Solstice Gold Corp. announced that it has established a combined 96 km strategic land position for the purpose of lithium pegmatite exploration located in the Frazer Lake area in NW Ontario, approximately 85 km NE of Thunder Bay and 10 km from the town of Nipigon, Ontario which is located on the Trans-Canada Highway. The new acquisitions comprise a southern staked area of 55 km (261 claims) referred to as the Church Lake Project and an option to acquire 100% of a further 41 km (14 claims) located to the northeast.

Key Features of CLP The CLP is located approximately 5 km south of claims controlled by Pegmatite One Lithium (?PGA?)1 which host a new LCT (Lithium-Cesium-Tantalum) pegmatite discovery. The CLP lies within the halo of a two-mica granite mapped by the Ontario Geological Survey (P3562), which may be the source of LCT pegmatites in the area. The OGS documents numerous tourmaline pegmatites proximal to this intrusive.

A small two-mica granite/tourmaline occurrence 1 km to the west of the CLP boundary is also described. The CLP lies at the southern end of a prominent, regional north-south fault which is coincident with several >95%ile Li lake sediment anomalies. There are also prominent east-west structures throughout the area along its length.

Recent prospecting at CLP has led to the discovery of five 12-30m-wide pegmatites within a 1km x 0.5km area, located close to the main N-S structure noted above, These typically contain quartz, albite and potassium feldspar along with books of muscovite and garnet. Trace minerals observed include beryl or fluor-apatite and an unidentified black prismatic mineral that registers 300-800 ppm Li using LIBS. Additional work will be required to definitively identify these trace minerals.

The pegmatites identified at CLP are often visible using satellite photography. Numerous similar responses are present at CLP. There is no record of any exploration over the CLP area.

Follow up prospecting, sampling and assaying of these pegmatites is ongoing at CLP and additional work will be carried out based on the results of this work. Taken together, the regional geological setting with the Quetico Subprovince, limited information to date from PGA and the identification of lithium indicator minerals on CLP claims are interpreted by Solstice to potentially represent a new, extensive area of LCT pegmatites which may represent the western continuation of the well-known Georgia Lake LCT deposits, located approximately 35 km to the east. Purdom Project The Purdom Project lies partially adjacent to, and east of, PGA claims. The Purdom Project lies approximately 3.5 km east of the OGS-mapped two-mica granite referred to above and is this well within the area where fertile pegmatites may be expected to be present.

Three >95%ile Li lake sediment anomalies lie within the Purdom Project. Given the development of similar anomalies in the PGA and CLP areas where LCT pegmatites are newly documented, the Purdom Project lake sediment anomalies are positive indications of the potential for pegmatite discoveries. There is no recorded historical exploration activity on the Purdom Project.

Examination of satellite materials suggests numerous responses which are similar to those over known pegmatites at CLP. Prospecting to commence before the end of the summer.