Delta Resources Limited announced that it will resume its drilling program starting January 11th, for volcanogenic massive sulphide (VMS) targets at the Delta-2 property, southeast of Chibougamau, Quebec. Delta wishes to assure its investors and the community of Chibougamau alike that all necessary precautions are being taken to prevent the further spread of the COVID-19 virus. Employees and contractors are isolated in "bubbles", living together to minimize their exposure to the community and all Quebec Government guidelines are being followed. Delta was also in contact with the community of Oujebougamau and is thankful for their continued support. The Delta-2 property covers over 177 square kilometres, located 35 kilometres southeast of the town of Chibougamau, Quebec. Delta is exploring for two distinct types of targets at the property: hydrothermal gold targets and gold-rich polymetallic VMS targets. Delta is planning between 2000 and 3175 metres of drilling in this second phase of drilling, testing up to 18 isolated, never-tested conductors of short strike length, located in the south-eastern portion of the property. The conductors are all located in proximity to the newly interpreted stratigraphic horizon that hosts the past producing Lemoine Mine north of the property (1975 to 1983: 757 585 tonnes @ 9.52% Zn, 4.18% Cu, 4.56 g/t Au and 82.26 g/t Ag) and are believed to hold excellent potential for similar VMS mineralization. In November and December 2020, Delta completed 20 drill holes at Delta-2, for a total of 3425 metres. The first 17 drill holes of the program were aimed at hydrothermal-gold targets in the area of the Snowfall Gold occurrence and between Snowfall and the R-14 Gold prospect while drill holes 18 to 20 were aimed at two VMS targets in the southeastern portion of the property. To date, preliminary results have been received for the first 13 drill holes and there are no significant results to report. Assay results from the last seven drill holes are pending. Drill holes D2-20-18 to D2-20-20, aimed at two VMS targets, were drilled to test conductors sitting on the newly interpreted Volcanogenic Sulphide Horizon. Holes were drilled from footwall to hanging wall and intersected wide sections of intensely altered mafic volcanics, capped by sulphide-bearing felsic tuffs. Alteration in the mafic footwall rocks is characteristic of VMS deposit alteration at amphibolite-grade metamorphism and consists of garnet- sillimanite-amphibole and sericite. The rocks are also crosscut by sulphide stringers of pyrrhotite-pyrite and lesser chalcopyrite. The mineralized felsic tuffs consist of ash to lapilli-size volcaniclastic rocks with semi- massive and disseminations of pyrrhotite and pyrite, with minor chalcopyrite and sphalerite. The holes confirm Delta's new stratigraphic interpretation in the area.