Chapter I: Preface

It has not been my object to present in the following pages even an approximately complete description of the volcanic and seismic phenomena of the globe; such an undertaking would involve an amount of labour which few would be bold enough to attempt; nor would it be compatible with the aims of the _Contemporary Science Series_.

I have rather chosen to illustrate the most recent conclusions regarding the phenomena and origin of volcanic action, by the selection of examples drawn from the districts where these phenomena have been most carefully observed and recorded under the light of modern geological science. I have also endeavoured to show, by illustrations carried back into later geological epochs, how the volcanic phenomena of the present day do not differ in kind, though they may in degree, from those of the past history of our globe. For not only do the modes of eruption of volcanic materials in past geological times resemble those of the present or human epoch, but the materials themselves are so similar in character that it is only in consequence of alterations in structure or composition which the original materials have undergone, since their extrusion, that any important distinctions can be recognised between the volcanic products of recent times and those of earlier periods.

I have, finally, endeavoured to find an answer to two interesting and important questions: (1) Are we now living in an epoch of extraordinary volcanic energy?--a question which such terrible outbursts as we have recently witnessed in Japan, the Malay Archipelago, and even in Italy, naturally suggest; and (2) What is the ultimate cause of volcanic action? On this latter point I am gratified to find that my conclusions are in accordance with those expounded by one who has been appropriately designated "the Nestor of Modern Geology," Professor Prestwich.

Within the last few years the study of the structure and composition of volcanic rocks, by means of the microscope brought to bear on their translucent sections, has added wonderfully to our knowledge of such rocks, and has become a special branch of petrological investigation. Commenced by Sorby, and carried on by Allport, Zirkel, Rosenbusch, Von Lasaulx, Teall, and many more enthusiastic students, it has thrown a flood of light upon our knowledge of the mutual relations of the component minerals of igneous masses, the alteration these minerals have undergone in some cases, and the conditions under which they have been erupted and consolidated. But nothing that has been observed has tended materially to alter conclusions arrived at by other processes of reasoning regarding volcanic phenomena, and for these we have to fall back upon observations conducted in the field on a more or less large scale, and carried on before, during, and after eruptions. Macroscopic and microscopic observations have to go hand in hand in the study of volcanic phenomena.

E. H.

CONTENTS.

PART I.

_INTRODUCTION._

PAGE

Chap. I. Historic Notices of Volcanic Action 1-9

" II. Form, Structure, and Composition of Volcanic
Mountains 10-19

" III. Lines and Groups of Active Volcanic Vents 20-29

" IV. Mid-ocean Volcanic Islands 30-40

PART II.

_EUROPEAN VOLCANOES._

Chap. I. Vesuvius 41-60

" II. Etna 61-68

" III. The Lipari Islands, Stromboli 69-75

" IV. The Santorin Group 76-83

" V. European Extinct or Dormant Volcanoes 84-91

" VI. Extinct Volcanoes of Central France 92-112

" VII. The Volcanic District of the Rhine Valley 13-125

PART III.

_DORMANT OR MORIBUND VOLCANOES OF OTHER PARTS OF THE WORLD._

Chap. I. Dormant Volcanoes of Palestine and Arabia 126-135

" II. The Volcanic Regions of North America 136-145

" III. Volcanoes of New Zealand 146-153

PART IV.

_TERTIARY VOLCANIC DISTRICTS OF THE BRITISH ISLES._

Chap. I. Antrim 154-159

" II. Succession of Volcanic Eruptions 160-171

" III. Island of Mull and Adjoining Coast 172-176

" IV. Isle of Skye 177-179

" V. The Scuir of Eigg 180-184

" VI. Isle of Staffa 185-186

PART V.

_PRE-TERTIARY VOLCANIC ROCKS._

Chap. I. The Deccan Trap-series of India 187-189

" II. Abyssinian Table-lands 190-193

" III. Cape Colony 194-195

" IV. Volcanic Rocks of Past Geological
Periods of the British Isles 196-199

PART VI.

_SPECIAL VOLCANIC AND SEISMIC PHENOMENA._

Chap. I. The Eruption of Krakatoa in 1883 201-216

" II. Earthquakes 217-224

PART VII.

_VOLCANIC AND SEISMIC PROBLEMS._

Chap. I. The Ultimate Cause of Volcanic Action 225-235

" II. Lunar Volcanoes 236-252

" III. Are we Living in an Epoch of Special
Volcanic Activity? 253-257