That this has no other caufe, is clear from the times 
wherein thefe Winds fet in: ijiz. in Jfril^ when the 6un be- 
gins to warm thofe Countries to the North, the S. W. Mo^^ 
Joo?z hogms, and blo ws during the Heats- till Of?- ^^r^ when 
the ^un being retired, and all things growing cooler North- 
ward, and the Heat encreafiag to tfie<Sbuth, the Nurch-Eait 
Winds enter and blow all the winter till Jpril again. And .t is 
undoubtedly from the fame Princip e that to the 6outhw ai ds 
of the Equator, in pare of the hdta/^ Ocean, the North- Weil 
Winds fuccced the 6buth-Eaft, when the Sun draws near the 
Tropick of Caprkor^; but Imuft confefs, that in this latter 
occurs a difficulty, not well to be accounted for, which is, 
why this Change of the Monfoom lliould be any more in this 
Ocean, than in the fame Latitudes in the ALthiopicky where 
there is no thing more certain than a S.E. Wind all the 
Year. : 
'Xis likewife very jiard to conceive why the limits of 
the Trade Wind fhould be fixt, about the thirtieth degree 
of Latitude all round the Globe j and that they fhould fb lel- 
dome tranfgrefs or fall fliort of thofe bounds; as alfo that^in 
the Indian Sea, only the Nor.tliern P^irt fliould be fubjed ta 
the chang-eable Monfoons^ and in the. .Southern there be ^ 
conltant S, E. " ^ 
. Thefe are particulars that merit to be confidered more at 
Large, andfitrnifha fufficient Subjeft for a juit Volume; 
which will be a very commendable Task for fuch, who be- 
ing ufed to Philofbphick C -ontempl^tion^^. fliali have leafure 
to apply their feripus thoughts about it. 
