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{{AberfoyleSD}}
The Quaternary deposits and landforms of the western Forth and upper Clyde areas, straddled by Sheet 38E, are some of the finest in Scotland and are of international importance. They provide a detailed record of glacial and postglacial environmental change, including sea level rise and fall due to eustatic and isostatic processes, from the Late Pleistocene through to the Holocene (Smith 1993<ref name="Smith 1993">Smith, D E. 1993. Western Forth Valley. 456–463 in Quaternary of Scotland. Gordon, J E, and Sutherland, D G, (editors). ''Geological Conservation Review Series'', No. 6. (London: Chapman & Hall.)</ref>; Sutherland 1993<ref name="Sutherland 1993">Sutherland, D G. 1993. Western Highland Boundary. 435–474 in Quaternary of Scotland. Gordon, J E, and Sutherland, D G, (editors). ''Geological Conservation Review Series'', No. 6. (London: Chapman & Hall.)</ref>).

==References==
<References/>

== Geology of the Aberfoyle district - contents ==
{{Aberfoylepages}}

[[category:Aberfoyle - the geology of the district| 15]]

Geology of the Aberfoyle district: Quaternary - Revision history

Dbk: 1 revision imported

Geosource>Ajhil at 07:34, 19 August 2016