Following the sound of detonations, the Killeter meteorite fell as a shower of stones in the early hours of April 29th 1844. A total mass of 140 g was recovered. Read more
Title: On the shower of aerolithes that fell at Killeter, county of Tyrone, on the 29th of April, 1844. Authors: The Rev. Samuel Haughton, F. R. S. Fellow of trinity College, Dublin
On the 29th of April, 1844, a shower of Meteoric Stones fell, in the sight of several people, at Killeter, near Castlederg, Co. Tyrone; they broke into small fragments by the fall, one piece only being found entire. It was (according to the testimony of a resident) "about as long as a joint of a little finger." The account given by three gentlemen, who, however, did not actually see the shower fall, was that they were at a distance of three or four miles, up the hills in the neighbourhood; it was a fine sunny evening, three or four o'clock. They heard "music" towards Killeter, which they supposed to proceed from a strolling German band, which they knew to be in the neighbourhood; they are under the impression that they heard the music several times in the course of the evening; they remember also to have noticed clouds in the direction of Killeter. On reaching Killeter the same evening, they were told of the wonderful shower of stones which had spread over several fields. I received the fragments of these stones from the Rev. Dr. M'Ivor, ex-Fellow of Trinity College, Dublin, and rector of Ardstraw; he writes to me that "it is now very difficult to get either a specimen of a stone or any very distinct intelligence of them: even the very rumour of them has nearly died out, and you might ask intelligent middle-aged men about the neighbourhood who had never heard them mentioned." He adds that the people of that locality are very "uncurious," and that if these were a veritable burning bush thereabouts, few would "turn aside to see." The largest specimen given to me by Dr. M'Ivor weighed 22.23 grs. in air, and 16.32 grs. in water, showing that its specific gravity is 3.761. Both it and the smaller fragments presented the usual black crust and internal greyish-white crystalline structure and appearance, with specks of metallic lustre, occasioned by the iron and nickel alloy that was present. I analysed it in the usual manner; but, owing to an accident, I was unable to determine the composition of the earthly portion soluble in muriatic acid.