Canada Silver Cobalt Works Inc. provided an exciting update on its ongoing exploration efforts within the Sangster property. As part of commitment to unlocking the full mineralization potential of this high-value area, have divided Sangster into three distinct zones: Sangster West, T-Bone Lake, and Sangster East. TKey Achievements in Sangster West: Confirmation of Pegmatite Presence: Fieldwork conducted in Sangster West has confirmed the presence of pegmatites, in alignment with historical data filed by Noranda. Notably, there is extensive outcrop exposure, facilitating exploration efforts. However, orientation of these pegmatites appears to be different from the original Noranda mapping and additional
field mapping will be required in the spring, following geochemical analyses of recent samples. Rock Sampling: A total of 18 rock samples have been collected from the area. Fourteen
samples are from pegmatite, the rest are from adjacent granite. These samples are now awaiting transport to the laboratory for comprehensive whole-rock analysis and geochemistry. This data will play a pivotal role in advancing the development of a lithogeochemical map, enhancing understanding of the geological formations in Sangster West and possibly chemical zonation providing data to vector follow up exploration. XRF Readings: In addition to the laboratory analysis, X-ray fluorescence (XRF) readings have been conducted on the collected rock samples. The aim is to establish potential correlations between the XRF readings and laboratory results. These correlations will be explored in the future. If successful, in-field XRF readings could prove to be a valuable tool for pinpointing mineralization. Pegmatite Characteristics: Multiple pegmatites discovered in Sangster West appear to exhibit a north-south trending pattern. The largest of these pegmatites measures approximately 20m meters in width, and can be followed over a distance of at least 70 meters. Additionally, pathfinder minerals such as garnet up to 1 mm diameter in about 25% of the outcrops and a gold-green muscovite have been observed in multiple samples. The pegmatites at Sangster have two types of feldspar, a white/pink potassium-rich feldspar and a grey/blue calcium-rich feldspar. While the presence of heavy moss cover poses some challenges, these areas hold significant potential for future stripping and exploration activities, for next field season. Reinterpretation and Mapping: Following the receipt of initial laboratory results and data, a priority will be to reevaluate and map the Sangster pegmatites. This is part of broader regional lithogeochemical program, aimed at refining understanding of the geological characteristics in this promising zone.