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.

Howgill Fells

This little guide contains excursion guides explaining and exploring the relationship in the UK between hillslope gully erosion and the response by stream and valley systems within the Howgill Fells of Cumbria. The author’s choice of this area rests on the fact that it is one of the most active landscapes in Britain from the point of view of erosion, with the steep slopes of the headwater valleys, which are riddled by networks of erosional gullies that have been active in the relatively recent past.

Normally, I wouldn’t be interested in semi-precious stones and other pretty things. Personally, I prefer grubbing around in the dirt, perhaps for those far more beautiful, elusive and perfectly formed Cretaceous terebratulids or Silurian trilobites. However, some semi-precious stones have the advantage of also providing a tangible link to the ancient history of life that is so fascinating.

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.

Almeria is a province in southeast Spain, situated in the furthest southeast part of the Iberian Peninsula. And it is a classic area for southern European and Mediterranean Neogene and Quaternary geology. In fact, it is not far north of the southern boundary of the European tectonic plate and, as a result, has been profoundly affected by the interaction of this and the African plate.

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.

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.

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.

There are only a few good books on the London Clay and its fossils, but this little guide from the Geologists’ Association is a good start for beginners, children and teenagers. Rockwatch, which published this guide, is the national geology club for young people, the junior club of the GA. Having said that, this guide does not dumb down the information it contains.

This is certainly a somewhat different sort of book from those I usually review. As it makes clear, women have always played key roles in the field of vertebrate palaeontology, going back centuries. However, other than perhaps the most best known historical female vertebrate palaeontologists, comparatively little is known about these women scientists. As a result, their true contributions have probably been obscured. In this context, the book aims to reveal this hidden history, thereby celebrating the diversity and importance of women VPs.

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.

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”.

Graptolites lived in the earth’s oceans from 540 million years ago to 320 million years ago, when they became extinct. The book provides a summary of the state of knowledge relating to graptolites, and the specialists, who contribute to the book, also address the biological questions raised by these fossils, and provide pointers for further research.

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.

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.

I have known Neale Monks for many years. He knows his stuff and some of that stuff is ammonites. Their beautiful spiral shells make them among the most sought after. However, until this book was published in 2002, little had been published about ammonites other than in geological journals.

The very small number of books published by the Medway Fossil and Mineral Society are without exception, wonderful and this is probably the best. And, there are very few guides on the London Clay. Therefore, this guide is invaluable and more than welcome.

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.