Lincoln Sea Lincoln Sea Lincoln Sea (; ) is a body of water in the Arctic Ocean, stretching from Cape Columbia, Canada, in the west to Cape Morris Jesup, Greenland, in the east. The northern limit is defined as the great circle line between those two headlands. It is covered with sea ice throughout the year, the thickest sea ice in the Arctic Ocean, which can be up to thick. Water depths range from to . Water and ice from Lincoln Sea empty into Robeson Channel, the northernmost part of Nares Strait, most of the time. The sea was named after Robert
East Siberian Railway carried continued its increase along with the reconstruction of transportation facilities and introduction of new technology. In 1948, the East Siberian Railway reached its pre-war loading and cargo-turnover level. In 1958, they commissioned the new Taishet-Bratsk-Lena railway, which connected the basins of the Angara and Lena Rivers with the rest of the Siberian railroad network, providing immediate access to mineral deposits in the Angara basin (e.g. the Korshunovskoye iron ore deposit) and abundant logging regions and ensuring an uninterrupted supply of cargo to the northern areas of Irkutsk Oblast and Yakutia. At the end of 1965, a long Abakan-Taishet section