Travels in the Interior of Brazil: Principally through the northern provinces, and the gold and diamond districts, during the years 1836-1841Gardner, George
History
Travels in the Interior of Brazil: Principally through the northern provinces, and the gold and diamond districts, during the years 1836-1841
Gardner, George
Brazil -- Description and travel; Mines and mineral resources -- Brazil
I had now reached the most northerly point of the Brazilian empire, that
had previously been visited by any naturalist, for neither Pohl nor
Burchell had extended their excursions beyond Natividade. It is true that
Spix and Martius also travelled in the north of Brazil, but their route
was in a very different direction. As I was here informed that these
travellers had not ascended the neighbouring lofty Serra, I was resolved
to do so, for the double purpose of making botanical collections, and of
examining its geological structure. On this journey I was accompanied by
Mr. Walker, a black shoe-maker, who acted as a guide, and one of my own
men. Following the banks of a small stream which comes from the Serra,
and which passing near the north end of the Villa, yields it a constant
supply of clear and cool water, we reached the foot of the Serra, and
shortly afterwards, by a gradual ascent, arrived on the top of a low
branch, where we found a broad shallow valley, the soil of which had been
completely turned over in search of gold; and near the centre of it, we
came upon the ruins of what we were told had been the original site of
the Villa. It was founded by those who first ventured into this distant
region in search of gold, and was abandoned about sixty or seventy years
ago, when this metal became scarce, and when cattle farms were found to
be more productive than mines. Near the top of this valley there is a
small artificial lake, which must have been formed at a great expense,
and from it the water was led in small streams to the places where the
washings were going on. The soil in which the gold was found, is a
ferruginous gravel, formed from the disintegration of the primitive rocks
of which the Serra is composed.
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