Page:A Voyage of Discovery and Research in the Southern and Antarctic Regions Vol 2.djvu/490

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, in his General Theory of Terrestrial Magnetism, states, that "the exact computation of the places of these two poles, according to our elements, gives them as follows:—

"1. In 73° 35′ north latitude, and 95° 39′ west longitude from Greenwich, the total intensity being 1.701 on the unity in common use.

"2. In 72° 35′ south latitude, and 152° 30′ east longitude, the total intensity 2.253.

"According to Captain James Ross's observation, the north magnetic pole falls 3° 35′ to the south of its position, according to our calculation, which gives at that place a direction of the magnetic force differing 1° 12′ from observation, as may be seen in the table of comparisons. We must expect a considerably greater displacement of the position of the southern pole. At Hobart Town, which is the nearest station to this pole, calculation gives too low a dip by 3° 38′, as far as the observation can be depended upon. It seems probable, therefore, that the actual south magnetic pole is considerably to the north of the position given by our calculation; and that it may be looked for in about 66° S. latitude, and 146° E. longitude."

It was this last paragraph in which M. Gauss infers the place of the south magnetic pole, that was the occasion of my instructions directing me to seek it in latitude 66° S., rather than in the position which M. Gauss's theory places