292
m
r. Henshaw affirmed that there was a way by w
ch. the whole
body of sea salt might be conuerted into an /insipid water./
alcalizatesalt viz
t. by heating of it very hott & suffering it to run
per Deliquium then Heating the Remainder and suffering
that to Run al
so and by soe continuing to Heat the Re=
mainder the whole body of the salt will at la
st be
conuerted into an
true Alcalizate Salt Insipid liquor -
much after the manner as D
r Dickenson had by long cir
culation conuerted the /18/20 of
the/
whole body of water into white
earth.
Herevpon was occasioned a
great Di
scourse about the cau
se
of the salt ne
sse of the sea, some being of opinion
that the saltne
sse of the sea proceeded only from
the Heat of the sun vpon the sea in the Torrid
Zone, though the greater part were of Opinion
that the saltne
sse of the sea proceeded from the
Di
ssolution of the salt mineralls of the earth either
at the Bottom or sides of
the sea or brought into it
by salt springs made by the Raine waters pa
ssing
through salt mines.
m
r. Hally related two ^ /magneticall/ obseruations he had made in his Voy
=age to S
t. Helens .
The first was that the Dipping needle Lay horezontall at about
15 degrees behither the AEquinoctiall Line.
The second
was was that northward of that place an Iron bein
held perpendicular the lower end would attract the south
pole and southwards of it the Lower end attracted
thenorth -
The Reason of w
ch. m
r. Hooke
Alledg supposed to be for that
The northern magneticall pole (As he had formerly shewd in
this society from the Examination of the variations obserued
in captain Iames his voyage to Hud
sons Bay) was placed beyond
the Pole of the earth. towards our horizon. and not between the pole
of the earth and vs as m
r. Bond supposed, and becau
se that the
Ref: CELL/RS/HF_294 © Centre for Editing Lives and Letters