[Ceylon; an Account of the Island Physical, Historical, and by James Emerson Tennent]@TWC D-Link book
Ceylon; an Account of the Island Physical, Historical, and

CHAPTER I
100/172

The first fall of rain was preceded by a downward blast of cold air, accompanied by hailstones which outstripped the rain in their descent.
Rain and hail then poured down together, and, eventually, the latter only spread its deluge far and wide, In 1852, the hail which thus fell at Kornegalle was of such a size that half-a-dozen lumps filled a tumbler, In shape, they were oval and compressed, but the mass appeared to have formed an hexagonal pyramid, the base of which was two inches in diameter, and about half-an-inch thick, gradually thinning towards the edge.

They were tolerably solid internally, each containing about the size of a pea of clear ice at the centre, but the sides and angles were spongy and flocculent, as if the particles had been driven together by the force of the wind, and had coalesced at the instant of contact.

A phenomenon so striking as the fall of ice, at the moment of the most intense atmospherical heat, naturally attracts the wonder of the natives, who hasten to collect the pieces, and preserve them, when dissolved, in bottles, from a belief in their medicinal properties.

Mr.
Morris, who has repeatedly observed hailstones in the Seven Korles, is under the impression that their occurrence always happens at the first outburst of the monsoon, and that they fall at the moment, which is marked by the first flash of lightning.
[Footnote 1: It is stated in the _Physical Atlas_ of KEITH JOHNSTON, that hail in India has not been noticed south of Madras.

But in Ceylon it has fallen very recently at Korngalle, at Badulla, at Kaduganawa; and I have heard of a hail storm at Jaffna.


<<Back  Index  Next>>

D-Link book Top

TWC mobile books