Age and origin of ice‐cored moraines in Jotunheimen and Breheimen, southern Norway: insights from Schmidt‐hammer exposure‐age dating. Issue 4 (21st April 2014)

• Record Type: Journal Article
• Authors: Matthews, John A.; Winkler, Stefan; Wilson, Peter
• Is Part Of: Geografiska annaler. Volume 96:Issue 4(2014)
• Page Start: 531
• Page End: 548
• Publication Date: 2014-04-21
• Subjects: Physical geography -- Periodicals; 551.4
• DOI: 10.1111/geoa.12046
• Languages: English
• ISSNs: 0435-3676

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>High‐precision Schmidt‐hammer exposure‐age dating (SHD) is applied to ice‐cored moraine‐ridge complexes at three high‐alpine glaciers in Jotunheimen and Breheimen, southern Norway. Local calibration curves were established using moraine ridges dating from the last 50 years and bedrock surfaces deglaciated ∼9700 years ago. SHD ages, with 95% statistical confidence intervals, ranged from 3920 ± 790 years to a negative (futuristic) age of –890 ± 580 years at Gråsubreen, 420 ± 700 to 260 ± 710 years at Vesle‐Juvbreen and 2250 ± 450 to 1605 ± 410 years at Østre Tundradalskyrkjabreen. Negatively skewed <italic>R</italic>‐value distributions were interpreted as the result of weathered boulders from reworked surfaces. This leads to the interpretation of these SHD ages as <italic>maximum</italic> estimates of moraine‐ridge age. Østrem's hypothesis (that the proximal ridges are the oldest and survived being overridden many times) is rejected on the basis of our SHD ages. Although ice‐cored moraine ridges resemble the flow structures of rock glaciers, Barsch's hypothesis (that these ice‐cored moraine complexes are rock glaciers) is also rejected. Instead, the ice‐cored moraine‐ridge complexes are considered to be glaciotectonic structures produced by the interaction of polythermal glaciers and alpine permafrost over the late Holocene. All the individual ridges were essentially formed during the 'Little Ice Age' glacier advance from material deposited earlier by multiple neoglacial events. The considerable size of the moraine complexes is attributed not only to the accumulation of material from these different events over a long period of time but also to their survival in the landscape during phases of glacier retreat when ice cores do not melt and fluvial and other destructive processes remain ineffective in the permafrost environment.</p> </abstract>