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An informative guide to the geology of the Stoke – On – Trent Area, published by the Geologists Association. Includes small diagrams and maps.
Out of stock
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An informative guide to the geology of the Stoke – On – Trent Area, published by the Geologists Association. Includes small diagrams and maps.
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The Chalk of Sussex and Kent (1997)
A comprehensive series of 8 inland and coastal itineraries extending from Lewes and the Newhaven-Brighton area , via Beachy Head, Folkestone and The White Cliffs of Dover, to Thanet illustrating the variable lithology and stratigraphy of England’s best-known and world-famous flint-bearing fossiliferous rock type. Examine the evidence for structural controls on chalk deposition, rhythmic sedimentation and transgressive and regressive events in this well-illustrated guide in which safety factors are fully considered.’
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During the last 16 million years (up to recent times) igneous rocks with a variety of compositions have been extruded and then moved E or W of the rift valley which marks the central line of the Mid-Atlantic Ridge The ice sheets and their associated glaciers formed by the accumulation of snow over hundreds of years, occupy 11% of Iceland. The pressure on water trapped in geothermally heated cavities close to the land surface is occasionally relieved generating Geysers. The itineraries in the Guide provide a representative selection of sites of the above.
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Anglesey contains a fascinating variety of rock types and geological structures, best exposed in a magnificent coastline ‘Hard rock’ and structural geology interests are catered for in Precambrian and Ordovician areas, palaeontology in the Ordovician and Carboniferous and sedimentology in all the systems. The ten itineraries are roughly in stratigraphical order but each itinerary covers a particular area. An indication of the approximate length of each itinerary and their dependence on tides.
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The geology of Hadrian’s Wall falls naturally into three sectors: in the East the wall is over Upper Carboniferous Coal Measures and Millstone Grit; the Central Section is underlain by Lower Carboniferous intruded by the Great Whin Sill and in the Western sector the Wall crosses the New Red Sandstone. Glacial drift is widespread. All three sectors are described with specific sites in detail.
Out of stock
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Out of stock
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2 in stock
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Out of stock
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Out of stock
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The purpose of this field guide is twofold: to provide a general introduction to the island’s geology and secondly to provide descriptive accounts of locations which can be visited to see this geology. The island is an importance source of fossils and has some of the richest collecting locations in Britain. It is commonly known as the ‘Dinosaur Island’.
1 in stock
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