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 the southern coast of the gulf has totaled 90 m. In the interval from 9,500–5,000 years ago the uplift rate was of 9–13 mm/yr. Prior to the Atlantic period the uplift rate had decreased to 5–5.5 mm/yr, to then rose briefly before arriving at the present uplift rate of 4 mm/yr.