Omari Gates
Austria is a landlocked country in Central Europe with a diverse terrain and topography. The country is bordered by eight countries: Germany, the Czech Republic, Slovakia, Hungary, Slovenia, Italy, Switzerland, and Liechtenstein. The Austrian landscape is characterised by mountains and forests, with the Austrian Alps forming the physical backbone of the country. The Alps extend from Switzerland into Austria, with several branches including the Bavarian, Carnic, and Otztaler ranges. The tallest peaks are in the central Tauern Range. The Northern Alpine Foreland, which includes the Danube Valley, is moderately hilly or flat. The Austrian Plateau, located in the northeastern part of the country, is another diverse region with rolling hills, plateaus, and fertile plains.
| Characteristics | Values |
|---|---|
| Terrain | Diverse, including mountains, rolling hills, plateaus, valleys, and lakes |
| Geography | Landlocked, located in Central Europe, South-Central Europe, or Eastern Hemisphere |
| Area | 83,879 sq. km (32,386 sq mi) |
| Bordering Countries | 8: Germany, Czech Republic, Slovakia, Hungary, Slovenia, Italy, Switzerland, and Liechtenstein |
| Mountain Ranges | The Alps, Northern Calcareous Alps, Southern Calcareous Alps, Central Alps, Bavarian, Carnic, Otztaler, Tauern Range |
| Highest Mountain | Großglockner, 3,797 m |
| Rivers | Danube, Drau, Enns, Inn, Mur, Raab, and Traun |
| Lakes | Lake Constance, Lake Neusiedler (lowest point in Austria) |
| Climate | Oceanic (Cfb), Cool/Warm-summer humid continental (Dfb), Subarctic/Subalpine (Dfc), Tundra/Alpine (ET), Ice-Cap (EF) |
| Weather Systems | Atlantic Maritime, Continental, Mediterranean |
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What You'll Learn
The Austrian Alps
The Alps serve as a watershed for Europe's three major kinds of weather systems that influence Austrian weather. The Atlantic maritime climate from the northwest is characterized by low-pressure fronts, mild air from the Gulf Stream, and precipitation. The continental climate is characterized by low-pressure fronts with precipitation in summer and high-pressure systems with cold and dry air in winter. It affects mainly eastern Austria. The Mediterranean high-pressure systems from the south are characterized by few clouds and warm air, and they influence the weather of the southern slopes of the Alps, making them the most temperate part of Austria.
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The Danube Valley
The Wachau is 36 kilometres (22 miles) long and is located midway between the towns of Melk and Krems. The area is known for its architectural elegance, including ancient monasteries such as Melk Abbey and Göttweig Abbey, castles, and ruins, as well as its urban architecture. The town of Dürnstein is a well-known tourist attraction, where King Richard I of England (Richard the Lionheart) was held captive in the 12th century.
The river valley's geological formation is primarily of crystalline rocks, with Tertiary and Quaternary deposits in wider areas of the valley and the Spitzer Graben. The land formation is influenced by clay and silt deposits around Weissenkirchen and at the beginning of the Wachau stretch. The Wachau's wine-growing tradition dates back to the medieval period of Roman settlements in the area.
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Northeastern Austrian Plateau
Northeastern Austria is characterised by the Danube River, which winds between the eastern edge of the Alps and the hills of Bohemia and Moravia in its journey toward the Alföld, or Hungarian Plain. Vienna lies in the area where the Danube emerges from between the mountains into the drier plains.
The Austrian Alps form the physical backbone of the country. They may be subdivided into a northern and a southern limestone range, each of which is composed of rugged mountains. These two ranges are separated by a central range that is softer in form and outline and composed of crystalline rocks. The highest mountain in Austria is Großglockner, which stands at 3,797 m.
The Alps serve as a watershed for Europe's three major kinds of weather systems that influence Austrian weather. The Atlantic maritime climate from the northwest is characterised by low-pressure fronts, mild air from the Gulf Stream, and precipitation. Mediterranean high-pressure systems from the south are characterised by few clouds and warm air, and they influence the weather of the southern slopes of the Alps and that of the Southeastern Alpine Foreland, making them the most temperate part of Austria.
The Northeastern Austrian Plateau, also known as the Austrian granite plateau, accounts for 10% of Austria's landmass. It is located in the central area of the Bohemian Mass, north of the Danube Valley. The granite massif of the Bohemian Forest, a low mountain range with bare and windswept plateaus and a harsh climate, is located here.
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Northern Alpine Foreland
The Northern Alpine Foreland is a geographic feature of Austria, covering just over 28% of the country. It is a hilly subalpine region, stretching between the northern Alps and the Danube. The area includes the Danube Valley, and the lowlands and hilly regions in northeastern and eastern Austria.
The Northern Alpine Foreland is influenced by the continental climate, characterised by low-pressure fronts with precipitation in summer and high-pressure systems with cold and dry air in winter. This climate affects mainly eastern Austria. The weather systems that determine the country's climate also bring pollution into Austria from northwestern Europe.
The Northern Alpine Foreland is an area of interest for geothermal energy studies. The 3D conductive thermal field of the North Alpine Foreland Basin has been studied to understand the influence of the deep structure and the adjacent European Alps on the temperature distribution in the area. The study found that the thermal field is controlled by conduction in the lithospheric mantle and the crystalline crust.
The Northern Alpine Foreland has a rich settlement history dating back to the Neolithic period. Archaeologists and researchers have studied the settlement patterns and cultural boundaries of this region to understand the social relations and continuity in the landscape. The individual houses and settlements of the Neolithic period were generally short-lived, suggesting fluidity in social relations at the local level.
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Bohemian Massif
The Bohemian Massif is a geomorphological province in Central Europe. It is a large massif that spans the majority of the Czech Republic, eastern Germany, southern Poland, and northern Austria. The massif is made up of crystalline rocks that are more than 300 million years old, dating back to the Permian period. The Bohemian Massif is divided into six subprovinces:
- Sudetes: This subprovince includes mountain ranges such as the Lusatian Mountains, Jizera Mountains, Giant Mountains, Owl Mountains, and Stołowe Mountains.
- Ore Mountains: This subprovince includes the Ore Mountains themselves, as well as the Elbe Sandstone Mountains and the Central Bohemian Upland.
- Bohemian Forest: This subprovince includes the Bohemian Forest, Bavarian Forest, Upper Palatine Forest, Gratzen Mountains, and the Granite and Gneiss Plateau.
- Bohemian-Moravian: This subprovince includes the Bohemian-Moravian Highlands and Brno Highlands.
- Poberoun: This subprovince includes the Brdy mountain range and the Prague Plateau.
- Bohemian Table: This subprovince includes the lowlands around the Elbe River.
The landscapes within the Bohemian Massif are mostly characterised by rolling hills, with gentle valleys and broad, flat ridges and hilltops to the north of the Danube River. The massif also includes plateaus, such as the Prague Plateau, and water gaps, such as the Wachau and the Strudengau. Geologically, the Bohemian Massif is part of the Hercynian Forest subsystem and borders the Western Carpathians to the east, the Eastern Alps to the south, the North European Plain to the north, and the Central Uplands to the west.
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Frequently asked questions
The terrain of northern Austria is largely mountainous, with the Northern Alpine Foreland and the Danube Valley being the only moderately hilly or flat regions. The Northern Calcareous Alps, which run from Vorarlberg through Tyrol into Salzburg, are predominantly made of limestone and dolomite.
The tallest peaks in Austria are in the central Tauern Range. The highest mountain in the country is Großglockner, at 3,797 m.
The climate in northern Austria is influenced by the Alps, which bring cold and dry air in winter, and low-pressure fronts with precipitation in summer.
