An extensive permanent snowfield and the possible occurrence of permafrost in till in the Ridnitšohkka area, Finnish Lapland

• Published in: Bulletin of the Geological Society of Finland
• Main Authors: H. Hirvas, P. Lintinen, P. Kosloff
• Format: Article in Journal/Newspaper
• Language: English
• Published: Geological Society of Finland 2000
• Subjects: periglacial features; snow; firn; permafrost; till; drilling; Ridnitvsohkka; Lapland; Finland; Geology; QE1-996.5; Ice
• Online Access: https://doi.org/10.17741/bgsf/72.1-2.003; https://doaj.org/article/dcd101c747dd47639f90c9bf612442e4

An area of permanent snow and frozen ground was studied at the end of summer seasons during the years 1990–1993 near the summit of Ridnitvsohkka fell, which at 1317 m a.s.l. is the second highest peak in Finland. The eastern flank of Ridnitvsohkka has the most extensive area of permanent snow (3 km2) in Finland, while the summit region represents the highest single area of basal till devoid of vegetation cover and displaying patterned ground features. The ground penetrating radar results show that the form of the snowfield does not conform to the topography of the underlying bedrock and reveal the presence of several continuous reflectors dipping down-slope. Observations based on drilling and a single test pit indicate that the snowfield is 6.2 m thick and that it contains discontinuous lenses or layers of ice from 2 to 30 mm in thickness. Plant material from the depth of 4.05 m in the drilling core yielded a radiocarbon age of 35 years, while variations in the size of lichens growing at the edge of the snowfield indicated that the snowfield was of considerably greater extent some 100 to 150 years ago. The results suggest that the snowfield has been stable for a relatively long period but the “residence time” of snow in the snowfield is rather short, presumably less than 100 years and possibly only a few decades. Percussion drilling on the Ridnitvsohkka summit plateau, situating 1290 m a.s.l., revealed that the till was frozen at the depth of 1.9 m at the end of July 1993. Discovery of frozen till shows that frozen ground can locally survive from one season to the next, while the extent of the permanent snowfield and vegetation-free patterned ground suggest that the conditions favourable for permafrost might have existed over wider areas.