Titlebook: Landscapes and Landforms of Austria; Christine Embleton-Hamann Book 2022 Springer Nature Switzerland AG 2022 Austria.Austrian Geomorpholog

incredulity

Karst Landscapes in Austriaf lithologies—mainly limestone, dolomite, and marble—susceptible to dissolution (i.e. karstification). Those lithologies occur in every landscape including the complete range of altitude: Northern Calcareous Alps, Southern Calcareous Alps, Helvetic units, Central Eastern Alps, Bohemian Massif, Alpin

Galactogogue

Geomorphic Hazards in Austriarocesses affect assets such as exposed buildings or infrastructure lines, they turn into hazards. In particular in the mountainous parts and in the Alpine foreland geomorphic hazards of different magnitude and frequency have repeatedly led to economic losses and fatalities. Together, the mountains a

飛鏢

TIA742

HEDGE

Deeply Incised Valley Meanders of the Bohemian Massifplift and river channel incision starting before c. 5?Ma. The most impressive examples of incised valley meanders are located in the Waldviertel Highlands along the Thaya, Kamp and Krems rivers. In this chapter, some hotspot examples with canyon-like incised meanders and related other landforms with

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Wachau World Heritage Site: A Diverse Riverine Landscapef the Bohemian Massif. Middle Miocene (Badenian) sediments in the eastern part between Krems and Spitz indicate a pre-existent fjord-like bay of the Badenian Sea. Fluvial sediments in valleys north of the recent course of the Danube show a different, more northerly course of the Palaeo-Danube in the

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Sunken Roads and Palaeosols in Loess Areas in Lower Austria: Landform Development and Cultural Imporses of cultural and scientific importance. On the one hand, the presence of loess results in a particular set of landforms such as loess dells, gullies, sunken roads and sinkholes of both natural and anthropogenic origin. On the other hand, the many outcrops of loess with several metres of height st

Euthyroid

The Danube Floodplain National Park: A Fluvial Landscape with Expiration Date?ing floodplains in Central Europe. Here, the Danube River is still free flowing and forms the lifeline of the park. Prior to channelization in the nineteenth century, the Danube can be referred to as a high- to medium-energy variant of anabranching rivers that comprises both braiding and meandering

allergy

Lake Neusiedl Area: A Particular Lakescape at the Boundary Between Alps and Pannonian Basinan Basin, and therefore represents an important transition zone concerning terrain, climate, vegetation, fauna and cultures. We use geomorphological as well as geological data, topographical and historical maps plus historical charters to reconstruct the palaeohydrology of Lake Neusiedl and document

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