298 MR. LUBBOCK ON TIDE OBSERVATIONS. 



Table XI. (Interpolated from Table X.), showing the Interval between the Apparent 

 Time of the Moon's Transit and the Time of High Water at the Liverpool Old Docks 

 for every three degrees of her Declination north and south. 



Table XII., showing the Interval between the Apparent Time of the Moon's Transit 

 and the Time of High Water at the Liverpool Old Docks for every three degrees of 

 her Declination north or south. 



Table XIII., showing the Difference in the Interval between the Apparent Solar 

 Time of the Moon's Transit and the Time of High Water, and the Interval corre- 

 sponding to 15° Declination, for every three degrees of her Declination north and south. 



Table XIV., showing the Difference in the Interval between the Apparent Solar 

 Time of the Moon's Transit and the Time of High Water, and the Interval corre- 

 sponding to 15° Declination, for every three degrees of her Declination north or south. 



Table XV. (Interpolated from Table X.), showing the Height of High Water at 

 the Liverpool Docks for every three degrees of the Moon's Declination north and 

 south. 



Table XVI., showing the Height of High Water at the Liverpool Docks for every 

 three degrees of the Moon's Declination north or south. 



Table XVII., showing the Difference between the Height of High Water and the 

 Height corresponding to fifteen degrees of the Moon's Declination, for every three 

 degrees of her Declination north and south. 



Table XVIII., showing the Difference between the Height of High Water and the 

 Height corresponding to fifteen degrees of the Moon's Declination, for every three 

 degrees of her Declination north or south. 



Table XIX. results from Table I., if Mr. Hutchinson's Clock was regulated ac- 

 cording to Mean Solar Time, showing the Difference in the Interval between the 

 Mean Solar Time of the Moon's Transit and the Time of High Water, and the Mean 

 Interval, for every month in the year. 



Table XX. results from Table X., if Mr. Hutchinson's Clock was regulated ac- 

 cording to Mean Solar Time, showing the Difference in the Interval between the 

 Mean Solar Time of the Moon's Transit and the Time of High Water, and the In- 

 terval corresponding to 15° Declination, for every three degrees of her Declination 

 north and south. 



Table XXL, showing the Semimenstrual Inequality -j- a constant, or the Interval 

 between the Moon's Transit and the Time of High Water, her Parallax being 57', 

 and her Declination 15°. (This Table has been formed by interpolation from the 

 column corresponding to Parallax 57' in Table VII.) 



Table XXII., showing the Semimenstrual Inequality -f a constant, or the Height 

 of High Water at Liverpool, the Moon's Parallax being 57', and her Declination 1^°, 

 from the Sill of the Old Dock Gates. 



Table XXIII., showing the correction for the Moon's Parallax in the Time of 

 High Water at Liverpool. 



