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Ch. 12: San Romao | Diamond District

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346
TRAVELS IN BRAZIL.
he threw water on the fine gravel, which was thus washed out with great care into the canal, continuing in this manner until the Bateia was empty; it is in this last process that diamonds are expected to be found. A small Bateia, containing a little water, was placed on a low pedestal between the two overseers, and into this the diamonds were put as they were found, which on this occasion amounted to eleven, all of which, however, were small. In the bottom of the Bateias is always found a small quantity of gold dust, which is carefully preserved.
Although diamonds are usually found in the diluvial gravelly soil above described, that is not, however, the matrix in which they have originally been formed. Whatever may be the case in other countries, I remained perfectly satisfied that here, they have originally been formed in the metamorphic quarto-schistose rock, of which the mountains in the Diamond district are constituted, and that they have, during a long series of years, been washed down along with the other debris, to the places where they are now found so abundantly. These rocks are rather soft in their nature, and of course easily disintegrated; hence the many wild ravines winch intersect this range, excavated by the small streams that flow from it. Small masses of the rock have frequently been found containing diamonds imbedded in them; in the Cidade Diamantina I saw two beautiful specimens, in each of which one half of a small diamond was exposed; the extravagant price asked for them prevented me from purchasing either.
When we read in books, that the diamond is a production of the most recent geographical epoch, as stated, for instance, by Dr. A. Petzholdt, in Jamieson's Journal, no. 68, we cannot help imagining that those who promulgate such opinions, have been led astray by travellers, who have listened to the idle stories of the uneducated inhabitants of Diamond countries, who almost all assert, that diamonds are regenerated in the course of a few years, in the soil from which others had previously been taken. This I found to be a very common opinion in Brazil; but those best able to form a just conclusion on the subject, for instance, such intelligent miners as Captain Jose D'Almeida e Silva, believe
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