Historical Ostrobothnia was separated from southern Finland by
Suomenselkä, a
drainage divide which directs the flow of water north to the
Merenkurkku or
Perämeri and south to the
Gulf of Finland or
Selkämeri. To the east, it was bordered by Russian Karelia on the
Maanselkä watershed, which divides the estuaries of the
Oulujoki and
Iijoki from the estuaries of rivers flowing to the
White Sea. The northern borders are poorly defined, partly because permanently fixed habitations were a relatively new phenomenon at the time of the introduction of the
county system, which replaced the older provincial divisions. On the coast, the border ran somewhere between the
Torniojoki and Iijoki, without any formal definition inland, though the watershed between the
Kemijoki, Iijoki and
Olhavajoki estuaries serves as an approximate definition. 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
marsh. Inland the landscape is dominated by
coniferous forests and hills, with an occasional village or small town. The most important geographical feature of inland Ostrobothnia is the 887 km2 lake
Oulujärvi. Most activity in the region of Kainuu is centered around this lake, which is connected to the sea via the Oulujoki. North of Kainuu,
Koillismaa forms one of the most rural and poorest sub-regions in Finland. == Heraldry ==