logo
Normal view MARC view ISBD view

The lower new red sandstone of the crediton valley

By: Hutchins, P. F.
Material type: ArticleArticleDescription: 107-128pp.Subject(s): New red sandstone - Great Britain | Paleogeography | Sedimentary rock - Crediton valley - Great Britain In: Geological magazine : Vol. 100 Iss. 1-6 Year. 1963Summary: Extract The Lower New Red Sandstone of Devon outcrops in a north-south band near Torquay to Exmoor. It rests unconformably on the Devonian and Culm. Westwards of Tiverton and again west of Exeter the outcrop extends into the Culm synclinorium. The Lower New Red sediments in the second and longer of these narrow tongues, together with the associated Hatherleigh, Highhampton and Essworthy outliers, form the subject of this paper.
Tags from this library: No tags from this library for this title. Log in to add tags.
    Average rating: 0.0 (0 votes)
Item type Current location Collection Call number Status Date due Barcode
Article Article Library and Information Centre
Periodical Section
Bound Journal Collection Not for loan 002548_17
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002548

Extract
The Lower New Red Sandstone of Devon outcrops in a north-south band near Torquay to Exmoor. It rests unconformably on the Devonian and Culm. Westwards of Tiverton and again west of Exeter the outcrop extends into the Culm synclinorium. The Lower New Red sediments in the second and longer of these narrow tongues, together with the associated Hatherleigh, Highhampton and Essworthy outliers, form the subject of this paper.

There are no comments for this item.

Log in to your account to post a comment.

Copyright © 2019 Geological Survey & Mines Bureau. All Rights Reserved.

Developed in Association with Finco Technologies (Pvt) Ltd

Powered by Koha