THE HEIGHT OF THE ATMOSPHERE.

The differences existing between that which appertains to the air

of heaven (the realms of universal space) and that which belongs to

the strata of our terrestrial atmosphere are very striking. It is

not possible, as well-attested facts prove, perfectly to explain

the operations at work in the much-contested upper boundaries of

our atmosphere. The extraordinary lightness of whole nights in the

year 1831, during which small print might be read at midnight in

the latitudes of Italy and the north of Germany, is a fact directly

at variance with all we know according to the researches on the

crepuscular theory and the height of the atmosphere. The phenomena

of light depend upon conditions still less understood; and their

variability at twilight, as well as in the zodiacal light, excite our

astonishment. Yet the atmosphere which surrounds the earth is not

thicker in proportion to the bulk of our globe than the line of a

circle two inches in diameter when compared with the space which it

encloses, or the down on the skin of a peach in comparison with the

fruit inside.

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