[175
175] ON THE PORISM OF THE IN-AND-CIRCUMSCRIBED TRIANGLE. 75
class 4,
rk that
If a triangle be inscribed in a conic, and two of the sides touch conics having
double contact with the circumscribed conic, then will the third side touch a conic
viz. a
3 other
mstruct
pect to
.he two
angents
wo and
nd the
points)
having double contact with the circumscribed conic.
Secondly, the conics 21 and 33 may cut the conic © in the same four points.
Here it may be seen that there are an infinity of inscribed quadrilaterals of the
kind first considered, viz. of which two opposite sides touch the conic 21, and the
other two opposite sides touch the conic 33. Hence, the curve (5 is made up of
two coincident curves of the class 4. But the curve of the class 4 has in fact 4
double tangents, viz. considering each of the points of intersection of 21, 33, ©, and
drawing tangents to 21 and 35 meeting © in two new points, the line joining these
points is a double tangent of the curve in question, which is therefore of the 4th
33 has
points
double
order, and being of the class 4 with 4 double tangents, it must break up into two
curves of the second class, i.e. into two conics. Each of these conics passes through
the points of intersection of 21, 33, ©, and touches the four lines last referred to,
the conics would of course be completely determined by the condition of passing
curves
contact
which
5 21 is
for the
Dect to
points,
double
icident
hrough
conics,
tion of
through the four points and touching one of the four lines. Attending only to one
of the two conics, we have thus what I call the porism (allographic) of the in-and-
circumscribed triangle, viz.
If a triangle be inscribed in a conic, and two of the sides touch conics meeting
the circumscribed conic in the same four points, the remaining side will touch a
conic meeting the circumscribed conic in the four points.
The a posteriori demonstration of these theorems will form the subject of an
other paper, [178].
of the
But
S have
m the
conics,
igents,
ler 8;
curves
© in
nts of
double ] .
Gt is
sm of
n-and-
10—2