Category: History - Ancient

Volcanoes: Past and Present

There are no manifestations of the forces of Nature more calculated to inspire us with feelings of awe and admiration than volcanic eruptions preceded or accompanied, as they generally are, by earthquake shocks. Few agents have been so destructive in their effects; and to the...

Chapters

1. Chapter 1

2. Chapter 2

3. Chapter 3

4. Chapter 4

5. Chapter 5

6. Chapter 6

7. Chapter 7

8. Chapter 8

There are no manifestations of the forces of Nature more calculated to inspire us with feelings of awe and admiration than volcanic eruptions preceded or accompanied, as they ge...

9. Chapter 9

The conical form of a volcanic mountain is so generally recognised, that many persons who have no intelligent acquaintance with geological phenomena are in the habit of attribut...

10. Chapter 10

The globe is girdled by a chain of volcanic mountains in a state of greater or less activity, which may perhaps be considered a girdle of safety for the whole world, through whi...

11. Chapter 11

_Oceanic Islands._--By far the most extensive regions with sporadically distributed volcanic vents, both active and extinct, are those which are overspread by the waters of the...

12. Chapter 12

Having now dealt in a necessarily cursory manner with volcanoes of distant parts of the globe, we may proceed to the consideration of the group of active volcanoes which still s...

13. Chapter 13

(_a._) _Structure of the Mountain._--Etna, unlike Vesuvius, has ever been a burning mountain; hence it was well known as such to classic writers before the Christian era. The st...

14. Chapter 14

(_a._) A brief account of this remarkable group of volcanic islands must here be given, inasmuch as they seem to be representatives of a stage of volcanic action in which the ig...

15. Chapter 15

(_a._) Before leaving the subject of European active volcanoes, it is necessary to give some account of the remarkable volcanic island of Santorin, in the Grecian archipelago. T...

16. Chapter 16

We are naturally led on from a consideration of the active volcanoes of Europe to that of volcanoes which are either dormant or extinct in the same region. Such are to be found...

17. Chapter 17

(_a._) _General Structure of the Auvergne District._--From a granitic and gneissose platform situated near the centre of France, and separated from the western spurs of the Alps...

18. Chapter 18

The region bordering the Rhine along both its banks above Bonn, and extending thence along the valley of the Moselle and into the Eifel, has been the theatre of active volcanic...

19. Chapter 19

20. Chapter 20

(_a._) _Region east of the Jordan and Dead Sea._--The remarkable line of country lying along the valley of the Jordan, and extending into the great Arabian Desert, has been the...

21. Chapter 21

(_a._) _Contrast between the Eastern and Western Regions._--In no point is there a more remarkable contrast between the physical structure of Eastern and Western America than in...

22. Chapter 22

One other region of volcanic action remains to be noticed before passing on to the consideration of those of less recent age. New Zealand is an island wherein seem to be concent...

23. Chapter 23

It is an easy transition to pass from the consideration of European and other dormant, or extinct, volcanic regions to those of the British Isles, though the volcanic forces may...

24. Chapter 24

(_c._) _First Stage._--The earliest eruptions of lava in the North-east of Ireland belonged to the highly acid varieties, consisting of quartz-trachyte with tridymite.[1] This r...

25. Chapter 25

The Island of Mull, with the adjoining districts of Morvern and Ardnamurchan, forms the more southern of the two chief centres of Tertiary volcanic eruptions in the West of Scot...

26. Chapter 26

This is the largest and most important of all the Tertiary volcanic districts, but owing to the extensive denudation to which, in common with other Tertiary volcanic regions of...

27. Chapter 27

Amongst the more remarkable of the smaller islets are those of Eigg, Rum, Canna, and Muck, lying between Mull on the south and Skye on the north, and undoubtedly at one time phy...

28. Chapter 28

Reference has been made to this remarkable island in a former page, but some more extended notice is desirable before leaving the region of the Inner Hebrides. Along with the is...

29. Chapter 29

The great outpourings of augitic lava of Tertiary and recent times which we have been considering appear to have been anticipated in several parts of the world, more especially...

30. Chapter 30

Another region in which the volcanic phenomena bear a remarkable analogy to those of Central India, just described, is that of Abyssinia. Nor are these tracts so widely separate...

31. Chapter 31

_Basalt of the Plateau._--The extensive sheets of plateau-basalt forming portions of the Neuweld range and the elevated table-land of Cape Colony, may be regarded as forerunners...

32. Chapter 32

It is beyond the scope of this work to describe the volcanic rocks of pre-Tertiary times over various parts of the globe. The subject is far too large to be treated otherwise th...

33. Chapter 33

I propose to introduce here some account of one of the most terrible outbursts of volcanic action that have taken place in modern times; namely, the eruption of the volcano of K...

34. Chapter 34

_Connection of Earthquakes with Volcanic Action._--The connection between earthquake shocks and volcanic eruptions is now so generally recognised that it is unnecessary to insis...

35. Chapter 35

Volcanic phenomena are the outward manifestations of forces deep-seated beneath the crust of the globe; and in seeking for the causes of such phenomena we must be guided by obse...

36. Chapter 36

The surface of the moon presented to our view affords such remarkable indications of volcanic phenomena of a special kind, that we are justified in devoting a chapter to their c...

37. Chapter 37

The question which we are about to discuss in the concluding chapter of this volume is one to which we ought to be able to offer a definite answer. This can only be arrived at b...