- Geography of Szabolcs-Szatmár-Bereg
Szabolcs-Szatmár-Bereg is situated inHungary 's far east, at the north-eastern tip of the country. It borders theUkraine , theSlovak Republic andRomania , and has good communications both byroad and rail. Within Hungary, the county is bordered byBorsod-Abaúj-Zemplén county and the River Tisza from the north west andHajdú-Bihar county from the south west.The early Hungarians transformed this region significantly by clearing large areas of forest to make way for
pasture s and plough-land. Approximately 5 to 5 square kilometres offorest were cleared for the construction of theSzabolcs earthwork in the ninth and tenth centuries and its ruins are still present. With the subsequent development of the country, the region became marginalized in the 15th century. On goingcivil war ,rebellion andwar exacted a heavy price and further hindered the region's development.The county's borders have been altered frequently over the years, its current territory being established in 1950 with the amalgamation of the counties of Szabolcs-Ung and Szatmár-Bereg-Ugocsa.
There are many
forest s, fields,pasture s,meadow s andmoorland forests in the county. Thebog moss moors atCsaroda , the Nyíres lake and the Bábtava lake are especially valuable, as they contain many rare species of fauna and flora.Szabolcs-Szatmár-Bereg is Hungary's sixth biggest county with a total land area of 5 936 square kilometres. From a geographical aspect, it is possible to divide the county into two main regions: The Upper Tisza Valley and the Nyírség.
Tisza is the most importantriver of the county. It enters Szabolcs-Szatmár-Bereg - and Hungary - atTiszabecs , and leaves the county atTiszadob . Its segment in Szabolcs-Szatmár-Bereg county is 235 kilometres long, out of which 208 kilometres belongs to the Upper Tisza Valley, reaching the area ofTokaj andRakamaz .The northern part of Nyírség is covered with sandy forest soils, the southern areas have loose wind-blown sand. Alluvial and meadow soils are found in the Upper Tisza region.
The county has a
continental climate ; it is cooler than the Great Plain because it is further north. Summers are cooler than in other parts of the Plains. Annual precipitation is 550-600 millimetres. The higher than average number of days of sunshine make ideal conditions for the growing oftomato es,sunflower ,tobacco ,apple s and otherfruit s.The county has 229 settlements, of which 20 are towns. The county capital and largest city is
Nyíregyháza with apopulation of 116 900 in 2003. The other cities have relatively small populations, only those ofKisvárda andMátészalka having around 18 000 inhabitants. The eastern part of the county is lightly populated and is dotted with small villages which iften have very poor economic conditions.River Tisza
The Upper Tisza region has many
stream s andriver s, but the Nyírség region has little surface water. The most important of River Tisza's tributaries is the RiverSzamos , which is also characterised by great variations in water volume. There areirrigation systems, a waterbarrage and ahydro electric power station on the Tisza atTiszalök .Lakes of various sizes have evolved in sandy areas such as the basin of the Sóstó (Salty lake) of
Nyíregyháza , whosealkaline ,hydrogen carbonate d waters have medicinal qualities. Many waterreservoirs have been built according to local demand. Thermal waters of 55-65 °C can be brought to the surface from wells as shallow as 1 000 metres. The most important thermal water reserves are in Nyíregyháza, Kisvárda, Mátészalka and Tiszavasvári. The county'sgeothermal energy still awaits exploitation.The county has relatively few
mineral reserves. Almost all of the big energy source transporting systems cross the county.
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