408 Mr. Mallet's Notice of the British Earthquake of November 9, 1852. 



the region of shock for tlie day of the earthquake, and for the one preceding 

 and following. The results are given in the subjoined Table. 



Meteorological Table, referring to the British Earthquake of November 9, 1852, 



for five princijMl Stations. 



These results confirm the view (so far provisionally) deducible from all 

 earthquakes, namely, that meteorological phenomena have probably no true 

 causative connexion -with these disturbances, although they are often acted on 

 and modified by the secondary efiects due and subsequent to earthquakes. 



