To The Gold Coast for Gold: A Personal Narrative. Vol. IBurton, Richard Francis, Sir
History
To The Gold Coast for Gold: A Personal Narrative. Vol. I
Burton, Richard Francis, Sir
Ghana -- Description and travel; Gold mines and mining -- Ghana
Local tradition connects this ice-cave with the famous burial-cavern
near Ycod, on the northern coast; this would give a tunnel 8 miles long
and 11,040 feet high. Many declare that the meltings ebb and flow with
the sea-tide, and others recount that lead and lines of many fathoms
failed to touch bottom. We are told about the normal dog which fell in
and found its way to the shore through the cave of Ycod de los Vinos. In
the latter a M. Auber spent four hours without making much way; in parts
he came upon scatters of Guanche bones. Mr. Robert Edwards, of Santa
Cruz, recounted another native tradition--that before the eruption of
A.D. 1705 there was a run of water but no cave. Mr. Addison was let down
into it, and found three branches or lanes, the longest measuring 60-70
feet. What the _neveros_ call _el hombre de nieve_ (the
snow-man) proved to be a honeycombed mass of lava revetted with
ice-drippings. He judged the cave to be a crater of emission; and did
not see the smoke or steam issuing from it as reported by the
ice-collectors.
Professor P. Smyth goes, I think, a little too far in making this
contemptible feature compose such a quarrel as that between the English
eruptionist and the Continental upheavalist. Deciding a disputed point,
that elevation is a force and a method in nature, he explains the cave
by the explosion of gases, which blew off the surface of the dome, 'when
the heavy sections of the lava-roof, unsupported from below, fell
downward again, wedging into and against each other, so as nearly to
reform their previous figure.' But the unshattered state of the stones
and the rounded surfaces of the sides show no sign of explosion. The
upper _Piton_ is unfitted for retaining water, which must percolate
through its cinders, pumices, and loose matter into many a reservoir
formed by blowing-holes. Snow must also be drifted in and retain, the
cold. Moisture would be kept in the cavern by the low conducting power
of its walls; so Lyell found, on Etna, a bed of solid ice under a
lava-current. Possibly also this cave has a frozen substratum, like many
of the ice-pools in North America.
Public-domain text, read in full here on John Shaqi.
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