Fortress of Suomenlinna
Built in the second half of the 18th century by Sweden on a group of islands located at the entrance of Helsinki's harbour, this fortress is an especially interesting example of European military architecture of the time.
Old Rauma
Situated on the Gulf of Botnia, Rauma is one of the oldest harbours in Finland. Built around a Franciscan monastery, where the mid-15th-century Holy Cross Church still stands, it is an outstanding example of an old Nordic city constructed in wood. Although ravaged by fire in the late 17th century, it has preserved its ancient vernacular architectural heritage.
Petäjävesi Old Church
Petäjävesi Old Church, in central Finland, was built of logs between 1763 and 1765. This Lutheran country church is a typical example of an architectural tradition that is unique to eastern Scandinavia. It combines the Renaissance conception of a centrally planned church with older forms deriving from Gothic groin vaults.
Verla Groundwood and Board Mill
The Verla groundwood and board mill and its associated residential area is an outstanding, remarkably well-preserved example of the small-scale rural industrial settlements associated with pulp, paper and board production that flourished in northern Europe and North America in the 19th and early 20th centuries. Only a handful of such settlements survive to the present day.
Bronze Age Burial Site of Sammallahdenmäki
This Bronze Age burial site features more than 30 granite burial cairns, providing a unique insight into the funerary practices and social and religious structures of northern Europe more than three millennia ago.High Coast / Kvarken Archipelago
The Kvarken Archipelago (Finland) and the High Coast (Sweden) are situated in the Gulf of Bothnia, a northern extension of the Baltic Sea. The 5,600 islands of the Kvarken Archipelago feature unusual ridged washboard moraines, ‘De Geer moraines’, formed by the melting of the continental ice sheet, 10,000 to 24,000 years ago. The Archipelago is continuously rising from the sea in a process of rapid glacio-isostatic uplift, whereby the land, previously weighed down under the weight of a glacier, lifts at rates that are among the highest in the world. As a consequence islands appear and unite, peninsulas expand, and lakes evolve from bays and develop into marshes and peat fens. The High Coast has also been largely shaped by the combined processes of glaciation, glacial retreat and the emergence of new land from the sea. Since the last retreat of the ice from the High Coast 9,600 years ago, the uplift has been in the order of 285 m which is the highest known ''rebound''. The site affords outstanding opportunities for the understanding of the important processes that formed the glaciated and land uplift areas of the Earth''s surface.Struve Geodetic Arc
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