Hostname: page-component-5c6d5d7d68-qks25 Total loading time: 0 Render date: 2024-08-15T12:59:17.791Z Has data issue: false hasContentIssue false
  • English
  • Français

On the Formation of certain Lakes in the Highlands

Published online by Cambridge University Press:  15 September 2014

Léon W. Collet ,
John Murray  and
T. N. Johnston
Get access

Extract

Loch Muick (see fig. 1) lies at the head of Glen Muick, at a height of 1310 feet, on the property of His Majesty the King. On both sides of the loch the mountain slopes rise precipitously from the water's edge, and reach a height of 2400 feet on the south-east and from 2326 to 3352 feet on the north-west. The rocks surrounding the lake are granite.

The loch trends in a N.E. and S.W. direction, and is miles in length, the maximum breadth being ½ mile at the north-eastern end. The maximum depth recorded is 256 feet, and the mean depth calculated from the volume of water is 111·69 feet, approaching the half of the extreme depth. The ratio of maximum depth to the length is 46.

Type
Proceedings
Information
Proceedings of the Royal Society of Edinburgh , Volume 26 , Issue 1 , 1906 , pp. 107 - 112
Copyright
Copyright © Royal Society of Edinburgh 1906

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 108 note * DrPenck, A., “Glacial Features on the Surface of the Alps,” Geogr. Teacher, vol. iii., p. 49, 1905.Google Scholar