Hostname: page-component-78c5997874-8bhkd Total loading time: 0 Render date: 2024-11-08T06:31:34.577Z Has data issue: false hasContentIssue false

The Geology of the Fintry, Gargunnock, and Touch Hills

Published online by Cambridge University Press:  01 May 2009

Extract

The area included in this survey comprises that part of the Clyde Plateau Lavas and associated sediments which lie within the Geological Survey 1 in. Sheet, number 39. This northern portion of the Campsie Fells was previously mapped for the Geological Survey by Peach and Jack, but the lavas were not separated into their petrographic types. It is this latter task that constitutes the main part of the work of this paper.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1938

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

REFERENCES

(1)Geology of the Glasgow District,” p. 166, Mem. Geol. Surv.Google Scholar
(2)Geology of the Stirling and Clackmannan Coalfield,” Mem. Geol. Surv.Google Scholar
(3)Mem. Geol. Surv., p. 8.Google Scholar
(4)Geology of the N. Ayrshire Coalfield,” p. 65, Mem. Geol. Surv.Google Scholar
(5)Geology of the Ayrshire Coalfield, Area IV,” p. 21, Mem. Geol. Surv.Google Scholar
(6)Geology of the Ayrshire Coalfield, Area II,” p. 9, Mem. Geol. Surv.Google Scholar
(7)Geikie, , Ancient Volcanoes, i, 361.Google Scholar
(8)Trans. Glasgow Geol. Society, xiii, 240. Martin and Tyrrell on a puddle trench section at North Third.Google Scholar