Die untere Grenze von Strukturbodenformen in den Gurktaler und Seetaler Alpen

Gudrun Höhl
On account of numerous miniature stone networks observed in the examined region down to 1500 metres, the question is raised, whether the „border-line of climatic patterned ground" — which is supposed to run in an altitude of 1800 or 2000 metres in the zone around the Central Alpes — should not include another zone (of the „initial forms") below the above mentioned line. And the question arises: isn't this the real lower border-line?