Light Science for Leisure Hours: A series of familiar essays on scientific subjects, natural phenomena, &c.Proctor, Richard A. (Richard Anthony)
Science
Light Science for Leisure Hours: A series of familiar essays on scientific subjects, natural phenomena, &c.
Proctor, Richard A. (Richard Anthony)
Science
It has, indeed, been well pointed out by Sir Charles Lyell that ‘the
general tendency of subterranean movements, when their effects are
considered for a sufficient lapse of ages, is eminently beneficial,
and that they constitute an essential part of that mechanism by which
the integrity of the habitable surface is preserved. Why the working
of this same machinery should be attended with so much evil, is a
mystery far beyond the reach of our philosophy, and must probably
remain so until we are permitted to investigate, not our planet alone
and its inhabitants, but other parts of the moral and material universe
with which they may be connected. Could our survey embrace other
worlds, and the events, not of a few centuries only, but of periods
as indefinite as those with which geology renders us familiar, some
apparent contradictions might be reconciled, and some difficulties
would doubtless be cleared up. But even then, as our capacities are
finite, while the scheme of the universe must be infinite, both in time
and space, it is presumptuous to suppose that all sources of doubt and
perplexity would ever be removed. On the contrary, they might, perhaps,
go on augmenting in number although our confidence in the wisdom of the
plan of nature might increase at the same time; for it has been justly
said’ (by Sir Humphry Davy) ‘that the greater the circle of light, the
greater the boundary of darkness by which it is surrounded.’
(From the _Cornhill Magazine_, March 1868.)
_THE EARTHQUAKE IN PERU._
The intelligence published last Saturday (see date of article) is
sufficient to prove that the great earthquake which has devastated
Peru fully equalled, if it did not surpass, the most terrible
catastrophes which have ever befallen that country. It presents, too,
all the features which have hitherto characterised earthquakes in this
neighbourhood. These are well worthy of careful study, and appear to
have an important bearing on the modern theory of earthquakes.
It has been commonly held that the seat of disturbance in the
earthquakes which have shaken the country west of the Andes has lain
always at some point or other beneath that range of mountains. The
fact that several large volcanoes are found in the Cordilleras has
seemed confirmatory of this view. The account we have also of the great
earthquake at Riobamba in 1797, seems only explicable by supposing
that the seat of disturbance lay almost immediately beneath that city.
The inhabitants were flung vertically upwards into the air, and to
such a height that Humboldt found the skeletons of many of them on the
summit of the hill La Culca, on the farther side of the small river on
which Riobamba is built. The ruins of many houses were also flung to
the same spot. Here, therefore, was evidence of that vertical (or, as
Humboldt expresses it, explosive) force which is only to be looked for
immediately above the centre of concussion.
Public-domain text, read in full here on John Shaqi.
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