Кандалакшский залив
Since deglaciation the rate of post-glacial rebound in the Kandalaksha Gulf has varied. Since the White Sea connected to the World's oceans uplift along southern coast of the gulf has totaled 90 m. In the interval 9,500–5,000 years ago uplift rate was of 9–13 mm/yr. Prior to the Atlantic period uplift rate had decreased to 5–5.5 mm/yr, to then rise briefly before arriving at the present uplift rate is of 4 mm/yr.