Science for the School and Family, Part I. Natural PhilosophyHooker, Worthington
Science
Science for the School and Family, Part I. Natural Philosophy
Hooker, Worthington
Physics; Science
406. =Declination of the Needle.=--The declination of the needle is
its deviation from a north and south line. It is in comparatively
few parts of the earth's surface that there is no deviation from
this line to the east or the west. "True as needle to the pole" has
become a proverb, and when it was first uttered it was supposed
to be founded in strict truth; but modern investigation has shown
not only that the needle varies in its pointing in different
localities, but that it varies to some little degree in its
variations. The declination of the needle was first observed by
Columbus in his first voyage of discovery, and it occasioned great
alarm among the sailors, who, as Irving states, "thought the laws
of nature were changing, and that the compass was about to lose its
mysterious power." Notwithstanding these and other observations of
a similar character, no great account was made of the declination
of the needle till the middle of the seventeenth century. But
since that time extensive records of its declinations at different
localities have been made, and tables and charts have been
constructed exhibiting them. These declinations are not constant,
but vary somewhat every day, from the influence, it is supposed, of
the sun upon the earth.
407. =Dip of the Needle.=--It is found that in most parts of the
earth, if a needle be balanced before it is magnetized, and then
be suspended from the same point, it will not be balanced, but
one end will dip downward. This fact was discovered by Norman,
a London optician, in 1576. He found that the dip at London was
toward the north at an angle of 72°. In pursuing the investigation
of this phenomenon it was found that going from the north toward
the equator the dip constantly lessened, until a point was reached
where the needle was horizontal. Then, on going south of this, a
reverse dip occurred, that of the south pole, and the farther
south the needle was carried the greater was the dip. In the north,
Captain Ross in 1832 came to a locality north of Hudson's Bay, in
lat. 70° 5′ N., long. 96° 45′ W., where the magnetic needle, freely
suspended, was in a vertical line. No such locality has yet been
discovered toward the south pole.
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