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JOHN WILLIAM

AND SOLD BY

PARKER, WEST STRAND, LONDON;

J. & J. J. DEIGHTON; AND T. STEVENSON, CAMBRIDGE.

M.DCCC.XXXVIII.

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CONTENTS OF THE SIXTH VOLUME.

PAGE

ADVERTISEMENT.

THE Society as a body is not to be considered responsible for any
facts and opinions advanced in the several Papers, which must rest
entirely on the credit of their respective Authors.

THE Society takes this opportunity of expressing its grateful
acknowledgments to the Syndics of the University Press, for their
liberality in taking upon themselves the expense of printing this
Part of its TRANSACTIONS.

I. Researches in Physical Geology. By WILLIAM HOPKINS, M.A., Fellow of the Cambridge Philosophical Society, and of the Geological Society, and Mathematical Lecturer of St Peter's College, Cambridge.

[Read May 4, 1835.]

INTRODUCTION.

NOTWITHSTANDING the appearances of irregularity and confusion in the formation of the crust of our globe which are presented to the eye in the contemplation of its external features, geologists have been able in numerous instances to detect, in the arrangement and position of its stratified masses, distinct approximations to geometrical laws. In the phenomena of anticlinal lines, faults, fissures, mineral veins, &c., such laws are easily recognized; and though, when we consider how large a portion of the surface of the earth remains geologically unexplored, it may appear premature to assert that these are perfectly general laws, yet, founding our reasoning on our knowledge, and not on our ignorance, and feeling that confidence which we are entitled to feel in the universality of the laws and operations of nature, we shall, I conceive, be justified, if not in the absolute conclusion, at least in the presumption, that the laws already observed in phenomena such as those above mentioned will be found, by the wider extension and increased accuracy of geological research, to be the approximative general laws of those phenomena.

If the legitimacy of this inference be allowed, we are necessarily led to the conclusion, that the phenomena alluded to are referrible not to the particular and irregular action of merely local causes, but to the more widely diffused action of some simple cause, general in its nature with respect to every part of the globe, and general in its action at least with respect to the whole of each district throughout VOL. VI. PART I.

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