|
Tápió
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 when the Pa ... [...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 and Southeast Europe. Roughly long, it is the third-longest European mountain range after the Ural Mountains, Urals at and the Scandinavian Mountains at . The highest peaks in the Carpathians are in the Tatra Mountains, exceeding , closely followed by those in the Southern Carpathians in Romania, exceeding . The range stretches from the Western Carpathians in Austria, the Czech Republic, Slovakia and Poland, clockwise through the Eastern Carpathians in Ukraine and Romania, to the Southern Carpathians in Romania and Serbia.About the Carpathians – Carpathian Heritage Society [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Surface Runoff
Surface runoff (also known as overland flow or terrestrial runoff) is the unconfined flow of water over the ground surface, in contrast to ''channel runoff'' (or ''stream flow''). It occurs when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is #Saturation excess overland flow, saturated by water to its full capacity, and the rain arrives #Infiltration excess overland flow, more quickly than the soil can absorb it. Surface runoff often occurs because wikt:impervious#Adjective, impervious areas (such as roofs and Road surface, pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or human-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of Soil erosion#Rainfall and runoff, soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vác
Vác (; ; ; ) is a thousand-year old city 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 Carpathian Mountains, 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 Bishop, 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". It has bee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esztergom
Esztergom (; ; or ; , known by Names of European cities in different languages: E–H#E, 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 Capitals of Hungary, 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 (bishop), Primate) of the Catholic Church in Hungary, and the former seat of the Constitutional Court of Hungary. The city has a Keresztény Múzeum, Christian Museum with the largest ecclesiastical collection in Hungary. Its cathedral, Esztergom Basilica, is the largest church in Hungary. Near the Basilica there is a campus of the Pázmány Péter Catholic University. Toponym The Roman town was called ''Solva''. The medieval Latin name was ''Strigoniu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Danube Bend
The Danube Bend () 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 Treffen Ungar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fluvial Terrace
Fluvial terraces are elongated Terrace (geology), 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. 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 in elevation can be due to changes in the base level (elevation of the lowest point in the fluvial system, usually the drainage basin) of the fluvial system, which leads to headward erosion along the length of either a stream or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (; archaic British English spelling: ''cañon''), gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the 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 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. Examples of mountain- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Börzsöny
Börzsöny (; or ''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 Divisions of the Carpathians are a categorization of the Carpathian mountains system. Below is a detailed overview of the major subdivisions and ranges of the Carpathian Mountains. The Carpathians are a "subsystem" of a bigger Alps-Himalaya S .... 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, 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-f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonic Uplift
Tectonic uplift is the orogeny, geologic uplift of Earth#Surface, Earth's surface that is attributed to plate tectonics. While Isostasy, isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of Thrust tectonics, crustal thickening (such as Mountain formation, mountain building events), changes in the density distribution of the crust and underlying Mantle (geology), 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 C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Plain
The Great Plains is a broad expanse of flatland in North America. The region stretches east of the Rocky Mountains, much of it covered in prairie, steppe, and grassland. They are the western part of the Interior Plains, which include the mixed grass prairie, the tallgrass prairie between the Great Lakes and Appalachian Plateau, and the Taiga Plains and Boreal Plains ecozones in Northern Canada. "Great Plains", or Western Plains, is also the ecoregion of the Great Plains or the western portion of the Great Plains, some of which in the farthest west is known as the High Plains. The Great Plains lie across both the Central United States and Western Canada, encompassing: *Most or all of the U.S. states of Kansas, Nebraska, and North and South Dakota; *Eastern parts of the U.S. states of Colorado, Montana, and Wyoming; *Parts of the U.S. states of New Mexico, Oklahoma, Texas; *Sometimes western parts of Iowa, Minnesota, and Missouri; *The southern portions of the Canadian province ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drava
The Drava or Drave (, ; ; ; ; ), historically known as the Dravis or Dravus, is a river in southern Central Europe.''Utrata Fachwörterbuch: Geographie - Englisch-Deutsch/Deutsch-Englisch'' by Jürgen Utrata (2014). Retrieved 10 Apr 2014. With a length of ,Joint Drava River Corridor Analysis Report , 27 November 2014 or , if the length of its Sextner Bach source is added, it is the fifth or sixth longest tributary of the |
