CONJECTURES IN REGARD TO METEORIC EPOCHS.
It is highly probable that aerolites and shooting-stars are derived
either from rings thrown off in the planes of the solar or planetary
equators, or from streams of nebulous matter drawn into the solar
system by the sun's attraction. Such annuli or streams would probably
each furnish an immense number of meteor-asteroids. If any rings
intersect the earth's orbit, our planet must encounter such masses as
happen at the same time to be passing the point of intersection. This
must be repeated _at the same epoch_ in different years; the frequency
of the encounter of course depending on the closeness and regularity
with which the masses are distributed around the ring. Accordingly it
has been found that not only the meteors of November 14th and of the
epochs named in Chapter II. have their respective radiants, but also
those of many other nights. Mr. Alexander S. Herschel, of Collingwood,
England, states that fifty-six such points of divergence are now well
established. We have mentioned in a previous chapter that Mr. Greg, of
Manchester, has specified several epochs at which fire-balls appear,
and meteoric stone-falls occur, with unusual frequency. The number
of these periods will probably be increased by future observations.
Perhaps the following facts may justify the designation of July
13th-14th as such an epoch:
1. On the 13th of July, 1797, a large fire-ball was seen in Göttingen.
2. On the 14th of July, 1801, a fire-ball was seen in Montgaillard.
3. On the 14th of July, 1845, a brilliant meteor was seen in London.
4. On the 13th of July, 1846, at about 9h. and 30m. P.M., a brilliant
fire-ball passed over Maryland and Pennsylvania, and was seen also in
Virginia, Delaware, New Jersey, New York, and Connecticut. Its course
was north, about thirty degrees east, and the projection of its path
on the earth's surface passed about four miles west of Lancaster,
Pennsylvania, and nearly through Mauch Chunk, in Carbon County. When
west of Philadelphia its angle of elevation, as seen from that city,
was forty-two degrees. Consequently its altitude, when near Lancaster,
was about fifty-nine miles. The projection of its visible path, on the
earth's surface, was at least two hundred and fifty miles in length.
Its height, when nearest Gettysburg, was about seventy miles, and it
disappeared at an elevation of about eighteen miles, near the south
corner of Wayne County, Pennsylvania. Its apparent diameter, as seen
from York and Lancaster, was about half that of the moon, and its
estimated heliocentric velocity was between twenty and twenty-five
miles.
The author was assured by persons in Harford County, Maryland, and also
in York, Pennsylvania, that shortly after the disappearance of the
meteor a distinct report, like that of a distant cannon, was heard.
As might be expected, their estimates of the interval which elapsed
were different; but Daniel M. Ettinger, Esq., of York, who was paying
particular attention, in expectation of a report, stated that it was
a little over six minutes. This would indicate a distance of about
seventy-five miles. The sound could not therefore have resulted from
an explosion at or near the termination of the meteor's observed path.
The inclination of the meteoric track to the surface of the earth
was such that the body could not have passed out of the atmosphere.
As no aerolites, however, were found beneath any part of its path,
perhaps the entire mass may have been dissipated before reaching the
earth.--_Silliman's Journal_ for May, 1866.
5. On the 14th of July, 1847, a remarkable fall of aerolites was
witnessed at Braunau, in Bohemia. Humboldt states that "the fallen
masses of stone were so hot, that, after six hours, they could not be
touched without causing a burn." An analysis of some of the fragments,
by Fischer and Duflos, gave the following result:
Iron 91·862
Nickel 5·517
Cobalt 0·529
Copper, manganese, arsenic, calcium, magnesium,
silicium, carbon, chlorine and sulphur. 2·072
-------
100·000
6. On the 13th of July, 1848, a brilliant fire-ball was seen at
Stone-Easton, Somerset, England.
7. On the 13th of July, 1852, a large bolide was seen in London.
8. On the 14th of July, 1854, a fire-ball was seen at Senftenberg.
9. On the 13th of July, 1855, a meteor, three times as large as
Jupiter, was seen at Nottingham, England.
10. "One of the most celebrated falls that have occurred of late years
is that which happened on the 14th of July, 1860, between two and
half-past two in the afternoon, at Dhurmsala, in India. The aerolite in
question fell with a most fearful noise, and terrified the inhabitants
of the district not a little. Several fragments were picked up by
the natives, and carried religiously away, with the impression that
they had been thrown from the summit of the Himalayas by an invisible
Divinity. Lord Canning forwarded some of these stones to the British
Museum and to the Vienna Museum. Mr. J. R. Saunders also sent some
of the stones to Europe. It appears that, soon after their fall, the
stones were _intensely cold_.[15] They are ordinary earthy aerolites,
having a specific gravity of 3·151, containing fragments of iron and
iron pyrites; they have an uneven texture, and a pale-gray color."
11. At a quarter-past ten o'clock on the evening of July 13th, 1864,
a large fire-ball was seen in New England.[16] The hour of its
appearance, it will be observed, was nearly the same with that of the
bolide of July 13th, 1846; and it is also worthy of remark that their
_directions_ were nearly the same. The meteor of 1864 had a tail three
or four degrees in length, and the body, like that of 1846, exploded
with a loud report.
12. On the 8th of July, 1186, an aerolite fell at Mons, in Belgium
(Quetelet's _Physique du Globe_, p. 320). A forward motion of the node,
somewhat less than that observed in the rings of November and August,
would give a correspondence of dates between the falls of 1186, 1847,
and 1860.
With the exception of the last, which is doubtful, these phenomena all
occurred within a period of 67 years.
THE EPOCH OF NOVEMBER 29.
It has been stated that in different years meteoric stones have
fallen about the 29th of November. One of the most recent aerolites
which can be assigned to this epoch is that which fell on the 30th of
November, 1850, at Shalka, in Bengal. It may be mentioned, as at least
a coincidence, that the earth passes the approximate intersection of
her orbit with that of Biela's comet at the date of this epoch. Do
other bodies besides the two Biela comets move in the same ellipse? It
is worthy of remark that two star showers have been observed at this
date: one in China, A.D. 930, the other in Europe, 1850 (see Quetelet's
Catalogue). It is certainly important that the meteors of this epoch
should be carefully studied.