INCLINATION OF THE AXIS.

By whatever means the two planes first became permanently inclined, we

see that it is a necessary consequence of the admission of these

principles, not only that the axis of the vortex should be drawn aside

by the momentum of the earth and moon, ever striving, as it were, to

maintain a dynamical balance in the system, in accordance with the

simple laws of motion, and ever disturbed by the action of gravitation

exerted on the grosser matter of the system; but also, that this axis

should follow, the axis of the lunar orbit, at the same mean

inclination, during the complete revolution of the node. The mean

inclination of the two axes, determined by observation, is 2d 45', and

the monthly equation, at a maximum, is about 15', being a plus

correction in the northern hemisphere, where the moon is between her

descending and ascending node, reckoned on the plane of the vortex, and

a minus correction, when between her ascending and descending node. And

the mean longitude of the node will be the same as the true longitude of

the moon's orbit node,--the maximum correction for the true longitude

being only about 5d +/-.

[Illustration: Fig. 7]

In the following figure, P is the pole of the earth; E the pole of the

ecliptic; L the pole of the lunar orbit; V the mean position of the pole

of the vortex at the time; the angle [ARIES]EL the true longitude of the

pole of the lunar orbit, equal to the _true_ longitude of the ascending

node +/- 90d. VL is therefore the mean inclination +/- 2d 45'; and the

little circle, the orbit described by the pole of the vortex _twice_ in

each sidereal revolution of the moon. The distance of the pole of the

vortex from the mean position V, may be approximately estimated, by

multiplying the maximum value 15' by the sine of twice the moon's

distance from the node of the vortex, or from its mean position, viz.:

the true longitude of the ascending node of the moon on the ecliptic.

From this we may calculate the true place of the node, the true

obliquity, and the true inclination to the lunar orbit. Having indicated

the necessity for this correction, and its numerical coefficient, we

shall no longer embarrass the computation by such minutiae, but consider

the mean inclination as the true inclination, and the mean place of the

node as the true place of the node, and coincident with the ascending

node of the moon's orbit on the ecliptic.

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