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Charles Lyell - Principles of Geology

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One of the key works in the nineteenth-century battle between science and Scripture
Charles Lyells Principles of Geology (1830-33) sought to explain the geological state of the modern Earth by considering the long-term effects of observable natural phenomena. Written with clarity and a dazzling intellectual passion, it is both a seminal work of modern geology and a compelling precursor to Darwinism, exploring the evidence for radical changes in climate and geography across the ages and speculating on the progressive development of life. A profound influence on Darwin, Principles of Geology also captured the imagination of contemporaries such as Melville, Emerson, Tennyson and George Eliot, transforming science with its depiction of the powerful forces that shape the natural world.
For more than seventy years, Penguin has been the leading publisher of classic literature in the English-speaking world. With more than 1,700 titles, Penguin Classics represents a global bookshelf of the best works throughout history and across genres and disciplines. Readers trust the series to provide authoritative texts enhanced by introductions and notes by distinguished scholars and contemporary authors, as well as up-to-date translations by award-winning translators.

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PRINCIPLES OF GEOLOGY

CHARLES LYELL was born in November 1797 at Kinnordy House near Kirriemuir, Forfarshire, Scotland, and was the son of a botanist. His family moved to Hampshire, on the border of the New Forest, before he was one year old. Lyell was educated at Ringwood, Salisbury, Midhurst and Exeter College, Oxford, from which he graduated in classics in 1819. He entered Lincolns Inn to study law, but a weakness in his eyes temporarily prevented him from continuing, a difficulty which increased in later years. He published his first scientific papers in 1825 and in the following year became a Fellow of the Royal Society. Lyell also began contributing to the Quarterly Review and gradually abandoned legal practice, having found his vocation in authorship. The first volume of his masterpiece Principles of Geology was published in 1830, and the second and third volumes appeared in 1832 and 1833 respectively. Lyells vision of a world shaped by uniformly acting natural processes became central to public controversy about the place of human beings in nature. Its impact is evident in a wide range of Victorian literary, philosophical and scientific works, notably those of Charles Darwin, who became a close friend. In 1831 Lyell was appointed a professor of geology at Kings College, London (although he soon resigned), and a year later he married Mary Horner, who assisted in his work and became a leading hostess in metropolitan intellectual society. He was elected President of the Geological Society of London in 18357 and 184951. A great admirer of the United States, Lyell lectured extensively there, and in 1845 and 1849 he published lively descriptions of his travels in North America. He continued to revise Principles of Geology, which appeared in its final two-volume form in 18678. Among his other books, all of which appeared in many editions, are Elements of Geology (1838) and The Antiquity of Man (1863). He was knighted in 1848 and became a baronet in 1864. His health deteriorated rapidly after the death of Lady Lyell in 1873, but he continued with research until his death in 1875. He is buried in the nave of Westminster Abbey.

J IM SEGORD is a lecturer in the Department of History and Philosophy of Science at the University of Cambridge. Born in Madison, Wisconsin, he studied geology, literature and history at Pomona College and Princeton University, and has lived in England since 1980. He is the author of Controversy in Victorian Geology (1986), editor of Robert Chamberss Vestiges of the Natural History of Creation (1994) and co-editor (with N. Jardine and E. Spary) of Cultures of Natural History (1996).

Charles Lyell

PRINCIPLES OF GEOLOGY

Edited with an introduction by
JAMES A. SEGORD

PENGUIN BOOKS

PENGUIN BOOKS

Published by the Penguin Group
Penguin Books Ltd, 80 Strand, London WC2R 0RL , England
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First published 183033
This selected text published in Penguin Classics 1997
13

This edition copyright James A. Secord, 1997
All rights reserved

The moral right of the editor has been asserted

Except in the United States of America, this book is sold subject to the condition that it shall not, by way of trade or otherwise, be lent, re-sold, hired out, or otherwise circulated without the publishers prior consent in any form of binding or cover other than that in which it is published and without a similar condition including this condition being imposed on the subsequent purchaser

ISBN: 978-0-14-193680-2

Contents

1316, 17 How the Remains of Man
and his Works are becoming Fossil beneath the Waters

VOLUME I

Frontispiece. This representation of the present state of the Temple of Serapis has been carefully reduced from that given by the Canonico Andrea de Jorio in his Ricerche sul Tempio di Serapide, in Puzzuoli. Napoli, 1820

. Transverse section of the Italian peninsula

. Diagram explanatory of the sinuosity of river-courses

. Diagram showing the recent excavation of lava at the foot of Etna by the river Simeto

. Chart and section of Santorin and the contiguous islands in the Grecian Archipelago

. View of the Isle of Palma, and of the Caldera in its centre

. View of the cone and crater of Barren Island in the Bay of Bengal

. Supposed section of the same

. Deep fissure near Polistena in Calabria, caused by the earthquake of 1783

. Shift or fault in the round tower of Terranuova in Calabria, occasioned by the earthquake of 1783

. Shift in the stones of two obelisks in the Convent of S. Bruno

. Fissures near Jerocarne in Calabria, caused by the earthquake of 1783

. Landslips near Cinquefrondi, caused by earthquake of 1783

. Ground plan of the coast of the Bay of Bai in the environs of Puzzuoli

. Two sections, the one exhibiting the relation of the recent marine deposits to the more ancient in the Bay of Bai to the north of Puzzuoli, and the other exhibiting the same relation to the south-east

. View of the crater of the great Geyser in Iceland

. Supposed section of the subterranean reservoir and pipe of a Geyser in Iceland

VOLUME II

Frontispiece. View of part of the Valley del Bove, on the East side of the great Cone of Etna [Part of a panoramic drawing made by Lyell in 1828, this appeared in the first edition with hand-colouring Ed.]

. Maldiva Isles

. View of Witsunday Island

. Section of a coral island

. Ditto of part of a coral island

VOLUME III

Frontispiece. View of the volcanoes around Olot, in Catalonia [From a sketch by Lyell, which appeared in the first edition with hand-colouring and an accompanying geological key Ed.]

. Diagram showing the order of succession of stratified masses

. Diagram showing the relative position of the Primary, Secondary, and Tertiary strata

. Diagram showing the relative age of the strata of the Paris basin, and those of the basin of the Loire, in Touraine

. Diagram showing the same in the strata of Suffolk and Piedmont

. Wood-cut showing the great valley on the east side of Etna

. View of dikes at the base of the Serre del Solfizio, Etna

. View of tortuous dikes or veins of lava, Punto di Guimento, Etna

. View of the rocks Finochio, Capra, and Musara, in the Val del Bove

. View from the summit of Etna into the Val del Bove

Introduction

The great merit of the Principles, Charles Darwin once said, was that it altered the whole tone of ones mind, & therefore that, when seeing a thing never seen by Lyell, one yet saw it partially through his eyes.

The Principles, as Darwin recognized, is about seeing. In it, theology, political economy and the philosophy of perception are united with natural history, anthropology, geography and travel. The title proclaimed heroic ambitions no less than doing for the study of the earth what Isaac Newton had done for astronomy and natural philosophy in the

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