A history of the Brazil : $b comprising its geography, commerce, colonization, aboriginal inhabitants, &c. &c. &c.Henderson, James
History
A history of the Brazil : $b comprising its geography, commerce, colonization, aboriginal inhabitants, &c. &c. &c.
Henderson, James
Brazil; Brazil -- History -- To 1822
On the 1st of January, 1772, the diamond district came under the
immediate management of the government. But diamonds alone do not
constitute the riches and celebrity of this district; other precious
stones concur in rendering it important, such as sapphires, emeralds,
aqua-marinas, chrysolites, topazes, &c. All these stones are produced
in the serras, from whence they descend to the rivers, with the waters
of the copious thunder showers. This district also possesses mines of
all the metals, the extraction of which is rigorously prohibited on
account of the diamonds.
Around the diamond district there are various military detachments, to
prevent the plunder of those stones, or of gold; and also to exact the
duties paid upon entrance. Amongst those stations may be enumerated,
first, Milho Verde; and, next in rotation, Pirahuna, Gouvea, Rio Pardo,
Chapada, Arraial, Hinhahy, Rio Manço. The diamond demarcation, afar
off exhibits a black perspective, swelling into a thousand rugged and
uneven serras; on one hand are elevated mountains of one single stone,
cut by nature into precipices that raise their heads to the clouds;
on the other, are extended serras, composed of detached rocks and
stones, accumulated on each other in chaotic piles, covered with a
grey moss, and sparingly dressed in creeping brushwood. A thousand
pure and crystalline rills warble across its rude tracts formed by
the miner, and roll into his _gamella_[25] their rich offerings.
The waters of some are dashed over the sides of mountains, others
descend divided between broken rocks to the base of the serras, from
whence, accumulating, they flow in serpentine courses in search of
larger rivers, running sometimes tamely and tranquilly between spacious
banks; at others, precipitated amongst approximating and steep serras,
with loud and interesting murmurs. For a time they often disappear
altogether from the sight, are again visible, flowing on in foaming
fury. The crystallizations of diamonds are obtained near the surface
of the earth. Their form is triangular, round, pointed on one side,
with the face always smooth; this proves that the crystallization is
dispersed and solitary.
Public-domain text, read in full here on John Shaqi.
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