Ostrobothnia (historical province)
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Ostrobothnia,
in the east.Etymology
The word pohja means either "north" or "bottom", and maa is "land". There are two possible explanations for the dual meaning of pohja. The first is based on the ancient Scandinavian belief that the north was the bottom of the world,[citation needed] where the Sun disappeared each night. The second explanation points to the fact that houses were constructed with their backs to the north, the coldest direction, which may have given rise to the association.
Government
Ostrobothnia corresponds to the following modern
History
The earliest evidence of humans in Ostrobothnia is at the
During the Bronze and Iron Ages an agrarian society eventually replaced earlier structures in southern Ostrobothnia, whereas traditional economies survived much longer in the northern and inland locations. During the early
During the late stages of the war, the Swedish crown stationed regular troops in the province to help defend the population. This was in marked contrast to the earlier practice of making the province responsible for its own defence. After the war, the Ostrobothnians revolted against the troops' continued presence, leading to the
Katarina Asplund (1690–1758), a Finnish pietist, was a leading figure within the pietism movement in Ostrobothnia, and was often in conflict with the authorities on charges of blasphemy.[3]
The first towns in Ostrobothnia were established in the 17th century, obtaining prominence through the import of
In 1809 all of Finland, including Ostrobothnia, was separated from Sweden, though the regions of Norrbotten and Västerbotten remained on the Swedish side.
Geography
Historical Ostrobothnia was separated from southern Finland by
The stereotypical topographic feature of historical Ostrbothnia was the coastal plain north of Suomenselkä, in the modern regions of Ostrobothnia, Southern Ostrobothnia and Central Ostrobothnia. It is glacial (Weichselian glaciation) seabed, flat with a few hills, and characterized by rivers formed at the end of the glaciation period which run southeast to northwest. Post-glacial rebound is still causing the ground level to rise at a rate of about 9 mm per annum. Due to the flat terrain, this causes the Gulf of Bothnia to recede several kilometers each century, impacting navigation and the harbours of coastal cities in the region. The bedrock in the area, where exposed, features southeast-northwest oriented lines carved by rocks pushed by the advancing ice mass during the glaciation. When the ice melted, huge boulders (glacial erratics) and sand pits were also left behind.
On the coast of modern Northern Ostrobothnia, the topography remains flat, but instead of the fields of modern Central and Southern Ostrobothnia, the land is largely covered with
Heraldry
The
References
- ^ "Bottenhavet, Bottniska viken". Svensk etymologisk ordbok (1st ed.). 1922 – via Project Runeberg.
- ^ ISBN 9047418921.
- ^ Suomen kansallisbiografia/Finlands nationalbiografi
- ISBN 951-0-23739-6
External links
- Wolf Cave – Varggrottan – Susiluola A Pre-Ice Age Archaeological Find in Lappfjärd, Finland