The Baltic Klint (Clint, Glint; Estonian: Balti klint, Swedish: Baltiska klinten, Russian: Балтийско-Ладожский уступ, Глинт) is an erosional limestone escarpment and cuesta on the coast of the mainland and several islands of the Baltic Sea in Sweden, Estonia, and Russia. The Baltic Klint is active landform showing some retreat in the present. However, it is not known to which degree the Baltic Klint originated in postglacial time or if it evolved from cliff-like forms sculpted by the Fennoscandian Ice Sheet. In the island of Gotland, 20th century cliff retreat rates have been estimated at 0.
https://en.wikipedia.org/wiki/Baltic_Klint
The Baltic Klint (Clint, Glint; Estonian: Balti klint, Swedish: Baltiska klinten, Russian: Балтийско-Ладожский уступ, Глинт) is an erosional limestone escarpment and cuesta on the coast of the mainland and several islands of the Baltic Sea in Sweden, Estonia, and Russia. The Baltic Klint is active landform showing some retreat in the present. However, it is not known to which degree the Baltic Klint originated in postglacial time or if it evolved from cliff-like forms sculpted by the Fennoscandian Ice Sheet. In the island of Gotland, 20th century cliff retreat rates have been estimated at 0.
