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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] |
