Faroe Islands Following the turmoil caused by the Napoleonic Wars (1803-1815) in 1816, the Faroe Islands became a county in the Danish Kingdom. As part of Mercantilism, Denmark maintained a monopoly over trade with the Faroe Islands and forbade their inhabitants trading with others (e.g. the geographically close Britain). The trade monopoly in the Faroe Islands was abolished in 1856, after which the area developed as a modern fishing nation with its own fishing fleet. The national awakening from 1888 initially arose from a struggle to maintain the Faroese language and was thus culturally oriented, but after 1906 it became more political
Geology of the Faroe Islands erupted, plate tectonics has slowly moved the Faroe Islands away from the active volcanic region, which today is concentrated in Iceland and along the Mid-Atlantic Ridge. Meanwhile, the majority of the Faroe–Rockall Plateau has subsided beneath sea level while erosive forces–especially during the last few million years of alternating glacial and interglacial periods–have sculpted the landscape into their present-day shape. The overall thickness of volcanic and intervening rock layers of the Faroe Islands is more than , of which only is located above the present sea level. A deep well in Lopra, Suðuroy, has revealed details of the lower strata.