech lands were joined to Nazi Germany as the Sudetenland, in 1990, the name was changed to the Czech Republic, which become a separate state in 1993 with the dissolution of Czechoslovakia. Until 1948, Bohemia was a unit of Czechoslovakia as one of its lands. Bohemia was bordered in the south by Upper and Lower Austria, in the west by Bavaria and in the north by Saxony and Lusatia, in the northeast by Silesia, and in the east by Moravia. In the 2nd century BC, the Romans were competing for dominance in northern Italy, the Romans defeated the Boii at the Battle of Placentia and the Battle of Mutina. After this, many of the Boii retreated north across the Alps, much later Roman authors refer to the area they had once occupied as Boiohaemum. The earliest mention was by Tacitus Germania 28, and later mentions of the name are in Strabo. The name appears to include the tribal name Boi- plus the Germanic element *haimaz home and this Boiohaemum was apparently isolated to the area where King Marobods kingdom was centred, within the Hercynian forest. The Czech name Čechy is derived from the name of the Slavic ethnic group, the Czechs, Bohemia, like neighbouring Bavaria, is named after the Boii, who were a large Celtic nation known to the Romans for their migrations and settlement in northern Italy and other places. Another part of the nation moved west with the Helvetii into southern France, to the south, over the Danube, the Romans extended their empire, and to the southeast in Hungaria, were Sarmatian peoples. In the area of modern Bohemia the Marcomanni and other Suebic groups were led by their king Marobodus and he took advantage of the natural defenses provided by its mountains and forests. In late classical times and the early Middle Ages, two new Suebic groupings appeared to the west of Bohemia in southern Germany, the Alemanni, many Suebic tribes from the Bohemian region took part in such movements westwards, even settling as far away as Spain and Portugal. With them were also tribes who had pushed from the east, such as the Vandals, other groups pushed southwards towards Pannonia. These are precursors of todays Czechs, though the amount of Slavic immigration is a subject of debate. The Slavic influx was divided into two or three waves, the first wave came from the southeast and east, when the Germanic Lombards left Bohemia. Soon after, from the 630s to 660s, the territory was taken by Samos tribal confederation and his death marked the end of the old Slavonic confederation, the second attempt to establish such a Slavonic union after Carantania in Carinthia. Other sources divide the population of Bohemia at this time into the Merehani, Marharaii, Beheimare, Christianity first appeared in the early 9th century, but only became dominant much later, in the 10th or 11th century
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Sternstein
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The Sternstein Mountain is situated in the north of Upper Austria, Austria in the districts of Bad Leonfelden and Vorderweißenbach. On its north flank it also reaches into the Czech Republic, as measured by the height above sea level of its summit it is 1125 meters high. Geologically it belongs to the Bohemian Massif and is the most eastern part of the Bohemian Forest, as the average temperature in the surroundings of the mountain over the year is less than 6°C, it is one of the coldest regions of Upper Austria. The municipalities of Vorderweißenbach and Bad Leonfelden get their supplies from springs arising from lower parts of the mountain. In the year 1898 a 20 meter high Observation Tower was built on top of the mountain, in honor to the K. u. K. Today it is one of the main tourist attractions of the region. During the winter the mountain can be used for winter sports, also cross country skiing is very popular in the area of the Sternstein. During the other seasons the mountain is a destination for hikers, furthermore, it is situated along a long-distance hiking path, the Nordwaldkammweg
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Bog
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A bog is a wetland that accumulates peat, a deposit of dead plant material—often mosses, and in a majority of cases, sphagnum moss. It is one of the four types of wetlands. Other names for bogs include mire, quagmire, and muskeg and they are frequently covered in ericaceous shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink, Bogs occur where the water at the ground surface is acidic and low in nutrients. In some cases, the water is derived entirely from precipitation, water flowing out of bogs has a characteristic brown colour, which comes from dissolved peat tannins. In general, the low fertility and cool climate results in relatively slow plant growth, large areas of landscape can be covered many metres deep in peat. Bogs have distinctive assemblages of animal, fungal and plant species, Bogs are widely distributed in cold, temperate climes, mostly in boreal ecosystems in the Northern Hemisphere. The worlds largest wetland is the bogs of the Western Siberian Lowlands in Russia. Large peat bogs also occur in North America, particularly the Hudson Bay Lowland and they are less common in the Southern Hemisphere, with the largest being the Magellanic moorland, comprising some 44,000 square kilometres. Sphagnum bogs were widespread in northern Europe but have often been cleared and drained for agriculture, a 2014 expedition leaving from Itanga village, Republic of the Congo discovered a peat bog as big as England which stretches into neighboring Democratic Republic of Congo. There are many highly specialised animals, fungi and plants associated with bog habitat, most are capable of tolerating the combination of low nutrient levels and waterlogging. Sphagnum moss is generally abundant, along with ericaceous shrubs, the shrubs are often evergreen, which is understood to assist in conservation of nutrients. In drier locations, evergreen trees can occur, in case the bog blends into the surrounding expanses of boreal evergreen forest. Sedges are one of the more common herbaceous species, carnivorous plants such as sundews and pitcher plants have adapted to the low-nutrient conditions by using invertebrates as a nutrient source. Orchids have adapted to these conditions through the use of fungi to extract nutrients. Some shrubs such as Myrica gale have root nodules in which nitrogen fixation occurs, Bogs are recognized as a significant/specific habitat type by a number of governmental and conservation agencies. They can provide habitat for mammals, such as caribou, moose, the United Kingdom in its Biodiversity Action Plan establishes bog habitats as a priority for conservation. Russia has a reserve system in the West Siberian Lowland
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Drainage divide
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A drainage divide, water divide, divide, ridgeline, watershed, water parting, is the line that separates neighbouring drainage basins. In hilly country, the divide lies along topographical ridges, and may be in the form of a range of hills or mountains. In flat country—especially where the ground is marshy—the divide may be harder to discern, a valley floor divide is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Settlements are often built on valley-floor divides in the Alps, examples are Eben im Pongau, Kirchberg in Tirol and Waidring. Extremely low divides with heights of less than two metres are found on the North German Plain within the Urstromtäler, for example, between Havel and Finow in the Eberswalde Urstromtal. In marsh deltas such as the Okavango, the largest drainage area on earth, or in large areas, such as the Finnish Lakeland. Another case is bifurcation, where the watershed is effectively in the river bed, in pre-industrial times, water divides were crossed at portages. Later, canals connected adjoining drainage basins, a key problem in such canals is ensuring a sufficient water supply, category, Drainage basins List of watershed topics European watershed Scottish watershed River source
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Black Sea
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The Black Sea is a body of water between Eastern Europe and Western Asia, bounded by Bulgaria, Georgia, Romania, Russia, Turkey, and Ukraine. It is supplied by a number of rivers, such as the Danube, Dnieper, Rioni, Southern Bug. The Black Sea has an area of 436,400 km2, a depth of 2,212 m. It is constrained by the Pontic Mountains to the south and by the Caucasus Mountains to the east, the longest east-west extent is about 1,175 km. The Black Sea has a water balance, that is, a net outflow of water 300 km3 per year through the Bosphorus. Mediterranean water flows into the Black Sea as part of a two-way hydrological exchange, the Black Sea drains into the Mediterranean Sea and then the Atlantic Ocean, via the Aegean Sea and various straits. The Bosphorus Strait connects it to the Sea of Marmara, and these waters separate Eastern Europe and Western Asia. The Black Sea is also connected to the Sea of Azov by the Strait of Kerch, the water level has varied significantly. Due to these variations in the level in the basin. At certain critical water levels it is possible for connections with surrounding water bodies to become established and it is through the most active of these connective routes, the Turkish Straits, that the Black Sea joins the world ocean. When this hydrological link is not present, the Black Sea is a basin, operating independently of the global ocean system. Currently the Black Sea water level is high, thus water is being exchanged with the Mediterranean. The Turkish Straits connect the Black Sea with the Aegean Sea, and comprise the Bosphorus, the Sea of Marmara, the International Hydrographic Organization defines the limits of the Black Sea as follows, On the Southwest. The Northeastern limit of the Sea of Marmara, a line joining Cape Takil and Cape Panaghia. Strabos Geographica reports that in antiquity, the Black Sea was often just called the Sea, for the most part, Graeco-Roman tradition refers to the Black Sea as the Hospitable sea, Εὔξεινος Πόντος Eúxeinos Póntos. This is a euphemism replacing an earlier Inhospitable Sea, Πόντος Ἄξεινος Póntos Áxeinos, strabo thinks that the Black Sea was called inhospitable before Greek colonization because it was difficult to navigate, and because its shores were inhabited by savage tribes. The name was changed to hospitable after the Milesians had colonized the southern shoreline and it is also possible that the epithet Áxeinos arose by popular etymology from a Scythian word axšaina- unlit, dark, the designation Black Sea may thus date from antiquity. A map of Asia dating to 1570, entitled Asiae Nova Descriptio, from Abraham Orteliuss Theatrum Orbis Terrarum, english-language writers of the 18th century often used the name Euxine Sea to refer to the Black Sea
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North Sea
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The North Sea is a marginal sea of the Atlantic Ocean located between Great Britain, Scandinavia, Germany, the Netherlands, Belgium, and France. An epeiric sea on the European continental shelf, it connects to the ocean through the English Channel in the south and it is more than 970 kilometres long and 580 kilometres wide, with an area of around 570,000 square kilometres. The North Sea has long been the site of important European shipping lanes as well as a major fishery, the North Sea was the centre of the Vikings rise. Subsequently, the Hanseatic League, the Netherlands, and the British each sought to dominate the North Sea and thus the access to the markets, as Germanys only outlet to the ocean, the North Sea continued to be strategically important through both World Wars. The coast of the North Sea presents a diversity of geological and geographical features, in the north, deep fjords and sheer cliffs mark the Norwegian and Scottish coastlines, whereas in the south it consists primarily of sandy beaches and wide mudflats. Due to the population, heavy industrialization, and intense use of the sea and area surrounding it. In the southwest, beyond the Straits of Dover, the North Sea becomes the English Channel connecting to the Atlantic Ocean, in the east, it connects to the Baltic Sea via the Skagerrak and Kattegat, narrow straits that separate Denmark from Norway and Sweden respectively. In the north it is bordered by the Shetland Islands, and connects with the Norwegian Sea, the North Sea is more than 970 kilometres long and 580 kilometres wide, with an area of 570,000 square kilometres and a volume of 54,000 cubic kilometres. Around the edges of the North Sea are sizeable islands and archipelagos, including Shetland, Orkney, the North Sea receives freshwater from a number of European continental watersheds, as well as the British Isles. A large part of the European drainage basin empties into the North Sea including water from the Baltic Sea, the largest and most important rivers flowing into the North Sea are the Elbe and the Rhine – Meuse watershed. Around 185 million people live in the catchment area of the rivers discharging into the North Sea encompassing some highly industrialized areas, for the most part, the sea lies on the European continental shelf with a mean depth of 90 metres. The only exception is the Norwegian trench, which extends parallel to the Norwegian shoreline from Oslo to a north of Bergen. It is between 20 and 30 kilometres wide and has a depth of 725 metres. The Dogger Bank, a vast moraine, or accumulation of unconsolidated glacial debris and this feature has produced the finest fishing location of the North Sea. The Long Forties and the Broad Fourteens are large areas with uniform depth in fathoms. These great banks and others make the North Sea particularly hazardous to navigate, the Devils Hole lies 200 miles east of Dundee, Scotland. The feature is a series of trenches between 20 and 30 kilometres long,1 and 2 kilometres wide and up to 230 metres deep. Other areas which are less deep are Cleaver Bank, Fisher Bank, the International Hydrographic Organization defines the limits of the North Sea as follows, On the Southwest
21.
Vltava
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It is commonly referred to as the Czech national river. The Vltava river is 430 kilometres long and drains an area about 28,090 square kilometres in size, over half of Bohemia, as it runs through Prague, the river is crossed by 18 bridges and covers 31 kilometres within the city. The water from the river was used for drinking until 1912 and it is, however, the source of drinking water in case of failures/repairs to the water supply from the Želivka and Kárané sources. The Podolí water processing plant is on standby for such cases with the section of the river upstream of the Podolí plant under the stricter. Several dams were built on it in the 1950s, the Orlík Dam supports the largest reservoir on the Vltava by volume, while the Lipno Dam in the Bohemian Forest retains the largest reservoir by area. North of Prague the Štěchovice Reservoir has been built over the site of the St Johns Rapids. The river also features numerous locks and weirs that help mitigate its flow from 1,172 metres in elevation at its source near the German border to 155 metres at its mouth in Mělník. The height difference from source to mouth is about 1,016 metres, the Vltava itself originates by a confluence of two streams, the Warm Vltava, which is longer, and the Cold Vltava, sourcing in Bavaria. Along its course, Vltava receives many tributaries, the biggest being Otava and Berounka from the left and Lužnice and its section around Český Krumlov is a very popular destination of water tourism. Both the Czech name Vltava and the German name Moldau are believed to originate from the old Germanic words wilt ahwa, in Annales Fuldenses it is called Fuldaha, from 1113 AD it is attested as Wultha. In Chronica Boemorum it is attested for the first time in its Bohemian form as Wlitaua, on the other side there is a river Ltava in Ukraine with no traces of Germanic origins. The name of a settlement on this river was mentioned in the Hypatian Chronicle in 1174, traditionally connected to the name of the city of Poltava, there are many theories describing etymology of Ltava. The Vltava basin has flooded multiple times throughout recorded history, markers have been created along the banks denoting the water line for notable floods in 1784,1845,1890,1940, and the highest of all in 2002. It left the oldest bridge in Prague, Charles Bridge, seriously weakened, Prague was again flooded in 2013. Nine hydroelectric dams have been built on the Vltava to regulate the water flow, beginning at the headwaters, these are, Lipno, Lipno II, Hněvkovice, Kořensko, Orlík, Kamýk, Slapy, Štěchovice and Vrané. One of the works of classical music by a Czech composer is Bedřich Smetanas Vltava. It is from the Romantic era of music and is a musical depiction of the rivers course through Bohemia. A minor planet 2123 Vltava discovered in 1973 by Soviet astronomer Nikolai Stepanovich Chernykh is named after the river, Smetanas symphonic poem also inspired a song of the same name by Bertolt Brecht
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Otava (river)
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The Otava is a river in West and South Bohemia, Czech Republic. It is 112 kilometres long and is a tributary of the Vltava. The river flows through several towns, including Sušice, Strakonice, the rivers name is of Celtic origin. It is a river for water sports. The local dialect of Prachens also uses the name Wotāva, information at the Water Management Research Institute
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Lipno Dam
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The Lipno Dam is a dam and hydroelectric plant constructed along the Vltava River in the Czech Republic. Due to frequent flooding and subsequent damage, the Vltava River in Southern Bohemia was problematic for Český Krumlov, to harness the power of the river, and to prevent continued catastrophe, it was decided that a hydroelectric plant would be built high on the Vltava. Preparatory work at the town of Lipno began in 1951, construction on the dam began in 1952, and the dam was completed in 1960. The stream bed of the Vltava near Lipno was chosen because it has a slight incline, the dam is built along the highest-elevated stage of the Vltava Rivers cascade, thus enabling large amounts of hydropower out-put. This area is mountainous, and borders the Šumava National Park, a smaller reservoir near Vyšší Brod is linked to the main reservoir by an artificial underground waterway. This smaller reservoir, named Lipno II, serves to level the water of the main reservoir, Lipno Hydro Power Plant has two turbines with a nominal capacity of 64 MW each having a total capacity of 128 MW. Media related to Lipno_Dam at Wikimedia Commons http, //www. pvl. cz
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Reservoir
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A reservoir is a storage space for fluids. These fluids may be water, hydrocarbons or gas, a reservoir usually means an enlarged natural or artificial lake, storage pond or impoundment created using a dam or lock to store water. Reservoirs can be created by controlling a stream that drains a body of water. They can also be constructed in river valleys using a dam, alternately, a reservoir can be built by excavating flat ground or constructing retaining walls and levees. Tank reservoirs store liquids or gases in storage tanks that may be elevated, at grade level, tank reservoirs for water are also called cisterns. Underground reservoirs are used to store liquids, principally either water or petroleum, a dam constructed in a valley relies on the natural topography to provide most of the basin of the reservoir. Dams are typically located at a part of a valley downstream of a natural basin. The valley sides act as walls, with the dam located at the narrowest practical point to provide strength. In many reservoir construction projects, people have to be moved and re-housed, construction of a reservoir in a valley will usually need the river to be diverted during part of the build, often through a temporary tunnel or by-pass channel. In hilly regions, reservoirs are constructed by enlarging existing lakes. Sometimes in such reservoirs the new top water level exceeds the height on one or more of the feeder streams such as at Llyn Clywedog in Mid Wales. In such cases additional side dams are required to contain the reservoir, where water is pumped or siphoned from a river of variable quality or quantity, bank-side reservoirs may be built to store the water. Such reservoirs are usually formed partly by excavation and partly by building a complete encircling bund or embankment, the water stored in such reservoirs may stay there for several months, during which time normal biological processes may substantially reduce many contaminants and almost eliminate any turbidity. The use of reservoirs also allows water abstraction to be stopped for some time. Service reservoirs store fully treated potable water close to the point of distribution, many service reservoirs are constructed as water towers, often as elevated structures on concrete pillars where the landscape is relatively flat. Other service reservoirs can be almost entirely underground, especially in hilly or mountainous country. In the United Kingdom, Thames Water has many underground reservoirs, sometimes called cisterns, built in the 1800s. A good example is the Honor Oak Reservoir in London, constructed between 1901 and 1909, when it was completed it was said to be the largest brick built underground reservoir in the world and it is still one of the largest in Europe
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Cirque
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A cirque is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie and cwm, a cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, cliff-like slopes down which ice and glaciated debris combine and converge from the three or more higher sides. The fluvial cirque or makhtesh, found in karst landscapes, is formed by intermittent river flow cutting through layers of limestone, a common feature for all fluvial-erosion cirques is a terrain which includes erosion resistant upper structures overlying materials which are more easily eroded. Glacial cirques are found amongst mountain ranges throughout the world, classic cirques are typically about one kilometer long, situated high on a mountainside near the firn line, they are typically partially surrounded on three sides by steep cliffs. The highest cliff often is called a headwall, the fourth side forms the lip, threshold or sill, the side at which the glacier flowed away from the cirque. Many glacial cirques contain tarns dammed by either till or a bedrock threshold, when enough snow accumulates it can flow out the opening of the bowl and form valley glaciers which may be several kilometers long. These areas are sheltered from heat, encouraging the accumulation of snow, if the accumulation of snow increases, the process of nivation follows, whereby a hollow in a slope may be enlarged by ice segregation weathering and glacial erosion. Ice segregation erodes the rock vertical rock face and causes it to disintegrate, eventually, this hollow may become large enough that glacial erosion intensifies. The enlarging of this open ended concavity creates a larger leeward deposition zone, debris in the ice also may abrade the bed surface, should ice move down a slope it would have a ‘sandpaper effect’ on the bedrock beneath, on which it scrapes. Eventually, the hollow may become a bowl shape in the side of the mountain, with the headwall being weathered by ice segregation. The basin will become deeper as it continues to be eroded by ice segregation and abrasion, should ice segregation, plucking and abrasion continue, the dimensions of the cirque will increase, but the proportion of the landform would remain roughly the same. A bergschrund forms when the movement of the glacier separates the moving ice from the ice forming a crevasse. The method of erosion of the headwall lying between the surface of the glacier and the floor has been attributed to freeze-thaw mechanisms. The temperature within the bergschrund changes very little, however, studies have shown that ice segregation may happen with only changes in temperature. Water that flows into the bergschrund can be cooled to freezing temperatures by the ice allowing freeze-thaw mechanisms to occur. If two adjacent cirques erode toward one another, an arête, or steep sided ridge, forms, when three or more cirques erode toward one another, a pyramidal peak is created. In some cases, this peak will be accessible by one or more arêtes
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Iron Curtain
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The Iron Curtain was the name for the boundary dividing Europe into two separate areas from the end of World War II in 1945 until the end of the Cold War in 1991. A term symbolizing the efforts by the Soviet Union to block itself and its satellite states from open contact with the West, on the east side of the Iron Curtain were the countries that were connected to or influenced by the Soviet Union. The most notable border was marked by the Berlin Wall and its Checkpoint Charlie, the events that demolished the Iron Curtain started in discontent in Poland, and continued in Hungary, the German Democratic Republic, Bulgaria, Czechoslovakia, and Romania. Romania became the only communist state in Europe to overthrow its government with violence. The use of the iron curtain as a metaphor for strict separation goes back at least as far as the early 19th century. It originally referred to fireproof curtains in theaters, various usages of the term iron curtain pre-date Churchills use of the phrase. The term iron curtain has since been used metaphorically in two different senses - firstly to denote the end of an era and secondly to denote a closed geopolitical border. The source of these metaphors can refer to either the safety curtain deployed in theatres or to roller shutters used to secure commercial premises. The first metaphorical usage of iron curtain, in the sense of an end of an era, perhaps should be attributed to British author Arthur Machen, who used the term in his 1895 novel The Three Impostors. The door clanged behind me with the noise of thunder, and I felt that an iron curtain had fallen on the passage of my life. Queen Elisabeth of the Belgians used the term Iron Curtain in the context of World War I to describe the situation between Belgium and Germany in 1914. The passage runs, With clanging, creaking, and squeaking, time to put on your fur coats and go home. We looked around, but the fur coats and homes were missing, chesterton used the phrase in a 1924 essay in The Illustrated London News. Chesterton, while defending Distributism, refers to that iron curtain of industrialism that has cut us off not only from our neighbours condition, how, a moment before the iron curtain was wrung down on it, did the German political stage appear. All German theatres had to install an iron curtain as a precaution to prevent the possibility of fire spreading from the stage to the rest of the theatre. Such fires were common because the decor often was very flammable. In case of fire, a wall would separate the stage from the theatre. Douglas Reed used this metaphor in his book Disgrace Abounding, The bitter strife had only hidden by the iron safety-curtain of the Kings dictatorship
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Ecosystem
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An ecosystem is a community of living organisms in conjunction with the nonliving components of their environment, interacting as a system. These biotic and abiotic components are regarded as linked together through nutrient cycles, as ecosystems are defined by the network of interactions among organisms, and between organisms and their environment, they can be of any size but usually encompass specific, limited spaces. Energy, water, nitrogen and soil minerals are other essential components of an ecosystem. The energy that flows through ecosystems is obtained primarily from the sun and it generally enters the system through photosynthesis, a process that also captures carbon from the atmosphere. By feeding on plants and on one another, animals play an important role in the movement of matter and they also influence the quantity of plant and microbial biomass present. Ecosystems are controlled both by external and internal factors, other external factors include time and potential biota. Ecosystems are dynamic entities—invariably, they are subject to disturbances and are in the process of recovering from some past disturbance. Ecosystems in similar environments that are located in different parts of the world can have different characteristics simply because they contain different species. The introduction of species can cause substantial shifts in ecosystem function. Internal factors not only control ecosystem processes but are controlled by them and are often subject to feedback loops. Other internal factors include disturbance, succession and the types of species present, although humans exist and operate within ecosystems, their cumulative effects are large enough to influence external factors like climate. Biodiversity affects ecosystem function, as do the processes of disturbance, classifying ecosystems into ecologically homogeneous units is an important step towards effective ecosystem management, but there is no single, agreed-upon way to do this. The term ecosystem was first used in 1935 in a publication by British ecologist Arthur Tansley, Tansley devised the concept to draw attention to the importance of transfers of materials between organisms and their environment. He later refined the term, describing it as The whole system, including not only the organism-complex, but also the whole complex of physical factors forming what we call the environment. Tansley regarded ecosystems not simply as natural units, but as mental isolates, Tansley later defined the spatial extent of ecosystems using the term ecotope. G. Raymond Lindeman took these ideas one step further to suggest that the flow of energy through a lake was the driver of the ecosystem. Most mineral nutrients, on the hand, are recycled within ecosystems. Ecosystems are controlled both by external and internal factors, external factors, also called state factors, control the overall structure of an ecosystem and the way things work within it, but are not themselves influenced by the ecosystem
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Habitat
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A habitat is an ecological or environmental area that is inhabited by a particular species of animal, plant, or other type of organism. The term typically refers to the zone in which the organism lives and it is the natural environment in which an organism lives, or the physical environment that surrounds a species population. Every organism has certain habitat needs for the conditions in which it will thrive, habitat types include polar, temperate, subtropical and tropical. The terrestrial vegetation type may be forest, steppe, grassland, the word habitat has been in use since about 1755 and derives from the Latin third-person singular present indicative of habitāre, to inhabit, from habēre, to have or to hold. Habitat can be defined as the environment of an organism. It is similar in meaning to a biotope, an area of environmental conditions associated with a particular community of plants. Generally speaking, animal communities are reliant on specific types of plant communities, some plants and animals are generalists, and their habitat requirements are met in a wide range of locations. The small white butterfly for example is found on all the continents of the world apart from Antarctica and its larvae feed on a wide range of Brassicas and various other plant species, and it thrives in any open location with diverse plant associations. Disturbance is important in the creation of biodiverse habitats, in the absence of disturbance, a climax vegetation cover develops that prevents the establishment of other species. Lightning strikes and toppled trees in tropical forests allow species richness to be maintained as pioneering species move in to fill the gaps created. Similarly coastal habitats can become dominated by kelp until the seabed is disturbed by a storm, another cause of disturbance is when an area may be overwhelmed by an invasive introduced species which is not kept under control by natural enemies in its new habitat. Terrestrial habitat types include forests, grasslands, wetlands and deserts, within these broad biomes are more specific habitats with varying climate types, temperature regimes, soils, altitudes and vegetation types. Many of these habitats grade into each other and each one has its own communities of plants. A habitat may suit a particular species well, but its presence or absence at any particular location depends to some extent on chance, on its dispersal abilities, freshwater habitats include rivers, streams, lakes, ponds, marshes and bogs. Although some organisms are found across most of these habitats, the majority have more specific requirements, similarly, aquatic plants can be floating, semi-submerged, submerged or grow in permanently or temporarily saturated soils besides bodies of water. Marine habitats include brackish water, estuaries, bays, the sea, the intertidal zone. Further variations include rock pools, sand banks, mudflats, brackish lagoons, sandy and pebbly beaches, the benthic zone or seabed provides a home for both static organisms, anchored to the substrate, and for a large range of organisms crawling on or burrowing into the surface. A desert is not the kind of habitat that favours the presence of amphibians, with their requirement for water to keep their skins moist, nevertheless, some frogs live in deserts, creating moist habitats underground and hibernating while conditions are adverse
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UNESCO
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The United Nations Educational, Scientific and Cultural Organization is a specialized agency of the United Nations based in Paris. It is the heir of the League of Nations International Committee on Intellectual Cooperation, UNESCO has 195 member states and nine associate members. Most of its offices are cluster offices covering three or more countries, national and regional offices also exist. UNESCO pursues its objectives through five major programs, education, natural sciences, social/human sciences, culture and it is also a member of the United Nations Development Group. UNESCO and its mandate for international cooperation can be traced back to a League of Nations resolution on 21 September 1921, on 18 December 1925, the International Bureau of Education began work as a non-governmental organization in the service of international educational development. However, the work of predecessor organizations was largely interrupted by the onset of World War II. On 30 October 1943, the necessity for an organization was expressed in the Moscow Declaration, agreed upon by China, the United Kingdom, the United States. This was followed by the Dumbarton Oaks Conference proposals of 9 October 1944, a prominent figure in the initiative for UNESCO was Rab Butler, the Minister of Education for the United Kingdom. At the ECO/CONF, the Constitution of UNESCO was introduced and signed by 37 countries, the Preparatory Commission operated between 16 November 1945, and 4 November 1946—the date when UNESCOs Constitution came into force with the deposit of the twentieth ratification by a member state. The first General Conference took place between 19 November to 10 December 1946, and elected Dr. Julian Huxley to Director-General and this change in governance distinguished UNESCO from its predecessor, the CICI, in how member states would work together in the organizations fields of competence. In 1956, the Republic of South Africa withdrew from UNESCO claiming that some of the organizations publications amounted to interference in the racial problems. South Africa rejoined the organization in 1994 under the leadership of Nelson Mandela, UNESCOs early work in the field of education included the pilot project on fundamental education in the Marbial Valley, Haiti, started in 1947. This project was followed by missions to other countries, including, for example. In 1948, UNESCO recommended that Member States should make free primary education compulsory, in 1990, the World Conference on Education for All, in Jomtien, Thailand, launched a global movement to provide basic education for all children, youths and adults. Ten years later, the 2000 World Education Forum held in Dakar, Senegal, UNESCOs early activities in culture included, for example, the Nubia Campaign, launched in 1960. The purpose of the campaign was to move the Great Temple of Abu Simbel to keep it from being swamped by the Nile after construction of the Aswan Dam, during the 20-year campaign,22 monuments and architectural complexes were relocated. This was the first and largest in a series of campaigns including Mohenjo-daro, Fes, Kathmandu, Borobudur, the organizations work on heritage led to the adoption, in 1972, of the Convention concerning the Protection of the World Cultural and Natural Heritage. The World Heritage Committee was established in 1976 and the first sites inscribed on the World Heritage List in 1978, since then important legal instruments on cultural heritage and diversity have been adopted by UNESCO member states in 2003 and 2005
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Man and the Biosphere Programme
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As of March 2016,669 biosphere reserves in 120 countries, including 16 transboundary sites, have been included in the World Network of Biosphere Reserves. Biosphere reserves are areas comprising terrestrial, marine and coastal ecosystems, each reserve promotes solutions reconciling the conservation of biodiversity with its sustainable use. Biosphere reserves are nominated by governments and remain under the sovereign jurisdiction of the states where they are located. Their status is internationally recognized. The buffer zone surrounds or adjoins the core areas, and is used for activities compatible with sound ecological practices that can reinforce scientific research, monitoring, training and education. The transition area is the part of the reserve where the greatest activity is allowed, fostering economic, participating countries establish MAB National Committees that ensure maximum national participation in the international programme, defining and implementing each country’s activities. MAB currently operates through 158 National Committees established among the 195 Members States, the agenda of the MAB Programme is defined by its main governing body, the International Coordinating Council. The MAB Council consists of 34 member states elected by UNESCO’s General Conference, the council elects a chair and five vice-chairpersons from each of UNESCO’s geopolitical regions, one of which functions as a rapporteur. Its staff members draw on expertise in many and varied disciplines, the programme can grant seed funding to assist countries in developing projects and/or to secure appropriate partnership contributions. The latest World Congress of Biosphere Reserves took place in Lima, Peru and this will be the 4th World Congress of Biosphere Reserves and it shall develop a new vision for the decade 2016–2025. The World Network of Biosphere Reserves is supported by different regional, sub-regional or thematic networks and these are as follows, The African Biosphere Reserves Network was created in 1996 and comprises 33 African countries. The ArabMAB Network was officially launched in 1997 and represents 18 Arab countries, the East Asian Biosphere Reserve Network was launched in 1994. Today, it consists of China, the Democratic People’s Republic of Korea, Japan, Kazakhstan, Mongolia, the Republic of Korea, euroMAB is the network of biosphere reserves in Europe and North America. Created in 1987, it is the largest MAB Regional Network with 53 countries, the Ibero-American MAB Network was created in 1992. It comprises 22 countries from Latin American and the Caribbean, Spain, the Pacific Man and the Biosphere Network was created in 2006 and comprises the Federated States of Micronesia, Kiribati, Palau, Papua New Guinea, Samoa and Tonga. The South and Central Asia MAB Network was created in 2002 and comprises Afghanistan, Bangladesh, Bhutan, India, Iran, Kazakhstan, Maldives, Nepal, Pakistan, the Southeast Asian Biosphere Reserve Network was created in 1998. Today, it comprises Cambodia, China, Indonesia, Japan, Lao PDR, Malaysia, Myanmar, Philippines, Thailand, the East Atlantic Biosphere Reserve Network was created in 1994. It comprises the Canary Islands, Cape Verde, Guinea Bissau, Madeira and Azores, Mauritania, Morocco, Sao Tomé and Principe, the World Network of Island and Coastal Biosphere Reserves was established in 2012 and comprises 22 countries. Agenda 21 Searchable list of UNESCO World Network of Biosphere Reserves Frequently Asked Questions on Biosphere Reserve A-Z of Areas of Biodiverity Importance, Biosphere Reserves
31.
Bavarian Forest National Park
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The Bavarian Forest National Park is a national park in the Eastern Bavarian Forest immediately on Germanys border with the Czech Republic. It was founded on 7 October 1970 as the first national park in Germany, since its expansion on 1 August 1997 it has covered an area of 24,250 hectares. Together with the neighbouring Czech Bohemian Forest the Bavarian Forest forms the largest contiguous area of forest in Central Europe, especially protected are the Norway spruce–dominated highland forests, mixed mountain forests of European silver fir, European beech and spruce trees and water meadow spruce woods in the valleys. Although a few remnants of ancient forest remain, the National Park area is heavily influenced by the former forestry industry. Since nature is now left to take its course again, there is no human intervention when there are events such as large scale bark beetle infestation. As the result of a compromise, bark beetle is now fought in the buffer area, the most important peaks in the National Park are the Großer Falkenstein, the Lusen and the Großer Rachel. With over 700,000 visitors per year, the National Park is an important economic factor in the underdeveloped region of the Bavarian Forest. The National Park runs along the ridge of the Bavarian Forest from the Großer Falkenstein in the northwest past the Großer Rachel to the Lusen in the southeast. According to the classification of the natural regions of Germany it is part of the Rear Bavarian Forest in the Upper Palatine-Bavarian Forest. On the other side of the border in the Czech Republic and it borders on the municipalities of, Bayerisch Eisenstein, Zwiesel, Lindberg, Frauenau, Spiegelau, Sankt Oswald-Riedlhütte, Neuschönau, Hohenau and Mauth. Parts of the National Park are located on the territory of the respective communities, there are many enclaves in the national park, especially around the edges, Zwieslerwaldhaus at the foot of the Großer Falkenstein belongs to the municipality Lindberg. Schleicher and Kreuzstraßl belong to Lindberg, sagwasser-Säge and Weidhütte form a joint functional enclave belonging to Hohenau and which is joined to the rest of the country, but can only be accessed on a road passing through the national park. In addition, there are several enclaves that comprise just one or a few small plots. These numerous enclaves, especially in the Altgebiet make the very long there, and the buffer zone. Hans Bibelriether, Hartmut Strunz, Unterwegs im Nationalpark Bayerischer Wald, ein Führer für Wanderer und Naturfreunde. Morsak, Grafenau 1990,213 S. ISBN 3-87553-353-4 Hans Bibelriether, Hannes Burger,182 S. ISBN 3-930977-26-5 Marco Heurich, Markus Neufanger, Die Wälder des Nationalparks Bayerischer Wald. Ergebnisse der Waldinventur 2002/2003 im geschichtlichen und waldökologischen Kontext, Nationalpark Bayerischer Wald, Wissenschaftliche Reihe, Heft 16. Nationalparkverwaltung Bayerischer Wald, Grafenau 2005,176 S. ISBN 3-930977-28-1 Stefan Nüßlein, berichte aus der Bayerischen Landesanstalt für Wald und Forstwirtschaft, Nr.25
32.
Hiking
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Hiking is the preferred term, in Canada and the United States, for a long, vigorous walk, usually on trails, in the countryside, while the word walking is used for shorter, particularly urban walks. On the other hand, in the United Kingdom, and the Republic of Ireland, the word hiking is also often used in the UK, along with rambling, hillwalking, and fell walking. The term bushwalking is endemic to Australia, having been adopted by the Sydney Bush Walkers club in 1927, in New Zealand a long, vigorous walk or hike is called tramping. It is an activity with numerous hiking organizations worldwide. In the United States, Canada, the Republic of Ireland, a day hike refers to a hike that can be completed in a single day. However, in the United Kingdom, the walking is also used, as well as rambling. In Northern England, Including the Lake District and Yorkshire Dales, fellwalking describes hill or mountain walks, hiking sometimes involves bushwhacking and is sometimes referred to as such. This specifically refers to walking through dense forest, undergrowth, or bushes. In extreme cases of bushwhacking, where the vegetation is so dense that human passage is impeded, the Australian term bushwalking refers to both on and off-trail hiking. Common terms for hiking used by New Zealanders are tramping, walking or bushwalking, trekking is the preferred word used to describe multi-day hiking in the mountainous regions of India, Pakistan, Nepal, North America, South America, Iran and in the highlands of East Africa. Hiking a long-distance trail from end-to-end is also referred to as trekking, in North America, multi-day hikes, usually with camping, are referred to as backpacking. The idea of taking a walk in the countryside for pleasure developed in the 18th-century, in earlier times walking generally indicated poverty and was also associated with vagrancy. Thomas West, an English priest, popularized the idea of walking for pleasure in his guide to the Lake District of 1778. To this end he included various stations or viewpoints around the lakes, published in 1778 the book was a major success. Another famous early exponent of walking for pleasure, was the English poet William Wordsworth, in 1790 he embarked on an extended tour of France, Switzerland, and Germany, a journey subsequently recorded in his long autobiographical poem The Prelude. His famous poem Tintern Abbey was inspired by a visit to the Wye Valley made during a tour of Wales in 1798 with his sister Dorothy Wordsworth. Wordsworths friend Coleridge was another keen walker and in the autumn of 1799, he and Wordsworth undertook a three weeks tour of the Lake District. John Keats, who belonged to the generation of Romantic poets began, in June 1818, a walking tour of Scotland, Ireland
33.
Bark beetle
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The unrelated sawyer beetles and some other wood-boring beetle taxa are sometimes called bark beetles, too. A bark beetle is one of about 220 genera with 6,000 species of beetles in the subfamily Scolytinae, traditionally, this was considered a distinct family Scolytidae, but is now understood to be very specialized members of the true weevil family. The mountain pine beetle Dendroctonus ponderosae, southern pine beetle Dendroctonus frontalis, a similarly aggressive species in Europe is the spruce ips Ips typographus. A tiny bark beetle, the coffee borer, Hypothenemus hampei is a major pest on coffee plantations around the world. Bark beetles reproduce in the bark of trees. Many species, such as the pine beetle attack and kill live trees. Most, however, live in dead, weakened, or dying hosts, Bark beetles play an important role in forest ecology, for example by creating complex early successional forest. Infestations can have significant economic impact, in undisturbed forests, bark beetles serve the purpose of hastening the recycling and decomposition of dead and dying wood and renewing the forest. A few species are aggressive and can develop large populations that invade, Bark beetles of the family Scolytidae feed and breed between the bark and the wood of various tree species, including spruces. More than 20 species feed on weakened, dying, or dead spruce, fir, most restrict breeding area to one part of the tree, twig, branch, stem, or root collar. Some breed in trees of one species, others in trees of many species. Bark beetles often attack trees that are weakened by disease, drought, smog, overcrowding, conspecific beetles. Under outbreak conditions, the number of beetles can overwhelm the trees defences with resulting impacts on the lumber industry, water quality, fish and wildlife. According to the United States Department of Agriculture, native bark beetles can cause high levels of mortality in California. Massive outbreaks of mountain pine beetles in western North America after about 2005 have killed millions of acres of forest from New Mexico to British Columbia. The outbreaks could be a consequence of global warming, the winters in the region allow various species to expand their ranges. Most studies of wildfire after beetle outbreaks have found no effect of beetle-caused tree mortality on wildfire size or severity, some bark beetles form a symbiotic relationship with certain Ophiostomatales fungi, and are named ambrosia beetles after these ambrosia fungi. The ambrosia beetles feed on fungal gardens and are one of only three groups known to farm fungi
34.
Boii
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The Boii were a Gallic tribe of the later Iron Age, attested at various times in Cisalpine Gaul, Pannonia, parts of Bavaria, in and around Bohemia, and Gallia Narbonensis. In addition the archaeological evidence indicates that in the 2nd century BC Celts expanded from Bohemia through the Kłodzko Valley into Silesia, now part of Poland and the Czech Republic. They first appear in history in connection with the Gallic invasion of north Italy,390 BC, after a series of wars they were decisively beaten by the Romans in a battle near Mutina and their territory became part of the Roman province of Cisalpine Gaul. Around 60 BC, a group of Boii joined the Helvetiis ill-fated attempt to land in western Gaul and were defeated by Julius Caesar, along with their allies. Caesar settled the remnants of that group in Gorgobina, from where they sent two thousand to Vercingetorixs aid at the battle of Alesia six years later, the eastern Boii on the Danube were incorporated into the Roman Empire in 8 AD. From all the different names of the same Celtic people in literature and inscriptions it is possible to abstract a continental Celtic segment, There are two major derivations of this segment, both presupposing that it belongs to the family of Indo-European languages, from cow and from warrior. The Boii would thus be either the people or the warrior people. The cow derivation depends most immediately on the Old Irish legal term for outsider, ambue, from Proto-Celtic *ambouios, not a cattle owner. The latter were presumably the *ambouii, as opposed to the man of status, who was *bouios, an owner, and the *bouii were originally a class. Boii would be from the o-grade of *bhei-, which is *bhoi-, such a connection is possible if the original form of Boii belonged to a tribe of Proto-Indo-European speakers long before the time of the historic Boii. If that is the case, then the Celtic tribe of central Europe must have been a final population of a linguistically diversifying ancestor tribe. Indo-European reconstructions can be made using *gʷou- cow as a basis, contemporary derived words include Boiorix and Boiodurum in Germany. According to the ancient authors, the Boii arrived in northern Italy by crossing the Alps and it remains therefore unclear where exactly the Central European origins of the Boii lay, if somewhere in Gaul, Southern Germany or in Bohemia. Polybius relates that the Celts were close neighbors of the Etruscan civilization, invading the Po Valley with a large army, they drove out the Etruscans and resettled it, the Boii taking the right bank in the center of the valley. Strabo confirms that the Boii emigrated from their lands across the Alps and were one of the largest tribes of the Celts, the Boii occupied the old Etruscan settlement of Felsina, which they named Bononia. Their possessions consisted of cattle and gold, because these were the things they could carry about with them everywhere according to circumstances. They treated comradeship as of the greatest importance, those among them being the most feared and most powerful who were thought to have the largest number of attendants and associates. The archaeological evidence from Bologna and its vicinity contradicts the testimony of Polybius and Livy on some points and it much rather indicates that the Boii neither destroyed nor depopulated Felsinum, but simply moved in and became part of the population by intermarriage
35.
Ancient Rome
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In its many centuries of existence, the Roman state evolved from a monarchy to a classical republic and then to an increasingly autocratic empire. Through conquest and assimilation, it came to dominate the Mediterranean region and then Western Europe, Asia Minor, North Africa and it is often grouped into classical antiquity together with ancient Greece, and their similar cultures and societies are known as the Greco-Roman world. Ancient Roman civilisation has contributed to modern government, law, politics, engineering, art, literature, architecture, technology, warfare, religion, language and society. Rome professionalised and expanded its military and created a system of government called res publica, the inspiration for modern republics such as the United States and France. By the end of the Republic, Rome had conquered the lands around the Mediterranean and beyond, its domain extended from the Atlantic to Arabia, the Roman Empire emerged with the end of the Republic and the dictatorship of Augustus Caesar. 721 years of Roman-Persian Wars started in 92 BC with their first war against Parthia and it would become the longest conflict in human history, and have major lasting effects and consequences for both empires. Under Trajan, the Empire reached its territorial peak, Republican mores and traditions started to decline during the imperial period, with civil wars becoming a prelude common to the rise of a new emperor. Splinter states, such as the Palmyrene Empire, would divide the Empire during the crisis of the 3rd century. Plagued by internal instability and attacked by various migrating peoples, the part of the empire broke up into independent kingdoms in the 5th century. This splintering is a landmark historians use to divide the ancient period of history from the pre-medieval Dark Ages of Europe. King Numitor was deposed from his throne by his brother, Amulius, while Numitors daughter, Rhea Silvia, because Rhea Silvia was raped and impregnated by Mars, the Roman god of war, the twins were considered half-divine. The new king, Amulius, feared Romulus and Remus would take back the throne, a she-wolf saved and raised them, and when they were old enough, they returned the throne of Alba Longa to Numitor. Romulus became the source of the citys name, in order to attract people to the city, Rome became a sanctuary for the indigent, exiled, and unwanted. This caused a problem for Rome, which had a large workforce but was bereft of women, Romulus traveled to the neighboring towns and tribes and attempted to secure marriage rights, but as Rome was so full of undesirables they all refused. Legend says that the Latins invited the Sabines to a festival and stole their unmarried maidens, leading to the integration of the Latins, after a long time in rough seas, they landed at the banks of the Tiber River. Not long after they landed, the men wanted to take to the sea again, one woman, named Roma, suggested that the women burn the ships out at sea to prevent them from leaving. At first, the men were angry with Roma, but they realized that they were in the ideal place to settle. They named the settlement after the woman who torched their ships, the Roman poet Virgil recounted this legend in his classical epic poem the Aeneid
36.
Celtic tribes
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This is a list of Celtic tribes, listed in order of the Roman province or the general area in which they lived. This geographical distribution of Celtic tribes does not imply that tribes that lived in the general geographical area were more related. Some tribes or tribal names are listed under more than one region because they dwelt in several of them. Central Europe, roughly upper Danube river basin and neighboring regions, is hypothesized as the area of the Celts. Some closely fit the concept of a tribe, others are confederations or even unions of tribes. Agri Decumates Helvetii – original dwellers of the region, unknown named tribes of the Helvetii tribal confederation, also dwelt to the South, Decumates may have meant Ten Cantons. Latobrigi/Latovici - uncertain location, maybe to the north or northeast of the Helvetii in the upper Danube and upper Rhine river basins, tulingi – localisation unclear, possibly Southern Germany, Switzerland or Austria, also may have been a Germanic tribe. Moravian Volcae - roughly in todays Moravia, noricum Norici/Taurisci - a tribal confederation Alauni - in the middle Aenus river basin, east of the Aenus in the Eastern Alps, Chiemsee and Attersee lakes region. Ambidravi/Ambidrani - in the upper and middle Dravus river basin in the Eastern Alps and also in the Mur/Mura river basin, ambilici - in the Dravus river basin, east of the Ambidravi/Ambidrani. Ambisontes/Ambisontii - in the Alpes Noricae, in the upper Salzach river basin, sevaces - in the low Aenus river basin, east of the Aenus and south of the Danubius, roughly in todays Upper Austria. Pannonia Arabiates - areas of modern Western Hungary and eastern Austria, belgites - areas of modern Western Hungary, west of Danubius river. Cornacates - areas of modern Western Hungary, west of Danubius river, cotini – areas of modern Slovakia and Western Hungary, west of Danubius river. Eravisci/Aravisci – areas of modern Western Hungary, west of Danubius river, hercuniates/Hercuniatae - areas of modern Western Hungary, west of Danubius river. Latobici/Latovici - not the tribe as the Latobrigi but could be related, areas of modern Western Hungary. Scordisci – areas of modern Serbia, Croatia, Austria, Romania, serrapilli - areas of modern Western Hungary, west of Danubius river. Serretes - areas of modern Western Hungary, west of Danubius river, Varciani – areas of modern Slovenia, Croatia. Rhaetia Rhaetian people – central parts of present-day Switzerland, the Tyrol in Austria, there is evidence that the non-Celtic elements had, by the time of Augustus, been assimilated by the influx of Celtic tribes and had adopted Celtic speech. Benlauni - Upper valley of fl. Aenus in todays North Tirol, Austria, along with the Breuni, not the same as the Breuni, breuni/Brenni/Breones - Upper valley of fl
37.
Gaul
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It covered an area of 190,800 sq mi. According to the testimony of Julius Caesar, Gaul was divided into three parts, Gallia Celtica, Belgica and Aquitania, during the 2nd and 1st centuries BC, Gaul fell under Roman rule, Gallia Cisalpina was conquered in 203 BC and Gallia Narbonensis in 123 BC. Gaul was invaded after 120 BC by the Cimbri and the Teutons, Gallia remains a name of France in modern Greek and modern Latin. The Greek and Latin names Galatia, and Gallia are ultimately derived from a Celtic ethnic term or clan Gal-to-. Galli of Gallia Celtica were reported to refer to themselves as Celtae by Caesar. Hellenistic folk etymology connected the name of the Galatians to the supposedly milk-white skin of the Gauls, modern researchers say it is related to Welsh gallu, Cornish galloes, capacity, power, thus meaning powerful people. The English Gaul is from French Gaule and is unrelated to Latin Gallia, as adjectives, English has the two variants, Gaulish and Gallic. The two adjectives are used synonymously, as pertaining to Gaul or the Gauls, although the Celtic language or languages spoken in Gaul is predominantly known as Gaulish. The Germanic w- is regularly rendered as gu- / g- in French, also unrelated in spite of superficial similarity is the name Gael. The Irish word gall did originally mean a Gaul, i. e. an inhabitant of Gaul, but its meaning was later widened to foreigner, to describe the Vikings, and later still the Normans. The dichotomic words gael and gall are sometimes used together for contrast, by 500 BC, there is strong Hallstatt influence throughout most of France. By the late 5th century BC, La Tène influence spreads rapidly across the territory of Gaul. The La Tène culture developed and flourished during the late Iron Age in France, Switzerland, Italy, Austria, southwest Germany, Bohemia, Moravia, Slovakia, farther north extended the contemporary pre-Roman Iron Age culture of northern Germany and Scandinavia. By the 2nd century BC, the Romans described Gallia Transalpina as distinct from Gallia Cisalpina, while some scholars believe the Belgae south of the Somme were a mixture of Celtic and Germanic elements, their ethnic affiliations have not been definitively resolved. One of the reasons is political interference upon the French historical interpretation during the 19th century, in addition to the Gauls, there were other peoples living in Gaul, such as the Greeks and Phoenicians who had established outposts such as Massilia along the Mediterranean coast. Also, along the southeastern Mediterranean coast, the Ligures had merged with the Celts to form a Celto-Ligurian culture, the prosperity of Mediterranean Gaul encouraged Rome to respond to pleas for assistance from the inhabitants of Massilia, who were under attack by a coalition of Ligures and Gauls. The Romans intervened in Gaul in 154 BC and again in 125 BC, whereas on the first occasion they came and went, on the second they stayed. Massilia was allowed to keep its lands, but Rome added to its territories the lands of the conquered tribes. The direct result of conquests was that by now, Rome controlled an area extending from the Pyrenees to the lower Rhône river
38.
France
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France, officially the French Republic, is a country with territory in western Europe and several overseas regions and territories. The European, or metropolitan, area of France extends from the Mediterranean Sea to the English Channel and the North Sea, Overseas France include French Guiana on the South American continent and several island territories in the Atlantic, Pacific and Indian oceans. France spans 643,801 square kilometres and had a population of almost 67 million people as of January 2017. It is a unitary republic with the capital in Paris. Other major urban centres include Marseille, Lyon, Lille, Nice, Toulouse, during the Iron Age, what is now metropolitan France was inhabited by the Gauls, a Celtic people. The area was annexed in 51 BC by Rome, which held Gaul until 486, France emerged as a major European power in the Late Middle Ages, with its victory in the Hundred Years War strengthening state-building and political centralisation. During the Renaissance, French culture flourished and a colonial empire was established. The 16th century was dominated by civil wars between Catholics and Protestants. France became Europes dominant cultural, political, and military power under Louis XIV, in the 19th century Napoleon took power and established the First French Empire, whose subsequent Napoleonic Wars shaped the course of continental Europe. Following the collapse of the Empire, France endured a succession of governments culminating with the establishment of the French Third Republic in 1870. Following liberation in 1944, a Fourth Republic was established and later dissolved in the course of the Algerian War, the Fifth Republic, led by Charles de Gaulle, was formed in 1958 and remains to this day. Algeria and nearly all the colonies became independent in the 1960s with minimal controversy and typically retained close economic. France has long been a centre of art, science. It hosts Europes fourth-largest number of cultural UNESCO World Heritage Sites and receives around 83 million foreign tourists annually, France is a developed country with the worlds sixth-largest economy by nominal GDP and ninth-largest by purchasing power parity. In terms of household wealth, it ranks fourth in the world. France performs well in international rankings of education, health care, life expectancy, France remains a great power in the world, being one of the five permanent members of the United Nations Security Council with the power to veto and an official nuclear-weapon state. It is a member state of the European Union and the Eurozone. It is also a member of the Group of 7, North Atlantic Treaty Organization, Organisation for Economic Co-operation and Development, the World Trade Organization, originally applied to the whole Frankish Empire, the name France comes from the Latin Francia, or country of the Franks
39.
Cisalpine Gaul
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Cisalpine Gaul, also called Gallia Citerior or Gallia Togata, was the part of Italy inhabited by Celts during the 4th and 3rd centuries BC. Conquered by the Roman Republic in the 220s BC, it was a Roman province from c.81 BC until 42 BC, when it was merged into Roman Italy. Until that time, it was considered part of Gaul, precisely that part of Gaul on the side of the Alps. Gallia Cisalpina was further subdivided into Gallia Cispadana and Gallia Transpadana, i. e. its portions south and north of the Po River and they brought a new funerary practice—cremation—which supplanted inhumation. Livy has the Insubres, led by Bellovesus, arrive in northern Italy during the reign of Tarquinius Priscus, Milan itself is presumably a Gaulish foundation of the early 6th century BC, its name having a Celtic etymology of in the middle of the plain. Polybius in the 2nd century BC wrote about co-existence of the Celts in northern Italy with Etruscan nations in the period before the Sack of Rome in 390 BC. Ligures lived in Northern Mediterranean Coast straddling South-east French and North-west Italian coasts, including parts of Tuscany, Elba island, Ligurian tribes were also present in Latium and in Samnium. According to Plutarch they called themselves Ambrones, which could indicate a relationship with the Ambrones of northern Europe, little is known of the Ligurian language. Only place-names and personal names remain and it appears to be an Indo-European branch with both Italic and particularly strong Celtic affinities. Because of the strong Celtic influences on their language and culture, modern linguists, like Xavier Delamarre argues that Ligurian was a Celtic language, similar to, but not the same as Gaulish. The Ligurian-Celtic question is discussed by Barruol. Ancient Ligurian is either listed as Celtic, or Para-Celtic, the Veneti were an Indo-European people who inhabited north-eastern Italy, in an area corresponding to the modern-day region of the Veneto. By the 4th century BC the Veneti had been so Celticized that Polybius wrote that the Veneti of the 2nd century BC were identical to the Gauls except for language. He further suggested that the identification of the Adriatic Veneti with the Paphlagonian Enetoi led by Antenor — which he attributes to Sophocles — was a due to the similarity of the names. The Roman army was routed in the battle of Allia, the defeat of the combined Samnite, Celtic and Etruscan alliance by the Romans in the Third Samnite War ending in 290 BC sounded the beginning of the end of the Celtic domination in mainland Europe. At the Battle of Telamon in 225 BC, a large Celtic army was trapped between two Roman forces and crushed, in the Second Punic War, the Boii and Insubres allied themselves with the Carthaginians, laying siege to Mutina. In response, Rome sent an expedition led by L. Manlius Vulso, vulsos army was ambushed twice, and the Senate sent Scipio with an additional force to provide support. These were the Roman forces encountered by Hannibal after his crossing of the Alps, the Romans were defeated in the Battle of the Ticinus, leading to all the Gauls except for the Cenomani to join the insurgency
40.
Italy
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Italy, officially the Italian Republic, is a unitary parliamentary republic in Europe. Located in the heart of the Mediterranean Sea, Italy shares open land borders with France, Switzerland, Austria, Slovenia, San Marino, Italy covers an area of 301,338 km2 and has a largely temperate seasonal climate and Mediterranean climate. Due to its shape, it is referred to in Italy as lo Stivale. With 61 million inhabitants, it is the fourth most populous EU member state, the Italic tribe known as the Latins formed the Roman Kingdom, which eventually became a republic that conquered and assimilated other nearby civilisations. The legacy of the Roman Empire is widespread and can be observed in the distribution of civilian law, republican governments, Christianity. The Renaissance began in Italy and spread to the rest of Europe, bringing a renewed interest in humanism, science, exploration, Italian culture flourished at this time, producing famous scholars, artists and polymaths such as Leonardo da Vinci, Galileo, Michelangelo and Machiavelli. The weakened sovereigns soon fell victim to conquest by European powers such as France, Spain and Austria. Despite being one of the victors in World War I, Italy entered a period of economic crisis and social turmoil. The subsequent participation in World War II on the Axis side ended in defeat, economic destruction. Today, Italy has the third largest economy in the Eurozone and it has a very high level of human development and is ranked sixth in the world for life expectancy. The country plays a prominent role in regional and global economic, military, cultural and diplomatic affairs, as a reflection of its cultural wealth, Italy is home to 51 World Heritage Sites, the most in the world, and is the fifth most visited country. The assumptions on the etymology of the name Italia are very numerous, according to one of the more common explanations, the term Italia, from Latin, Italia, was borrowed through Greek from the Oscan Víteliú, meaning land of young cattle. The bull was a symbol of the southern Italic tribes and was often depicted goring the Roman wolf as a defiant symbol of free Italy during the Social War. Greek historian Dionysius of Halicarnassus states this account together with the legend that Italy was named after Italus, mentioned also by Aristotle and Thucydides. The name Italia originally applied only to a part of what is now Southern Italy – according to Antiochus of Syracuse, but by his time Oenotria and Italy had become synonymous, and the name also applied to most of Lucania as well. The Greeks gradually came to apply the name Italia to a larger region, excavations throughout Italy revealed a Neanderthal presence dating back to the Palaeolithic period, some 200,000 years ago, modern Humans arrived about 40,000 years ago. Other ancient Italian peoples of undetermined language families but of possible origins include the Rhaetian people and Cammuni. Also the Phoenicians established colonies on the coasts of Sardinia and Sicily, the Roman legacy has deeply influenced the Western civilisation, shaping most of the modern world
41.
Moravia
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Moravia is a historical country in the Czech Republic and one of the historical Czech lands, together with Bohemia and Czech Silesia. Moravia has an area of over 22,348.87 km2 and about 3 million inhabitants, the statistics from 1921 states, that the whole area of Moravia including the enclaves in Silesia covers 22,623.41 km2. The people are historically named Moravians, a subgroup of Czechs, the land takes its name from the Morava river, which rises in the northern tip of the region and flows southward to the opposite end, being its major stream. Moravias largest city and historical capital is Brno, however before being sacked by the Swedish army during the Thirty Years War, though officially abolished by an administrative reform in 1949, Moravia is still commonly acknowledged as a specific land in the Czech Republic. Moravian people are aware of their Moravian identity and there is some rivalry between them and the Czechs from Bohemia. Moravia occupies most of the part of the Czech Republic. Moravian territory is naturally strongly determined, in fact, as the Morava river basin, with effect of mountains in the west and partly in the east. Moravia occupies a position in Central Europe. All the highlands in the west and east of part of Europe run west-east. Moravia borders Bohemia in the west, Lower Austria in the south, Slovakia in the southeast, Poland very shortly in the north and its natural boundary is formed by the Sudetes mountains in the north, the Carpathians in the east and the Bohemian-Moravian Highlands in the west. The Thaya river meanders along the border with Austria and the tripoint of Moravia, Austria and Slovakia is at the confluence of the Thaya, the northeast border with Silesia runs partly along the Moravice, Oder and Ostravice rivers. Between 1782–1850, Moravia also included a portion of the former province of Silesia – the Austrian Silesia. Geologically, Moravia covers an area between the Bohemian Massif and the Carpathians, and between the Danube basin and the North European Plain. Its core geomorphological features are three wide vales, namely the Dyje-Svratka Vale, the Upper Morava Vale and the Lower Morava Vale, the former two form the westernmost part of the Subcarpathia, the latter one is the northernmost part of the Vienna Basin. The vales surround the low range of Central Moravian Carpathians, the highest mountains of Moravia are situated on its northern border in Hrubý Jeseník, the highest peak is Praděd. Second highest are the Moravian-Silesian Beskids at the very east, with Smrk, the White Carpathians along the southeastern border rise up to 970 m at Velká Javořina. The spacious, but moderate Bohemian-Moravian Highlands on the west reach 837 m at Devět skal. The fluvial system of Moravia is very cohesive, as the border is similar to the watershed of the Morava river
listen)) and in German as Böhmerwald, is a low mountain range in Central Europe. Geographically, the mountains extend from Plzeň Region and South Bohemia in the Czech Republic to Austria and Bavaria in Germany, and form the highest truncated uplands of the Bohemian Massif, up to 50 km wide. They create a natural border between the Czech Republic on one side and Germany and Austria on the other.
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