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  • Gibsonvale tin field is situated approximately three miles southeast of the village of Kikoira. This preliminary report was prepared following an examination of the tin field by the writer. Aspects of the general and economic geology of the field are discussed herein.

  • No. 1 Bore, Arcadia is situated in the parish of Arcadia, county of Westgrove, 85 miles north of Roma and 40 miles north-north-east of Injune, the nearest rail town. Drilling operations extended from 1936 to 1939. The Arcadia bore it the second deep bore in Queensland (the first being Hutton Creek bore) from which a comprehensive series of samples has been examined for their micro-faunal content. This examination was carried out on 1,256 samples consisting of drill cuttings taken over every five feet and of cores taken at numerous depths below 4,112 feet.

  • The mine is situated on Black Andrew Mountain about 4 miles south of the wall of Burrinjuck Dam and in the parishes of Goodradigbee and Childowla. Surface features were mapped by C.H. Zelman and H.B. Owen in November, 1942 by stadia alidade and planetable, and underground mapping was brought up to date by F. Canavan and H.B. Owen on 20th March, 1944 using tape, alidade and clinometer. This report details the production history, general geology, and economic geology of the Black Andrew mine.

  • Quartz crystals occur in the county of Dampier near the head of Tuross River 13 miles east-southeast from Countegany and about 5 miles east-southeast from Tuross Post Office. The presence of small quartz crystals in this locality has been known to Mr. L.W. Schaeffer of Tuross for many years, but only recently has he found larger crystals and undertaken more systematic prospecting. This report comprises notes on the quartz crystals, following an examination of the locality, 1944.

  • Rumbalara is a small siding on the Adelaide-Alice Springs railway line. It is about 120 miles by rail and 143 miles by road south of Alice Springs. The mine is 35 miles by road northeast of the siding. The object of the visit was to determine, if possible, the extent of the deposits and to decide whether they are likely to be able to supply the requirements of the Australian paint industry, particularly during the present war. The period 29th July to 2nd August, 1943, was spent in the field. During this time a plane table survey was made of the deposit and its environs. The underground workings were surveyed by chain and compass. Half a day was also spent at the field on the 18th January, 1944, in collecting specimens and making a brief inspection of new workings.

  • The Sydney Harbour Degaussing Range is situated opposite Bradley Head. The purpose of the survey was twofold. First, to determine the average normal values of the vertical (Z) and Horizontal (H) force components of the Earth's magnetic field in that part of the harbour which would be occupied by a ship passing over the coils. Secondly, to measure the magnetic elements, i.e. the Declination, Inclination and Horizontal Intensity of the Earth's field at a base station conveniently situated for use by naval personnel for the purpose of calibrating Pot Magnetometers, etc. The particulars of this survey work and given in this report.

  • This sample of bryozoal marl from Montagu, Tasmania, was collected by Mr. F. Canavan. It contains a faunal assemblage typical of the Balcombian Stage of the Middle Miocene as found in Victoria and can be referred to Longford substage of the Balcombian.

  • The presence of foraminifera in the Permian sediments of Australia was recorded as early as 1882. Some systematic work was done up to 1905, but there was no further investigation into these micro-fossils until 1937. A considerable amount of research is still necessary before it can be stated whether or not a definite system of zoning, based on micro-faunas, can be applied to the Permian rocks of Australia. It seems possible, however, that certain species may be characteristic of the Upper and Middle Permian deposits. In the extensive collections of Permian rocks examined from the Hunter River District in New South Wales, assemblages of foraminifera rather than restricted species have proved useful for zonal purposes and this method of zoning should prove valuable when more material is examined from the Permian deposits of other States.

  • The Gawler talc deposit is situated about 2 miles south from Ulverston and about half a mile north from Gawler where the bitumen road ends. The lease is held by Messrs. Pearson and Smith, and one man is working on it at present. A geological examination and plane table survey of the deposit was conducted on the 1st May, 1944.

  • Gypsum has been found in all the states of the Commonwealth, but, as far as known at present, deposits of commercial importance are limited to New South Wales, Victoria, South Australia and Western Australia. South Australia is the major producer and provides approximately 80 percent of the total Australian production. An account of gypsum deposits and occurrence by state is given in this report.