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...
Published in: | Scottish Geographical Journal |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2018
|
Subjects: | |
Online Access: | https://research-portal.st-andrews.ac.uk/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 |