The is a second edition of Prof John Cope’s excellent geological guide to the Dorset coast for the Geologists’ Association. It is slightly shorter than the first edition, with some minor corrections and some of the figures revised, together with new photographs. It also now includes the huge quantity of data amassed over last few decades during the hydrocarbon exploration work in the county.

This 4th edition is the first edition of this book to be published with full colour illustrations throughout, and is presented as an enhancement and revision to the text to reflect advances in sedimentology since the publication the 3rd edition. Therefore, I suspect that it retains its place as a leading geological text and reference book for professional geologists and students alike.

This is the second Geologists’ Association guide by Professor John Cope. The other is the second edition of his excellent Dorset guide. And, on the grounds that “if it ain’t broken, don’t mend it”, this guide to the south Devon coast follows the highly successful basic plan of that other guide, including the extensive use of colour photos and diagrams.

Dunedin Academic Press has once again added a title to its series of introductions to scientific subjects. This one is a short introduction to an essential subject to any budding geologist (essential, because, as the author points out, 70% of the rocks on the Earth’s service are sedimentary in origin and are of the utmost economic importance to all of us.

I have reviewed some excellent previous guides in this series (Iceland: Classic Geology in Europe 3), but this one is closer to home and covers an area that I have fond memories of from my Munro-bagging days. This is more a companion guide for those walking in the Highlands, especially those on geological field trips.

This is a guide to the collection, preservation and display of fossils from more than 50 locations in the UK. It is unashamedly based on the UK fossils format, but obviously, rather than being an online resource, it is a pocket sized book to be taken and read on site.

Geology of South Wales

I quite like regional guides books, even about areas I haven’t been to and am unlikely to visit. That isn’t the case for South Wales, which is one of my favourite areas in the UK for both scenery and geology. Therefore, this guide is another good addition to my collection and will no doubt accompany me soon on another holiday in the Principality.

Those of you who have read a few of my book reviews will know that I love geo-guides to small geographical areas, rather than just the big geological scientific issues. In fact, there are lots of good UK guides like this one, to areas such as Dorset and Yorkshire, and many areas of Scotland and Wales, for example. And this is another excellent example of that genre.

For anyone like me who finds the immensity of geological time (‘deep time’) both fascinating and fundamentally difficult – both emotionally and intellectually – this is a great book. Paul Lyle has written it for environmentalists and policy makers to help them explain their concerns and decisions more clearly in the context of geological time, but these are not the only people who should read it.

The fossil bearing rocks of the British Isles contain the remains of life from the last 2,900Ma and the UK is seen by many as the cradle of modern geology. With this is mind and using a geological map of Britain, palaeontologist Peter Doyle offers a comprehensive guide to UK fossils.

As a former ‘Munro bagger’ and now keen geologist, this book combines two of my favourite pastimes. While the body is not quite so willing as before, the ability to read about the geology of some of my favourite Scottish walks is an absolute pleasure.

This was the first GA guide I ever bought, and I suspect it is still the best. My copy is more than well-thumbed and water-damaged, through many a happy trip to the south of England to collect, what a friend describes as “white fossils in white rock”.

This is another of GA’s guides, this time to the geology and geomorphology of the popular holiday destination of the Castleton Area in Derbyshire. I love this area and have visited there both for the geology and the beautiful scenery.

The island of Cyprus is a truly classic area of geology in Europe. Perhaps nowhere else on Earth does so small an area provide such an excellent illustration of the dynamics of Earth processes through abundant exposures of spectacular and diverse geology.

As the author says, “The abundance and diversity of Foraminifera … make them uniquely useful in studies of modern marine environments and the ancient rock record”. And this book represents an interesting, enjoyable and informative ‘one-stop-shop’ treatment of precisely that subject.

Red Coast Revealed

The Jurassic Coast Trust has certainly producing some good books. As is well known, in recognition of its wonderful geology, the coast between Orcombe Rocks in southeast Devon and Old Harry Rocks in south Dorset was granted World Heritage status in December 2001. In this respect, these two guides cover the western and the eastern thirds of this remarkable coastline.

The second edition of Microfossils, published in 2005, is still the definitive guide to all the major microfossil groups and the essential reference tool and laboratory guide for undergraduate and graduate students of micropalaeontology.

The graptolites constitute one of the geologically most useful taxonomic groups of fossils for dating rock successions, understanding paleobiogeography and reconstructing plate tectonic configurations in the Lower Palaeozoic.

I always wait expectantly for the publication of a new Palaeontological Association guide to fossils and, when they turn up, I am never disappointed. This is undoubtedly another triumph. This guide attempts to bring the diversity of its flora and fauna together in a single work, for the first time.

South Wales is a great place to do geology, both because of the variety of what can be seen and the general beauty of the area and its surrounds. In fact, the sedimentary rocks here (largely from the Palaeozoic and late Triassic/Lower Jurassic) were deposited in a wide range of environments, for example, deep-sea fans, clastic-carbonate shelf seas, beaches, estuaries and deltas, and rivers and floodplain swamps, to name but a few.