133
but hypotheticall what was alledged, and It was not very euident that there was any such
thing as an aether much Le
sse was it vnder
stood what it was and what propertys
It had, nor that the air did con
si
st of such parts as was alledged, m
r Hooke affirmed
that by multitudes of Experiments he could make it very euident fir
st that there
was such a body, and secondly what many of the propertys of that body were
thirdly how very considerable and powerful tho
se propertys were in producing
multitudes of effects a
scribed to other cau
ses generally. fourthly he could shew -
how tho
se propertys might be examined and e
ssayed and reduced
. . . into a Stan
derd to wit to number weight mea
sure &
. . . consequently make
it a subiect fitt to be
. . . farther inquired into by this Society. who
se
Business /De
signe/
is to be Directed by the Great Scoolmi
stress of Rea
son, Experience. And not to be
ruled by groundle
sse fantcys & conceipts -
By these ways he supposed the phenomena of the great grauity of the air vpon the -
long blowing of an eastwordly, and the Great lightne
sse vpon the blowing of a
Southwardly wind, /The air/ the one comming ouer a va
st tract of Land & soe taking vp into
into it self great qu
alitys of
vapours exhalations w
ch. remaine su
spended
and mixt w
th it by rea
son of their congruity, & the other blowing ouer a great space
of sea
and soe taking vp only such parts . . . w
ch affords le
sse quantity of
parts di
spo
sed to make air. He al
so further explained the rea
son of the ready conuerting
of vapours into water by the cold of the air, tho
se watery parts being more easily pre
cipitated or separated from the air by the want of heat to keep them agitated
as was In
stanced in the appearing of Ones breath in Cold Weather, and the ea
sy
conuer
sions of the
va wind produced by
. . . water heated in an aeolipile
into water againe by the want of
tht heat & agitation
how ^ /wherefore/ the Grauity of the air ari
sing only from the quality of tho
se grauitating parts
w
ch. were kept su
spended in the form of air, the greater the one is the greater
al
so must con
sequently be the other
m
r Ol: Hill now comming In affirmed that there was noe such thing as grauity in the
air but that air was po
sitiuely light, and that all that belieud otherwi
se were mi
sta
ken and in a great error as he would pre
sently make appear both by rea
sons & Experi
ments and to this pupo
se alledged many things which he affirmed he had more at
large explained & better Dige
sted in a Di
scour
se which he had then about him
of that subiect and that he had made it on purpo
se for this meeting and that
he would Read It if they thought fit and continue tho
se his Di
scour
ses if they
met w
th entertainment worthy of them -
After w
ch. He read his paper a coppy of w
ch he promi
sed to Deliuer to the Se=
cretary between that and the next meeting that an account thereof might be
taken by him.
At the same time al
so he Deliuerd in a Coppy of his Di
scour
se w
ch. he had made
the La
st meeting about
. . . the wormes in pepper water. Intituled
Reflections on the transactions of the Royall Society in their meeting on -
thursday Dec: 6. 1677-
Ref: CELL/RS/HF_135 © Centre for Editing Lives and Letters