BARISAL GUNS. (_See page 221._)

Readers not acquainted with this phenomenon may be referred to an

interesting correspondence in the pages of _Nature_ (Oct. 1895, and

_Seq._), opened by Professor G.H. Darwin--

"In the delta of the Ganges," he says, "dull sounds, more or less

resembling distant artillery, are often heard. These are called

Barisal guns, but I do not know the meaning of the term."

The same sounds have been recorded by M. Rutot of the Geological

Survey along the Belgian coast, and are alleged to be pretty common in

the North of France. M. van der Broeck, Conservator of the Museum of

Natural History of Belgium, says--

"I have constantly noticed these sounds in the plain of Limburg since

1880;--more than ten of my personal acquaintances have observed the

fact. The detonations are dull and distant, and are repeated a dozen

times or more at irregular intervals. They are usually heard in the

daytime, when the sky is clear, and especially towards evening after a

very hot day. The noise does not at all resemble artillery, blasting

in mines, or the growling of distant thunder."

M. van der Broeck elsewhere refers to "similar noises heard on

Dartmoor, and in some parts of Scotland." Readers of Blackmore's story

of "Lorna Doone" will remember, among other valuable observations of

out-door life, his accounts of "the hollow moaning sound" during the

intense cold of the winter, of which he gives so graphic an account.

It was "ever present in the air, morning, noon, and night time, and

especially at night, whether any wind was stirring or whether it were

a perfect calm" (Chap. xlvi.).

Another correspondent in _Nature_ refers to remarkable noises among

the hills of Cheshire: "When the wind is easterly, and nearly calm on

the flats, a hollow moaning sound is heard, popularly termed the

Soughing of the Wind, which Sir Walter Scott, in his glossary to 'Guy

Mannering,' interprets as a hollow blast or whisper."

Another writer quotes experiences in East Anglia, tending to show that

such sounds may be reports arising from the process of "faulting"

going on, on a small scale, at a great depth, and not of sufficient

intensity to produce a perceptible vibration at the earth's surface.

It would seem that in districts such as Comrie in Perthshire, East

Hadden in Connecticut, Pignerol in Piedmont, Meleda in the Adriatic,

&c., sounds without shocks are common during intervals, which may last

for several years. Remarkable sounds, not apparently accounted for,

are reported to proceed from Lough Neagh in Ireland.

See _Nature_, Oct. 1895, and following numbers; articles by M. van der

Broeck in _Ciel et Terre_ (Belgium), Dec. 1, 1895, and following

numbers, also _Geol. Mag._, vol. ix. 1892, pp. 208-18.

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