Defining the centre of glacio-isostatic uplift of the last Scottish ice-sheet: The Parallel Roads of Glen Roy, Scottish Highlands

Journal of Quaternary Science

Volumn 17, Issue 5-6, 2002, Pages 527-533

  Dawson, Alastair G ^a   Hampton, Shaun ^a   Fretwell, Peter ^a   Harrison, Stephan ^a   Greengrass, Peter ^a  

^a Institute for Clean Growth and Future Mobility   (United Kingdom)

Author keywords

Glacio isostatic uplift; Ice dammed lakes; Shorelines; Younger Dryas

Indexed keywords

GLACIAL REBOUND; GLACIOISOSTASY; ICE SHEET; LAKE LEVEL; SHORELINE; UPLIFT; YOUNGER DRYAS;

UNITED KINGDOM;

EID: 0036662751     PISSN: 02678179     EISSN: None     Source Type: Journal    
DOI: 10.1002/jqs.712     Document Type: Article

References (17)

1. Shore erosion by frost: An example from the Scottish Lateglacial
2. Distribution and development of the Main Rock Platform, western Scotland: Reply
3. Late Devensian and Holocene glacio-isostatic uplift patterns in Scotland
4. Postglacial tectonics of the Scottish glacioisostatic uplift centre
5. The Main Rock Platform of the Firth of Lorn, western Scotland
6. Low-level shore platforms in the south-west Scottish Highlands: Altitude, age and correlation
7. On the parallel roads of Glen Roy, and their place in the history of the glacial period
8. Glacial rebound and sea level change in the British Isles
9. Late Devensian and Holocene shorelines of the British Isles and North Sea models of glacio-hydro-isostatic rebound
10. The parallel roads of Glen Roy and adjacent glens, Scotland
11. Catastrophic lake drainage in Glen Spean and the Great Glen, Scotland
12. Differential glacio-isostatic uplift of coastal blocks at Glen Roy, Scotland
13. Patterns of isostatic land uplift during the Eolocene: Evidence from mainland Scotland