Pôdy minerálne slabé vznikajú najmä na horninách:
kremité žuly
porfýr
pararula
svorov
fylit
niektoré pieskovce
droby
piesky.
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This blog is edited by Peter Pišút, Comenius University, Faculty of Natural Sciences, Department of Physical Geography and Geoecology, Mlynská dolina, 842 15, Bratislava 4, Slovakia
