Search over 40,000 articles from the original, classic Encyclopedia Britannica, 11th Edition.
See also:DECLINATION (from See also:Lat. declinare, to decline) , in See also:magnetism the See also:angle between true See also:north and magnetic north, i.e. the variation between the true See also:meridian and the magnetic meridian. In 1596 at See also:London the angle of declination was 11° E. of N., in 1652 magnetic north was true north, in 1815 the magnetic See also:needle pointed 241° W. of N., in 1891 18° W., in 1896 17° 56' W. and in 1906 17° 45'. The angle is gradually diminishing and the declination will in See also:time again be o°, when it will slowly increase in an easterly direction, the north magnetic See also:pole oscillating slowly around the North Pole. See also:Regular daily changes of declination also occur. Magnetic storms cause irregular See also:variations sometimes of one or two degrees. (See MAGNETISM, TERRESTRIAL.) In See also:astronomy the declination is the angular distance, as seen from the See also:earth, of a heavenly See also:body from the See also:celestial See also:equator, thus corresponding with terrestrial See also:latitude. End of Article: DECLINATION (from Lat. declinare, to decline)Additional information and CommentsThere are no comments yet for this article.
» Add information or comments to this article.
Please link directly to this article:
Highlight the code below, right click, and select "copy." Then paste it into your website, email, or other HTML. Site content, images, and layout Copyright © 2006 - Net Industries, worldwide. |
|
[back] DECLARATOR |
[next] DECOLOURIZING |