[4] This member is composed mostly of the product of the regional erosion of older layers — conglomerates, gravelstones, quartz sandstones, and others — that were deposited in a mostly continental setting.

[4] In some outcrops the Fytyn Member is absent, as result of a regional uplift, with the sedimentary material transported from this area to central parts of the Greater Caucasus.

[4] The Faraskat section began its deposition when the local layers were accompanied by a slow subsidence of the land and sedimentation on the previously denuded area.

[5] The Faraskat sequence represents the first proper coastal deposit in the unit and is composed by a mixture of coarse material, as well as wood fragments and siderite, with some layers being highly bioturbated.

[4] The transition between the Faraskat and Mizur members is gradual, forming a large sedimentary cycle from clayey to sandstone-dominated rocks.

[3] The Mizur Member contains numerous fragments of plants — stems, wood, and leaves — suggesting a clear influence of nearby emerged settings.

Some alterations near the tracks have been interpreted as derived from displaced sediments moved by the dinosaur upper limb during a search for burrowing organisms.