My uncle said it was time to go to sleep. We ate without talking, and
went to sleep without reflection.
Our arrangements for the night were very simple; a railway rug each,
into which we rolled ourselves, was our sole covering. We had neither
cold nor intrusive visits to fear. Travellers who penetrate into the
wilds of central Africa, and into the pathless forests of the New
World, are obliged to watch over each other by night. But we enjoyed
absolute safety and utter seclusion; no savages or wild beasts
infested these silent depths.
Next morning, we awoke fresh and in good spirits. The road was
resumed. As the day before, we followed the path of the lava. It was
impossible to tell what rocks we were passing: the tunnel, instead of
tending lower, approached more and more nearly to a horizontal
direction, I even fancied a slight rise. But about ten this upward
tendency became so evident, and therefore so fatiguing, that I was
obliged to slacken my pace.
"Well, Axel?" demanded the Professor impatiently.
"Well, I cannot stand it any longer," I replied.
"What! after three hours' walk over such easy ground."
"It may be easy, but it is tiring all the same."
"What, when we have nothing to do but keep going down!"
"Going up, if you please."
"Going up!" said my uncle, with a shrug.
"No doubt, for the last half-hour the inclines have gone the other
way, and at this rate we shall soon arrive upon the level soil of
Iceland."
The Professor nodded slowly and uneasily like a man that declines to
be convinced. I tried to resume the conversation. He answered not a
word, and gave the signal for a start. I saw that his silence was
nothing but ill-humour.
Still I had courageously shouldered my burden again, and was rapidly
following Hans, whom my uncle preceded. I was anxious not to be left
behind. My greatest care was not to lose sight of my companions. I
shuddered at the thought of being lost in the mazes of this vast
subterranean labyrinth.
Besides, if the ascending road did become steeper, I was comforted
with the thought that it was bringing us nearer to the surface. There
was hope in this. Every step confirmed me in it, and I was rejoicing
at the thought of meeting my little Gräuben again.
By mid-day there was a change in the appearance of this wall of the
gallery. I noticed it by a diminution of the amount of light
reflected from the sides; solid rock was appearing in the place of
the lava coating. The mass was composed of inclined and sometimes
vertical strata. We were passing through rocks of the transition or
silurian [1] system.
"It is evident," I cried, "the marine deposits formed in the second
period, these shales, limestones, and sandstones. We are turning away
from the primary granite. We are just as if we were people of Hamburg
going to Lübeck by way of Hanover!"
I had better have kept my observations to myself. But my geological
instinct was stronger than my prudence, and uncle Liedenbrock heard
my exclamation.
Public-domain text, read in full here on John Shaqi.
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