I even thought, after some examination, that we were actually tending
upwards. About ten o'clock in the day this state of things became so
clear that, finding the change very fatiguing, I was obliged to slacken
my pace and finally come to a halt.
"Well," said the Professor quickly, "what is the matter?"
"The fact is, I am dreadfully tired," was my earnest reply.
"What," cried my uncle, "tired after a three hours' walk, and by so easy
a road?"
"Easy enough, I dare say, but very fatiguing."
"But how can that be, when all we have to do is to go downwards."
"I beg your pardon, sir. For some time I have noticed that we are going
upwards."
"Upwards," cried my uncle, shrugging his shoulders, "how can that be?"
"There can be no doubt about it. For the last half hour the slopes have
been upward--and if we go on in this way much longer we shall find
ourselves back in Iceland."
My uncle shook his head with the air of a man who does not want to be
convinced. I tried to continue the conversation. He would not answer me,
but once more gave the signal for departure. His silence I thought was
only caused by concentrated ill-temper.
However this might be, I once more took up my load, and boldly and
resolutely followed Hans, who was now in advance of my uncle. I did not
like to be beaten or even distanced. I was naturally anxious not to lose
sight of my companions. The very idea of being left behind, lost in that
terrible labyrinth, made me shiver as with the ague.
Besides, if the ascending path was more arduous and painful to clamber,
I had one source of secret consolation and delight. It was to all
appearance taking us back to the surface of the earth. That of itself
was hopeful. Every step I took confirmed me in my belief, and I began
already to build castles in the air in relation to my marriage with my
pretty little cousin.
About twelve o'clock there was a great and sudden change in the aspect
of the rocky sides of the gallery. I first noticed it from the
diminution of the rays of light which cast back the reflection of the
lamp. From being coated with shining and resplendent lava, it became
living rock. The sides were sloping walls, which sometimes became quite
vertical.
We were now in what the geological professors call a state of
transition, in the period of Silurian stones, so called because this
specimen of early formation is very common in England in the counties
formerly inhabited by the Celtic nation known as Silures.
"I can see clearly now," I cried; "the sediment from the waters which
once covered the whole earth formed during the second period of its
existence these schists and these calcareous rocks. We are turning our
backs on the granite rocks, and are like people from Hamburg who would
go to Lubeck by way of Hanover."
I might just as well have kept my observations to myself. My geological
enthusiasm got the better, however, of my cooler judgment, and Professor
Hardwigg heard my observations.
Public-domain text, read in full here on John Shaqi.
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