hope in this. Every step confirmed me in it, and I was rejoicing at the thought of meeting my little Gräuben again.
By midday 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 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.
“What’s that you are saying?” he asked.
“See,” I said, pointing to the varied series of sandstones and limestones, and the first indication of slate.
“Well?”
“We are at the period when the first plants and animals appeared.”
“Do you think so?”
“Look close, and examine.”
I obliged the Professor to move his lamp over the walls of the gallery. I expected some signs of astonishment; but he spoke not a word, and went on.