Part,  Chapter

 1 1,0|           and there were traces of lava. Sulphur springs sometimes
 2 1,0|        still in activity. Hardened lava and crusted scoria formed
 3 1,1|             large thick streaks of lava wound over the sides of
 4 1,1|             Traces of very ancient lava were noticed, which probably
 5 1,1|       passage, and a large heap of lava had spread to the narrow
 6 1,2|       there were here no traces of lava, which was spread more particularly
 7 1,4|             mingled with debris of lava. A few sea-birds frequented
 8 2,0|           enclosed in the frame of lava. ~"Well," said Pencroft, "
 9 2,0|            formed by two rivers of lava, thrown out by the volcano,
10 2,0|            And, in fact, the steep lava cliffs did not afford a
11 2,0|            coast. ~To the enormous lava rocks succeeded soon those
12 3,3|      ravines, among the streams of lava, that this dwelling and
13 3,3|         masses of rock, paved with lava, and varied with great blocks
14 3,3|          the overflow of smoke and lava, would escape, as it did
15 3,3|    customary outlet." ~"Unless the lava opened a new way for itself
16 3,3| considerably depressed, and if the lava should ever take a course
17 3,3|           rocks, cinders, hardened lava, and that this valve of
18 3,5|            shown by the streams of lava hardened on the northern
19 3,5|            outlets for the burning lava. ~Cyrus Harding explained
20 3,8|           the ancient track of the lava is still open; and thanks
21 3,8|     results of an eruption. If the lava, in consequence of the position
22 3,8|        side, granite on the other, lava on the north, rich soil
23 3,8|       feared, since the vapors and lava have found a free outlet." ~"
24 3,8|           it did not seem that the lava, though swollen by the internal
25 3,8|        discover no traces of fresh lava. ~The engineer became more
26 3,8|          ground; but no current of lava burst from the mouth of
27 3,8|          should then know that the lava had followed its accustomed
28 3,8|            ancient channels of the lava. There was no doubt in his
29 3,9|          the island to the boiling lava, Lincoln Island will that
30 3,9|        23rd, in consequence of the lava attaining the level of the
31 3,9|         the same time a torrent of lava, bursting from the new summit,
32 3,9|        towards the corral that the lava was rushing as the new crater
33 3,9|        hour afterwards the boiling lava filled the corral, converting
34 3,9|       direction this inundation of lava was about to take. The soil
35 3,9|       Franklin had fallen, but the lava arrested their progress.
36 3,9|            crossing the torrent of lava; on the contrary, the colonists
37 3,9|         sides an unceasing flow of lava poured forth, thus forming
38 3,9|          rain around them, but the lava, overflowing the bed of
39 3,9|       inclination of the soil, the lava gained rapidly in the east,
40 3,9|            already consumed by the lava. ~The colonists halted near
41 3,9|         arrest the progress of the lava, and a part of the island
42 3,9|          this instant the river of lava, after having broken a passage
43 3,9|         the barrier. The stream of lava swelled like a river about
44 3,9|           contact with the boiling lava. The vapor whirled in the
45 3,9|   replenished, while the stream of lava, fed from an inexhaustible
46 3,9|        matter. ~The first waves of lava which fell in the lake immediately
47 3,9|         the water displaced by the lava being evaporated. The hissing
48 3,9|          longer, and the blocks of lava piled themselves one on
49 3,9|            irresistible torrent of lava. ~This time water would
50 3,9|     colonists that the effusion of lava should have been in the
51 3,9|         night and day. The flow of lava continued, but perhaps less
52 3,9|    entirely choked up, and if more lava should accumulate it would
53 3,9|         fact, the second stream of lava, which had followed the
54 3,9|          trees than the current of lava at their bases. ~Thus it
55 3,9|      Tadorn Marsh. The eruption of lava had been complete. Where
56 3,9|       thirst. But, fortunately the lava had spared the southern
57 3,9|         volcano still vomits forth lava, but somewhat less abundantly,
58 3,9|           the 7th of February, the lava continued to flow, but the
59 3,9|        like glass, formed of fluid lava, fell like rain upon the
60 3,9|      crater was again boiling with lava which overflowed the back
61 3,0|      asunder by the explosion; the lava jaws of Shark Gulf, the