Slope dynamics in relation to the occupation and abandonment of a mountain farm in þistilfjörður, northeast iceland

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SUMMARY

    Iceland is a geologically and geomorphologically active island whose regional-scale landscape is the result of glacial, volcanic, and tectonic processes. This study focuses on three main farm sites: (a) the Flautafell farm (FLA); (b) the Several additional, deep, modern drainage ditches have also been dug with mechanical abandoned Nor(ur Hús farm site (NDH); and_(c) a group of unnamed archaeological ruins equipment in and around the wet hayfield. There is a clear overlap between the slope deposits, the field, and the farm buildings in the area. The presence of farms in . . .

     

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