New Energy Metals Corp. announced the initiation of exploration activities at the Roslyn Lithium Property (Property) in the Georgia Lake Pegmatite Field located 50 km northeast of Nipigon, Ontario. The Property comprises of 8 mining claims (195 cells) covering approximately 4,215 hectares.

The Georgia Lake Pegmatite Field is being aggressively explored and developed by Roch Tech Lithium, Imagine Lithium and Ultra Lithium. Field crews have mobilized and are conducting mapping, prospecting, and sampling. Highlights: During the current phase of exploration, an experienced field team has been deployed to conduct field prospecting activities across the claim block.

This process will involve the systematic examination and sampling of the potential fertile granitic pegmatite dykes for lithium and other rare elements. This crucial step will provide valuable insights into the mineralogy and lithium content of the identified pegmatites, aiding in the development of an extensive understanding of the property's lithium exploration potential for further work. Initial scanning of samples will be carried out by a handheld laser-induced breakdown spectroscopy (LIBS), which has recently emerged as a tool for instant geochemical analysis versus traditional laboratory analysis and resultant lag time.

The LIBs can measure Li in minerals, rocks, soils, and brines in-situ in the field. Roslyn Lithium Property: The Georgia Lake Pegmatite Field represents the largest concentration of rare-element mineralization in northwestern Ontario. The 32x105 km field hosts 38 rare-element occurrences and 10 spodumene pegmatite deposits (Breaks et al., 2008).

Breaks et al, 2008 discovered 19 additional rare-element occurrences and recommended additional exploration proximal to the fertile Glacier Lake Batholith bodies in contact with metasediments. The Property is hosted by a muscovite-bearing granite, an S-type peraluminous fertile parental granite according to Breaks et al., 2003 and in contact with metasediments which make excellent hosts for pegmatites. Numerous faults transect the Property providing excellent pathways for granitic melts and evolving pegmatites.

Several white pegmatites with garnet and tourmaline have been documented and mapped on the Property by the OGS in 1970 (Ontario Department of Mines map M2293). These are very good indications of fertile granitic melts.