of the Barometer near Edinburgh. 



173 



CONVENT OF THE GRAND ST BERNARD. 



It can hardly require a word from me to point out how well 



the individual results justify the deductions of the mean, so that 



there are only three results in the summer period, and only 



five + in the winter one ; therefore, instead of an oscillation 



corresponding to the Temperate Zone in summer, and to the 



VOL. XII. PART I. Z 



