vuoristotunturien

Vuoristotunturien is a Finnish term that translates to "mountain fells" or "fell mountains." It refers to a type of high-altitude terrain characterized by rounded, treeless peaks and slopes that are often covered in heather, moss, and lichen. These landscapes are distinct from rugged, sharp-peaked mountains, featuring instead a more weathered and undulating topography.

Geologically, vuoristotunturien are typically formed by ancient bedrock that has been eroded over long periods by glaciation and weathering. The summits are usually broad and relatively flat, a result of glacial scouring and subsequent erosion. Vegetation above the treeline consists primarily of low-lying arctic-alpine flora, adapted to harsh conditions, including strong winds, cold temperatures, and a short growing season.

These formations are most commonly found in the northern parts of Fennoscandia, particularly in Finland, Sweden, and Norway, as well as in other arctic and subarctic regions. In Finland, the fells are a significant feature of Lapland, offering distinctive landscapes for tourism and recreation. Hiking, skiing, and observing the aurora borealis are popular activities in these areas. The term emphasizes the rounded, plateau-like nature of these elevated landforms, differentiating them from more dramatic mountain ranges.