Reconstructing late holocene sea-level changes in the Forth Valley, Scotland (UK)*

The research contributes to the understanding of late Holocene environmental changes in the Forth Valley.Scotland has been greatly affected by differential glacio-isostatic uplift after the demise of the late British-Irish ice sheet. This has been one of the main causes for fluctuations in sea-level...

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Bibliographic Details
Main Author: McLaughlin, A-M.
Format: Other/Unknown Material
Language:English
Published: Coventry University 2014
Subjects:
Online Access:http://curve.coventry.ac.uk/open/items/63eb1b7f-996b-411e-add5-3c7e45adb358/1
Description
Summary:The research contributes to the understanding of late Holocene environmental changes in the Forth Valley.Scotland has been greatly affected by differential glacio-isostatic uplift after the demise of the late British-Irish ice sheet. This has been one of the main causes for fluctuations in sea-levels during the Holocene as recorded previously from the Forth lowland. Previous studies have attempted to determine late Holocene sea-level changes in the Forth lowland on the basis of archaeological evidence (e.g. Smith et al 2010). However, little is known about these changes in the Forth Valley.