Page:Scientific Memoirs, Vol. 2 (1841).djvu/209

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TERRESTRIAL MAGNETISM.
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than a given value , It is clear that may either be one connected surface or several detached spaces, and that , on the bounding lines or lines which separate from other parts where is less than ; by increasing or diminishing , we enlarge or contract the space .

Now let us assume to be a second point of similar properties to so that at it also may have a maximum value . As according to what has been before noticed, may have a value less than , and differing from it by so small an amount that shall fall outside that part of in which is situated; then if we arrange (as we may do) that shall not be less than , it will be greater than , and will necessarily also belong to a part of . Thus and will both be situated in , but in separate portions of it. On the other hand, it is evident that may be taken so small that and shall both be situated in one connected part of ; for by only taking small enough, may be made to embrace the whole surface of the earth.

If then be made to pass progressively through all the values between the first and the second values spoken of, there must be amongst them one which we will call , characterised by being the lowest at which and are still situated in separate portions of , which separate portions will unite whenever is diminished further.

If this union occur at a point , the bounding line on which will have the form of an , crossing at that point; where also we may easily satisfy ourselves that the horizontal intensity must . In fact, the crossing either does or does not take place under an angle of sensible amount.

In the first case, the horizontal force, if it be not , must be directed in the normal to the two different tangents, which is absurd; in the second case, in which the two halves of the touch each other at , or would have the same tangent, the force normal to this tangent could only be directed towards the interior of one half surface of the , which involves a contradiction, as the value of increases towards both sides; therefore is a true magnetic pole according to our definition, but must be considered as a south pole as regards the points nearest to it inside the two openings of the , and as a north pole as regards the points which lie outside. Figure 1. illustrates this form of the system of lines.