Frontier and pioneer life -- Australia -- Queensland
Apart, therefore, from the 5.552 per cent. of chloride of sodium, the
deposit consists of sequi carbonate of soda or native "Trona," and as
such is used by the settlers for culinary purposes, etc.
PALÆOZOIC.
"Carboniferous."--Whilst the affinities of the southern coalfield of
Queensland are mesozoic, a northern field, of even larger extent, has a
distinct fauna more resembling the Palæozoic Carboniferous areas of
Europe.
The Dawson, Comet, Mackenzie, Isaacs, and Bowen Rivers drain this
carboniferous area; and numerous outcrops of coal have been observed on
these streams. No commercial use, however, has yet been made of any of
these deposits, as the measures generally are too far inland to be made
available until the railway system of the country is extended in that
direction.
"Devonian."--From the southern boundary of Queensland up to latitude 18
deg. S., a series of slates, sandstones, coral limestones, and
conglomerates extend to a distance 200 miles inland; these are sometimes
overlain by coal measures, sometimes by volcanic rocks, and consequently
do not crop out on the surface over such districts. North of latitude 18
deg. S., however, over the Cape York Peninsula, this series (so far as
we have any evidence), is absent, granites and porphyries capped by
"Desert Sandstone" forming the ranges on the eastern, and their abraded
ingredients the sandy ti-tree flats, those on the western side of that
inhospitable tract of country, a never-ending flat of poor
desert-looking sandy ti-tree country, stretching away to the shores of
the Gulf of Carpentaria.
In the limestone bands, which form the lower portion of the series,
corals are very numerous; in fact, the limestones, where little
alteration has taken place, are a mass of aggregated corals; and as this
class of rock has resisted aerial destruction better than the associated
slates and sandstones, the barriers thus formed mark the trend of the
rock system to which they belong, in a very picturesque and decided
manner; their bold, massive, and varied outline chiselled into the most
delicate fretwork by Nature's hand, is relieved by a wealth of
richly-tinted foliage, unknown in the surrounding bush; and the eye
jaded with the monotony of the eternal gum tree turns with delight to
the changing tints and varied scenery presented by these barrier-like
records of the past. This class of country is very much in evidence at
Chillagoe. On the track from the Broken River to the Gilbert diggings,
Devonian rocks several thousand feet thick may be observed, as they are
continuous in dip, without being repeated, for at least five miles
across the strike, with an average inclination of 60 deg.
Although on the Broken River and its tributaries a breadth of thirty
miles with a length of sixty miles, is occupied by a persistent outcrop
of Devonian strata, gold has only been discovered in remunerative
quantities in a small gully, where a trapdyke has penetrated the
Palæozoic rocks of the district.
Public-domain text, read in full here on John Shaqi.
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