Climate and Time in Their Geological RelationsFront matterReading editionChapter navigation37 reading sectionsGo to chapterChoose a chapter…Front matterCLIMATE AND TIME IN THEIR GEOLOGICAL RELATIONSPREFACELIST OF PLATES.Chapter I · INTRODUCTION.Chapter II · OCEANS-CURRENTS IN RELATION TO THE DISTRIBUTION OF HEAT OVER THE GLOBE.Chapter III · OCEAN-CURRENTS IN RELATION TO THE DISTRIBUTION OF HEAT OVER THE GLOBE.—(Continued.)Chapter IV · OUTLINE OF THE PHYSICAL AGENCIES WHICH LEAD TO SECULAR CHANGES OF CLIMATE.Chapter V · REASON WHY THE SOUTHERN HEMISPHERE IS COLDER THAN THE NORTHERN.Chapter VI · EXAMINATION OF THE GRAVITATION THEORY OF OCEANIC CIRCULATION.—LIEUT. MAURY’S THEORY.Chapter VII · EXAMINATION OF THE GRAVITATION THEORY OF OCEANIC CIRCULATION.—LIEUT. MAURY’S THEORY (continued).Chapter VIII · EXAMINATION OF THE GRAVITATION THEORY OF OCEANIC CIRCULATION.—DR. CARPENTER’S THEORY.Chapter IX · EXAMINATION OF THE GRAVITATION THEORY OF OCEANIC CIRCULATION.—THE MECHANICS OF DR. CARPENTER’S THEORY.Chapter X · EXAMINATION OF THE GRAVITATION THEORY OF OCEANIC CIRCULATION.—DR. CARPENTER’S THEORY.—OBJECTIONS CONSIDERED.Chapter XI · THE INADEQUACY OF THE GRAVITATION THEORY PROVED BY ANOTHER METHOD.Chapter XII · MR. A. G. FINDLAY’S OBJECTIONS CONSIDERED.Chapter XIII · THE WIND THEORY OF OCEANIC CIRCULATION.Chapter XIV · THE WIND THEORY OF OCEANIC CIRCULATION IN RELATION TO CHANGE OF CLIMATE.Chapter XV · WARM INTER-GLACIAL PERIODS.Chapter XVI · WARM INTER-GLACIAL PERIODS IN ARCTIC REGIONS.Chapter XVII · FORMER GLACIAL EPOCHS.—REASON OF THE IMPERFECTION OF GEOLOGICAL RECORDS IN REFERENCE TO THEM.Chapter XVIII · FORMER GLACIAL EPOCHS; GEOLOGICAL EVIDENCE OF.Chapter XIX · GEOLOGICAL TIME.—PROBABLE DATE OF THE GLACIAL EPOCH.Chapter XX · GEOLOGICAL TIME.—METHOD OF MEASURING THE RATE OF SUBAËRIAL DENUDATION.Chapter XXI · THE PROBABLE AGE AND ORIGIN OF THE SUN.Chapter XXII · A METHOD OF DETERMINING THE MEAN THICKNESS OF THE SEDIMENTARY ROCKS OF THE GLOBE.Chapter XXIII · THE PHYSICAL CAUSE OF THE SUBMERGENCE AND EMERGENCE OF THE LAND DURING THE GLACIAL EPOCH.Chapter XXIV · THE PHYSICAL CAUSE OF THE SUBMERGENCE AND EMERGENCE OF THE LAND DURING THE GLACIAL EPOCH.—Continued.Chapter XXV · THE INFLUENCE OF THE OBLIQUITY OF THE ECLIPTIC ON CLIMATE AND ON THE LEVEL OF THE SEA.Chapter XXVI · COAL AN INTER-GLACIAL FORMATION.Chapter XXVII · PATH OF THE ICE-SHEET IN NORTH-WESTERN EUROPE AND ITS RELATIONS TO THE BOULDER CLAY OF CAITHNESS.[250]Chapter XXVIII · NORTH OF ENGLAND ICE-SHEET, AND TRANSPORT OF WASTDALE CRAG BLOCKS.[266]Chapter XXIX · EVIDENCE FROM BURIED RIVER CHANNELS OF A CONTINENTAL PERIOD IN BRITAIN.[279]Chapter XXX · THE PHYSICAL CAUSE OF THE MOTION OF GLACIERS.—THEORIES OF GLACIER-MOTION.Chapter XXXI · THE PHYSICAL CAUSE OF THE MOTION OF GLACIERS.—THE MOLECULAR THEORY.APPENDIX.INDEX.Beginning of this editionNext chapter →CLIMATE AND TIME IN THEIR GEOLOGICAL RELATIONSAll chapters and sections (37)Opening pagesFront matterOther sectionsCLIMATE AND TIME IN THEIR GEOLOGICAL RELATIONSPREFACELIST OF PLATES.Chapters12345678910111213141516171819202122232425262728293031Other sectionsAPPENDIX.INDEX.CLIMATE AND TIME◇FRONTISPIECE◇W. & A. K. Johnston, Edinbr. and London.◇CLIMATE AND TIME IN THEIR GEOLOGICAL RELATIONS →
