hours without loss, and if we diminish the time, the wind is still more
southerly. Meteorologists usually cite the falling of ashes at Jamaica
during the eruption of Coseguina, in Guatamala, in February 1835, as
coming from south-west, whereas the true direction was about west
south-west, and the trade wind below was about north. But do we deny
that there is an interchange between the frigid and torrid zones? By no
means; but we would show that the great controlling power is external to
our atmosphere, and that the relative velocities of the earth and the
atmosphere is not alone adequate to account for it. By this view the
polar current is a north-west wind (which is impossible by Professor
Dove's theory), or is carried eastward by electric convection.


HUTTON'S THEORY.

Whether we adopt the views of Fourier or Poullet, as to the temperature
of the planetary spaces, it is certain that it is at least equal to, or
less than, the lowest temperature of our globe. It is also a well-known
fact, that the capacity of air to hold vapor in solution, increases in a
higher ratio than the temperature, so that the intermingling of
saturated portions of air, at different temperatures, must _necessarily_
be attended by precipitation of moisture. This idea was advanced by
Doctor Hutton, and considered competent to account for the prominent
meteorological phenomena, until Professor Espy broached a questionable
principle, (and which is rendered still more so by the late
investigations of Regnault,) in opposition to Hutton's theory. That the
theory is deficient, no one can gainsay. That Espy has rendered the
question clearer, is equally hazardous to assert. Hutton failed in
showing a cause for such intermingling on a sufficient scale; while
Espy, it may be suspected, has misinterpreted facts, and incautiously