Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-06T09:19:30.295Z Has data issue: false hasContentIssue false

Seismic Refraction Investigations of the Preglacial Valley of the River Teifi near Cardigan

Published online by Cambridge University Press:  01 May 2009

Adrian Allen
Affiliation:
Department of Geology, The University, Birmingham.

Abstract

Two short seismic refraction profiles have been shot across the former valley of the River Teifi, above and below Cardigan, with the object of determining the depth to the rock floor. This was found to lie 75 feet below O.D. at Castle Malgwyn, near Llechryd and 107 feet below O.D. at the present estuary. These figures are consistent with the glacial history of the valley indicated by the geological evidence.

Type
Articles
Copyright
Copyright © Cambridge University Press 1960

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

VII. REFERENCE

Hagedoorn, J. G., 1959. The Plus-Minus Method of Interpreting Seismic Refraction Sections. Geophysical Prospecting, vii, No. 2, 158183.Google Scholar