Sea level change is something that probably everyone who does their best to keep up to date about climate change, thinks they know about and on which they will have an opinion. However, this guide clearly shows that there are important misconceptions about the topic, and recent newspaper articles, TV and radio presentations unfortunately tend to bear little relation to reality.
By David N Thomas and David G Bowers The extent to which our planet is covered by oceans and seas (about 70%), and the increasing concern that right-minded people have about climate change, means that there is a both a desire and an urgent need…
I like fossils, but it is always nice to have a brief but informative guide to the actual science behind one’s finds. And this Dunedin guide certainly fits the bill for amateurs and undergraduates alike.
In recent years, Graham Park has been prolific in his writing for Dunedin Academic Press. In this new tome, he has produced what I suspect is a really great introduction to a range of key concepts and geological processes for both undergraduates and the interested, moderately well-informed amateur.
This is a new guide in Dunedin’s ‘Introducing …’ range of books, covering the branch of geology that studies rock layers (strata) and layering (stratification), primarily in sedimentary rocks, but also layered igneous rocks. In this way, it is intended for students and amateur geologist, rather than the academic earth scientist.
I really like the ‘Introducing ….’ series publish by Dunedin Academic Press, as you will have ascertained, if you have read the many reviews I have included in this magazine. This second edition of Introducing Sedimentology by Stuart Jones updates the version I reviewed a while ago (see Book review: Introducing Sedimentology, by Stuart Jones), and I found it equally enjoyable.
I have to admit that I hadn’t heard of ‘hydrogeology’ before, but I should have. Hydrogeology is an important and vibrant sub-set of geological science, dealing with the distribution and movement of water –groundwater – in the Earth’s soil and rocks. Groundwater transport is one part of the overall hydrological cycle in which water is transferred by evaporation from the oceans and seas into the atmosphere.
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!
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.
In these times, when the classic discipline of palaeontology is diminishing, there is a demanding need to inspire the next generation of palaeontologists – and perhaps also to make this field of scientific research more approachable. Otherwise, we are in the risk of losing generations of knowhow and a great tradition of studying time, through the evolution of life.
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.
Recently, I have finished the Great Silurian Controversy, a magnificent book about the nineteenth century arguments over the age of the lower Palaeozoic greywackes/sediments of Devon, and the creation of the concept of the Devonian. And reading The Lewisian: Britain’s oldest rocks by Graham Park, it occurs to me that this should perhaps be called, The Great Lewisian Controversy. It shares the same historical and scientific intentions, and the same grand sweep of scientific history, this time from the early twentieth century – namely, the exploration over decades of the geology of the Lewisian of northwest Scotland.
This is an interesting little booklet and very much a new departure for the Palaeontological Association. Rather than covering specific fossils, it contains colourful, detailed, artistic illustrations, accompanied by concise explanatory text by palaeoartist, James McKay.
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.
If you can see past the somewhat robust title (a reference to James Hutton’s discomfort riding around Scotland on horseback during his geological investigations), this is an interesting read, combining both geological science and humour in just about the right measures.
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.
I remember reading and enjoying this book when the first edition came out many years ago. I am also a keen hillwalker and have stood on top of many of the Scottish mountains referred to in the text. In fact, I particularly enjoyed climbing Ben More on the island of Mull, which I remember reading was the last volcano in northwest Europe.
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.
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.
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.
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.
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.
