Dr Kirkbride studied the formation of corries in the Cairngorms.
A corrie is a basin-shaped feature created by glaciations in the mountains.
“present climate warming means there is little chance of a return of glacier ice to the Highlands for the foreseeable future”
Dr Stephan Harrison
University of Exeter
Using a technique called
cosmogenic 10Be dating, Dr Kirkbride showed that a small glacier in a
Cairngorms corrie piled up granite boulders to form moraine ridges
within the past few centuries, during the period of cool climate known
as the Little Ice Age.
Dr Kirkbride teamed up with Dr Jez Everest at the British Geological Survey in Edinburgh, and the Cosmogenic Isotope Analysis Facility at the Scottish Universities Environmental Reactor Centre in East Kilbride, to carry out the research.
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