Galilei, Galileo
,
De Motu Antiquiora
Text
XML
Document information
None
Concordance
Thumbnails
List of thumbnails
<
1 - 10
11 - 20
21 - 30
31 - 40
41 - 50
51 - 60
61 - 70
71 - 80
81 - 90
91 - 100
101 - 110
111 - 120
121 - 130
131 - 140
141 - 150
151 - 160
161 - 161
>
1
2
3
4
5
6
7
8
9
10
<
1 - 10
11 - 20
21 - 30
31 - 40
41 - 50
51 - 60
61 - 70
71 - 80
81 - 90
91 - 100
101 - 110
111 - 120
121 - 130
131 - 140
141 - 150
151 - 160
161 - 161
>
page
|<
<
of 161
>
>|
Now
since
in
the
preceding
{1}
chapter
those
things
have
been
demonstrated
that
concern
the
state
of
rest
,
we
must
now
consider
things
that
pertain
to
motion
upward
.
I
say
,
then
,
that
magnitudes
lighter
than
water
,
when
let
down
into
water
,
are
not
completely
submerged
,
but
that
a
certain
part
protrudes
.
Accordingly
let
the
first
position
of
the
water
,
before
the
magnitude
is
let
down
,
be
along
surface
ef;
and
let
magnitude
a
,
lighter
than
water
,
when
let
down
into
the
water
,
be
completely
submerged
,
if
this
can
be
done
,
and
let
the
water
be
raised
up
to
surface
cd;
and
,
if
it
is
possible
,
let
both
the
water
and
the
magnitude
remain
in
this
position
.
Now
,
the
heaviness
,
with
which
the
magnitude
exerts
pressure
and
raises
water
cf,
will
be
equal
to
the
heaviness
with
which
water
cf
exerts
pressure
in
order
to
raise
magnitude
a
.
But
the
size
of
water
cf
is
equal
to
the
size
of
magnitude
a
.
There
are
thus
two
magnitudes,
one
which
is
a
,
the
other
which
is
water
cf;
and
the
heaviness
of
this
a
is
equal
to
that
of
this
cf,
and
the
size
a
is
also
equal
to
the
size
of
this
water
cf:
therefore
,
the
magnitude
a
is
equally
as
heavy
as
water
:
which
is
surely
absurd
;
for
it
has
been
assumed
that
the
magnitude
is
lighter
than
water
.
Consequently
,
magnitude
a
will
not
remain
completely
submerged
under
the
water
;
therefore
it
will
necessarily
be
carried
upward
.
Text layer
Dictionary
Text normalization
Original
Regularized
Normalized
Search
Exact
All forms
Fulltext index
Morphological index