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The Ancient Volcanoes of Great Britain, Volume 1 (of 2)

Geikie, Archibald · Public domain text

221,044 words · about 15 h 29 min to read

About this edition

The text of The Ancient Volcanoes of Great Britain, Volume 1 (of 2) comes from Project Gutenberg e-text #66492. It is public domain in the United States. Project Gutenberg’s header and license text are removed, and RedLectern sets the text out for reading on screen; no words of the book are rewritten or summarized. More formats (EPUB, Kindle) · How RedLectern is built

This text-only edition leaves out 180 illustrations. See the illustrated edition at Project Gutenberg.

This book is long enough to be split into 7 parts, so each one loads quickly on its own.

About this book

Author
Archibald Geikie (1835–1924)
Language
English
Subjects
Volcanoes › Great Britain
Length
221,044 words · about 15 h 29 min
Sections
58 reader sections · Table of contents
Contents (58)
  1. Opening about 1 min
  2. Preface about 11 min
  3. I. PAGE under 1 min
  4. Chapter II under 1 min
  5. Chapter III under 1 min
  6. Chapter IV under 1 min
  7. Chapter V under 1 min
  8. Chapter VI under 1 min
  9. Chapter VII under 1 min
  10. VIII. Pre-Cambrian Volcanoes under 1 min
  11. IX. Characteristics of the Cambrian System in Britain under 1 min
  12. Chapter X under 1 min
  13. Chapter XI under 1 min
  14. Chapter XII under 1 min
  15. XIII. The Eruptions of Llandeilo and Bala Age under 1 min
  16. Chapter XIV under 1 min
  17. Chapter XV under 1 min
  18. XVI. The Volcanoes of the Old Red Sandstone under 1 min
  19. Chapter XVII under 1 min
  20. Chapter XVIII under 1 min
  21. XIX. Volcanoes of the Lower Old Red Sandstone of "Lake Caledonia" under 1 min
  22. Chapter XX under 1 min
  23. Chapter XXI under 1 min
  24. Chapter XXII under 1 min
  25. XXIII. The Carboniferous System of Britain and its Volcanic Records under 1 min
  26. XXIV. Carboniferous Volcanic Plateaux of Scotland under 1 min
  27. Chapter XXV under 1 min
  28. XXVI. The Carboniferous Puys of Scotland under 1 min
  29. XXVII. Geological Structure of the Carboniferous Puys of Scotland under 1 min
  30. XXVIII. Illustrative Examples of the Carboniferous Puys of Scotland about 11 min
  31. Chapter I about 18 min
  32. II. The Nature and Causes of Volcanic Action--Modern Volcanoes about 8 min
  33. Chapter III about 44 min
  34. Chapter IV about 25 min
  35. Chapter V about 50 min
  36. Chapter VI about 49 min
  37. Chapter VII about 17 min
  38. VIII. PRE-CAMBRIAN VOLCANOES about 1 h
  39. IX. CHARACTERISTICS OF THE CAMBRIAN SYSTEM IN BRITAIN about 13 min
  40. X. THE CAMBRIAN VOLCANOES OF SOUTH WALES about 26 min
  41. Chapter XI about 28 min
  42. Chapter XII about 58 min
  43. XIII. THE ERUPTIONS OF LLANDEILO AND BALA AGE about 1 h 19 min
  44. XIV. THE SILURIAN VOLCANOES OF IRELAND about 39 min
  45. XV. THE DEVONIAN VOLCANOES about 12 min
  46. XVI. THE VOLCANOES OF THE OLD RED SANDSTONE about 18 min
  47. Chapter XVII about 21 min
  48. Chapter XVIII about 23 min
  49. XIX. VOLCANOES OF THE LOWER OLD RED SANDSTONE OF "LAKE CALEDONIA" about 44 min
  50. Chapter XX about 35 min
  51. Chapter XXI about 24 min
  52. Chapter XXII about 9 min
  53. XXIII. THE CARBONIFEROUS SYSTEM OF BRITAIN AND ITS VOLCANIC RECORDS about 23 min
  54. XXIV. CARBONIFEROUS VOLCANIC PLATEAUX OF SCOTLAND about 26 min
  55. Chapter XXV about 46 min
  56. XXVI. THE CARBONIFEROUS PUYS OF SCOTLAND about 20 min
  57. XXVII. GEOLOGICAL STRUCTURE OF THE CARBONIFEROUS PUYS OF SCOTLAND about 59 min
  58. XXVIII. ILLUSTRATIVE EXAMPLES OF THE CARBONIFEROUS PUYS OF SCOTLAND about 31 min

The opening of Preface

In no department of science is the slow and chequered progress of investigation more conspicuous than in that branch of Geology which treats of volcanoes. Although from the earliest dawn of history, men had been familiar with the stupendous events of volcanic eruptions, they were singularly slow in recognizing these phenomena as definite and important parts of the natural history of the earth. Even within the present century, the dominant geological school in Europe taught that volcanoes were mere accidents, due to the combustion of subterranean beds of coal casually set on fire by lightning, or by the decomposition of pyrites. Burning mountains, as they were called, were believed to be only local and fortuitous appearances, depending on the position of the coal-fields, and having no essential connection with the internal structure and past condition of our planet. So long as such fantastic conceptions prevailed, it was impossible that any solid progress could be made in this branch of science. A juster appreciation of the nature of the earth's interior was needed before men could recognize that volcanic action had once been vigorous and prolonged in many countries, where no remains of volcanoes can now be seen.

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