Chapter XII
THE ATTEMPTS WHICH HAVE BEEN MADE TO EXPLAIN
THE CAUSES OF VOLCANIC ACTION
331
INDEX
371
ILLUSTRATIONS.
Sections of igneous rocks illustrating the passage from the glassy to the crystalline structure
_Frontispiece_
Fig. Page
1. Stromboli, viewed from the north-west, April 1874 _to face p._ 10
2. Map of the Island of Stromboli 11
3. Section through the Island of Stromboli from north-west to
south-east 13
4. The crater of Stromboli as viewed from the side of the
Sciarra during an eruption on the morning of April 24,
1874. 14
5. Vesuvius in eruption, as seen from Naples, April 26, 1872.
(_From a photograph_) _to face p._ 24
6. View of Vulcano, with Vulcanello in the foreground--taken
from the south end of the Island of Lipari 43
7. Minute cavities, containing liquids, in the crystals of rocks.
(_After Zirkel_) _to face p._ 60
8. Minute liquid-cavity in a crystal, with a moving bubble.
(_After Hartley_) 63
9. Cavity in crystal, containing carbonic-acid gas at a
temperature of 86° F., and passing from the liquid to
the gaseous condition. (_After Hartley_) 64
10. Monte Nuovo (440 ft high) on the shores of the Bay of Naples.
(_After Scrope_) 76
11. Map of the district around Naples, showing Monte Nuovo and the
surrounding volcanoes of older date 78
12. Outlines of the summit of Vesuvius during the eruption of
1767. (_After Sir W. Hamilton_) _to face p._ 80
13. Crater of Vesuvius formed during the eruption of 1822
(_After Scrope_) 82
14. Crater of Vesuvius in 1756, from a drawing made on the spot.
(_After Sir W. Hamilton_) 84
15. The summit of Vesuvius in 1767, from an original drawing.
(_After Sir W, Hamilton_) 85
16. Summit of Vesuvius in 1843 86
17. Outlines of Vesuvius, showing its form at different periods
of its history 87
18. Cascade of lava tumbling over a cliff in the Island of
Bourbon. (_After Capt. S. P. Oliver, R.A._) 93
19. Lava-stream (obsidian) in the Island of Vulcano, showing
the imperfect liquidity of the mass 95
20. Interior of a rhyolitic lava-stream in the Island of Lipari,
showing broad, sigmoidal folds, produced by the slow
movements of the mass 96
21. Interior of a rhyolitic lava-stream in the Island of Lipari,
showing the complicated crumplings and puckerings,
produced by the slow movements of the mass 96
22. Vesuvian lava-stream of 1858, exhibiting the peculiar
'ropy' surfaces of slowly-moving currents.
(_From a photograph_) _to face p._ 98
23. Vesuvian lava-stream of 1872, exhibiting the rough cindery
surfaces characteristic of rapidly flowing currents.
(_From a photograph_) _to face p._ 96
24. Concentric folds on mass of cooled lava. (_After Heaphy_) 100
25. Mass of cooled lava formed over a spiracle on the slopes
of Hawaii. (_After Dana_) 100
26. Group of small cones thrown up on the Vesuvian lava-current
of 1855. (_After Schmidt_) 101
27. Natural section of a lava-stream in the Island of Vulcano,
showing the compact central portion and the scoriaceous
upper and under surfaces 104
28. Section of a lava-stream exposed on the side of the river
Ardèche, in the south-west of France. (_After Scrope_) 106
29. Portion of a basaltic column from the Giant's Causeway,
exhibiting both the ball-and-socket and the
tenon-and-mortise structure 107
30. Vein of green pitchstone at Chiaja di Luna, in the Island
of Ponza, breaking up into regular columns and into
spherical masses with a concentric series of joints.
(_After Scrope_) 108
31. Illustration of the 'perlitic structure' in glassy rocks 109
32. Transverse section of a lava-stream 111
33. The Kammerbühl, or Kammerberg, Bohemia (as seen from
the south-west) 113
34. Section of the Kammerbühl in Bohemia 114
35. Natural section of a volcanic cone in the Island of Vulcano 116
36. Section in the side of the Kammerbühl, Bohemia 118
37. Experimental illustration of the mode of formation of
volcanic cones, composed of fragmental materials 120
38. Natural section of a tuff-cone, forming the Cape of Misenum,
and exhibiting the peculiar internal arrangement,
characteristic of volcanoes composed of fragmentary
materials. (_After Scrope_) 121
39. Section of a small scoria-cone formed within the crater of
Vesuvius in the year 1835, illustrating the filling up of
the central vent of the cone by subsequent ejections.
(_After Abich_) 122
40. Volcanic cones composed of scoriæ, and breached on one
side by the outflow of lava-currents. (_After Scrope_) 128
41. Campo Bianco, in the Island of Lipari. A pumice-cone
breached by the outflow of an obsidian lava-stream
_to face p._ 124
42. Volcanic cones in Auvergne, which have suffered to some
extent from atmospheric denudation. (_After Scrope_) 124
43. Experimental illustration of the mode of formation of
volcanic cones composed of viscid lavas. (_After Reyer_) 126
44. The Grand Puy of Sarcoui, composed of trachyte, rising
between two breached scoria-cones (Auvergne). (_After
Scrope_) 126
45. Volcanic cone (Mamelon) composed of very viscid lava
(Island of Bourbon). (_After Bory de St. Vincent_) 127
46. Another Mamelon in the Island of Bourbon, with a crater
at its summit. (_After Bory de St. Vincent_) 127
47. Cliff-section in the Island of Madeira, showing how a
composite volcano is built up of lava-streams, beds of
scoriæ, and dykes. (_After Lyell_) 125
48. Section seen at the cascade, Bains du Mont Dore. (_After
Scrope_) 130
49. Section in the Island of Ventotienne, showing a great
stream of andesitic lava overlying stratified tuffs.
(_After Scrope_) 130
50. Cliff on the south side of the Island of San Stephano 131
51. The headland of Monte della Guardia, in the Island of Ponza 131
52. Western side of the same headland, as seen from the north
side of Luna Bay 132
53. Sea-cliff at Il Capo, the north-east point of Salina,
showing stratified agglomerates traversed by numerous
dykes, the whole being unconformably overlaid by
stratified, aqueous deposits 137
54. Section observed in the Val del Bove, Etna, showing a
basaltic dyke, from the upper part of which a
lava-current has flowed 138
55. Basaltic dykes projecting from masses of stratified scoriæ
in the sides of the Val del Bove, Etna 134
56. Sheets of igneous rock (basalt) intruded between beds of
sandstone, clay, and limestone (Island of Skye) 137
57. Plan of the dissected volcano of Mull in the Inner
Hebrides _to face p._ 142
58. Section of the volcano of Mull along the line A B " 142
59. Summit of the volcano of Monte Sant' Angelo, in Lipari,
exhibiting a crater with walls worn down by denudation 158
60. Outlines of lava-cones 160
61. Diagram illustrating the formation of parasitic cones along
lines of fissure formed on the flanks of a great volcanic
mountain 162
62. Outline of Etna, as seen from Catania 162
63. Outline of Etna, as seen from the Val del Bronte 163
64. Plan of the volcano forming the Island of Ischia 163
65. A primary parasitic cone, with a secondary one at its
base--Ischia 164
66. Scoria-cone near Auckland, New Zealand, with a lava-current
flowing from it. (_After Heaphy_) 165
67. Section of rocks below the ancient triassic volcano of
Predazzo in the Tyrol 165
68. Cotopaxi, as seen from a distance of ninety miles. (_After
Humboldt_) 168
69. Citlaltepetl, or the Pic d'Orizaba, in Mexico, as seen from
the Forest of Xalapa. (_After Humboldt_) 169
70. Lac Paven, in the Auvergne. (_After Scrope_) 171
71. The crater-lake called Lago del Bagno, in Ischia, converted
into a harbour 172
72. Lake of Gustavila, in Mexico. (_After Humboldt_) 172
73. Peak of Teneriffe, surrounded by great crater-rings. (_After
Piazzi-Smyth_) 175
74. The volcano of Bourbon, rising in the midst of a crater-ring
four miles in diameter. (_After Bory de St. Vincent_) 176
75. The volcano of Bourbon, as seen from another point of
view, with three concentric crater-rings encircling its
base. (_After Bory de St. Vincent_) 176
76. Vesuvius as seen from Sorrento, half encircled by the
crater-ring of Somma 177
77. Outlines of various volcanoes illustrating the different
relations of the craters to cones _to face p._ 178
78. Island thrown up In the Mediterranean Sea in July and
August, 1831. (_After the Prince de Joinville_) 179
79. Sinter-cones surrounding the orifices of geysers 183
80. Diagram illustrating the mode of formation of travertine-
and sinter-terraces on the sides of a hill of tuff 185
81. Map of the volcanic group of the Lipari Islands, illustrating
the position of the lines of fissure upon which
the volcanoes have been built up 192
82. The Puy de Pariou, in the Auvergne, illustrating the shifting
of eruption along a line of fissures 193
83. Ideal section of the Puy de Pariou 194
84. Fissure formed on the flanks of Etna during the emotion
of 1865. (_After Silvestri_) 194
85. Plan of the Island of Vulcano, based on the map of the
Italian Government 196
86. Vulcanello, with its three craters 197
87. Section of basalt from Ovifak, Greenland, with particles of
metallic iron diffused through its mass 319
88. Diagram illustrating the relations between the terrestrial
and the extra-terrestrial rocks _to face p._ 322
89. A group of sun-spots. (_After Secchi_) 362
90. A sun-spot, showing the great masses of incandescent
vapour rising or falling within it. (_After Secchi_) 363
91. The edge of a sun-spot, showing a portion of the prominent
masses of incandescent gas (A) which detached itself
at B and floated into the midst of the cavity.
(_After Norman Lockyer_) 363
92. Drawing of a solar prominence made by Mr. Norman
Lockyer, March 14, 1869, at 11 h. 5 m. A.M. 364
93. The same object, as seen at 11 h. 15 m. on the same day.
(_After Norman Lockyer_) 365
94. Drawings of a solar prominence at four different periods
on September 7, 1871. (_After Young_) 366
95. A group of Lunar craters (Maurolycus, Barocius, &c.), the
largest being more than sixty miles in diameter 368
VOLCANOES.
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Volcanoes: What They are and What They TeachChapter XII
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