Citigold Corporation Limited announced details of the stream sediment exploration program undertaken by Citigold over its Charters Towers land tenure. This announcement is a synopsis of the results of this overall program. A geochemical sampling program was completed at the end of December 2020 with assay results being returned in January to March 2021. This first-pass sampling program has now been completed, with samples taken at 84 sites. Three types of samples were taken at each site: 3-5kg of -2mm sand analysed for gold by Bulk Cyanide Leach (BCL), 1-3kg of rock chip or rock float from the stream bed, and 3-5kg of -2mm sand. The rock chips and -2mm sand were analysed for gold by 50g fire assay and for a 35-element scan by Inductively Couple Plasma Atomic Emission Spectroscopy (ICP-AES). Gold at Charters Towers is known to be associated with elevated lead and zinc values, low levels of arsenic and to a lesser extent, elevated copper. Results were statistically assessed using log-probability plots, and anomalies were defined as those BCL gold values over 100ppb, gold in fire assays over 0.1 g/t Au, ICP-AES copper, lead and zinc values over 100 ppm and arsenic values over 20 ppm. Of the 82 rock float samples collected, 19 were below detection limit, 29 were considered anomalous (greater than 0.1 g/t Au) and of these, 16 were greater than 0.5 g/t Au. Eight samples were 1 g/t Au or higher. Three anomalous rock float samples over 0.5 g/t Au (Sample Nos. 51, 55 and 69) were located at the northern extremity of the Exploration Permits, five to eight kilometres north of the centre of Charters Towers and returning gold values of 0.59, 0.51 and 0.83 g/t Au respectively. These are considered highly significant, as the historical workings at Charters Towers were not considered to persist north of the city. The occurrence of rock float samples 5-8 km north of the city indicate that gold-bearing outcrops are shedding into creeks in an area not previously known to be mineralised. There are no known or previously-mined gold deposits in this area, so these three samples have highlighted new mineralisation with the potential for northern extensions of the known cross veins and new east-west lodes. Rock chip Sample No. 74 is considered highly significant. It has a base metal and silver signature that more closely matches a Volcanogenic Massive Sulphide (VMS) deposit than the traditional Charters Towers style of mineralisation. The sample returned 2.03% zinc, 0.8% lead, 0.07% copper and nearly an ounce to the tonne silver (29 g/t Ag). It is located 200m northeast of the northeast corner of ML 10335 that covers the eastern extensions of the Imperial Mine lodes. There is no known mineralisation in the 1.5 kilometres drainage basin upstream of the float sample location. This sample may indicate potential for a VMS style of deposit in the drainage basin, similar to VMS mineralisation found the south at Liontown and to the west at Thalanga. Several anomalies in different sampling media are coincident and others are stand-alone. Areas of interest for detailed follow-up sampling are the rock chip/float samples at the northern part of the land tenure, the coincident anomalies where two or more sampling media returned anomalous results, and a potential Volcanogenic Massive Sulphide target upstream of Sample No. 74 to the east of the Imperial mine area. Some of the coincident anomalies relate to known old workings but provide new target areas for more advanced exploration in the near term. Infill stream sediment sampling will commence at the end of the Wet Season (late March to mid-April) together with follow-up sampling, particularly the rock float areas north of Charters Towers and the stream anomalies that appear unrelated to known mineralised areas.