I will now relate some of my experiences of the efficacy of the divining rod.
It is my custom to use a compass to define the course of the underground stream, which I leave on paper with the manager or owner to show in which direction the stream is running.
I was engaged by Messrs. Philp, Forsyth and Munro to mark sites for tube bores on their property at Thylungra Station. After marking several sites on the station, when passing through Brisbane later, on my way to Cowley Station on the same errand, I interviewed Messrs. Philp and Forsyth, who told me there had been a well sunk on my site and no water obtained, but that the contractor had sunk a three-inch bore, where my peg was, and had obtained good water for his camp use. I may state here that where water is unobtainable close to the workings, this was a usual occurrence. As the three partners were about to visit the station, I asked them to discontinue working, and I would meet them there at a certain date. This I did, and found in their presence that the well had been put down two feet outside the breadth of the stream in the opposite direction to which it was running. I advocated a new well being sunk in the proper place, but they preferred driving in the direction to which I had placed the peg. Such action may prove a partial failure, as they might not strike the strong stream. I have not heard the result of their decision, but it is certain that my directions of the course of the stream have not been followed. Either Sir Robert Philp or Messrs. Forsyth or Munro could corroborate the above statements.
The Dalrymple Shire Council obtained my services to inspect a well which had been sunk at Oakey Creek, distant about 15 miles from Charters Towers, which they told me would only water twelve horses and then the supply gave out. I found the well was on the edge of a strong stream, the outer edge of which ran through the centre of the well, consequently the rod would not work at the outer edge of the well. I marked the site for a new one about six yards farther in. The members of the Council decided to put down a circular cement well. They tapped the water under 40 feet and obtained an inexhaustible supply. When I received the letter enclosing my fee, it contained a vote of thanks from the committee for the good work done. No better place could be chosen for a demonstration of the efficacy of the divining rod.
Later, the Directors of the Carrington United Mine invited me to visit their well at Lion's town, about 30 miles from Charters Towers, which had become dry. I found this well was not on any stream, but that a drive had been put in to drain the soakage from a sandy creek, which was in close proximity, and the season being a dry one, this had also failed to give any soakage. I crossed this creek, and found a stream 13 yards wide, which I marked. Being located on a flat, I had the idea that probably there might be more water further over. My surmise was right, for on investigation I found another stream 14 yards wide, but running in the direction as if it would join the other. This proved correct, the whole width of the two streams measuring 27 yards. I told the manager, who was present, I could get him a good site at a spot most suitable to himself. The site was marked in the centre of the 27 yards.
Miners were put on to work night and day, as about 100 men had been thrown out of employment owing to the failure of the water supply. Water was struck at 30 feet, which rose seven feet in the shaft in ten minutes. The sinking was continued to 40 feet, the water rising to within ten feet of the surface. When one considers the well was six feet square, the supply can be imagined.
Unknown to the man who was pumping the water to the mill, I later visited the site and enquired if the water could be reduced in the shaft. He replied:—"I have kept the pump going night and day, but cannot lessen the supply." I then asked him if I might lift the slabs which were covering the well. I did so with his permission, and saw the water flowing in a steady stream across it. This satisfied me as to the supply.
At Avon Downs Station, near Clermont, a large well had been sunk near a creek, with a diminishing supply of water. On investigation, I found the well had been sunk on the edge of an underground stream. I advised a drive to be put in towards the centre of the stream (which I marked). Mr. Sutherland (the Inspector for the Australian Estates at that time) informed me later that my advice had been carried out, and they had obtained very satisfactory results.
At Gindie State Farm, I was accompanied by Mr. Hamlyn (the Public Service Improvement Engineer) to mark sites for the Department of Agriculture. Mr. Jarrott, the manager, took us to a dry well sunk to a depth of 80 feet. I could not feel any indication of water there, but a few hundred yards away, on rising ground, I located two streams crossing each other, and by the assistance of pegs, marked a site in the centre of the two streams. Some months afterwards I met the manager in Emerald, who said:—"Mr. Corfield, when you were marking that site at Gindie State Farm, where the two streams crossed each other, the engineer and myself were laughingly criticising your action, but never more will I doubt your ability to find water." The Secretary of Agriculture later informed me by letter that the top stream only yielded a small supply, but the second stream, struck at 165 feet, augmented the supply that it could not be lowered by the pump more than 35 feet, and that the estimated yield of both streams was 10,000 gallons per day.
In 1907, I marked several sites in the vicinity of Winton, and between then and 1911, I travelled by coach and train, but principally by buggy, an approximate distance of 20,000 miles, marking sites at different stations, ranging from Charleville in the south-west, to Granada in the north-west, in the back blocks of this State, besides locating water on several stations on and near the eastern coast, and was successful in locating water to the satisfaction of those interested.