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Meteorology   
hitherto.
Let us recall our fundamental principle and then explain our
views. We have already laid down that the outermost part of what is
called the air is potentially fire and that therefore when the air
is dissolved by motion, there is separated off a kind of matter-and of
this matter we assert that comets consist. We must suppose that what
happens is the same as in the case of the comets when the matter
does not form independently but is formed by one of the fixed stars or
the planets. Then these stars appear to be fringed, because matter
of this kind follows their course. In the same way, a certain kind
of matter follows the sun, and we explain the halo as a reflection
from it when the air is of the right constitution. Now we must
assume that what happens in the case of the stars severally happens in
the case of the whole of the heavens and all the upper motion. For
it is natural to suppose that, if the motion of a single star
excites a flame, that of all the stars should have a similar result,
and especially in that region in which the stars are biggest and
most numerous and nearest to one another. Now the circle of the zodiac
dissolves this kind of matter because of the motion of the sun and the
planets, and for this reason most comets are found outside the
tropic circles. Again, no fringe appears round the sun or moon: for
they dissolve such matter too quickly to admit of its formation. But
this circle in which the milky way appears to our sight is the
greatest circle, and its position is such that it extends far
outside the tropic circles. Besides the region is full of the
biggest and brightest constellations and also of what called
'scattered' stars (you have only to look to see this clearly). So
for these reasons all this matter is continually and ceaselessly
collecting there. A proof of the theory is this: In the circle
itself the light is stronger in that half where the milky way is
divided, and in it the constellations are more numerous and closer
to one another than in the other half; which shows that the cause of
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