The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
History
The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
Astronomy; Earth (Planet); Natural history
One of the Istrian rivers, the subterranean course of which, although
still unknown as regards a great number of points, has given rise to
a most continuous course of investigations, is the celebrated Timavus
(Timavo), which falls into the sea near Duino, about twelve miles
to the north of Trieste. Virgil’s description no longer applies to
the mouths of the Timavo; at present they do not reach the number
of nine, because the extermination of the woods of the Carso has
diminished the mass of the water, or the action of the stream and
the alluvium of the delta have modified the form of the shore. But
still it is a magnificent spectacle to see the outlet of the three
principal torrents of water which rush foaming out of the heart of
the rocks, and are navigable from their mouths to their very source.
A river of this importance must certainly receive the drainage of
a vast basin, and yet all the neighboring valleys seem perfectly
devoid of rivulets, and their surface presents little else but the
bare rock; in fact, the whole of the rain and snow-water runs away
through underground caverns.
The most remarkable network of caverns in this region of the Alps is
that which spreads out from the southwest to the northeast across
the Adelsberg group of mountains, between Fiume and Laibach. The
principal cave is especially curious on account of its size, the
variety of its calcareous concretions, and the torrent which runs
roaring through it.
North of the town of Adelsberg the traveler passes along the base of
a hill with steep and bare sides, bringing into view the sharp edges
of its highly pitched calcareous beds. On the right the stream of
the Poik winds peaceably in the valley; and then, its course being
arrested by a headland, turning suddenly, it flows into the interior
of the mountain through a kind of high portal, opening between two
parallel beds of rocks. Unless the water in the stream is very low,
it is impossible to follow it over the accumulation of rocks upon its
bed; but on the right, at a height of a few yards, there is another
entry, through which the traveler may descend dry-shod into a vast
cavity or chamber, where the Poik again appears issuing from its
narrow passage of rocks.
Public-domain text, read in full here on John Shaqi.
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