Glacially moulded landslide runout debris in the Scottish Highlands

A tongue of hummocky terrain ∼1 km long and ∼400 m wide extends downslope from the source area of a rock-slope failure that formed the summit arête of Sgùrr nan Ceathreamhnan in the NW Highlands. The tongue descends from ∼810 m to ∼650 m, crosses a corrie obliquely and laps onto an opposing slope. I...

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Bibliographic Details
Published in:Scottish Geographical Journal
Main Author: Ballantyne, Colin K.
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://risweb.st-andrews.ac.uk/portal/en/researchoutput/glacially-moulded-landslide-runout-debris-in-the-scottish-highlands(c7f3747e-6089-481e-8e88-a25e2f0ad1ad).html
https://doi.org/10.1080/14702541.2018.1501085
https://research-repository.st-andrews.ac.uk/bitstream/10023/18130/1/Ballantyne_2018_SGJ_Glaciallymoulded_AAM.pdf