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Published online by Cambridge University Press: 16 March 2015
The absolute westerly declination at Makerstoun, for the mean epoch, June 1844 = 25° 17′·12.
The annual motion of the north end of the needle towards the east = 5′·67.
The annual period of magnetic declination consists of a double oscillation, having nearly the following epochs of maxima and minima.
page 144 note * By maximum is always meant an extreme westerly position of the north end of the needle, and by minimum an extreme easterly (or rather northerly) position.