Southern England

Southern England
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Illustrated with beautifully detailed photographs throughout, New Naturalist Southern England comprehensively explores the formation of these wonderful landscapes that are so universally admired.Most people share an enthusiasm for beautiful and breathtaking scenery, explored variously through the physical challenge of climbing to the top of the tallest mountains or the joy of viewing the work of a painter; but while easy to admire from a distance, such landscapes are usually difficult to explain in words. Harnessing recent developments in computer technology, the latest New Naturalist volume uses the most up-to-date and accurate maps, diagrams and photographs to analyse the diverse landscapes of Southern England.Peter Friend highlights the many famous and much loved natural landscapes of the southern half of England, ranging from the Chalk Downs to the bays of Cornwall, Devon and Dorset, and provides detailed explanations for the wide variety of natural events and processes that have caused such an exciting range of surroundings.Setting apart the topography that has resulted from natural rather than man-made occurrences, Friend focuses on each region individually, from East Anglia to London and the Thames Valley, and explains the history and development of their land structures through detailed descriptions and colourful diagrams.

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Peter Friend. Southern England

Southern England. Peter Friend

Editors

Table of Contents

Editor’s Preface

Picture Credits

Author’s Foreword and Acknowledgements

CHAPTER 1 Looking at Southern England’s Landscapes. FIRST APPROACHES

MAPPING AND ANALYSING SOUTHERN ENGLAND

LANDSCAPE CHANGE

CHAPTER 2 Time, Process Southern England’s Landscapes. BEDROCK AND SURFACE BLANKET

THREE DIFFERENT TIMESCALES

THE BEDROCK TIMESCALE

LANDSCAPE MODIFICATION BY RIVERS

THE ICE AGE TIMESCALE AND LANDSCAPE MODIFICATION

THE LAST 30,000 YEARS TIMESCALE AND RECENT MODIFICATION

SEA-LEVEL CHANGE

DEVELOPMENT BY PEOPLE

CHAPTER 3 Movement of the Earth’s Surface from Within. WIDESPREAD MOVEMENTS OF THE EARTH’S SURFACE

UNDERSTANDING SURFACE MOVEMENTS

Horizontal movements as part of convergence, divergence or lateral transfer

Vertical crustal movements as part of other crustal movements

Vertical changes by erosion or deposition

Vertical crustal movements resulting from loading or unloading

Vertical movements by expansion or contraction

HOW CAN LOCAL SURFACE MOVEMENTS BE DETECTED?

CHAPTER 4 The Southwest Region. GENERAL INTRODUCTION

Bedrock foundations and early history. Sedimentation and surface movement before the mountain building

Crustal convergence that created the mountain belt

Granites and valuable minerals

Younger episodes. Sedimentary markers

Drainage patterns

Ice Age episodes

AREA 1: WEST CORNWALL

Landscape A: Granite areas

Landscape B: The Lizard

Landscape C: Cornish killas

AREA 2: EAST CORNWALL AND SOUTH DEVON

Landscape A: Granite areas

Landscape B: Killas and other Devonian bedrock

Landscape C: The Carboniferous Culm of Devon

Landscape D: New Red Sandstone and younger bedrock

AREA 3: NORTH DEVON AND WEST SOMERSET

Landscape A: Exmoor’s Devonian bedrock

Landscape B: The Culm (Carboniferous) bedrock area

Landscape C: New Red Sandstone and younger bedrock

Landscape D: Lundy Island

CHAPTER 5 The South Coast Region. GENERAL INTRODUCTION

Bedrock movement, uplift and erosion by rivers

Modification under Ice Age conditions

Coastal shape and location

AREA 4: EAST DEVON, SOMERSET AND DORSET

Landscape A: The Brendon and Quantock Hills, Vale of Taunton and East Devon Redlands

Landscape B: The Somerset Levels and Moors and the Mid-Somerset Hills

Landscape C: The Blackdown Hills and Sidmouth to Lyme Bay

Landscape D: The Yeovil Scarplands

Landscape E: Blackmoor Vale and the Vale of Wardour

Landscape F: The Wiltshire and Dorset Downs and Cranborne Chase

Landscape G: The Dorset Heaths

Landscape H: The Weymouth Lowlands and the Isle of Portland

Landscape I: South Purbeck

AREA 5: HAMPSHIRE AND THE ISLE OF WIGHT

Landscape A: The Isle of Purbeck

Landscape B: The Isle of Wight

Landscape C: The Dorset Heaths

Landscape D: The New Forest

Landscape E: The South Hampshire Lowlands and the western South Coast Plain

Landscape F: The southern Salisbury Plain, Hampshire Downs and western South Downs

Landscape G: The western outcrop area of the Wealden Greensand

Review of the landscape history

AREA 6: SUSSEX

Landscape A: The High Weald

Landscape B: The Low Weald

Landscape C: The Wealden Greensand

Landscape D: The South Downs

Landscape E: The South Coastal Plain

Landscape F: The Pevensey Levels

Review of the landscape history

AREA 7: EAST SUSSEX AND SOUTHEAST KENT

Landscape A: The High Weald

Landscape B: The Low Weald

Landscape C: The Wealden Greensand

Landscape D: The North Downs

Landscape E: The Dungeness and Romney Marshes

Review of the landscape history

CHAPTER 6 The Severn Valley Region. GENERAL INTRODUCTION

AREA 8: BRISTOL

Landscape A: The Quantock Hills and Fringes

Landscape B: The Somerset Levels and Moors and the Mid-Somerset Hills

Landscape C: The Mendip Hills

Landscape D: The Bristol and Avon Valleys and Ridges

Landscape E: The Severn Vale

Landscape F: The Cotswolds

AREA 9: THE COTSWOLDS AND THE MIDDLE SEVERN

Landscape A: Carboniferous and earlier bedrock

Landscape B: New Red Sandstone bedrock

Landscape C: Jurassic bedrock

(1) The Rhaetic (labelled R on Figs 151 and 168)

(2) The Marlstone Rock Bed (labelled M on Figs 151 and 168)

(3) The Northampton Sand (labelled N on Figs 151 and 168)

(4) The Middle Jurassic oolitic limestones (labelled O on Figs 151 and 168)

(5) The Portlandian (labelled P on Figs 151 and 168)

Landscape D: Early Cretaceous bedrock

Younger drainage and erosion patterns

Drainage to the Severn Estuary

Drainage towards the Wash on the east coast

Drainage towards the Thames and the southeast coast

CHAPTER 7 London and the Thames Valley Region. GENERAL INTRODUCTION

Modification under Ice Age conditions

Coastlines and sea-level rise

AREA 10: THE COTSWOLDS TO READING

Landscape A: The Cotswold Hills of Middle Jurassic limestone

Landscape B: The Mudstone Lowlands of Late Jurassic to Early Cretaceous bedrock

.Landscape C: The Downs of Late Cretaceous Chalk

Landscape D: The Kennet Valley with Early Tertiary bedrock

AREA 11: LONDON

Landscape A: The Vale of Aylesbury

Landscape B: The Wealden margin

Landscape C: The Chiltern Hills

Landscape D: The North Downs, Hog’s Back and Greensand

Landscape E: The Thames Valley and the London hills

Landscape F: The Thames Basin Western Heaths

Landscape G: The Hertfordshire Plateau

AREA 12: THE THAMES ESTUARY

Landscape A: The Northern Weald

Landscape B: The North Downs and Isle of Thanet

Landscape C: The Thames and tributary estuaries

Landscape D: South Essex and the Northern Thames Basin

CHAPTER 8 The East Anglia Region. GENERAL INTRODUCTION

Bedrock structure and early history

Surface blanket and more recent history

East Anglia’s flatness

AREA 13: NORTHAMPTON TO CAMBRIDGE

Landscape A: Jurassic limestone hills

Landscape B: Clay-Greensand-Gault belt

Landscape C: Chalk hills and valleys

Landscape D: Bishop’s Stortford Clay hills

Landscape E: The Fen edge

AREA 14: SUFFOLK AND NORTH ESSEX

Landscape A: The Fen-edge Claylands (Late Jurassic and Early Cretaceous)

Landscape B: The Chalk Hills (Late Cretaceous)

Landscape C: The Essex Claylands (Early Tertiary)

Landscape D: Suffolk Coast and Heaths (Late Tertiary)

AREA 15: LEICESTER TO THE FENS

Landscape A: Triassic bedrock and the River Trent

Landscape B: Jurassic hills and valleys

Landscape C: The Fens

Landscape D: Early Cretaceous Fenland foothills

AREA 16: NORFOLK

Landscape A: Late Jurassic mudstones of the Fens

Landscape B: Early Cretaceous foothills

Landscape C: North Norfolk coast and the Late Cretaceous Chalk hills

Landscape D: Late Tertiary Crag hills and the Broads

CHAPTER 9 The Making of Southern England

EPISODE 1: THE VARISCAN MOUNTAIN BUILDING

EPISODE 2: THE SOUTHEAST ENGLAND BASIN

A: Lower New Red Sandstone level

B: Middle Jurassic level

C: Late Cretaceous Chalk level

EPISODE 3: RIVER EROSION, FREEZING CLIMATES AND SEA-LEVEL MOVEMENTS

THE SHAPE, FORM AND LOCATION OF SOUTHERN ENGLAND. What has given Southern England its 100-km-scale inland landscape features?

What has given the coastline of Southern England its 100-km-scale location and shape?

Why is Southern England where it is?

Further Reading

SOURCES (REGIONAL GUIDES, LOCAL GUIDES, BOOKS AND MAPS)

CHAPTERS 1–3, GENERAL INTRODUCTION

General coverage of Southern England

Geological maps

Detailed stratigraphic reviews across Southern England

British Geological Survey Regional Guides

CHAPTER 4, THE SOUTHWEST REGION

CHAPTER 5, THE SOUTH COAST REGION

CHAPTER 6, THE SEVERN VALLEY REGION

CHAPTER 7, LONDON AND THE THAMES VALLEY REGION

CHAPTER 8, THE EAST ANGLIA REGION

CHAPTER 9, THE MAKING OF SOUTHERN ENGLAND

Index

The New Naturalist Library

About the Author

Copyright

About the Publisher

Отрывок из книги

Collins New Naturalist Library

PROF. RICHARD WEST, ScD, FRS, FGS

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FIG 24. Cross-section of a beach barrier formed as sea level rises over a very gently sloping landscape.

FIG 25. Beach barrier on Scolt Head Island, Norfolk. (Photograph held at Cambridge University Collection of Air Photographs, Unit for Landscape Modelling)

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