Mountain Ranges, Deserts and Landforms of Slovakia

Geography

Although commonly referred to as a mountain chain, the Carpathians do not form an uninterrupted chain of mountains, but consist of several orographically and geologically distinctive groups. The northwestern Carpathians begin in Slovakia and southern Poland. They surround Transcarpathia and Transylvania in a large semicircle, sweeping towards the southeast, and end on the Danube near Orșova in Romania. The total length of the Carpathians is over 1,500 km (930 mi).

The mountain chain's width varies between 12 and 500 km (7 and 311 mi). The highest altitudes of the Carpathians occur where they are widest, in the Transylvanian plateau and in the southern Tatra Mountains group.

Geology

The area now occupied by the Carpathians was once occupied by smaller ocean basins. The Carpathian mountains were formed during the Alpine orogeny in the Mesozoic and Cenozoic by moving the ALCAPA (Alpine-Carpathian-Pannonian), Tisza and Dacia plates over subducting oceanic crust.

The mountains take the form of a fold and thrust belt with generally north vergence in the western segment, northeast to east vergence in the eastern portion and southeast vergence in the southern portion. Currently, the area is the most seismically active in Central Europe.

The external, generally northern, portion of the orogenic belt is a Tertiary accretionary wedge of a so-called Flysch belt (the Carpathian Flysch Belt) created by rocks scraped off the sea bottom and thrust over the North-European plate.

Ecology

The ecology of the Carpathians varies with altitude, ranging from lowland forests to alpine meadows. Foothill forests are primarily of broadleaf deciduous trees, including oak, hornbeam, and linden. European beech is characteristic of the montane forest zone. Higher-elevation subalpine forests are characterized by Norway spruce (Picea abies). Krummholz and alpine meadows occur above the treeline.

Wildlife in the Carpathians includes Eurasian brown bear (Ursus arctos arctos), Eurasian wolf (Canis lupus lupus), Eurasian lynx (Lynx lynx), European wildcat (Felis silvestris), Tatra chamois (Rupicapra rupicapra tatrica), European bison (Bison bonasus), and golden eagle (Aquila chrysaetos).

Geography

Its territory covers approximately 52,000 km2 (20,000 sq mi) of Hungary, approximately 56% of its total area of 93,030 km2 (35,920 sq mi). The highest point of the plain is Hoportyó (183 m (600 ft)); the lowest point is the Tisza River. The terrain ranges from flat to rolling plains.

The most important Hungarian writers inspired by and associated with the plain are Ferenc Móra and Zsigmond Móricz, as well as the poets Sándor Petőfi and Gyula Juhász.

Hungarian scientists born on the plain include Zoltán Bay, physicist; János Irinyi, chemist, inventor of the noiseless match; János Kabay, pharmacologist; Gábor Kátai, physician and pharmacist; and Frigyes Korányi, physician and pulmonologist.

History

During the prehistoric era, the Great Hungarian Plain was a place of cultural and technological changes, as well as an important meeting point of cultures of Eastern and Western Europe. It is a region of great archaeological importance to major European cultural transitions.

Agriculture began in the Great Hungarian Plain with the Early Neolithic Körös culture, located in present-day Serbia, 6000–5500 B.C.E. followed 5500 B.C.E. by the Linear Pottery culture (LBK) which later became the dominant agricultural culture of Europe. The LBK was followed by the Lengyel culture in the Late Neolithic 5000–3400 BC.

Terminology disputes about wider location of the Plain

The Great Hungarian Plain is often depicted as "part of" the Pannonian Basin, however it is often disputed by Hungarian geographers, due to its erroneous and unhistorical nature of the "Pannonian Basin" term.

Regarding the name as such, in terms of ancient history, namely that the northern and eastern boundary line of the namesake Roman province of Pannonia was formed by the River Danube. The Roman province Pannonia was bounded on the north and east by the Danube river, thus the Great Hungarian Plain was clerly not part of that ancient Roman province.

Climate

The Tatras lie in the temperate zone of Central Europe. They are an important barrier to the movements of air masses. Their mountainous topography causes one of the most diverse climates in that region.

The highest precipitation figures are recorded on the northern slopes. In June and July, monthly precipitation reaches around 250 mm (10 in). Precipitation occurs from 215 to 228 days a year. Thunderstorms occur 36 days a year on average.

Peaks are sometimes covered with snow or ice throughout the year. Avalanches are frequent.

Extreme temperatures range from −40 °C (−40 °F) in the winter to 33 °C (91 °F) in warmer months. Temperatures also vary depending on the altitude and sun exposure of a given slope. Temperatures below 0 °C (32 °F) last for 192 days on the summits.

Overview

The Tatras are a mountain range of a corrugated nature, originating from the Alpine orogeny, and therefore characterized by a relatively young-looking lie of the land, quite similar to the landscape of the Alps, although significantly smaller. It is the highest mountain range within the Carpathians.

The overall nature of the Tatras, together with their easy accessibility, makes them a favorite with tourists and researchers. Therefore, these mountains are a popular winter sports area, with resorts such as Poprad and the town Vysoké Tatry (The Town of High Tatras) in Slovakia created in 1999, including former separate resorts: Štrbské Pleso, Starý Smokovec, and Tatranská Lomnica or Zakopane, called also "winter capital of Poland".

Tourism

In 1683, an anonymous author published a book of adventures and excursions in the Tatras titled Ungarischer Oder Dacianischer Simplicissimus, Vorstellend Seinen wunderlichen Lebens-Lauff, und sonderliche Begebenheiten gethaner Raisen, Nebenst Wahrhafter Beschreibung dess vormals im Nor gestandenen und offters verunruhigten Urgerland, which translates roughly to Hungarian or Dacian Simplicissimus, presenting his strange life and the peculiar events of his adventures, together with a true description of the ancient lands that once stood in the north and were often troubled. The author was later discovered to be Daniel Speer of Wrocław, who lived in the sub-Tatra region for about six years.