The rock that hung in the sky of Servia—

Upon October 13, 1872, a stone fell from the sky, to this earth, near

the town of Soko-Banja, Servia. If it were not a peculiar stone, there

is no force to this datum. It is said that it was unknown stone. A name

was invented for it. The stone was called _banjite_, after the town near

which it fell.

Seventeen years later (Dec. 1, 1889) another rock of banjite fell in

Servia, near Jelica.

For Meunier’s account of these stones, see _L’Astronomie_, 1890-272, and

_Comptes Rendus_, 92-331. Also, see _La Nature_, 1881-1-192. According

to Meunier these stones did fall from the sky; indigenous to this earth

there are no such stones; nowhere else have such stones fallen from the

sky; they are identical in material; they fell seventeen years apart.

* * * * *

At times when we think favorably of this work of ours, we see in it a

pointing-out of an evil of modern specialization. A seismologist studies

earthquakes, and an astronomer studies meteors; neither studies both

earthquakes and meteors, and consequently each, ignorant of the data

collected by the other, sees no relation between the two phenomena. The

treatment of the event in Servia, Dec. 1, 1889, is an instance of

conventional scientific attempts to understand something by separately,

or specially, focussing upon different aspects, and not combining into

an inclusive concept. Meunier writes only upon the stones that fell from

the sky, and does not mention an earthquake at the time. Milne, in his

_Catalogue of Destructive Earthquakes_, lists the occurrence as an

earthquake, and does not mention stones that fell from the sky. All

combinations greatly affect the character of components: in our

combination of the two aspects, we see that the phenomenon was not an

earthquake, as earthquakes are commonly understood, though it may have

been meteoric; but was not meteoric, in ordinary terms of meteors,

because of the unlikelihood that meteors, identical in material, should,

seventeen years apart, fall upon the same part of this earth’s surface,

and nowhere else.

This occurrence was of course an explosion in the sky, and its

vibrations were communicated to the earth below, with all the effects of

any other kind of earthquakes. Back in our earliest confusion of the

data of a century’s first quarter, we had awareness of this combination

and its conventional misinterpretation: that many concussions that have

been communicated from explosions in the sky have been cataloged in

lists of subterranean earthquakes. We are farther along now, in our data

of the 19th century, and now we come across awareness, in other minds,

of this distinguishment. At 8:20 A. M., Nov. 20, 1887, was heard and

felt something that was reported from many places in the region that is

known to us as the London Triangle, as an earthquake, though in some

towns it was thought that a great explosion, perhaps in London, had

occurred. It was reported from Reading, and from four towns near

Reading, and Reading is said to be one of the places where the

concussion was greatest. There were several accounts of slight alarm

among sheep, which are sensitive to meteors and earthquakes. But, in

_Symons’ Met. Mag._, Mr. H. G. Fordham wrote that the occurrence was not

an earthquake; that a meteor had exploded. He had very little to base

this opinion upon: out of scores of descriptions, he had record of only

two assertions that something had been seen in the sky. Nevertheless,

because the sound was so much greater than the concussion, Mr. Fordham

came to his conclusion.

In _Symons’ Met. Mag._, 23-154, Dr. R. H. Wake writes that, upon the

evening of Nov. 3, 1888, in a region about four miles wide and ten or

fifteen miles long, in the Thames Valley (near Reading) flocks of sheep

had rushed from their folds in a common alarm. About a year later, in

the Chiltern Hills, which extend in a northeasterly direction from the

Thames Valley, near Reading, there was another such occurrence. In the

London _Standard_, Nov. 7, 1889, the Rev. J. Ross Barker, of Chesham, a

town about 25 miles northeast of Reading, writes that, upon Oct. 25,

1889, many flocks of sheep, in a region of 30 square miles, had, by

common impulse, broken from their folds. Mr. Barker asks whether anyone

knew of a meteor or of an earthquake at the time. In vol. 24, _Symons’

Met. Mag._, Mr. Symons accepts that all three of these occurrences were

effects of meteoric explosions in the sky. The phenomena are

insignificant relatively to some that we have considered: the

significance is in this definite recognition in orthodoxy, itself, that

some supposed earthquakes, or effects of supposed earthquakes, are

reactions to explosions in the sky.

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