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The aim of the article is to analyse the relationship between Quaternary geology, the idea of land elevation, nationalism and regionalism in Scandinavia, with special regard to the contribution of Swedish geologists at the end of the nineteenth century. From a scientific point of view, the idea of land elevation was connected to the acceptance of the glaciation theory and the elevation theory of Thomas F. Jamieson, but analysed in a wider cultural context it is possible to understand both the professionalization of Quaternary geology and the new theory of shore-line displacement as expressions of Swedish cultural nationalism. As a complement to the specific cultural history, the Quaternary geology enterprise was a way of constituting a unique natural history of the nation. One of the new theories that developed in this process was that of the Highest Marine Border, a complex concept established by the distinguished geologist Gerard De Geer at the end of the 1880s in order to defend the theory of land elevation, which was threatened by the work of Eduard Suess. The line was considered to be a geographical border that both expressed the elevation pattern and sharply divided Sweden into one part that had been covered by water during the post-glacial period and another part that had not. The study continues by looking more closely at the construction of the border in the north of Sweden. Through an account of a subsequent scientific dispute between De Geer and the geologist Arvid Gustaf Hogbom it is clear that the concept of the Highest Marine Border was shaped not only by nationalism but also by regionalism.
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