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Hydrography Of Hungary
The hydrology of Hungary, is mostly determined by Hungary's lying in the middle of the Carpathian Basin, half surrounded by the Carpathian Mountains. All parts of the country have some outflow. All surface water gravitates towards its southern center, and from there, is united in the Danube, which flows into the Black Sea. The whole of Hungary lies within the Danube drainage basin. The total length of all the irrigation systems and inland waterways in the country is about . The annual water balance of the country shows a surplus. Yearly about of water leaves the country towards the Black Sea. From that, precipitation amounts for only 10%, the rest being provided by the incoming rivers of surrounding countries. Rivers Hydro graphically Hungary can be divided into two roughly equal parts: the drainage basins of the Danube and the Tisza. The present network of Hungary's rivers began to take shape at the end of the Tertiary and the beginning of the Quaternary periods w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpathian Basin-Pannonian Basin
The Carpathian Mountains or Carpathians () are a range of mountains forming an arc across Central Europe. Roughly long, it is the third-longest European mountain range after the Ural Mountains, Urals at and the Scandinavian Mountains at . The range stretches from the far eastern Czech Republic (3%) and Austria (1%) in the northwest through Slovakia (21%), Poland (10%), Ukraine (10%), Romania (50%) to Serbia (5%) in the south. "The Carpathians" European Travel Commission, in The Official Travel Portal of Europe, Retrieved 15 November 2016 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vác
Vác (; german: Waitzen; sk, Vacov; yi, ווייצען) is a town in Pest county in Hungary with approximately 35,000 inhabitants. The archaic spelling of the name is ''Vácz''. Location Vác is located north of Budapest on the eastern bank of the Danube river, below the bend where the river changes course and flows south. The town is seated at the foot of the Naszály Mountain in the foothills of the Carpathians. Modern Vác Vác is a commercial center as well as a popular summer resort for citizens of Budapest. The Vác Cathedral, built 1761–1777, was modelled after St. Peter's Basilica in Rome. The episcopal palace houses a museum for Roman and medieval artifacts. The city is also known for its 18th-century arch of triumph and for its beautiful baroque city center. History Settlement in Vác dating as far back as the Roman Empire has been found. The origin of its name is debated. One hypothesis says that the name comes from a Hungarian tribal name "Vath". Another theor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esztergom
Esztergom ( ; german: Gran; la, Solva or ; sk, Ostrihom, known by alternative names) is a city with county rights in northern Hungary, northwest of the capital Budapest. It lies in Komárom-Esztergom County, on the right bank of the river Danube, which forms the border with Slovakia there. Esztergom was the capital of Hungary from the 10th until the mid-13th century when King Béla IV of Hungary moved the royal seat to Buda. Esztergom is the seat of the ''prímás'' (see Primate) of the Roman Catholic Church in Hungary, and the former seat of the Constitutional Court of Hungary. The city has a Christian Museum with the largest ecclesiastical collection in Hungary. Its cathedral, Esztergom Basilica, is the largest church in Hungary. Toponym The Roman town was called ''Solva''. The medieval Latin name was ''Strigonium''. The first early medieval mention is "''ſtrigonensis trigonensiscomes''" (1079-1080). The first interpretation of the name was suggested by Antonio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Danube Bend
The Danube Bend ( hu, Dunakanyar) is a curve of the Danube in Hungary, close to the town of Visegrád. Geology The present-day U-shaped loop is probably the result of an eruption of the volcano stretching over the whole area some 15 million years ago. The caldera of Keserűs Hill-volcano, with the associated lava dome formed a later eroded central in the north. The river follows the southern edge of this caldera. The region This region is touristically very significant. The landscape and the river attracts a lot of visitors both from the homeland and abroad. The most important towns are Visegrád, Szentendre and Budapest, while on the other (left) bank of the river can be found Vác, Nagymaros and some smaller towns, villages. The islands of the region are also interesting, mainly the large Szentendrei-sziget and Margaret Island (Margitsziget) within the capital city. Gallery Catedral of Vác.jpg, The Cathedral of Vác Visegrad danube.jpg, Szentendrei-sziget RedBio T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fluvial Terrace
Fluvial terraces are elongated terraces that flank the sides of floodplains and fluvial valleys all over the world. They consist of a relatively level strip of land, called a "tread", separated from either an adjacent floodplain, other fluvial terraces, or uplands by distinctly steeper strips of land called "risers". These terraces lie parallel to and above the river channel and its floodplain. Because of the manner in which they form, fluvial terraces are underlain by fluvial sediments of highly variable thickness.Fairbridge, R. W., 1968, ''Encyclopedia of Geomorphology.'' Reinhold Book Company, New York.Blum, M., and T.E. Tonqvist, 2000, ''Fluvial responses to climate and sea-level change, a review and look forward.'' Sedimentology. v. 47 suppl. 1, pp. 2-48. River terraces are the remnants of earlier floodplains that existed at a time when either a stream or river was flowing at a higher elevation before its channel downcut to create a new floodplain at a lower elevation. Changes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Börzsöny
Börzsöny (; sk, Novohradské hory, New City Mountains) is a mountain range in Northern Hungary. Its tallest peak is the Csóványos with . It is the westernmost member of the North Hungarian Mountains, which belongs to the Inner Western Carpathians. The varied landscape offers good hiking opportunities. A large part of the Börzsöny is national park. From the top of Csóványos we can see one of the country's most beautiful panorama on the Danube Bend (''Dunakanyar''). Geography The mountain is structurally divided into four parts: High Börzsöny, Northern Börzsöny, Western Börzsöny and Southern Börzsöny. High Börzsöny Here are the highest peaks of Börzsöny: the Csóványos (938 m), Magos-fa (916 m), Nagy-hideg Hill (864 m) and Nagy-Inóc (826 m). Northern Börzsöny Western Börzsöny Southern Börzsöny Hydrography There are about 470 creeks in Börzsöny. The major parts of the creeks are clean water. The mountain's longest and largest river is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Visegrád
Visegrád (; german: Plintenburg; la, Pone Navata or ; sk, Vyšehrad) is a castle town in Pest County, Hungary. It is north of Budapest on the right bank of the Danube in the Danube Bend. It had a population of 1,864 in 2010. The town is the site of the remains of the Early Renaissance summer palace of King Matthias Corvinus of Hungary and a medieval citadel. Etymology The name ''Visegrád'' (''Vyšehrad'') is of Slavic origin, meaning acropolis, literary "the upper castle" (the castle with a privileged position) or "the upper settlement". In modern Slovak and Czech, the form is ''Vyšehrad''. The castle of Visegrád is called ''Fellegvár'' (Citadel) in Hungarian,Antal Papp: Magyarország (Hungary), Panoráma, Budapest, 1982, , p. 860, pp. 229-236 In German, the town is called ''Plintenburg''. The German name ''Plintenburg'' or ''Blendenburg'' is said to come from the beautiful view that one has from the castle and is "blinded"/"dazzled" by this view. History Visegrád was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonic Uplift
Tectonic uplift is the geologic uplift of Earth's surface that is attributed to plate tectonics. While isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening (such as mountain building events), changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere. Tectonic uplift results in denudation (processes that wear away the earth's surface) by raising buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting an isostatic response in the region of denudation (which can cause local bedrock uplift). The timing, magnitude, and rate of denudation can be estimated by geologists using pressure-temperature studies. Crustal thickening Crustal thickening has an upward component of motion and often occurs when continental crus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Plain
The Great Plains (french: Grandes Plaines), sometimes simply "the Plains", is a broad expanse of flatland in North America. It is located west of the Mississippi River and east of the Rocky Mountains, much of it covered in prairie, steppe, and grassland. It is the southern and main part of the Interior Plains, which also include the tallgrass prairie between the Great Lakes and Appalachian Plateau, and the Taiga Plains and Boreal Plains ecozones in Northern Canada. The term Western Plains is used to describe the ecoregion of the Great Plains, or alternatively the western portion of the Great Plains. The Great Plains lies across both Central United States and Western Canada, encompassing: * The entirety of the U.S. states of Kansas, Nebraska, North Dakota and South Dakota; * Parts of the U.S. states of Colorado, Iowa, Minnesota, Missouri, Montana, New Mexico, Oklahoma, Texas and Wyoming; * The southern portions of the Canadian provinces of Alberta, Saskatchewan and Manitoba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drava
The Drava or Drave''Utrata Fachwörterbuch: Geographie - Englisch-Deutsch/Deutsch-Englisch'' by Jürgen Utrata (2014). Retrieved 10 Apr 2014. (german: Drau, ; sl, Drava ; hr, Drava ; hu, Dráva ; it, Drava ) is a river in southern Central Europe. With a length of ,Joint Drava River Corridor Analysis Report 27 November 2014 including the Sextner Bach source, it is the fifth or sixth longest tributary of the Danube, after the Tisza, Sava, Prut, Mureș (river), Mureș and perhaps Siret (river), Siret. The Drava drains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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