TDG Gold Corp. provided a second set of longitudinal sections and cross sections from its interpretation work of the historical drilling and exploration undertaken on the former producing high-grade gold and silver Shasta Mine located in the Toodoggone Region of northern British Columbia. The sections presented in this news release cover the JM-Cayley-Rainier Zones and the O Zone. JM-Cayley-Rainier Zones: The JM, Cayley and Rainier Zones lie to the south and southeast of the historically mined Creek and JM Zones and represent geologically continuous mineralized zones, segregated by minor fault offsets. Collation of historical work also highlights the presence of anastomosing vein sets that have been both mapped at surface and intersected during prior drilling, forming a "horsetail" splay of structures which creates broad zones of near-surface mineralization with an indicated strike length of approximately 1 kilometre with only 300 metres accessed through the historical underground workings. Historical drill holes within these veins are more widely spaced than within the workings itself but demonstrate comparable widths and grades which remain open to the south and at depth. Previous operators also selectively assayed samples from drill core using visual identification of minerals so the full potential of any mineralized gold-silver halo is currently untested. An interval in hole DD83-03 in the southern JM and Cayley Zone (190 metres south of historical workings) returned 66.1 metres at 0.51 grams per tonne ("gpt") gold and 8.81 gpt silver, including 9.1 metres of 3.01 gpt gold and 37.29 gpt silver. This appears to represent a central higher-grade mineralized core surrounded by a broader lower-grade halo. An additional step out 300 metres south within the Rainier Zone returned intervals including 16.2 metres at 2.58 gpt gold and 15.66 gpt silver in hole DD10-05. Collectively these historical results indicate the potential for consistent mineralization which remains open along strike and at depth. O Zone: The O Zone was identified through prospecting and limited drilling during the late 1980s and consisted of limited vein exposures at surface paralleling a fault which appears to be an extension to the JM fault and vein system although there is an untested gap of 350 metres between the two areas. Like other programs on site, assay samples were selected upon a visual assessment and so significant lengths of drill core have not been sampled. Initial reviews suggest mineralization is hosted within a gold-silver bearing breccia along the fault and within the footwall rocks, with sample assays returning intervals such as 3.0 metres grading 2.05 gpt gold and 8.47 gpt silver in hole DD88-25. The O Zone has a known strike length of 320 metres and is open to the southeast and northwest. Shasta Exploration Area Longitudinal Sections for JM-Cayley-Rainier Zones & O Zone: Historical drilling and assay results south of the Creek and JM Zone mine workings are presented here in long section in the target areas known as the JM-Cayley-Rainier Zone and the O Zone. These sections illustrate the southerly extension of gold-silver mineralization from the previously worked Creek and JM zones. The sections demonstrate significant sections of core were not sampled historically. The sections illustrate the potential for further mineralization along strike and down dip.