Trillium Gold Mines Inc. reported findings from the spaciotemporal geochemical hydrocarbon (SGH) sampling program completed during the summer on the Company's Confederation Belt properties. The 39,300 hectare contiguous land position lies directly on trend with important discoveries currently unfolding in the Red Lake Mining District and represents one of the and most prospective land packages assembled. Concurrent with the program, prospecting and sampling was carried out over the property which results are still pending.

Independent results and interpretations provided by Activation Laboratories Ltd. ("Actlabs"), from the 17 SGH regional soil sampling grids (Figure 1), identified numerous gold pathfinder anomalies (with rating categories ranging from 1-6), establishing the gold exploration potential of the Company's properties. These encouraging anomalies will serve as priority targets for Trillium Gold's second phase of exploration work in the 2022 field season and, together with the sampling and prospecting program carried out concurrently, are expected to generate multiple drill targets. The three smaller grids in the southwest of the Joy Block were designed as orientation surveys over known base metal and minor gold mineralization intersected in historical drilling.

A large portion of the Joy-Copperlode Blocks are covered by variably conductive outwash and deglaciation sediments (not locally derived) and despite no outcrop identified in these areas, all three returned anomalies, the western-most two confirming the method over known drill hole results. On the Copperlode West block, the F-anomaly is a highly-rated anomaly cut by a NW-SE trending magnetic lineament (possibly D2 orientation?) and represents one of the more encouraging targets in the area. Also of high-rating is the I-anomaly which lies on the western extension of an EM conductor in an area with no known historical geological, geochemical or geophysical surveys.

The J-anomaly was identified as a potential Redox zone by Actlabs, similar to that at the Dixie Hinge and Limb zones sampled by Great Bear Resources The Block 1 anomalies lie within stratigraphy representing the eastern extension of that hosting the copper-molybdenum mineralization near Fredart Lake. The two geochemical signatures appear to be on strike from one another, hosted by iron formation or ferruginous sediments. There has been very little historical work in this area.

The Lucky 7 anomaly lies within an EM conductor trend that has been drilled, off-property, intersecting gold values up to 4 g/t over 1.5ft. Grab samples in the drilled area also ran up to 13 g/t gold. The Block 2 anomaly, among the rated by Actlabs, shows a significant number of high contrast peaks over a large, 600m x 450m area.

Actlabs identify it as a segmented nested-halo anomaly coincident to that of the Redox zone. The potential for gold mineralization here is believed to possibly exist directly below this anomaly. The Fly-Moth N and S grids serve as extensions to exploration work on known prospective and mineralized trends associated with the past-producing South Bay Mine.

There are anomalous gold values in historical lithogeochemical samples in the general area around the mine; however, samples further towards the southwest were not assayed for gold. The SGH grids fill in the data gaps and successfully highlight new gold anomalies. These anomalies are highly rated and show characteristics of Redox Zones as well.

Equally, the geometry of elevated gold in this package of rocks could be suggestive of syn-volcanic fault-controlled mineralization. At the southern edge of Triangle Lake, historical work identified anomalous gold that coincides with a previously mapped fault. These types of relationships bear investigating for refinement or confirmation of ideas with follow-up exploration work planned for 2022.

The Block 3 anomaly coincides with several important features: a regional-scale fault trace, a major volcanic break (cf. Thurston et al, 1980), and a property scale transition from felsic to mafic volcanic rocks. Historical work on the property identified several sulphide zones and/or geophysical conductors.

The few historical drill holes in the general area, inconsistently sampled for base metals and even more infrequently for precious metals, do show elevated copper, zinc and gold in these sulphide horizons.