Notes on granite and structural features following an examination of the granite outcrop at Balladonia Station. A sketch plan of the outcrop is included this report.

Results of micro-examination of samples from Bore No. 3825 on E.W. Langbien's property near Bourke, from 950 feet down to 1200 feet.

Report on the possibilities of underground water on Piney Creek pastoral lease. This report follows a visit to the lease conducted in response to a request for advice regarding water supply.

Red ochre of high quality has been produced from deposits in Ophthalmia Range since 1937. The bulk of the production has been derived from one lease, No. 37OH, the deposits on which are the subject of this report. The locality was visited in June, 1944. This reports comprises notes on access, topography, geology, economic geology, and production. A geological plan of the vicinty of the ochre deposits accompanies this report.

The presence of quartz crystals in the dump of an old gold mine, known as Black Charlie's mine, in the Strathbogie Ranges led to the reopening of part of the workings in the search for crystal suitable for piezo-electric applications. To date the search has met with success, and has resulted in the discovery of a second crystal deposit adjacent to the old workings. The mine which is now named the Crystal King mine was visited in December, 1944. The locality, topography, geology, economic geology, and production of the mine are discussed in this report. A sketch section of the mine is included.

The presence of asbestos at various places in the Harts Range has been reported from time to time, and, in recent months it was reported that the largest of these deposits consisted of Chrysotile. A brief examination of this deposit was made in October, 1944, and specimens of the asbestos then collected were specifically identified as anthophyllite. This report comprises notes on locality, geology, and mineral occurrence, and includes a locality and sketch plan.

This report deals with an investigation of the electrical resistivities of a variety of wet surface soils, gravels and sands. The work may be regarded as preliminary to an investigation by Mr. R.F. Thyer into the detection of electrically resistive bodies buried in wet soils at shallow depths. It was required to determine the range over which the resistivities of surface soils vary, and also the changes that may be expected in any one type of soil between measurements made within any 1 foot of each other. Measurements were made in four localities, three being in the bed or on the banks of the Molonglo River, where the surface materials are sand, gravel, silts, and in some places, clay. The fourth locality was near the head of Sullivan's Creek, where the soil is a heavy black clay.

This report deals with the problem of detecting electrically resistive bodies of small size buried at shallow depths in wet soils. Detection was attempted by means of measurements made on the surface of the soil using the electrical resistivity method. The present report can be regarded as an extension of an earlier one (No. 1943/64B). The purpose of the new tests was twofold. Firstly it was proposed to make tests of 'normal' resistivity effects using a constant electrode arrangement and measuring the resistivity at closely spaced points on water saturated soils. The second part of the testing programme was contingent on the first part proving that under saturated conditions soil resistivities were sufficiently constant to warrent an attempt being made at detection. If this condition of constancy existed, it was proposed to extend the work of the tests, reviewed in the previous report, to actual field conditions. This has been done and the present report deals with the results obtained.

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.

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.