Titlebook: Quaternary of Scotland; J. E. Gordon,D. G. Sutherland Book 1993 Springer Science+Business Media Dordrecht 1993 Coast.Moor.environment.quat

Vital-Signs

疼死我了

LAST

Detoxification

North-west Highlands, watershed breaching and corrie formation in a landscape that already had considerable pre-glacial relief. There is relatively little known about pre-Late Devensian events in this region. The cave systems of Sutherland have recently been found to contain fossil material and other sediments that pred

遺傳學(xué)

Inverness area,the glaciated valleys extending to the west and south-west, including the Great Glen (Figure 7.1). The principal focus of research on this area has centred on the evidence for the last ice-sheet, the pattern of deglaciation and the changes in relative sea level that both accompanied and followed the

陶器

breadth

Eastern Grampian Mountains,ley separates the western mountain areas, characterized by intense glacial erosion, and the eastern mountain plateau country, where glacial erosion has produced only specific features superimposed on an easily recognizable pre-existing landscape. There are three principal mountain groups in this are

釘牢

Chronic

theta-waves

Outer Hebrides,on the maritime fringe of the country makes them of particular interest for investigation of past vegetation patterns and of palaeoclimate in general. However, despite an initial period of interest in the Quaternary history of the islands during the last century it has only been within the last fift