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Volume 48, Number 2
1 February 2020
ISSN: 0091-7613
EISSN: 1943-2682
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Cover Image
Cover Image
COVER: The Mer de Glace glacier above Chamonix (European Alps), where Forbes bands were first described. Formed by the alternation of dust (in summer) and snow (in winter) falling in the Geant icefall, Forbes bands illustrate the ice velocity and the flow dynamic of the glacier. See Lehmann et al., “Postglacial erosion of bedrock surfaces and deglaciation timing: New insights from the Mont Blanc massif (western Alps)”, p. 139–144.
Photo by: B. Lehmann
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