he faintest; one about N.-W.,
towards Jupiter, and the brightest of the three; and another towards the
north. These were not cirrus streaks, but veritable streams of electric
matter, and had a very decided rotation from left to right, and
continued visible about twenty minutes, as represented above.

[17] This day the central vortex passed in about latitude 47d N.--the
southern margin cannot be nearer than 250 miles, throwing off the 40'
for the horizontal refraction, would give eight miles of altitude above
a tangential plane. Then another seven miles, for curvature, will give
an altitude of fifteen miles for the cumuli. The height of these
thunder-clouds has been much under-estimated. They seem to rise in
unbroken folds to a height of ten and twelve miles frequently; from the
data afforded by the theory, we believe they will be found much higher
sometimes--even as much as sixteen miles.

[18] These parallel bands, and bands lying east and west, are frequent
in fine weather between two vortices. Sailors consider them a sign of
settled weather. After dark there was frequently seen along the northern
horizon flashes of lightning in a perfectly clear sky. But they were
both faint and low, not reaching more than 4d or 5d above the horizon.
After sunset there were very distinct rays proceeding from the sun, but
they were shorter than on the evening of the 3d. These are caused by the
tops of the great cumuli of the storm, when sunk below the horizon,
intercepting the sun's rays, which still shine on the upper atmosphere.
The gradation was very marked, and accorded with the different distances
of the central vortex on the 3d and 4th--although, on the 4th, the
nearest distance must have been over four hundred miles to the southern
boundary of the storm.

[19] It is worthy of notice here, that New York, which only differs by
about 40 miles of latitude and 800 in longitude, had the storm earlier,
near the time of the passage, as appears by the appended account of it.
This proves, that a storm affects a particular latitude simultaneously,
or approximately so. If this had to travel eastward to reach New York,
it would have been the 10th instead of the 8th. The principal trouble
was, however, in the early part of the evening of the 8th, to the south
of Ottawa, where the strong wind was drawn in from the northward. If a
vortex passes from north to south, leaving the observer between the
passages, there must, nearly always, be a wi