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But look now, not explained in the same way, except thesethe most outstanding features of the Solar system, and otherssecondary. Let's start with the correlation between the planes of the planetary orbits andthe plane of the solar equator If at the time when the nebulous spheroidsubstances extended beyond the orbit of Neptune, all parts rotate inexactly the same plane, or rather in parallel planes; ifwould all its parts have the same axis, the plane of the rings serialwould coincide one with the other and with the plane of solar rotation. But enoughremember the early days of a thickening misty masses to understand that thiskind of perfect uniformity of motion could not exist. The flakes which,as we have said, was settled from the wrong, far scattered inthe space of the foggy mass, and with all points rushed to the Generalhis center of gravity had to move not in one plane, butcountless planes that intersect one another underall angles. The gradual establishment of that rotational motion,which, as we now see, pointed to the spiral nebulae, gradual approach to motion in one plane. But this plane canbe determined only over time. Those flakes which do not rotate in thisplane but are in between weight from various angles, willto strive to make its rotation around its center, each in itsplane, and only over time their movement will be partly destroyedthe opposite movements, partly merge with the General movement. Infeatures will long retain its more or less independentthe direction of those parts of a rotating mass is located on the outskirts ofit. That's why most likely, that the plane of the rings, the separated firstothers will vary considerably from the average plane of the entire mass, betweenthe plane of those rings, which are separated later will differ fromit less. Here again the conclusion is very much in line withobservation.
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