Odyssey Gold Limited announced highly encouraging drilling results which substantially enhance the potential of the area north of the Cable pit. Highlights: The Company has successfully extended gold mineralisation along the Cable-Bollard trend over a further 400m north of the Cable deposit, giving a total mineralisation extent of approximately 950m at the Cable-Bollard trend. The mineralisation is hosted within two parallel mineralised structures comprising sheared quartz veins in mafics and highly silicified sheared ultramafics and banded iron formations. Significant new intercepts include: 4m @ 27.7g/t from 196m - TCKRC0111; 20m @ 1.2g/t from 132m - TCKRC0117; 4m @ 4.1g/t from 52m - TCKRC0110, 4m @ 2.4g/t from 20m - TCKRC0114; 8m @ 2.0g/t from 32m - TCKRC0116. These results from wide space drilling confirm the potential for the continuity of mineralisation to the north of the Cable pit, which continues to be open down dip and plunge, and along strike. These results significantly increase the potential of the Cable-Bollard area and strongly complement the southern Cable-Bollard trend identified during the maiden drill program. The Company's Phase 2 exploration program comprises approximately 25,000m of drilling as well as a range of geophysical, geochemical, and geological surveys. The Phase 2 drill program includes approximately 20,500m (98 holes) of reverse circulation ("RC") and 4,500m (45 holes) of diamond core ("DD"), focussed mainly on the Bottle Dump and Cable-Bollard deposits, as well as a number of other known areas of gold mineralisation. Odyssey has drilled 8 RC holes in pairs at 100m line spacing along the Cable trend, north of the Cable pit, an area previously untested at depth, but where historical workings appear to extend the Cable-Bollard trend of mineralisation. Four of the eight holes encountered significant gold mineralisation, extending the known gold mineralisation potential approximately 400m north of the Cable pit. Three of four section lines intercepted mineralisation around the anticipated target depths. The section line for holes TCKRC0110 and TCKRC0111 60m north of the Cable pit, have successfully intercepted both the Cable West and Cable East mineralisation structures in a previously untested position, below historical workings. TCKRC0111 encountered 4m @ 27.7g/t from 196m (4m composite samples) in the interpreted Cable West BIF. Section line TCKRC0114-115 has low grade mineralisation disrupted by cross-cutting, late-stage felsic dykes. The current northern-most line (TCKRC0116-117) has intercepted wide (~20m & ~12m) mineralized quartz veins synonymous with the mineralisation along the Cable West trend and also sheared BIF/mafic sequences nearer-surface representing the interpreted continuity of the Cable East trend. The Cable-Bollard trend appears to continue significantly further north beyond the limit of this drilling. The limited historical mapping traces the BIF sequences at surface for approximately 500m further north. Next steps: Continue detailed field mapping north of the Cable pit (400m north is the current limit of the historical mapped mineralised structures). Soil geochemistry north of the Cable pit. Integration of soil geochemistry and detailed field mapping with recent UAV (unmanned aerial vehicle) high-resolution magnetic survey. Infill diamond core and RC drilling to further improve geological understanding and mineralization continuity along the Cable North trend, which is open down dip and plunge, and along strike. RC drilling to test the potential extension of the Cable-Bollard trend further north. Meanwhile, a substantial number of additional RC and diamond drill holes for both Cable-Bollard and Bottle Dump are in the process of sample preparation or assay.