Hostname: page-component-586b7cd67f-dsjbd Total loading time: 0 Render date: 2024-11-23T21:53:16.772Z Has data issue: false hasContentIssue false

XVII.—The Geology of Gigha

Published online by Cambridge University Press:  06 July 2012

W. J. McCallien
Affiliation:
Assistant in Geology, Glasgow University.

Extract

Gigha is a little-visited island off the western coast of Kintyre and between the latter and the island of Islay. It lies about 5¼ miles south-west of West Loch Tarbert, and a little over 1½ miles from the nearest point of Kintyre where the mainland runs out for 1½ miles in the low, sandy, raised beach of Runahaorine (figs. 1 and 10).

The island is 6 miles in length from north-east to south-west, and has a greatest breadth of 2 miles. All round it are innumerable smaller isles, all elongated in the same direction as Gigha. Of these the most important are Cara, 1 mile from north-east to south-west by ½ mile in breadth, and Gigalum, ½ mile by ⅕ mile, and Craro, which is smaller still (figs. 2 and 10). The island forming Ardminish Point, on the eastern coast of Gigha, and Eilean Garbh, at the north-eastern end, will be dealt with here as if they were part of the main island, since at low tide they are connected with it by sandy isthmuses.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1927

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 398 note * Q.J.G.S., lxxviii, pt. 2.

page 406 note * Trans. Geol. Soc. Glasgow, xvii, pt. 3, 19251926, pp. 377394Google Scholar.

page 407 note * Q.J.G.S., lxxviii, pt. 2, 1922, p. 96.

page 407 note † Trans. Geol. Soc. Glasgow, xvii, pt. 2, 19241925, p. 251Google Scholar.