i , /«Zr^ w .MDCCCXXXWLi : Za& HI p.220. 
Diagram showing the Diurnal inequalitij in the Interval 
and in the Height of high water as deduced [from Ohser- 
-vations at the London and Liverpool Do cksSeeTablesXi. sxxv. t , 020 and P i 34 
I NT E R VA L 
j London, 35 Tem-s _ 
Theory Ohseiwatwn '' London 19 Tears. . . ............ 
I Liverpool 
In this comparison of the London and Liverpool results the London corrections 
have heen sldfhed, to the left hag' an hour agreeably to die remark m p too and die 
signs reversed. The abscissa, represents die apparent solar time of moons tnuisitAT.M. 
Scale of i 
