Tenerife Canary Islands (2003) GA Guide

Geology of the Manchester Area (1991)
by R.M.C.Eagar & F.M.Broadhurst

The rocks exposed in the Manchester area range in age from Dinantian (Lower Carboniferous) to Triassic and superficial coverings of Pleistocene and Recent sediments. Of the sixteen itineraries described, two are devoted to Dinantian, five to the Silurian, four to the Triassic and three to the Pleistocene and Recent. The last two intineraries are concerned with mineralisation and mining and with the building stones of Manchester

Early Cretaceous Environments of the Weald (1996)
by Alastair Ruffell, Andrew Ross & Kevin Taylor

In order for the Guide not to become out-of-date it concentrates on exposures that are likely to remain in their present state for some time, thus some abandoned sites are omitted. The interested geologist will find the locations easily, observe the main features with no trouble, and be able to do this for some years to come.

Geology of the Dorset Coast (1993)
by Michael House

The guide aims to provide a general introduction to what may be seen and where in this coast of unsurpassed geological interest. Most emphasis is on the Jurassic rocks, rather less on Cretaceous and Tertiary which are seen as well or better elsewhere. An introductory section on Sedimentology and Palaeontology has been added by request to introduce terms to the general reader.

North Coast of Cornwall (1970)
The North Coast of Cornwall from Bude to Tintagel (1970)
by W.R.Dearman, E.C.Freshney, A.F.King, M.Williams and M.C.McKeown

The itineraries described in this guide have been designed to illustrate the stratigraphy and structure of a long coastal tract of Devonian and Carboniferous rocks. As some aspects of the coastal structures are to be related to granite intrusion, one itinerary deals with the northern part of the Bodmin Moor granite and its envelope.

The Coastal Landforms of West Dorset (1992)

A series of itineraries illustrating the geology and denudational history along the coastline of West Dorset. This most beautiful coast is world famous for its spectacular recurrent landslides and the causes of these are fully explored together with their effects on shingle movement at beach level, the latter and best known being Chesil Beach.