Torrens Mining Limited announced the results of additional rock chip sampling at the Goldie Prospect located within Mt Piper Gold Project in Central Victoria. The Goldie Prospect encompasses a series of historic shallow gold prospectors' workings extending over a strike length of 1.2 km. Workings are concentrated over a 120 m long by 150 wide corridor (Figure 1), where multiple parallel quartz veins have been prospected in shallow north-northeast trending trenches up to 2 m wide. The position of shallow historical shafts directly to the west of the prospectors' trenches suggest that the quartz veins probably dip to the west, mimicking the dip of the host Cambrian rocks of the Heathcote Greenstone Belt. Sampling of piles of quartz mined from the shallow workings have returned gold grades in excess of 30 g/t Au (Table 1) from fire assaying. The down-dip continuation of the mineralised veins remains open and untested. Torrens' geologists have exposed in-situ quartz veining up to 30 cm wide at the base of shallow workings in several test pits. Six samples taken from one of these veins assayed up to a maximum grade of 31.08 g/t Au. The highly weathered nature of the surrounding host rock at this horizon has so far prevented reliable structural measurements being taken. Mineralisation at Goldie is inferred to be associated with magmatic fluids derived from the Devonian intrusion, possibly in combination with or overprinting earlier `orogenic' style mineralisation common in the Bendigo Zone. There are several gold and tungsten occurrences in the area spatially associated with a subtly different phase of the Pyalong Granodiorite, implying a relationship between mineralisation and magmatic fluids. Felsic magmatism, including the intrusion of the Pyalong Granodiorite, which is dated at about 378 Ma, followed by the Baynton Granite at about 367 Ma, is associated with gold and antimony mineralisation in both the Bendigo and Melbourne Zones. The Toolleen and Golden Camel (previously known as Cornella) gold mines are hosted in the Heathcote Greenstone Belt north of Torrens' tenements, within the Knowsley East Shale and Goldie Chert, and within hematitic chert beds, respectively. Both deposits contain high gold grades, accompanied by variable amounts of arsenic and antimony. At both Toolleen and Golden Camel, mineralisation is associated with sheared and silicified faults with anomalous gold, arsenic and antimony (up to 10,000 ppm arsenic (As) at Golden Camel 2). Both recent and historic drilling at these orebodies has intersected grades of greater than 9 g/t Au from beneath Toolleen, and greater than 5 g/t Au from 160m depth beneath Golden Camel, below known orebodies and mine infrastructure 3. Mineralisation at both deposits remains open at depth. Mineralisation is interpreted to be controlled by the intersection of northeast-southwest trending faults (Figure 3) with sulphide-rich west-dipping stratigraphy of the Heathcote Greenstone Belt, producing steeply northwest- dipping ore shoots along the fault plane.