- Suitable for children
Vuoksenniska is part of the First Salpausselkä, where the Vuoksi outlet channel broke through 5,700 years ago as a result of the Greater Saimaa flood. In the Imatra region, the First Salpausselkä is between 1-2 kilometres wide due to the long deposition time of 200 years, during which time the ice edge also had time to move. The network of paths in the Vuoksenniska school area lead hikers to a delta plain dotted with a few kettles in its southern parts. Typical features of end moraine ridges can also be seen along the path: on the ice-sheet side to the northwest, the sides of the ridges are long and gentle, while the southeastern sides are steep, often with lots of boulders. There are Saimaa Geopark signs in the parking areas of Vuoksenniska school area and along the geological forest trail, which provide information on the geology of the area e.g. deltas, marginal-moraine ridges, rock types and kettle holes.
Contents of the Saimaa Geopark sign along the Vuoksenniskantie road below the school: https://saimaageopark.fi/wp-content/uploads/2019/12/vuoksenniska_1906_web.pdf
The contents of the signposts along the Vuoksenniska geological forest trail: https://saimaageopark.fi/wp-content/uploads/2019/12/vuoksenniska_a3_1906_web.pdf
Route description of the Vuoksenniska geological forest trail and instructions for arrival: https://ekarjala-retkeily.fi/en/routes-and-destinations/destination/?id=38917431
You can also find more information on the South Karelian Foundation for Recreation Areas’ webpages.
Coordinates: x= 596127,896 y= 6789069,720 (ETRS-TM35FIN)
The above coordinates are working in GPS-devices and karttapaikka.fi services.
The below coordinates are working in Google maps services.
Coordinates: 61.224138528, 28.790103449 (ETRS89 maantieteelliset(~WGS84))
The point on the map points to the place where Vuoksi begins.
Image: Arto Hämäläinen