Salpausselkä

Salpausselkä is an extensive ridge system left by the ice age in Southern Finland. It is a large terminal moraine formation that formed in front of the Baltic ice lake during the Younger Dryas period about 12.700-11.500 years ago. It runs from Hanko hundreds of kilometers to the east. It traps the extensive river and lake systems of Central Finland known as Finnish Lakeland ( _fi. Järvi-Suomi, "Lake Finland") and forces the water to flow through few breaches in the ridge. The Vuoksi River flows from lake Saimaa into lake Laatokka (Ladoga, Russia). From there the water subsequently flows through river Neva into the Gulf of Finland, bypassing the Salpausselkä. The Kymi River flows from Päijänne into the Gulf of Finland. An artificial breach from the Lakeland is the Saimaa Canal, from Saimaa into the Gulf of Finland. There are also a formations called "Second and Third Salpausselkä", which are similar in form but smaller. They are situated north of the main Salpausselkä, and were formed later respectively.