C H4 ) 
^lian before comparing them, I imagined. fl fpeak with 
relation to laO: Year only, having no other Obfervations.) 
For in Winter, although I imagine we have more warm 
days than they j and in Summer, that they have greater 
Heats than we 5 yet I obferve that the Colds and Heats in 
bo'h Places, begin and end nearly about the fame time: 
Yea, that oftentimes any remarkable Weather (efpecially 
if of fomewhat long continuance) affefteth one as well 
as the other place. Thus for inftance, f/we, which was 
pfuivc part of it at leaft, particularly the very day after 
the Solftitial-day, 12.) remarkably Cold in E»g- 
Uncl^ feems to have been not very different at Zurich 5 
Dr. ^cheuihzer'^s Thermometer divers times that Month 
("though not on the very fame days perhaps) defeending 
as low, or rather lower than in the Month before, yea 
as low as many days in the Winter Months. But one 
thing I farther obferved was, that all th-s Month their 
cold Weather conftantly preceded ours here about five or 
more Days. An Indication that (as dial I be farther ob- 
ferved hereafter) the Weather in both Places was influ- 
enced by the fame Caufes, whether the Alpine, Hills and 
Cold, or the Influx of the Moon and other heavenly Bo- 
d!cs, or any other Caufe, I fhall not enquire. 
And as in June there was a great agreement in the un- 
nfual Cold, fo in Augufi there was not much lefs agree- 
ment in Heat 5 the Heats in both places being great, and 
beginning to abate about the fame time, only a little 
fooncr here than there. 
In Winter alfo, although, as I faid, I imagine we have 
a greater nunober of warmer Days than they, yet I find 
that a warm Winter Month there is fo here 5 and a cold 
one there is a cold one here likewife. Thus in February 
and March ^ O&^ober and November, a great agreement feems 
to have been between the Heats and Colds of both Places, 
fome Days excepted. But January was at the beginning 
not fo conflantly Cold, for the Seafon, ait U^mwfier, as 
