TheNatwalBflory mttUi 



or uppermoft Strata with Watey • which 

 by degrees dram down into Wells y 

 Springs^ and RitferSf and fb makes an 

 Addition untci therri. And this is the 

 reafon that thefe abound with WMer vA 

 the colder Seafott ^b much more thari 

 they do in the hotter. 



That the Watery which is thus dif- 

 jjens'd to the Earth and Atmojphere by 

 the Gredt Abyfsy being carried dowrt, 

 by Rains and by Rivers into the Ocea^j 

 which, as we have faid, communicates^ 

 and ftands at an Equilibrium with that 

 fabterrantan Cohfervatoi^y, is by that 

 means reftored bdck to the Abyfs; 

 whence it returns again, in a continual 

 Circulation, to the Surface of the Earth, 

 inVapourSy and Springs. 



Thit thG final Cdufi of this i)iftribii- 

 fiori of Water, in fuch quantity, to all 

 parts of the Earth indifferently irt 

 Springs, Rivers, and Rain : and of 

 this perpetual Circulation aind Motion 

 of it, is the Propagation of Bodies^ Ani'- 

 malSy [Vegetables, arid Minerals , in at 

 cOntinqed Succeflion. That for Anii 

 mals, they either feed upon Vegetable^ 

 immediately : or, which comes to th6 

 iame at laft, upon other Animals which 

 MaVfe fed upon them j fo that Vegetal 



bin 



