After the ice : Lateglacial and Holocene landforms and landscape evolution in Scotland

• Published in: Earth and Environmental Science Transactions of the Royal Society of Edinburgh
• Main Author: Ballantyne, Colin K.
• Other Authors: University of St Andrews.School of Geography & Sustainable Development
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2018
• Subjects: Alluvial fan; Debris flow; Floodplain; Paraglacial; Periglacial; Permafrost; Postglacial; Rock-slope failure; Talus; Terraces; GE Environmental Sciences; General Environmental Science; General Earth and Planetary Sciences; T-NDAS; SDG 13 - Climate Action; GE; Sandar; Ice; Ice Sheet; permafrost
• Online Access: https://hdl.handle.net/10023/16465; https://doi.org/10.1017/S175569101800004X

During Lateglacial cold periods, permafrost developed throughout Scotland, sediment-mantled slopes were extensively modified by solifluction and other forms of periglacial mass movement, large-scale sorted patterned ground formed on plateaux, and enhanced rockfall resulted in talus accumulation belo...