Kummakivi Travel Guide

Kummakivi presents a truly unique and awe-inspiring sight: a massive boulder seemingly frozen in a perpetual balancing act. This natural wonder is a glacial erratic, transported to its current location during the last Ice Age approximately 11,000 to 12,000 years ago. The boulder rests on a convex bedrock surface, with only about 0.5 square meters of its area in contact with the supporting rock. This precarious positioning makes it appear as though it could topple at any moment, yet it remains firmly in place.Both Kummakivi and the bedrock beneath are composed of mixed granite-cordierite-mica gneiss, typical of the region. Grooves and chatter marks on the rocks bear witness to the glacial erosion that shaped the landscape. The area surrounding Kummakivi emerged from under the continental ice sheet around 11,500 years ago, when the environment was vastly different, with the boulder perched on the shore of an ancient ice lake.Located in a forest near the border of Ruokolahti and Puumala, Kummakivi has been a point of interest for tourists since the 19th century. To preserve this geological marvel, Kummakivi was protected as a natural monument in 1962 under the Nature Conservation Act. Visitors can explore the surrounding South Finnish coniferous forest and lake ecosystems, and also discover a nearby moss bridge ('sammalsilta' in Finnish) across Pitkäjärvi lake. This bridge was originally built in the 1930s by the Kaukas company for forest workers.