Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-17T14:36:27.452Z Has data issue: false hasContentIssue false

A Seismic Refraction Section of the Preglacial Teifi Valley near Cenarth

Published online by Cambridge University Press:  01 May 2009

T. J. G. Francis
Affiliation:
Dept. of Geodesy and Geophysics, Cambridge.

Abstract

A short seismic refraction line has been shot just north of Cenarth in Cardiganshire across the preglacial valley of the River Teifi. The deepest point on the Ordovician basement has been found to be 30 feet below O.D.

Type
Articles
Copyright
Copyright © Cambridge University Press 1964

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

Allen, A., 1960. Seismic Refraction Investigations of the Preglacial Valley of the River Teifi near Cardigan. Geol. Mag., 97, 276282.CrossRefGoogle Scholar
Coster, H. P., and Gerrard, J. A. F., 1947. A Seismic Investigation of the History of the River Rheidol in Cardiganshire. Geol. Mag., 84, 360–8.CrossRefGoogle Scholar
Hagedoorn, J. G., 1959. The Plus-Minus Method of Interpreting Seismic Refraction Sections. Geophysical Prospecting, 7, 158183.CrossRefGoogle Scholar