The Properties of Magnets
                
                  
                  Table of Contents
                
                
              
              145. The properties of magnetic force
The magnetic properties usually noted by their admirers are the following.
- There are 2 poles in a magnet
 
- one is everywhere directed towards the Earth’s northern pole
 - the other towards the southern pole.
 
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These magnetic poles incline in various ways towards its center, depending on their different places on the earth.
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If 2 magnets are spherical, one turns towards the other in the same way as each of them turns towards the Earth.
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After they have thus met, let them go to the opposite side.
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But if they are detained in the opposite situation, they should flee from each other.
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But if a magnet is divided by a plane, lines drawn parallel through its poles, the parts of the segments, which were previously joined, also repel each other
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But if it is divided by a plane, cutting a line drawn through the poles at right angles, 2 points must first be contiguous to the poles of opposite virtue, one in one, the other in another segment.
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One magnet only has 2 poles, one southern, the other northern.
 
Yet in each one of its fragments, 2 similar poles are also found; insomuch that his power, in so far as it is seen to be different by reason of the poles, is the same in any part and in the whole.
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The iron receives this force from the magnet only when it is moved to it.
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The magnet receives the iron in various ways.
 
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An oblong iron, in any way moved by a magnet, always receives it according to its length.
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A magnet loses nothing of its own power, although it shares it with steel.
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Steel is quickly united with the iron magentically.
 
But the longer the time passes, the steel is more strengthened in it.
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The hardest steel will receive iron more and will hold it more steadily than the lighter iron.
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More is communicated to it by a more perfect magnet, than by a less perfect one.
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The earth itself is also strong. It shares something of its own with iron.
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This force in the Earth, the greatest magnet, appears less strong than in most other lesser ones.
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That a needle, touched by a magnet, turns its ends towards the earth in the same way as the poles of the magnets.
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That they do not turn exactly towards the poles of the Earth, but in various places they deviate from them.
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That this decline may change with time.
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That there is nothing, as some say, or perhaps that it is neither the same nor so great, in a magnet erected perpendicularly above one of its poles, as in one whose poles are equally distant from the earth.
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That magnet draws iron.
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That armed magnets can withstand much more iron than bare ones.
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That its poles, although opposite, help each other in turn to support the same iron.
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The rotation of an iron roller, suspended by a magnet, in either direction is not hindered by the magnetic force.
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That the force of one magnet may be variously increased or diminished, by the application of various other magnets or of iron to it.
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That a magnet, however strong it may be, cannot draw back iron, removed from it, by the contact of another weaker magnet.
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As against a weak magnet, or a small piece of iron, /287/ it often separates another piece of iron contiguous to it from a stronger magnet.
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That the pole of the magnet, which we call Southern, supports more iron in these Boreal regions than that which we call Boreal.
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The filing of iron around one or more magnets arranges itself in certain ways.
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That the iron plate, attached to the pole of the magnet, deflects the force of the iron being drawn or turned.
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That the same should not be hindered by the interposition of any other body.
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A magnet remaining turned towards the Earth or other neighboring magnets in a different way than it would turn spontaneously, if there were nothing to hinder its motion, loses its force with the success of time.
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These things are also diminished by rust, humidity, and situation, and are removed by fire; but not by any other reason known to us.