| http://www.w3.org/ns/prov#value | - The sand is mostly composed of quartz and feldspar grains, derived from the granite bedrock.Linaria alpina, another plant colonising the new terrain.A crater-like depression, formed as a result of the melting of buried stagnant ice.Downhill creep of sediments has led to the formation of crevasse-like structures (top) and small overthrusts (bottom).Recent sedimentary terraces at the margin of th ol
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