, tile °p e1v 
to the axis noi o eil, l3 i! t the ceruy 1 0 11( -,ye °P ( , n 
ang, and because the s °uth pole > s ,n a bly 
than the north) t! ’ ,e ®-W. wind is P 1 '^,yards ' 
en sacked (by a partial vacuum ’ ^ ve co n- 
continuouslv within the sphere) trim m;<1 _ 
of an serial sphere above us, or from 
cave of an serial sphere above us, m earthV 
T . U)( re between sucii concave ami 
T P « their natural rarifaction, gteat eon 
5 ," Sion and consequent heat, indicate; the,.- 
^:» 1 nsd,h 1 ,sot,,!dindicatesy,atth=yt 
ked • owing to the rotation of the ear 1 o , 
£ ,"feast the action of the suction winds spiral- 
the east, ,„„ ml .,i a enuator, frorr 
* lllH l the earth towards the equator, from 
ty, n0 i e in a westwardly direction ; the 
-.ion, may he ttlmos, as si- 
P ?fmneous, from end to end, as that of the 
tides" or somewhat as water moves in a trough, 
when one end is depressed: this action may 
pass over or through the trade winds of the 
Suator. It appears, S.E. winds abound more 
-n Europe, than in Amenca; pevnaps this is 
owing to a partial continuation 01 the monsoons 
of India, or are partial northern monsoons It 
die spheres balance towards each other on the, 
side next the sun, it will account for winds 
prevailing more at midday than at midnight; 
as the polar openings should then better cor¬ 
respond with each other. . 
8 That, the N. polar opening is the source 
•whence the matter of our N. eastwardly snow 
storms, as well as that of most winter rams, are 
derived;—although the snow must be crystali- 
zed, on, or after, its passage over the icy hoop 
or circle. The expansion of the air, on its es¬ 
cape from the polar openings, must produce 
the great cold, that at times exist about the icy 
circles,and this expansion continued indefinite¬ 
ly towards our equator, should tend to produce 
cold here. 
9. That, when the sun is 23 degrees S. or the 
•equator, the line of latitude of greatest cold N. 
is 23 degrees S. of the polar opening or real 
ninetieth degree; and, when he is 23 degs. N. of 
the equator, the line of greatest cold, north, ex¬ 
ists no great distance beyond real 90th de¬ 
gree, although under the umbrage of tlie verge. 
10. That, the dark complexion of the nat ions 
high N , is derived from ancestors, that origin¬ 
ally dived in a hot climate further N. continu¬ 
ously and within the sphere. I 
1 i. That, when one is at 90 degrees real, re- 
■fractioh will so deceive, as to indicate 8 or 10 
degrees less than 90owing to the atmos- 
phere extending quite over the polar opening; 
(as there is reason to believe it does,) so as to 
cause the zenith of the atmosphere, at 90 de¬ 
grees real, (notthe zenith of the heavens,) to 
be de nressed at a considerable angle towards : 
the south —ter example; when a person trav¬ 
elling N. has passed 90 short degrees beyond 
*$ur ninetieth degree* hisreal h^-y 
