COSMOS, VOL. II - World eBook Library
COSMOS, VOL. II - World eBook Library COSMOS, VOL. II - World eBook Library
DISCOVERIES IN THE CELESTIAL SPACES. 735 two-fold origin of the masses by fusion and solidification, or by precipitation from the waters. The typical character and mmcralogical differences of rocks, or, in, other words, the associations of certain mostly crystallised substances recurring in the most remote regions, are as little made a subject of consideration in the Protogcea as in Hooke's geognostic views. Even in the last-named writer, physical speculations on the action of subterranean forces in earthquakes, in the sudden upheaval of the sea's bottom and of littoral districts, and in the origin of islands and mountains, hold a prominent place. The nature of the organic remains of a former world even led him to conjecture that the temperate zone must originally have enjoyed the heat of a tropical climate. It still remains for us to speak of the greatest of all geognostic phenomena, the mathematical figure of the earth, in which we distinctly trace a reflection of the primitive world in the condition of fluidity of the rotating mass, and The main out- its solidification into our terrestrial spheroid. lines of the figure of the earth were sketched as early as the. close of the seventeenth century, although the relation between the polar and equatorial axes was not ascertained with numerical exactness. Picard's measurement of a degree, made in 1670 with instruments which he had himself improved, is so much the more important, since it was the means of inducing Newton to resume with renewed zeal his theory of gravitation, (which he discovered as early as 1666, but had subsequently neglected,) by offering to that profound and successful investigator, the means of proving how the attraction of the earth maintained the moon in its orbit, whilst urged on its course by the centrifugal force. The fact of the compression of the poles of Jupiter, which was much earlier recognised,* had, as it is supposed, induced Newton to reflect on the causes of a form which deviated so con- siderably from sphericity. The experiments on the actual length of the seconds pendulum by Richer at Cayenne in 1673, and by Varin on the western coast of Africa, had been preceded by others of less decisive character, prosecuted in London, Lyons, and Bologna, at a difference of 7 of latitude.f * Cosmos, p. 156. t Delambre ; Hist, de I'Astronomie mod. t. ii, p. 601
736 COSMOS. The decrease of gravity from the poles to the equator, which even Picard had long denied, was now generally admitted. Newton recognised the polar compression, and the of its rotation ; spheroidal form of the earth as a consequence and he even vetured to determine numerically the amount of this compression, on the assumption of the homogeneous nature of the mass. It remained for the comparative measurements of degrees in the eighteenth and nineteenth centuries, at the equator, near the north pole, and in the tem- perate zones of both the southern and northern hemispheres, to determine exactly the mean amount of this compression, and by that means to ascertain the true figure of the earth. The existence of this compression announces, as has already been observed in the " Picture of Nature,"* that which may be named the most ancient of all geognostic events, the con- dition of general fluidity of a planet, and its earlier and pro- gressive solidification. We began our description of the great epoch of Galileo, Kepler, Newton, and Leibnitz, with the discoveries in the regions of space by means of the newly invented tele- scope, and we now close it with the figure of the earth, as it was then recognised from theoretical conclusions. " Newton was enabled to give an explanation of the system of the universe, because he succeeded in discovering the force,f from whose action the laws of Kepler necessarily result, and which most correspond with these phenomena since these, laws corresponded to and predicted them." The discovery of such a force, the existence of which Newton has developed in his immortal work, the Principia, (which comprise the general sciences of nature) was almost simultaneous with the opening of the new paths to greater mathematical * Cosmos, p. 154. The dispute regarding priority as to the knowledge of the earth's compression, in reference to a memoir read by Huygens, in!669, before the Paris Academy, was first cleared up by Delambre in his Hist, de I'Astr. mod. t. i. p. lii. and t. ii. p. 558. Richer's return, to Europe occurred indeed in 1673, but his work was not printed until 1679 and as ; Huygens left Paris in 1682, lie did not write the Additamentum to the Memoir of 1669, the publication of which was very late, until he had already before his eyes the results of liicher's Pen- dulum Experiments, and of Newton's great work, ralis Principia Mathematica. Philosophies f Bessel, in ScJmmacher's JaJt.rbuchfur 1843, s. 32.
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736 <strong>COSMOS</strong>.<br />
The decrease of gravity from the poles to the equator,<br />
which even Picard had long denied, was now generally<br />
admitted. Newton recognised the polar compression, and the<br />
of its rotation ;<br />
spheroidal form of the earth as a consequence<br />
and he even vetured to determine numerically the amount of<br />
this compression, on the assumption of the homogeneous<br />
nature of the mass. It remained for the comparative measurements<br />
of degrees in the eighteenth and nineteenth centuries,<br />
at the equator, near the north pole, and in the tem-<br />
perate zones of both the southern and northern hemispheres,<br />
to determine exactly the mean amount of this compression,<br />
and by that means to ascertain the true figure of the earth.<br />
The existence of this compression announces, as has already<br />
been observed in the " Picture of Nature,"* that which may<br />
be named the most ancient of all geognostic events, the con-<br />
dition of general fluidity of a planet, and its earlier and pro-<br />
gressive solidification.<br />
We began our description of the great epoch of Galileo,<br />
Kepler, Newton, and Leibnitz, with the discoveries in the<br />
regions of space by means of the newly invented tele-<br />
scope, and we now close it with the figure of the earth, as it<br />
was then recognised from theoretical conclusions.<br />
" Newton<br />
was enabled to give an explanation of the system of the<br />
universe, because he succeeded in discovering the force,f<br />
from whose action the laws of Kepler necessarily result, and<br />
which most correspond with these phenomena since these,<br />
laws corresponded to and predicted them." The discovery<br />
of such a force, the existence of which Newton has<br />
developed in his immortal work, the Principia, (which comprise<br />
the general sciences of nature) was almost simultaneous<br />
with the opening of the new paths to greater mathematical<br />
* Cosmos, p. 154. The dispute regarding priority as to the knowledge<br />
of the earth's compression, in reference to a memoir read by Huygens,<br />
in!669, before the Paris Academy, was first cleared up by Delambre<br />
in his Hist, de I'Astr. mod. t. i. p. lii. and t. ii. p. 558. Richer's return,<br />
to Europe occurred indeed in 1673, but his work was not printed until<br />
1679 and as ; Huygens left Paris in 1682, lie did not write the Additamentum<br />
to the Memoir of 1669, the publication of which was very<br />
late, until he had already before his eyes the results of liicher's Pen-<br />
dulum Experiments, and of Newton's great work,<br />
ralis Principia Mathematica.<br />
Philosophies<br />
f Bessel, in ScJmmacher's JaJt.rbuchfur 1843, s. 32.