Difference between revisions of "Land of Hungary"

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''Land of [[Hungary]]'''
Landlocked and lying approximately between latitudes 45° and 49° N and longitudes 16° and 23° E, Hungary shares a border to the north with Slovakia, to the northeast with Ukraine, to the east with Romania, to the south with Serbia (specifically, the Vojvodina region) and Croatia, to the southwest with Slovenia, and to the west with Austria.
'''Relief'''
Dominating the relief are the great lowland expanses that make up the core of Hungary. The Little Alföld (Little Hungarian Plain, or Kisalföld) lies in the northwest, fringed to the west by the easternmost extension of the sub-Alps along the border with Austria and bounded to the north by the Danube. The Little Alföld is separated from the Great Alföld (Great Hungarian Plain, or Nagy Magyar Alföld) by a low mountain system extending across the country from southwest to northeast for a distance of 250 miles (400 km). This system, which forms the backbone of the country, is made up of Transdanubia (Dunántúl) and the Northern Mountains, separated by the Visegrád Gorge of the Danube. Transdanubia is dominated by the Bakony Mountains, with dolomite and limestone plateaus at elevations between 1,300 and 2,300 feet (400 and 700 metres) above sea level. Volcanic peaks comprise the Mátra Mountains in the north, reaching an elevation of 3,327 feet (1,014 metres) at Mount Kékes, Hungary’s highest peak. Regions of hills reaching elevations of 800 to 1,000 feet (250 to 300 metres) lie on either side of the mountain backbone, while to the south and west of Lake Balaton is an upland region of more-subdued loess-covered topography.
The Great Alföld covers most of central and southeastern Hungary. Like its northwestern counterpart, it is a basinlike structure filled with fluvial and windblown deposits. Four types of surface may be distinguished: floodplains, composed of river alluvium; alluvial fans, wedge-shaped features deposited at the breaks of slopes where rivers emerge from the mountain rim; alluvial fans overlain by sand dunes; and plains buried under loess, deposits of windblown material derived from the continental interior. These lowlands range in elevation from about 260 to 660 feet (80 to 200 metres) above sea level, with the lowest point at 256 feet (78 metres), on the southern edge of Szeged, along the Tisza River. In the northeast, bordering Slovakia, is Aggtelek National Park; characterized by karst terrain and featuring hundreds of caves, the area was designated a UNESCO World Heritage site in the late 20th century.
'''Drainage and soils'''
Hungary lies within the drainage basin of the Danube, which is the longest river in the country. The Danube and two of its tributaries, the Rába and Dráva rivers, are of Alpine origin, while the Tisza River and its tributaries, which drain much of eastern Hungary, rise in the Carpathian Mountains to the east. The Danube floods twice a year, first in early spring and again in early summer. During these phases, discharge is up to 10 times greater than river levels recorded during the low-water periods of autumn and winter. The Tisza forms a floodplain as it flows through Hungary; large meanders and oxbow lakes mark former channels. At Szolnok, peak discharges 50 times greater than average have been recorded. Devastating floods have occurred on the Danube, the Tisza, and their tributaries. About 2,500 miles (4,000 km) of levees have been built to protect against floods. The relatively dry climate of the central and eastern areas of the Great Alföld has necessitated the construction of large-scale irrigation systems, mostly along the Tisza River.
There are few lakes in Hungary, and most are small. Lake Balaton, however, is the largest freshwater lake in central Europe, covering 231 square miles (598 square km). Neusiedler Lake—called Lake Fertő in Hungary—lies on the Austrian border and was designated a World Heritage site by UNESCO in 2001. Lake Velence lies southeast of Budapest.
Gray-brown podzolic (leached) and brown forest soils predominate in the forest zones, while rich black earth, or chernozem, soil has developed under the forest steppe. Sand dunes and dispersed alkali soils are also characteristic.
'''Climate'''
Because of its situation within the Carpathian Basin, Hungary has a moderately dry continental climate. The mean annual temperature is about 50 °F (10 °C). Average temperatures range from 25 to 32 °F (−4 to 0 °C) in January to 64 to 73 °F (18 to 23 °C) in July. Recorded temperature extremes are 109 °F (43 °C) in summer and −29 °F (−34 °C) in winter. In the lowlands, precipitation generally ranges from 20 to 24 inches (500 to 600 mm), rising to 24 to 31 inches (600 to 800 mm) at higher elevations. The central and eastern areas of the Great Alföld are the driest parts of the country, and the southwestern uplands are the wettest. As much as two-thirds of annual precipitation falls during the growing season.
'''Plant and animal life'''
Human activities over the ages have largely destroyed the natural vegetation of Hungary. Just about half of the land is regularly cultivated, and about one-sixth is used for nonagricultural purposes. The remainder comprises meadows and rough pasture as well as forest and woodland. No part of the country is of sufficient elevation to support natural coniferous forest. Beech is the climax community at the highest elevations; oak woodland alternating with scrubby grassland are the climax communities at lower elevations in the upland regions.
Deer and wild pigs are abundant in the forests at higher elevations, while rodents, hares, partridge, and pheasant inhabit the lowlands. The once-numerous varieties of marsh waterfowl survive only in nature reserves. There are diverse species of freshwater fish, including pike, bream, and pike perch. Significant water and air pollution occurs in some of the industrial regions of the country.

Latest revision as of 03:32, 10 March 2015

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