Loch Lomond Stadial and Flandrian shorelines in the inner Moray Firth area, Scotland
- 1 January 1989
- journal article
- Published by Wiley in Journal of Quaternary Science
- Vol. 4 (1) , 37-50
- https://doi.org/10.1002/jqs.3390040105
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- The Quaternary deposits and landforms of Scotland and the neighbouring shelves: A reviewPublished by Elsevier ,2003
- Variations in the pattern and rate of isostatic uplift indicated by a comparison of Holocene sea‐level curves from ScotlandJournal of Quaternary Science, 1989
- Flandrian sea‐level changes in the Fenland. II: Tendencies of sea‐level movement, altitudinal changes, and local and regional factorsJournal of Quaternary Science, 1986
- Flandrian relative sea level changes in the Ythan Valley, Northeast ScotlandEarth Surface Processes and Landforms, 1983
- Analysis and interpretation of Holocene sea-level dataNature, 1983
- Late Devensian raised shorelines in Angus and Kincardineshire, ScotlandBoreas, 1980
- Drift Stratigraphy and Buried Morphological Features in the Grangemouth-Falkirk-Airth Area, Central ScotlandTransactions of the Institute of British Geographers, 1969
- Relative Sea-Level Changes between 10,300 and 8,300 B. P. in Part of the Carse of StirlingTransactions of the Institute of British Geographers, 1966
- VIII.—Raised Shorelines Associated with the Perth Readvance in the Forth Valley and their Relation to Glacial IsostasyTransactions of the Royal Society of Edinburgh, 1965
- XIX.—The Physiography of the Moray Firth CoastTransactions of the Royal Society of Edinburgh, 1924