SEARCH FOR ORE
SUCCESS OF NEW METHODS. AUSTRALIA’S EXPERIENCE. SYDNEY, January 3. So encouraging have been the preliminary experiments in geophysical survey in Australia by electrical and gravimetrical methods that a new research section is now being formed to investigate the possibility of seismic methods. Fresh apparatus has arrived from Britain, and the personnel of the section is now being chosen. Experiments in geophysical survey are being conducted under the auspices of the Commonwealth Government, with the object of ascertaining Australia’s mineral resources. A party of scientists was brought from England last year, under the leadership of Mr Broughton Edge to conduct a two-vears’ investigation into the merits of the systems used. The scheme was suggested by the Empire .Marketing Board, which is sharing the cost with the Commonwealth Government. At present the two sections in existence are working separately in their search lor possiblefields of copper, iron, and sulphide ores. The electrical section will shortly go to Tasmania where work on the Aeolian, Rcad-Roscberry, and RennisonBcll mining fields has been suggested. The gravimetrical section, which has been mapping the outer reaches of the Brown coal fields in Victoria, will probably go to New South Wales. The work* is being followed closely by tlio various State Departments of Mines, for when the survey party presents its final report this will act as a guide for the State authorities as well as tor private interests. State authorities have suggested the various areas loi investigation, and State experts arc attached to the parties for experience, ’flic visiting scientists are also training four Australians in the methods used so that they will leave experts behind whim they return home at the end ol their engagement in 1930. The work is described as being very interesting from a scientific point of view, as it is based on new theories and has not yet been definitely proved. Valuable results are claimed for it in other countries, particularly in Scandinavia, where rich iron ore deposits have been discovered under glacier moraines, deposits ol earth and rock which had hitherto concealed the true nature ol tin* ground beneath. In the electrical method of survey, two steel stakes arc driven into the ground some distance apart, and alternating currents are passed from one to the other by Ricans of a dynamo. 'I lie current passes through the earth in various “lines of force” and these are thrown out of their different courses if ore deposits exist. Continuous trial enables the scientists to map out the area ol the ore field, and then the geologist is called in to determine the nature 1 of
the ore. In the gravimetric method the effect created on gravity forces by ore deposits beneath the ground is measured mathematically by means of a torsion balance. The new seismic section will adopt a method.of measuring concussion vibrations. A deposit of explosives will be placed in the centre of a circle of seismographs, which are more familiarly known as instruments for measuring earthquakes. When the explosive is fired oil the seismographs, it is expected, will bo able to indicate the amount of distortion of concussion vibration caused by the presence or absence o 4 ore.
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Hokitika Guardian, 17 January 1929, Page 2
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530SEARCH FOR ORE Hokitika Guardian, 17 January 1929, Page 2
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