Molards as an indicator of permafrost degradation and landslide processes

Molards have been defined in the past as conical mounds of debris that can form part of a landslide’s deposits. We present the first conclusive evidence that molards in permafrost terrains are cones of loose debris that result from thawing of frozen blocks of ice-rich sediments mobilised by a landsl...

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Bibliographic Details

Main Authors:	Costanza Morino, Susan J. Conway, Thorsteinn Saemundsson, Jon Kristinn Helgason, John Hillier, Frances E.G. Butcher, Matthew Balme, Colm J. Jordan, Tom Argles
Format:	Default Article
Published:	2019
Subjects:	Other earth sciences not elsewhere classified untagged Earth Sciences not elsewhere classified
Online Access:	https://hdl.handle.net/2134/37446
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