A Journey to the Interior of the Earth HTML version

Total Failure Of Water
This time the descent commenced by the new gallery. Hans walked first as was his
We had not gone a hundred yards when the Professor, moving his lantern along the walls,
"Here are primitive rocks. Now we are in the right way. Forward!"
When in its early stages the earth was slowly cooling, its contraction gave rise in its crust
to disruptions, distortions, fissures, and chasms. The passage through which we were
moving was such a fissure, through which at one time granite poured out in a molten
state. Its thousands of windings formed an inextricable labyrinth through the primeval
As fast as we descended, the succession of beds forming the primitive foundation came
out with increasing distinctness. Geologists consider this primitive matter to be the base
of the mineral crust of the earth, and have ascertained it to be composed of three different
formations, schist, gneiss, and mica schist, resting upon that unchangeable foundation,
the granite.
Never had mineralogists found themselves in so marvellous a situation to study nature in
situ. What the boring machine, an insensible, inert instrument, was unable to bring to the
surface of the inner structure of the globe, we were able to peruse with our own eyes and
handle with our own hands.
Through the beds of schist, coloured with delicate shades of green, ran in winding course
threads of copper and manganese, with traces of platinum and gold. I thought, what
riches are here buried at an unapproachable depth in the earth, hidden for ever from the
covetous eyes of the human race! These treasures have been buried at such a profound
depth by the convulsions of primeval times that they run no chance of ever being
molested by the pickaxe or the spade.
To the schists succeeded gneiss, partially stratified, remarkable for the parallelism and
regularity of its lamina, then mica schists, laid in large plates or flakes, revealing their
lamellated structure by the sparkle of the white shining mica.
The light from our apparatus, reflected from the small facets of quartz, shot sparkling
rays at every angle, and I seemed to be moving through a diamond, within which the
quickly darting rays broke across each other in a thousand flashing coruscations.
About six o'clock this brilliant fete of illuminations underwent a sensible abatement of
splendour, then almost ceased. The walls assumed a crystallised though sombre
appearance; mica was more closely mingled with the feldspar and quartz to form the