The Story of a Boulder; or, Gleanings from the Note-book of a Field GeologistGeikie, Archibald
Science
The Story of a Boulder; or, Gleanings from the Note-book of a Field Geologist
Geikie, Archibald
Geology; Petrology
I have been assured that it was no unfrequent occurrence for a pot of
potatoes capsized at the doorway to tumble down the slope and make no
stop until safely esconced at the sea-bottom.
The process whereby these fissures and caverns originate is the same as
that noticed already in the Spar Cave. Water containing an impregnation
of carbonic acid filters down through cracks and fissures of the
calcareous rock, dissolving out in its passage a portion of the lime
which it eventually carries back to the surface, and either deposits
there or transports into streams, and thence to the sea. Thus atom
by atom is removed wherever the percolating water reaches, until in
the course of ages an irregular cavern of greater or less extent is
produced. The decomposition of limestone at the surface results from
the same kind of action, that of carbonated water. Every shower of
rain insensibly carries away a fraction of the constituent parts of
the rock, so that the size and form of detached blocks as well as of
exposed cliffs is constantly changing. How often do we see the same
decay going on with a melancholy rapidity among the exposed marble
tombstones of our churchyards. In a few years the tablet gets worn
and furrowed as though it had stood there for centuries. Eventually,
too, the inscription becomes effaced, and perhaps ere the bones of the
deceased have mouldered away and mingled with their kindred dust, the
epitaph that recorded for the admiration of posterity his many virtues
and his vigorous talents, has faded from the stone--often, alas! only
too fit an emblem of how speedily the memory of the dead may fade away
out of the land of the living.
CHAPTER IX.
Public-domain text, read in full here on John Shaqi.
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