The ‘Bracklesham Beds’ are a series of predominantly soft silty sands and clayey silts laid down in a sub-tropical shallow marine environment around 46Ma. Fossils are readily eroded and can be found loose on the beach along with modern sea shells. The guide has simple maps to direct fossil hunters to the best areas for surface-picking and likely exposures when the beach sand has been removed.
I have to admit, I was beginning to wonder where Prof Rory Mortimore’s update of his excellent Chalk of Sussex and Kent was. And now I know. It wasn’t a second edition he was working on, but this magnificent magnum opus in two volumes covering a vastly greater area than that other guide. And the wait was more than worthwhile. The thoroughness, writing quality, content and publication standards are superb.
This is an interesting guide for someone like me who lives in the Southeast of England. In fact, I have commuted from London to Brighton by train, which took me through a cross-section of the Weald, which is the subject matter of this guide.
This is another of the GA’s short guides, being only 21 pages long and therefore easy to put in a cagoule pocket. Importantly, the five excursions described in the guide are centred on the city of Plymouth. Therefore, the logistics necessary to visit the itineraries should be relatively easy.
Fossil Hunting along the Jurassic Coast is presented by Dr Colin Dawes, a well-known, fossil hunting guide in the world-famous palaeontological site of Lyme Regis.
The Crowood Press are really developing a nice little series of books on the landscape and geology of select regions of the British Isles, and Tony Waltham’s addition to the series about the Peak District is well worth a read. This new one follows the same format as the others – beautiful, full colour photos and diagrams, a fascinating chapter on each of the important geological and geomorphological aspects of the area (including buildings and industry), and an author who knows his stuff and can write it down with an easy and authoritative style.
This GA guide is stated to be a “Geology Teaching Trail”. Well, it may be, but when I ambled along the trail with the guide in my hand, I certainly wasn’t in a teaching situation. Rather, I was out for a nice walk and a guide to explain what I was seeing. And it did just that and the classic Silurian/Ordovician unconformity you can see was just that. Classic!
Shropshire is one of my favourite areas for both geology and fossil collecting. The Silurian of this beautiful area is fascinating and, if you can get permission to get into one of the commercial quarries (and you will need permission), then the results will be remarkable.
West Dorset is rightly famous for its fossils, but few people visit its wonderful, fossiliferous cliffs to look at them as landforms, rather than as an endless source of ammonites and belemnites. This guide does just that and, covers a series of itineraries in the context of landform type.
This GA guide is intended as a major guidebook to the exposures of highly significant Precambrian, Carboniferous and Permo-Triassic sediments, through to Jurassic rocks of the East Midlands. Personally, it is an area I only partly know (I know Edale in the Peak District quite well) and, for that reason, is an interesting set of locations for me.
I approached this book with what turned out to be completely irrelevant preconceptions. I was very wrong. In fact, this is a little geological tour de force describing field locations and, what one reviewer described as “the logic of geology: how vanished land – and seascapes can be conjured back into existence from the raw rock record”.
After having favourably reviewed the first two books in this three part series, I must admit I was very much looking forward to the publication of this last one. And, of course, I wasn’t disappointed. This is the third in a series of guides to safe and responsible fossil collecting along (this time), the East Dorset coast from the Chalk cliffs at Bat’s Head, across what are some of Dorset’s more remote coastal locations, to Hengistbury Head.
This is one of GA’s little guides to a very specific area. This one is West Cornwall, a holiday destination that I recently visited during which I spent some time looking at the geology, along with the gardens and archaeological sites.
This is another lovely guide by the GA to an area that perhaps readers would not associate with good geology. But, of course, that is because of its title, because the areas like Pendle Hill and Derbyshire are wonderful, not just to visit for their geology, but also for their holiday appeal.
The aim of the guide is to help professional and interested amateur geologists to investigate the rocks themselves and to put them in a modern scientific context.
I like local geological guides, which aim to get you out and about, visiting areas you might not have known are worth a daytrip. And this is a good example. I sat down and read it cover to cover, as it is only 90 pages long. And I now really want to visit this bit of Kent coastline. Largely concentrating on the Upper Cretaceous Chalk, this guidebook explains and illustrates what seems to be some marvellous geology that can also be explored during what could be a lovely day out on the beach.
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 is one of the oldest of the GA’s guides and is currently in its third edition (the first having been published in 1957 and the second in 1972). Although there have been changes in classification and so on, the general exposures are largely as good as they used to be – or they were the last time I went!
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.
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.
The 71st GA guide is not really my area (I prefer palaeontology) and it covers quite a specialist subject, but it is definitely interesting. And this is surely the point of GA guides – to cover topics that other publishers might be reluctant to consider.
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.
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.
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 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.
