There is no water body within the European Union which is surrounded by more countries than the Baltic Sea likewise no water body is more diverse regarding geological environmental and ecological conditions In response to postglacial development there is isostatic uplift in the northern part of the Baltic Sea with rates of up to 9 mm/year the southern part is sinking at rates up to 2 mm/year Crystalline rocks in the area of uplift and soft glacial and postglacial deposits in the area of sinking result in erosion and coastal retreat along the southern Baltic Sea coastline whilst the northern countries ale gaining land Additionally the marine resources of raw materials such as sand gravel and stones are of limited extent and volume in the most south westerly and southerly part of the Baltic Sea due to the late glacial and Holocene development Such conditions, combined with the predicted sea level rise will lead to an increasing demand of aggregate resources in the future due to a higher demand for shot e protection measures as soft solutions like beach and dune nourishment are favoured in many countries At the same time restrictions due to EU and national directives are increasing limiting the number of resources which can be used This introduction gives both in overview about the environmental conditions of the Baltic Sea which arc controlling the availability of sand and gravel resources and is smell a short summary about the exploitation and use of sand and gravel in the countries surrounding the Baltic Sea
Alar Rosentau, Volker Klemann, Ole Bennike, Holger Steffen, Jasmin Wehr, Milena Latinović, Meike Bagge, Antti Ojala, Mikael Berglund, Gustaf Peterson, Kristian Schoning, Anton Hansson, Lars Nielsen, Lars B. Clemmensen, Mikkel Ulfeldt Hede, Aart Kroon, Morten Pejrup, Lasse Sander, Karl Stattegger, Klaus Schwarzer, Reinhard Lampe, Matthias Lampe, Szymon Uścinowicz, Albertas Bitinas, Ieva Grudzinska,
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