Buenos Ayres and the Provinces of the Rio de La Plata: Their Present State, Trade, and DebtParish, Woodbine, Sir
History
Buenos Ayres and the Provinces of the Rio de La Plata: Their Present State, Trade, and Debt
Parish, Woodbine, Sir
Argentina -- Description and travel; Argentina -- History
Don Luis himself, upon the recovery of Buenos Ayres, repaired thither,
and drew up the diary of his interesting journey, which, like those
of Villariño and Viedma, and many other interesting papers of the
same sort, was thenceforward consigned to oblivion in the secret
archivo.[33] The various important political events which shortly
afterwards began and rapidly succeeded each other were, however,
perhaps some excuse for its remaining unnoticed.
In describing the eastern parts of the Cordillera, Cruz says that, at
the time he was there, only the volcanoes of Antuco and Villarica were
in activity,[34] though the traces of others extinct might be seen in
every direction:--the evidences of their ancient eruptions, he says,
might be followed for thirty leagues continuously:--he speaks, amongst
other volcanic appearances, of hot springs resorted to by the Indians
for their medicinal qualities, and says so abundant is the sulphur in
all those parts that several rivers are strongly impregnated with
it; vast quantities also of bituminous substances are everywhere to
be seen, and beyond the Neuquen, he says, there is an abundance of
coal.[35] Nor is there good ground for doubting his assertion, since on
the opposite side of the Cordillera, in about the same latitude, coal
has long been known to exist, and has been occasionally used by the
foreign vessels trading with that part of Chile. Near the sources of
the Neuquen are mines of rock-salt: in the level lands, also, between
that river and the Chadi-leubú, salt may at all times be collected from
the surface of the ground, and the intermediate streams are all more or
less brackish from its influence.
Fossil marine remains appear to abound amongst the lower ranges of
the Cordillera which Cruz passed, not only strewed over the surface
at considerable elevations, but deeply imbedded in the soil, as
might be seen wherever sections were formed by the courses of the
mountain-torrents.
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