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

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Fluvial Geomorphology and River Restoration: Tiroler Lech Nature Parkech River is often considered the only near-natural river landscape in the northern Alps. Although it has undergone manifold alterations since the end of the nineteenth century—later than most other Alpine rivers—it is granted sufficient space to form a braided river landscape, with huge gravel bank

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The Imprint of Quaternary Processes on the Austrian Landscapeternary. The Early Pleistocene record consists of LPSs and gravel deposits with no indication of a glacier advance. Four major glaciations, namely Günz, Mindel, Riss and Würm (from oldest to youngest)—are known. These Ice Ages were characterized by a large complex of transection glaciers, i.e. an in

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River and Valley Landscapes, shaped the recent character of the valleys. Based on morphology and sedimentology, we provide a classification of valleys into 5 types. The sediment fills of the valleys are important for drinking water supply.

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Karst Landscapes in Austriariabilities are well-known hydrologic features. Austria hosts 18,100 caves, and some of them are amongst the longest and deepest in the world. Although the majority of the caves are of epigenetic origin, some caves are also related to hypogene speleogenesis. Imprints from human activities on the kar

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Geoheritage, Geotourism and Landscape Protection in Austrias?–?is unfortunately not included in Austria’s nature protection laws. Geotourism has the goal to raise the awareness of abiotic nature attributes, together with promoting a profound understanding of Earth sciences and the conservation of geodiversity. Geotourism and geoheritage are two sides of the

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Deeply Incised Valley Meanders of the Bohemian Massifaya Valley is cut into the Thaya granite and Bite? gneiss, and characterized by steep valley sides, castellated rock outcrops, boulder fields and block streams. Boulder fields and block streams developed by unloading of rocks in the Late Pleistocene and were accentuated during the Holocene by gravit

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