Our First Half-Century: A Review of Queensland Progress Based Upon Official InformationQueensland
History
Our First Half-Century: A Review of Queensland Progress Based Upon Official Information
Queensland
Queensland -- History
The report for 2nd October, 1896, brings records up to date. By map it
is shown that not only does the water-bearing country extend over 56
per cent. of the area of Queensland, but also continues into New South
Wales and South Australia, and enters Western Australia. It "marks
the position of the ancient Cretaceous sea which connected the Gulf
of Carpentaria with the Great Australian Bight," and "divided the
continent into two islands." "They were," wrote Dr. R. L. Jack, "laid
down by this sea; their present position is due to subsequent general
upheaval, and they lie directly and unconformably on schists and
slates of undetermined age, or on granite or gneiss. Except in
Queensland, where they are overlaid here and there by the remains of
the Upper Cretaceous or Desert Sandstone formations which have not
been removed by denudation, they seem to be covered to a considerable
extent by Tertiary rocks. The Desert Sandstone beds lie horizontally
but unconformably on those of the Rolling Downs, which dip to the
south." [e]
[Footnote e: See "Geology and Palaeontology of Queensland and
New Guinea," by R. L. Jack, F.G.S., Government Geologist,
and R. Etheridge, jun,. Government Palaeontologist, New South
Wales, page 390.]
IMPROVED DRILLING MACHINERY.
In the same report the improvement in drilling machinery is discussed,
and Queensland manufacturers are congratulated on making American
and Canadian machines with improvements which greatly add to their
efficiency. Bores in Queensland are generally begun with 10-in.
casing, and carried to not lower than 500 ft. Then 8-in., 6-in.,
and 5-in. casings are used. The necessity of these casings being as
perfect as possible is emphasised by the Engineer. The cost of sinking
bores by contract, which is almost the universal method, depends
upon the facilities offered by the site for the transport of wood and
water, but the range then was from 17s. to 24s. per foot for the first
500 ft., and increased with depth until, at 4,000 ft. odd, sinking
had cost 55s. per foot. The inspectors appointed the previous year had
done good work, though the wet season delayed travelling. Sectional
diagrams compiled from the inspectors' reports appear among the
appendices.
Then follows an interesting description of surface artesian water
known as Elizabeth Springs, in latitude half a degree south of the
tropic, and in 1403/4 degrees west longitude. The account of these
remarkable springs is well worth reading.[f]
[Footnote f: See Votes and Proceedings for 1897 for Hydraulic
Engineer's Report, 2nd October, 1896, page 5.]
PROGRESS TO 1896.
Number of bores in Western Queensland to October, 1896, 454; average
depth, 1,168 ft.; feet bored, 530,332 (nearly 100 miles); overflow,
193,000,000 gallons per diem. There were also nineteen deep bores on
the coast. The total cost had been L928,081.
BORES IN THE GULF TOWNS.
Public-domain text, read in full here on John Shaqi.
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