Southern Cross Gold Ltd. confirmed wide and high-grade gold-antimony mineralisation has been intersected in two drill holes (SDDSC038-39) over a 100 m distance, above and below drillhole SDDSC033 at the 100%-owned Sunday Creek Project in Victoria. These holes demonstrate wide and continuous zones of gold-antimony mineralisation over 100 m in the Apollo shoot with wide zones of mineralisation and more than a dozen high-grade intersections grading up to 130.0 g/t Au and 25.1% Sb with abundant visible gold. With 13,500 metres at Sunday Creek in less than two years the Company considers Sunday Creek to have the potential to be a truly significant exploration discovery in Victoria with fifteen (15) >100 cumulative grade x metres ("AuEq g/t x m") holes now intersected.

The two new drill holes (SDDSC038-39) form the 2nd and 4th best drill holes, after SDDSC033, to be drilled to date at Sunday Creek based on AuEq g/t x m. The 3rd best hole (MDDSC025 11.7 m @ 18.0 g/t AuEq) lies 200 m below SDDSC033 showing the scale of the developing system. Mineralisation remains open at depth and along strike. A 10 km mineralised trend that extends beyond the drill area is defined by historic workings and soil sampling at Sunday Creek which has yet to receive any exploration drilling and offers potential future upside.

The Sunday Creek epizonal-style gold project is located 60 km north of Melbourne within 19,365 hectares of granted exploration tenements. SXG is also the freehold landholder of 132.64 hectares that forms the key portion in and around the drilled area at the Sunday Creek Project. Geologically, the project is located within the Melbourne Structural Zone in the Lachlan Fold Belt.

The regional host to the Sunday Creek mineralisation is an interbedded turbidite sequence of siltstones, minor sandstones metamorphosed to sub-greenschist facies and folded into a set of open NW trending folds. Mineralisation at Sunday Creek is controlled by veining, stibnite-gold-matrix breccias and brittle faults. The immediate host for mineralisation is a zone of intensely altered white mica-pyritic siltstones, and white mica-pyrite-carbonate altered dyke rocks.