, he would assuredly
have supposed its internal structure to be altogether regulated by the
lines of bed or cleavage then in sight. Let him, however, wait for
another quarter of an hour, and he will see those lines fade entirely
away as the sun rounds them; and another set, perhaps quite adverse to
them and assuredly lying in another direction, will as gradually become
visible, to die away in their turn, and be succeeded by a third scheme
of structure.
"These 'dissolving views' of the geology of the aiguilles have often
thrown me into despair of ever being able to give any account of their
formation; but just in proportion as I became aware of the infinite
complexity of their framework, the one great fact rose into more
prominent and wonderful relief,--that through this inextricable
complexity there was always manifested _some_ authoritative principle.
It mattered not at what hour of the day the aiguilles were examined, at
that hour they had a system of structure belonging to the moment. No
confusion nor anarchy ever appeared amidst their strength, but an
ineffable order, only the more perfect because incomprehensible. They
differed from lower mountains, not merely in being more compact, but in
being more disciplined.
"For, observe, the lines which cause these far-away effects of shadow,
are not, as often in less noble rocks, caused by real cracks through the
body of the mountain; for, were this so, it would follow, from what has
just been stated, that these aiguilles were cracked through and through
in every direction, and therefore actually weaker, instead of stronger,
than other rocks. But the appearance of fracture is entirely external,
and the sympathy or parallelism of the lines indicates, not an actual
splitting through the rock, but a mere disposition in the rock to split
harmoniously when it is compelled to do so. Thus, in the shell-like
fractures on the flank of the Aiguille Blaitiere, the rock is not
actually divided, as it appears to be, into successive hollow plates. Go
up close to the inner angle between one bed of rock and the next, and
the whole mass will be found as firmly united as a piece of glass. There
is absolutely no crack between the beds,--no, not so much as would allow
the blade of a penknife to enter for a quarter of an inch;[124] but such
a subtle disposition to symmetry of fracture in the heart of the solid
rock, that the next thunderbolt which strikes on that edge of it will
rend away a
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