ORCID

Abstract

The coral-rich limestones of the English Riviera UNESCO Global Geopark were an important component of the original definition of the Devonian System, introduced by Sedgwick and Murchison in 1840. They are, therefore, both a local highlight of the geological succession but have an important position within the history of geology. Formed in the tropical seas of the Middle Devonian, 10°S of the Equator, they also demonstrate the history of Devon in terms of Continental Drift and Plate Tectonics. Caves in these limestones provide an important record of both marine and terrestrial Pleistocene history, including some important hominin remains.

DOI

10.30486/gcr.2021.1907467.1030

Publication Date

2021-06-01

Publication Title

Geoconservation Research

Volume

4

Issue

1

ISSN

2645-4661

Embargo Period

2023-10-14

Organisational Unit

School of Geography, Earth and Environmental Sciences

First Page

170

Last Page

195

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