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A compass points north because it is attracted to the south pole of earth's magnet | | | | | | |
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Comparison between the placement of the Magnetic Poles and the Geographical Poles |
The earth is a giant magnet in which there is a north pole and south
pole. In geograpghy class, students are taught geographical north and
south poles where the north pole is at
the top and the south pole is at the bottom of the earth. The "north"
and "south" poles of the earth gives people direction and therefore, are
given the names true north and true south. On the contrary, magnets
have a north and south poles in which north is attracted to south and
south is attracted to north. Therefore if a compass points north, the
compass is actually attracted to the south magnetic pole of the earth.
In actuality, with the science and physics of a magnet, the poles of
earth are switched and the north pole is the south pole of a magnetic
and the south pole is the north pole of a magnetic. These scientific
poles are called magnetic south, which is the north pole, and magnetic
north, which is the south pole. It can also be called Earth's south and
Earth's north. But how can people differentiate between these two and
which one is more reliable than the other? Geographical/ true north
& south are more reliable because they are situated at the top and
bottom of the earth unlike magnetic/ Earth's north & south, which is
tilted at an angle and continues to tilt and change angles. In summary,
in a geographical sense, the north pole is called the
geographical north and the south pole is called the geographical south.
Opposites attract so if the compass points north, that means it is
attracted to a south charge therefore the north pole is actually
magnetic south or Earth's south and the south pole is magnetic north or
Earth's north.
Magnets can also lose their north and
south magnetic properties when they are heated, therefore the Earth's
inner core does not have magnetic forces. Although, one theory believes
that the inner core, composed of liquid iron, eletrically conducts the
magnetic properties of earth's pole. Additionally, it is at the equator that the magnetic field
is perfectly parallel to earth's surface, the angle of difference
between other areas, other than the equator, is called magnetic
declination.
Works Cited
Castleman, A. (2008, February 28). The Earth Has More
Than One North Pole: Scientific American. Science News, Articles and
Information | Scientific American. Retrieved February 25, 2012, from
http://www.scientificamerican.com/article.cfm?id=the-earth-has-more-than-one-north-pole
Mista, C. (2011, November 23). This is a password
protected video on Vimeo. Vimeo, Video Sharing For You. Retrieved
February 25, 2012, from http://vimeo.com/29641648
Russell, R. (2009, April 17). Earth's North Magnetic Pole.
Windows to the Universe. Retrieved February 25, 2012, from
http://www.windows2universe.org/earth/Magnetosphere/earth_north_magnetic_pole.html