l more simple matter, only one
reagent being necessary, so that there is a greater probability of such
depositions obtaining than were a double process necessary. Knowing the
action of sulphides, the manner or the mode of formation of a portion at
least of these nuggets seems apparent. Conceive a stream or river fed
by springs rising in a country intersected by auriferous reefs, and
consequently in this case carrying gold in solution; the drift of such
a country must be to a greater or lesser extent pyritous, so that the
_debris_ forming the beds of these streams or rivers will certainly
contain nodules of such matters disseminated or even stopping them in
actual contact with the flow of water. It follows, then, from what has
been previously affirmed, that there will be a reduction of gold by
these nodules, and that the metal thus reduced will be firmly attached
to them, at first in minute spangles isolated from each other, but
afterwards accumulating and connecting in a gradual manner at that point
of the pyritous mass most subject to the current until a continuous film
of some size appears. This being formed the pyrites and gold are to a
certain extent polarised, the film or irregular but connected mass of
gold forming the negative, and the pyrites the positive end of a voltaic
pair; and so according as the polarisation is advanced to completion
the further deposition of gold is changed in its manner from an
indiscriminate to an orderly and selective deposition concentrated
upon the negative or gold plate. The deposition of gold being thus
controlled, its loss by dispersion or from the crumbling away of the
sustaining pyrites is nearly or quite prevented, a conservative effect
which we could scarcely expect to obtain if organic matter were the
reducing agent. Meanwhile there is a gradual wasting away of the pyrites
or positive pole, its sulphur being oxidised to sulphuric acid and its
iron to sesquioxide of iron, or hematite, a substance very generally
associated with gold nuggets. According to the original size of the
pyritous mass, the protection it receives from the action of oxidising
substances other than gold, the strength of the gold solution, length of
exposure to it, the rate of supply and velocity of stream, will be the
size of the gold nugget. As to the size of a pyritous mass necessary to
produce in this manner a large nugget, it is by no means considerable.
A mass of common pyrites (bisulphide of iron) weig