HEAT AND COLD. 



Americas. The reflex coming back onto the coast of 

 Asia, and making the high tide with regard to Asia. 



The secondary tide in all places is brought about 

 by the second rush of the waters, aided by the congeal- 

 ing action of the cold upon the particles that make up 

 the water. Sufficient time having elapsed in all lo- 

 calities by the time of the second rush of waters from 

 coast lines to be plentifully effected by the cohesive 

 tendency of water while yet within the degrees of co- 

 hesive temperatures. 



The contraction of the particles of water in a great 

 ocean being sufficient, along with a rushing motion 

 from continental outlines, to make quite a tidal flow. 



The change from ocean to ocean being about the 

 time of the secondary tide also affects the flow of the 

 secondary tide in all locations of the earth ; there being 

 about twelve hours between the extreme lift as applied 

 to each ocean. 



The cause of a difference in the time of tide each 

 day can be attributed to the effect in the rising sun act- 

 ing as a governor of the proceedings, acting for a time 

 in opposition to the tendency of cold on the particles 

 of water eastward. The sun being lifting in opposition 

 to the flow of the waters generated by the action of the 

 cold for a few hours. That few hours necessitates a 

 delay in the time the sun shall overcome the tendency 

 of the flowing waters in the easterly direction. And in 

 consequence a delay in the tidal lift oh the particular 

 ocean. Also the shift of the earth in its orbit affects 

 the tidal lift with regard to either ocean. 



58 



