Doctor Blagden (Philosophical Transactions, 1784,) considers
electricity as the general cause of these phenomena; Doctor
Gregory, and others, think they depend upon collections of highly
inflammable matter, as phosphorus, phosphorated hydrogen, &c. being
volatilized and congregated in the upper regions of the air.
Doctor Halley ascribes them to a fortuitous concourse of atoms,
which the earth meets in her annual track through the ecliptic;
and Sir John Pringle seems to regard them as bodies of a celestial
character, revolving round centres, and intended by the Creator
for wise and beneficent purposes, perhaps to our atmosphere, to
free it of noxious qualities, or supply such as are salutary. Many
other theories, as ingenious as fanciful, might be enumerated; but
without commenting on their comparative merit, I must acknowledge
that none of them have yet impressed my mind with a conviction of
their truth. A series of observations, however, have enabled the
moderns to ascertain, with apparent accuracy, several particulars
relative to these stupendous bodies, which add much to our
knowledge of their general character:--their velocity, equal to
30, and even 40 miles in a second of time; their altitude, from 20
to 100 miles; and their diameter, in some instances, more than a
mile, are facts we derive from respectable authority, and may aid
us, essentially, in forming just conceptions of their nature and
properties.
I believe meteoric stones to result from all meteoric explosions;
limiting, however, the term meteor to those phenomena, in the
higher regions of the air, denominated fire-balls, shooting-stars,
&c. That these bodies move in a resisting medium, must be
evident to every attentive observer; and that this medium is our
atmosphere, is pretty certain, 1st. Because we know of no other
resisting medium round the earth; 2dly. Because the same kind of
resistance is apparent at every intermediate altitude, from their
greatest to their least, which last we know to be far within our
atmospheric bounds; and, 3dly. Calculation has, in no instance,
assigned them an elevation beyond the probable height of the
atmosphere.
That meteors proceed from the earth, that they arise from certain
combinations of its elements with heat, and that meteoric
stones are the necessary result of the decompositions of these
combinations, are opinions I will endeavour to support, by the
following considerations.
1st. The properties and habitudes of matter, under certain
conditions and combinations.
2dly. The situation of the earth's surface in respect to the sun,
the influence of his rays thereon, and the nature of the elements
or compounds on which these rays act:
And 3dly. The identity that exists between the component parts of
meteoric stones, and the elements that enter abundantly into the
composition of our globe; and, by several other facts and arguments.
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