For the first time in his life, perhaps, in passing along the
Canongate, he did NOT TURN TO LOOK AT HOLYROOD, the palace
of the former sovereigns of Scotland. He did not notice the sentinels
who stood before its gateways, dressed in the uniform of their.Highland regiment, tartan
kilt, plaid and sporran complete. His
whole thought was to reach Callander where Harry Ford was
supposedly awaiting him.
The better to understand this narrative, it will be as well to hear
a few words on the origin of coal. During the geological epoch,
when the terrestrial spheroid was still in course of formation, a
thick atmosphere surrounded it, saturated with watery vapors, and
copiously impregnated with carbonic acid. The vapors gradually
condensed in diluvial rains, which fell as if they had leapt from the
necks of thousands of millions of seltzer water bottles. This liquid,
loaded with carbonic acid, rushed in torrents over a deep soft soil,
subject to sudden or slow alterations of form, and maintained in its
semi-fluid state as much by the heat of the sun as by the fires of
the interior mass. The internal heat had not as yet been collected
in the center of the globe. The terrestrial crust, thin and
incompletely hardened, allowed it to spread through its pores. This
caused a peculiar form of vegetation, such as is probably produced
on the surface of the inferior planets, Venus or Mercury, which
revolve nearer than our earth around the radiant sun of our system.
The soil of the continents was covered with immense forests.
Carbonic acid, so suitable for the development of the vegetable
kingdom, abounded. The feet of these trees were drowned in a sort
of immense lagoon, kept continually full by currents of fresh and
salt waters. They eagerly assimilated to themselves the carbon
which they, little by little, extracted from the atmosphere, as yet
unfit for the function of life, and it may be said that they were
destined to store it, in the form of coal, in the very bowels of the
earth.
It was the earthquake period, caused by internal convulsions,
which suddenly modified the unsettled features of the terrestrial
surface. Here, an intumescence which was to become a mountain,
there, an abyss which was to be filled with an ocean or a sea.
There, whole forests sunk through the earth's crust, below the
unfixed strata, either until they found a resting-place, such as the
primitive bed of granitic rock, or, settling together in a heap, they
formed a solid mass.
As the waters were contained in no bed, and were spread over
every part of the globe, they rushed where they liked, tearing from
the scarcely-formed rocks material with which to compose schists,
sandstones, and limestones. This the roving waves bore over the
submerged and now peaty forests, and deposited above them the
elements of rocks which were to superpose the coal strata. In
course of time, periods of which include millions of years, these.earths hardened in layers,
and enclosed under a thick carapace of
pudding-stone, schist, compact or friable sandstone, gravel and
stones, the whole of the massive forests.
And what went on in this gigantic crucible, where all this
vegetable matter had accumulated, sunk to various depths? A
regular chemical operation, a sort of distillation. All the carbon
contained in these vegetables had agglomerated, and little by little
coal was forming under the double influence of enormous pressure
and the high temperature maintained by the internal fires, at this
time so close to it.
Thus there was one kingdom substituted for another in this slow
but irresistible reaction. The vegetable was transformed into a