The rocky mass called Markovi Kuli are composed of numerous, diverse small denudation forms representing exceptionally fine sculpture of the relief. Similar shapes can be noted in the wider area of Prilep, from the area of Mariovo to Kajmakcalan, but such an intensive concentration and such diversity of micro relief forms as at Markovi Kuli have not been recorded so far in broader environment. This phenomenal wealth of shapes is due, mainly, to the geological composition of the terrain composed of metamorphic rocks (gneiss) broken through by younger granites¬granodiorites (ademelites), climate, relief and plant cover.
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