 The tops of the massif represent the first (advancing from west to east) in the Caucasus alpine-type peaks, that is, rising much higher than the upper boundary of the forest, having a wide belt of subalpine and alpine mountain meadows.In addition, Fisht is the westernmost peak of the Caucasus, which has glaciers on its slopes (Big and Small Fishtinsky glaciers) and considerable rock faults.Structurally, Fisht is a blocky uplift composed of layers of reef-limestone.