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" The true cause of the variation of the seasons consists in the inclination of the axis of the earth to the plane of its orbit; or, in other words, to the ecliptic. "
Lectures on Experimental Philosophy, Astronomy, and Chemistry: Intended ... - Page 4
by George Gregory - 1808
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An Elementary Astronomy for Academies and Schools: Illustrated by Numerous ...

Hiram Mattison - Astronomy - 1849 - 290 pages
...and south, and his apparent passage through the plane of the equinoctial, twice a year, are caused by the inclination of the axis of the earth to the plane of the ecliptic, and her revolution around the sun. What we have here said will serve more fully to illustrate Lesson 25,...
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The Complete Works of Thomas Dick, Volume 3

Thomas Dick - Educational sociology - 1850 - 586 pages
...heat of our summer is generally greatest. The true cause of the variation of the seasons consists in the inclination of the axis of the earth to the plane of its orbit ; or, in other words, to the ecliptic. If its axis were perpendicular to the ecliptic, the...
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Encyclopædia Americana: A Popular Dictionary of Arts, Sciences ..., Volume 11

Francis Lieber - Encyclopedias and dictionaries - 1851 - 618 pages
...given time than at others, so that the solar days cannot be equal. Another circumstance, dependent upon the inclination of the axis of the earth to the plane of the ecliptic, is also to be taken into the account. The apparent solar time, therefore, is distinguished from mean...
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Complete dictionary Polish and English

Alexander Chodźko - 1851 - 540 pages
...obliquity ol a line. — ekliptyki, the obliquity of the ecliptic. — osi ziemsktej do ekliptyki, the inclination of the axis of the earth to the plane of the ecliptic.-— crooked back, stooping posture. POCHYtY,A,E,sloping, slanting; inclined; crooked, bent down, stooping....
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A Manual for Joslin's New Solar Telluric Globe, Designed for the Use of ...

Gilman Joslin - 1852 - 54 pages
...curious phenomenon is furnished by PROBLEM III. To show that the changes of the seasons are produced by the inclination of the axis of the earth to the plane of its orbit. Bring the calendar index to the 21st of March ; then turn the base until the axis of the...
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The Complete Works of Thomas Dick, LL. D. ... Eleven Volumes in Two..., Volume 2

Thomas Dick - 1857 - 878 pages
...heat of our summer is generally greatest. The true cause of the variation of the seasons consists in the inclination of the axis of the earth to the plane of its orbit ; or, in other words, to the ecliptic. If its axis were perpendicular to the ecliptic, the...
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Dr. Irving's catechism of general knowledge, by a Cambridge M.A.

Christopher Irving - 1858 - 140 pages
...surface in which the ecliptic is situate. Q. What causes the difference in the seasons of the year *? A. The inclination of the axis of the earth to the plane of the ecliptic. If the earth's axis were perpendicular to the ecliptic the seasons would always be the same, and the...
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Reading lessons, ed. by E. Hughes, Book 4

Edward Hughes - 1858 - 474 pages
...the sun is subject to an annual fluctuation between 234° north and 23i° south, as a consequence of the inclination of the axis of the earth to the plane of the orbit in which it moves. He will have learnt little indeed if he does not know that this is one of...
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A Manual of Information and Suggestions for Object Lessons, in a Course of ...

Marcius Willson - Object-teaching - 1863 - 356 pages
...23° 28'." In Webster's large dictionary it is erroneously stated, under the word "inclination," that "the inclination of the axis of the earth to the plane of the ecliptic is 23° 28'." On the contrary, its axis inclines 23° 28' from a line perpendicular to the plane of...
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A New Manual of the Elements of Astronomy: Descriptive and Mathematical ...

Henry Kiddle - Astronomy - 1868 - 300 pages
...and the difference in the amount of heat received from the sun. 121. The CAUSES OF THE SEASONS are the inclination of the axis of the earth to the plane of its orbit, and its revolution around the sun ; and the vicissitudes are regular, that is, always hhe...
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