Hostname: page-component-78c5997874-4rdpn Total loading time: 0 Render date: 2024-11-14T22:15:16.439Z Has data issue: false hasContentIssue false

The Glacial and Recent Drainage of the Lintrathen Area

Published online by Cambridge University Press:  01 May 2009

Extract

Our knowledge of the geology of the district fringing the Grampians in Perthshire and Angus has been limited in the main to the published 1 inch maps of H.M. Geological Survey of Scotland (Sheets 48 and 56 in particular). A few papers in the Quarterly Journal of the Geological Society about the middle of the last century deal with certain exposures of special interest. The writer of the present contribution has conducted recently a detailed investigation of the area between Dunkeld and Fern, and an account of the solid geology has been published. The glacial geology presents no less interesting material or problems and, while the major portion of the results is being held over until further field-work is undertaken, one aspect, and over a limited area, will be considered here.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1929

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 27 note 1 Trans. Roy. Soc. Edin., vol. lvi, 1928, p. 57.Google Scholar

page 32 note 1 Geikie, A., The Scenery of Scotland, 3rd edition, 1901, p. 186.Google Scholar Mackinder, H. J., Britain and the British Seas, 1902, p. 127.Google Scholar Macnair, P., The geology and Scenery of the Grampians, 1908, vol. i, p. 61; vol. ii, pp. 159–62.Google Scholar Scott, A, “Dry Channels in Glen Lednock,” Trans. Geol. Soc. Glasgow, vol. xvi, 1916, p. 61.CrossRefGoogle Scholar

page 33 note 1 Following upon the cloudburst of 9th May, 1913, the Inzion Burn was unable to cope with the swollen waters of the Quharity, which discharged down the Carity causing serious flooding. There is a local legend that the mill-owners on the Carity used to bribe someone at Newton to divert periodically for their benefit the waters of the Quharity by means of a small drain.

page 38 note 1 Thomson Memorial Lectures delivered at Aberdeen in 1926 (unpublished).

page 38 note 2 Glacial Erosion in the Scottish Highlands,” Scot. Geographical Mag., vol. xxiv, 1908. p. 586.Google Scholar

page 38 note 3 Further Problems in the Glacial Geology of North-eastern Scotland,” Trans. Geol. Soc. Edin., vol. xii, 1928, p. 147.Google Scholar

page 39 note 1 Loc. cit. supra, 3rd edition, 1901, pp. 379, 396, etc.Google Scholar