Frontier and pioneer life -- Australia -- Queensland
The following districts, however, where Devonian rocks prevail, have
been the centres of gold mining enterprise:--Lucky Valley, Talgai,
Gympie, Calliope, Boyne, Morinish, Rosewood, Mount Wyatt, Broken River,
portion of Gilbert.
In every case here cited, the country is traversed by trap rocks of a
peculiar character, either diorite, diabase, or porphyrite; and
tufaceous representatives of these are also found interstratified in the
upper portion of the same formation, and occasionally throughout the
other beds.
At Gympie, the auriferous area is confined to veins traversing a
crystalline diorite, or within a certain limit of its boundary, marked by
the presence of fossiliferous diabase tufas.
Whatever may have been the solvent and precipitant of the nobler metals
in the auriferous veinstones associated with trap intrusions, all other
but hydrothermal action may safely be eliminated, the very nature of the
reefs, composed as they are of alternating layers of a promiscuous
mixture of quartz, calcspar, pyrites, etc., affording unmistakable
evidence on this point. The gold also contained in the trap dykes
themselves is always accompanied by pyrites, both (according to
Daintree), hydrothermal products separating out during the cooling down
of the trap intrusions. Auriferous lodes, occurring in areas where
hydrothermal action has attended trap disturbances of a special
character in Queensland, are generally thin--to be estimated by inches
rather than feet; but taken as a whole they are far richer in gold than
those enclosed by sedimentary rocks.
GRANITIC.
Outcrops of granite extend along the eastern coast of Queensland from
Broad Sound to Cape York, and inland as far as the heads of streams
running direct from the inner coast range to the sea.
Very little rock of this character is met with west and south of the
Dividing Range which separates rivers flowing to the eastern and
northern coast, and those trending south to the Murray or Cooper's
Creek.
The granites of Queensland vary very much in their crystalline texture,
passing from true granites into porphyry and quartz porphyry.
TRAPPEAN.
Much stress has been laid on the value of certain intrusive trap rocks
as specially influencing the production of auriferous veinstones in
Queensland.
The petrology of these may be divided into four type classes:--1.
Pyritous porphyrites and porphyries. 2. Pyritous diroites and diabases.
3. Chrome iron serpentines. 4. Pyritous felsites.
VOLCANIC.
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