The natural monument is a three-tiered cascade of waterfalls descending from the eastern cliff of the Askhi limestone massif into the valley of the Satsiskvilo River. The upper two tiers form on a right tributary of the Satsiskvilo: the first is about 25 m high, while the second waterfall reaches up to 70 m. Twenty meters after the stream joins the Satsiskvilo, the cascade's third tier forms, about 35 m high.