ebook img

Glacial geology : ice sheets and landforms PDF

402 Pages·2009·15.431 MB·English
Save to my drive
Quick download
Download
Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.

Preview Glacial geology : ice sheets and landforms

Glacial Geology Ice Sheets and Landforms Second Edition MATTHEW R. BENNETT School of Conservation Sciences, Bournemouth University, UK NEIL F. GLASSER Institute of Geography and Earth Sciences Aberystwyth University, UK AJohn Wiley & Sons, Ltd., Publication Glacial Geology Glacial Geology Ice Sheets and Landforms Second Edition MATTHEW R. BENNETT School of Conservation Sciences, Bournemouth University, UK NEIL F. GLASSER Institute of Geography and Earth Sciences Aberystwyth University, UK AJohn Wiley & Sons, Ltd., Publication Thiseditionfirstpublished2009 (cid:2)2009byJohnWiley&SonsLtd. Wiley-BlackwellisanimprintofJohnWiley&Sons,formedbythemergerofWiley’sglobalScientific, TechnicalandMedicalbusinesswithBlackwellPublishing. Registeredoffice JohnWiley&SonsLtd,TheAtrium,SouthernGate,Chichester,WestSussex, PO198SQ,UK OtherEditorialOffices 9600GarsingtonRoad,Oxford,OX42DQ,UK 111RiverStreet,Hoboken,NJ07030-5774,USA Fordetailsofourglobaleditorialoffices,forcustomerservicesandforinformationabouthow toapplyforpermissiontoreusethecopyrightmaterialinthisbookpleaseseeourwebsiteat www.wiley.com/wiley-blackwell Therightoftheauthortobeidentifiedastheauthorofthisworkhasbeenassertedinaccordancewiththe Copyright,DesignsandPatentsAct1988. Allrightsreserved.Nopartofthispublicationmaybereproduced,storedinaretrievalsystem,or transmitted,inanyformorbyanymeans,electronic,mechanical,photocopying,recordingorotherwise, exceptaspermittedbytheUKCopyright,DesignsandPatentsAct1988,withoutthepriorpermissionof thepublisher. Wileyalsopublishesitsbooksinavarietyofelectronicformats.Somecontentthatappearsinprintmay notbeavailableinelectronicbooks. Designationsusedbycompaniestodistinguishtheirproductsareoftenclaimedastrademarks.Allbrand namesandproductnamesusedinthisbookaretradenames,servicemarks,trademarksorregistered trademarksoftheirrespectiveowners.Thepublisherisnotassociatedwithanyproductorvendor mentionedinthisbook.Thispublicationisdesignedtoprovideaccurateandauthoritativeinformationin regardtothesubjectmattercovered.Itissoldontheunderstandingthatthepublisherisnotengagedin renderingprofessionalservices.Ifprofessionaladviceorotherexpertassistanceisrequired,theservices ofacompetentprofessionalshouldbesought. LibraryofCongressCataloging-in-PublicationData Bennett,Matthew(MatthewR.) Glacialgeology:icesheetsandlandforms/MatthewR.Bennett, NeilF.Glasser.—2nded. p. cm. Includesindex. ISBN978-0-470-51690-4—ISBN978-0-470-51691-1 1. Glaciallandforms. 2. Glaciers. I. Glasser,NeilF. II. Title. GB581.B452009 551.31—dc22 2008052800 ISBN:978-0-470-51690-4(HB) 978-0-470-51691-1(PB) AcataloguerecordforthisbookisavailablefromtheBritishLibrary. Setin10/12PalatinobyIntegraSoftwareServicesPvt.Ltd,PondicherryIndia PrintedinSingaporebyFabulousPrintersPteLtd. FirstImpression 2009 Contents Preface ix Acknowledgements xi Illustrations xiii Chapter1: Introduction 1 1.1 WhatisGlacialGeologyandWhyisitImportant? 1 1.2 TheAimandStructureofthisBook 6 Chapter2: GlaciationsAroundTheGlobe 7 2.1 TheAntarcticIceSheet 7 2.2 GreenlandintheGreenhouse 15 2.3 SouthernHemisphereTemperateGlaciers:Patagonia andNewZealand 17 2.4 NorthernHemisphereTemperateGlaciers:Alaska andIceland 21 2.5 High-AltitudeGlaciers:TheHimalaya 22 2.6 TropicalGlaciers:TheCordilleraBlanca,Peru 26 2.7 ArcticPolythermalGlaciers 29 2.8 Summary 33 SuggestedReading 33 Chapter3: MassBalanceandtheMechanismsofIceFlow 41 3.1 AnnualMassBalance 41 3.2 TheMassBalanceGradient:TheGlacialDrivingMechanism 44 3.3 MechanismsofIceFlow 47 3.4 ThePrinciplesofBasalThermalRegime 55 3.5 PatternsandRatesofIceFlow 63 3.6 GlacierResponsetoClimateChange 69 3.7 Summary 76 SuggestedReading 76 Chapter4: GlacierHydrology 81 4.1 GlacierHydrology 81 4.2 SourcesofGlacialMeltwater 82 4.3 StorageofWaterinGlaciers 83 4.4 MethodsofStudyingGlacierHydrology 84 4.5 GlacierHydrologicalSystems 86 4.6 SubglacialWaterPressure 90 vi Contents 4.7 DischargeFluctuations 97 4.8 GlacialMeltwaterErosion 102 4.9 Summary 104 SuggestedReading 104 Chapter5: TheProcessesofGlacialErosion 109 5.1 GlacialAbrasion 109 5.2 GlacialQuarrying 117 5.3 EstimatingRatesofGlacialErosion 125 5.4 PatternsofGlacialErosion 128 5.5 Summary 131 SuggestedReading 131 Chapter6: LandformsofGlacialErosion 135 6.1 MicroscaleFeaturesofGlacialErosion 135 6.2 MesoscaleFeaturesofGlacialErosion 147 6.3 MacroscaleFeaturesofGlacialErosion 157 6.4 LandscapesofGlacialErosion 174 6.5 Summary 179 SuggestedReading 179 Chapter7: GlacialDebrisEntrainmentandTransport 185 7.1 High-LevelDebrisTransport 185 7.2 DebrisEntrainment 190 7.3 Low-LevelDebrisTransport 193 7.4 DebrisTransferBetweenLowandHighLevels 197 7.5 DebrisTransfer 198 7.6 Summary 202 SuggestedReading 203 Chapter8: GlacialSedimentationonLand 207 8.1 DirectGlacialSedimentation 207 8.2 FluvialSedimentation 235 8.3 Summary 243 SuggestedReading 244 Chapter9: LandformsofGlacialDepositiononLand 247 9.1 Ice-MarginalMoraines 247 9.2 SubglacialLandformsFormedbyIceorSediment Flow 268 9.3 GlaciofluvialIce-MarginalLandforms 289 9.4 GlaciofluvialSubglacialLandforms 296 9.5 Summary 299 SuggestedReading 299 Chapter10: GlacialSedimentationinWater 305 10.1 SedimentationinLacustrineEnvironments 305 10.2 SedimentationinMarineEnvironments 315 10.3 DistinguishingGlaciolacustrineandGlaciomarine DiamictsfromGlacialTills 324 Contents vii 10.4 Summary 325 SuggestedReading 325 Chapter11: LandformsofGlacialDepositioninWater 329 11.1 GlaciolacustrineLandforms 330 11.2 GlaciomarineLandforms 336 11.3 Summary 343 SuggestedReading 343 Chapter12: Palaeoglaciology 347 12.1 TheMethodsUsedinPalaeoglaciology 347 12.2 TheKeyLandformsUsedinPalaeoglaciology 353 12.3 FormerSubglacialThermalRegimes 358 12.4 PalaeoglaciologicalReconstructions 367 12.5 Summary 370 SuggestedReading 372 Index 377

See more

The list of books you might like

Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.