The first person to give a correct scientific explanation of this phenomenon was Mikhail Lomonosov, around 1750. The density of ice is about 0.92 kg per liter, that of sea water is about 1.025 kg per liter. For this reason, 920 parts of the 1025, or about 90 percent, of the iceberg's volume need to be below the water line. Lomonosov grew up on the shore of the White Sea in the European part of Russia. He studied in Marburg, and is credited with introducing the word "iceberg" into the Russian language.