But this time, instead of Snæfell, an extinct volcano, we were inside
one in full activity. I wondered, therefore, where could this
mountain be, and in what part of the world we were to be shot out.
I made no doubt but that it would be in some northern region. Before
its disorders set in, the needle had never deviated from that
direction. From Cape Saknussemm we had been carried due north for
hundreds of leagues. Were we under Iceland again? Were we destined to
be thrown up out of Hecla, or by which of the seven other fiery
craters in that island? Within a radius of five hundred leagues to
the west I remembered under this parallel of latitude only the
imperfectly known volcanoes of the north-east coast of America. To
the east there was only one in the 80th degree of north latitude, the
Esk in Jan Mayen Island, not far from Spitzbergen! Certainly there
was no lack of craters, and there were some capacious enough to throw
out a whole army! But I wanted to know which of them was to serve us
for an exit from the inner world.
Towards morning the ascending movement became accelerated. If the
heat increased, instead of diminishing, as we approached nearer to
the surface of the globe, this effect was due to local causes alone,
and those volcanic. The manner of our locomotion left no doubt in my
mind. An enormous force, a force of hundreds of atmospheres,
generated by the extreme pressure of confined vapours, was driving us
irresistibly forward. But to what numberless dangers it exposed us!
Soon lurid lights began to penetrate the vertical gallery which
widened as we went up. Right and left I could see deep channels, like
huge tunnels, out of which escaped dense volumes of smoke; tongues of
fire lapped the walls, which crackled and sputtered under the intense
heat.
"See, see, my uncle!" I cried.
"Well, those are only sulphureous flames and vapours, which one must
expect to see in an eruption. They are quite natural."
"But suppose they should wrap us round."
"But they won't wrap us round."
"But we shall be stifled."
"We shall not be stifled at all. The gallery is widening, and if it
becomes necessary, we shall abandon the raft, and creep into a
crevice."
"But the water--the rising water?"
"There is no more water, Axel; only a lava paste, which is bearing us
up on its surface to the top of the crater."
The liquid column had indeed disappeared, to give place to dense and
still boiling eruptive matter of all kinds. The temperature was
becoming unbearable. A thermometer exposed to this atmosphere would
have marked 150°. The perspiration streamed from my body. But for the
rapidity of our ascent we should have been suffocated.
But the Professor gave up his idea of abandoning the raft, and it was
well he did. However roughly joined together, those planks afforded
us a firmer support than we could have found anywhere else.
About eight in the morning a new incident occurred. The upward
movement ceased. The raft lay motionless.
Public-domain text, read in full here on John Shaqi.
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