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TEACHING EARTH SCIENCES ● Volume 30 ● Number 1, 2005<br />
Reviews<br />
Classic Landforms of the Coast of the East Riding of Yorkshire<br />
Ada W. Pringle. Classic Landform Guides. Published by the Geographical <strong>Association</strong> in conjunction with the<br />
British Geomorphological Research Group, 2003. (Series editors: Christopher Green, Michael Naish and Sally Naish).<br />
£9.99 (sale price August 2004 £5.99). 64pp. ISBN 1-84377-071-7.<br />
This attractively produced booklet is one<br />
of a series on classic landforms in the<br />
British landscape, the aim of which is to<br />
provide concise, informative guides to<br />
parts of the country that are frequently<br />
visited by students and the general populace.<br />
Previously published titles include<br />
the Brecon Beacons, the Lake District,<br />
Morecambe Bay and Skye. All of the authors<br />
involved in their production have extensive<br />
knowledge of the areas concerned.<br />
The informative text of this guide is<br />
accompanied by several tables, 13 photographs<br />
of coastal scenery and 16 figures<br />
that consist of maps, stratigraphic<br />
sections and interpretative diagrams, all<br />
of which are in colour. Some of the<br />
maps have been specially drafted for the<br />
guide; others are extracts from Ordnance<br />
Survey maps.<br />
For those who worry about rising sea<br />
levels and the erosion of our coasts, the<br />
contents of this guide will not do anything<br />
to allay fears that large parts of lowland<br />
Britain may eventually be drowned<br />
beneath the waves, as has happened on<br />
many occasions in the geological past.<br />
Erosion of the Holderness cliffs to the<br />
south of prominent Flamborough Head is<br />
particularly rapid, with numerous<br />
settlements along the coast having been<br />
lost since Roman times.<br />
The guide begins logically with a<br />
chapter on the sedimentary and structural<br />
geology of Flamborough Head. The<br />
recently revised stratigraphy of the<br />
succession (formation and member<br />
subdivisions) is used, and compared on a<br />
figure with the former breakdown of<br />
Lower, Middle and Upper Chalk. It<br />
closes with a paragraph on the glacial<br />
deposits that serves as a lead into the next<br />
chapter, which considers the glaciation of<br />
Holderness and the various deposits of<br />
till, sand, silt, silty clay and chalky gravel<br />
that form the undulating topography of<br />
the region. An interesting chapter follows<br />
on the wave, tidal and storm-surge<br />
influences on the coast. The remaining<br />
seven chapters deal with sections of the<br />
coast in more detail, beginning with the<br />
vertical Bempton Cliffs of Flamborough<br />
Head and followed by the Flamborough<br />
Lighthouse area, Selwicks Bay and High<br />
Stacks, the buried cliff at Sewerby, the<br />
Barmston, Mappleton and Withernsea<br />
stretches of coast in North, Central and<br />
South Holderness respectively, and the<br />
sand and shingle spit of Spurn Head.<br />
Each considers the local geology and its<br />
considerable influence on topography and<br />
coastal configuration, and discusses the<br />
present-day processes that are causing the<br />
coastline to retreat. The problems<br />
associated with the erosion and attempts<br />
at reducing it dominate the chapters on<br />
Central and South Holderness.<br />
The shifting position of Spurn Head<br />
from 1066 onwards has been determined<br />
from old maps, charts and other<br />
historical documents, and more recently<br />
(from 1851 onwards) via Ordnance<br />
Survey mapping. Discussion of this and<br />
the various works that have been carried<br />
out when necessary to protect the spit,<br />
close breaches, and repair and replace the<br />
road along its length (originally<br />
constructed during the Second World<br />
War), make for interesting reading.<br />
The chapter on Spurn Head closes<br />
with a section on the beaches on the<br />
North Sea side of the spit, around the<br />
point, and in the Humber Estuary<br />
where, in the quieter conditions that<br />
prevail, the sandy strand is much<br />
narrower and mudflats dominate the<br />
scene. Further up the estuary, former<br />
upper beach and adjacent mudflats are<br />
covered with saltmarsh. The booklet is<br />
rounded of with a glossary and a list of<br />
references, its goals achieved.<br />
David J. Batten<br />
Institute of Geography and <strong>Earth</strong> <strong>Science</strong>s<br />
University of Wales, Aberystwyth,<br />
and Department of <strong>Earth</strong> <strong>Science</strong>s<br />
Manchester University<br />
Geological Map of Land and Sea Areas of Northern Europe.<br />
Norges Geologiske Undersokelse (NGU). N-7491 Trondheim, Norway. distribusjon@ngu.no www.ngu.no Printed map $32; digital version $125.<br />
This new geological map of northern<br />
Europe, on a scale of 1:4 million, is<br />
published under the aegis of the<br />
Commission for the Geological Map of<br />
the World. For the first time, it displays<br />
the geology of both land and sea areas of<br />
this large region, from Greenland and<br />
Svalbard in the north, to the northern<br />
coast of France and parts of Russia. The<br />
geology shown excludes Quaternary<br />
sediments, though it includes recent<br />
basalts, i.e. it is the bedrock geology<br />
which is featured. The map also shows<br />
fault zones, escarpments, spreading axes,<br />
magnetic reversals, and the boundary<br />
between continental and oceanic crust.<br />
Cross-sections are included, with special<br />
sections through all the deep-sea drilling<br />
sites in the oceanic areas. It is hoped that<br />
the map will be useful for all geologists,<br />
whatever their speciality, and should also<br />
prove instructive for students getting to<br />
grips with the geology of Europe and the<br />
North Atlantic. It is printed in both a<br />
Norwegian and English version.<br />
29 www.esta-uk.org