British Quarterly Review, American Edition, Vol. LIV: July and October, 1871Various
History
British Quarterly Review, American Edition, Vol. LIV: July and October, 1871
Various
English periodicals
In other planets, he urged, the same form is due manifestly to the
action of the same law. Venus, Mars, Saturn, oblate spheroids all,
have been similarly 'spun out by their rotatory motion in exactly the
line in which, as in the earth, that motion is greatest.' In these,
however, we can only approximately determine the lengths of the
equatorial and polar diameters; 'in one great planet, Jupiter, we can
ascertain them scarce less exactly than our own earth;' and Jupiter's
equatorial diameter bears exactly that proportion to his polar
diameter which 'the integrity of the law,' as exemplified in the
relation between the equatorial and polar diameters of the earth
demands. 'Here, then,' proceeds Miller, 'is demonstration that the
oblate sphericity of the earth is a consequence of the earth's diurnal
motion on its axis; nor is it possible that it could have received
this form when in a solid state.'
Sir Charles Lyell holds that the excess of the equatorial diameter
over the polar may be accounted for on uniformitarian principles. 'The
statical figure,' he says, 'of the terrestrial spheroid (of which the
longest diameter exceeds the shortest by about twenty-five miles), may
have been the result of gradual and even of existing causes, and not
of a primitive, universal, and simultaneous fluidity.' Miller denies
this possibility; and we confess that the passage in which he assails
the position of Sir Charles Lyell appears to us to have great force.
Let us hear him:--
'The laws of deposition are few, simple, and well known.
The denuding and transporting agencies are floods, tides,
waves, icebergs. The sea has its currents, the land its
rivers; but while some of these flow from the poles towards
the equator, others flow from the equator towards the poles
uninfluenced by the rotatory motion; and the vast depth and
extent of the equatorial seas show that the ratio of
deposition is not greater in them than in the seas of the
temperate regions. We have, indeed, in the Arctic and
Antarctic currents, and the icebergs which they bear,
agents of denudation and transport permanent in the present
state of things, which bring detrital matter from the
higher towards the lower latitudes; but they stop far short
of the tropics; they have no connection with the rotatory
motion; and their influence on the form of the earth must
be infinitely slight; nay, even were the case otherwise,
instead of tending to the formation of an equatorial ring,
they would lead to the production of two rings widely
distant from the equator. And, judging from what appears,
we must hold that the laws of Plutonic intrusion or
upheaval, though more obscure than those of deposition,
operate quite as independently of the earth's rotatory
motion. Were the case otherwise, the mountain systems of
the world, and all the great continents, would be clustered
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