TIDAL PHENOMENA OF THE ST. JOHN KIYER. i t 



column of Table V seems to show that between Indiantown and 

 Oak Point the low water is delayed over twenty minutes com- 

 pared with high water ; between Oak Point and Oromocto low 

 water travels as fast as high water, and between Oromocto and 

 Springhill low water again loses half an hour. 



Table IV. 



Table V. 



Place. 



Distance 

 from 

 Indian- 

 town. 



Mean 

 Spring 

 Range. 



Mean 

 Percent- 

 age of 

 St John 

 Range. 



H. W. later 



than at 



St. John. 



Delay of 

 L. W. 



Springhill . 

 Fredericton 

 Oromocto . 

 Gagetown . 

 Oak Point . 

 Westfield . . 

 Indiantown 



hr. min 



9 — 20 

 8 — 45 

 7 — 57 

 5 — 40 

 3 — 15 

 2 — 30 



O 9 



00 



49 

 20 

 24 

 24 

 24 

 



