An introduction to astronomy: designed as a text-book for the use of students in college. By Denison Olmsted ...

20 THE EARTH. and less, and consequently the motions of the heavenly bodies more and more oblique, until finally, at the pole, where the latitude is 90~, the angle of elevation of the equator vanishes, and the horizon and the equator coincide with each other, as before stated. 5 4. The CIRCLE OF PERPETUAL APPARITION/ is the boundary of that space around the elevated pole, where the stars never set. Its distance from the pole is equal to the latitude of the place. For, since the altitude of the pole is equal to the latitude, a star whose polar distance is just equal to the latitude, will, when at its lowest point, only just reach the horizon; and all the stars nearer the pole than this will evidently not descend so far as the horizon. Thus, mm (Fig. 5), is the circle of perpetual apparition, between which and the north pole, the stars never set, and its distance from the pole OP is evidently equal to the elevation of the pole, and of course to the latitude. 55. In the opposite hemisphere, a similar part of the sphere adjacent to the depressed pole never rises. Hence, The CIRCLE OF PERPETUAL OCCULTATION, is the boundary of that space around the depressed pole, within which the stars never rise. Thus, m'm' (Fig. 5), is the circle of perpetual occultation, between which and the south pole the stars never rise. 56. In an oblique sphere, the horizon cuts the circles of daily motion unequally. Towards the elevated pole, more than half the circle is above the horizon, and a greater and greater portion as the distance from the equator is increased, until finally, within the circle of perpetual apparition, the whole circle is above the horizon. Just the opposite takes place in the hemisphere next the depressed pole. Accordingly, when the sun is in the equator, as the equator and horizon, like all other great circles of the sphere, bisect each other, the days and nights are equal all over the globe. But when the sun is north of the equator, our days become longer than our nights, but shorter when the sun is south of the equator. Mloreover, the higher the latitude, the greater is the inequality in the

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Title
An introduction to astronomy: designed as a text-book for the use of students in college. By Denison Olmsted ...
Author
Olmsted, Denison, 1791-1859.
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Page 20
Publication
New York,: Collins & brother,
1865.
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Astronomy

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"An introduction to astronomy: designed as a text-book for the use of students in college. By Denison Olmsted ..." In the digital collection Making of America Books. https://name.umdl.umich.edu/ajn0587.0001.001. University of Michigan Library Digital Collections. Accessed June 7, 2025.
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