The Old Red Sandstone; or, New Walks in an Old Field
John Stuart Mill · en
One remark in the passing: it may teach the young geologist to be
cautious in his inferences, and illustrate, besides, those gaps
which occur in the geological scale. I had now discovered the
ichthyolite beds in five different localities; in one of these--the
first discovered--there is no overlying stratum; it seems as if
the bed formed the top of the formation: in all the others the
overlying stratum is different, and belongs to distant and widely
separated ages. We cut in one locality through a peat moss--part of
the ruins, perhaps, of one of those forests which covered, about the
commencement of the Christian era, well nigh the entire surface of
the island, and sheltered the naked inhabitants from the legions of
Agricola. We find, as we dig, huge trunks of oak and elm, cones of
the Scotch fir, handfuls of hazel-nuts, and bones and horns of the
roe and the red deer. The writer, when a boy, found among the peat
the horn of a gigantic elk. And, forming the bottom of this recent
deposit, and _lying conformably to it_, we find the ichthyolite
beds, with their antique organisms. The remains of oak and elm
leaves, and of the spikes and cones of the pine, lie within half
a foot of the remains of the _Coccosteus_ and _Diplopterus_. We
dig in another locality through an ancient burying-ground; we pass
through a superior stratum of skulls and coffins, and an inferior
stratum, barren in organic remains, and then arrive at the stratified
clays, with their ichthyolites. In a third locality we find these in
junction with the Lias, and underlying its lignites, ammonites, and
belemnites, just as we see them underlying, in the other two, the
human bones and the peat moss. And in yet a fourth locality we see
them overlaid by immense arenaceous beds, that belong evidently, as
their mineralogical character testifies, to either the Old or the
New Red Sandstone. The convulsions and revolutions of the geological
world, like those of the political, are sad confounders of place
and station, and bring into close fellowship the high and the low;
nor is it safe in either world,--such have been the effects of the
disturbing agencies,--to judge of ancient relations by existing
neighborhoods, or of original situations by present places of
occupancy. "Misery," says Shakspeare, "makes strange bedfellows."
The changes and convulsions of the geological world have made strange
bedfellows too. I have seen fossils of the Upper Lias and of the
Lower Old Red Sandstone washed together by the same wave, out of
what might be taken, on a cursory survey, for the same bed, and then
mingled with recent shells, algæ, branches of trees, and fragments of
wrecks on the same sea-beach.