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teaching - Earth Science Teachers' Association

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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

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