Global Energy Metals Corporation announced a renewed exploration strategy based on a reinterpretation of data resulting in a summer 2024 exploration plan at its Monument Peak Copper-Silver-Gold Project in Lemhi County, Idaho, United States. Monument Peak is located east of Salmon Idaho, along the Montana border. Highlights.

Monument Peak, consisting of 84 claims, is an exploration-staged, high-grade, copper-silver by the Fraser Institute. Monument Peak, consisting of 84 claims covering approximately 1,708 acres (approximately 691 hectares), is an exploration-staged, high-grade, copper-silver-gold project, which includes two small past-producing copper mines: Jackson and Hungry Hill. Sporadic exploration, development and production occurred in the region, primarily during the early 1900's, with some additional development in the 1950's. The most recent exploration occurred during the 1970's and 1980's. The Cu-Ag +/- Au mineralization at Monument Peak was described (Mitchel, 1972) as having "unusual continuity" in association with structural zones hosted by sericitic quartzites, which can be traced along a 3,200 m strike length.

Mineralized width generally ranges from 3 to 6 m but can reach up to 50 m. Meta- morphosed host quartzites are Proterozoic (1.47 - 1.37 Ma) of the Gunsight Formation and are underlain by the Yellow Lake Formation. Following a reinterpretation of both historical and more recent data, including field work conducted by Dahrouge Geological Consulting USA Ltd. (DGC), a new geological model has been proposed and warrants further investigation. Of particular interest is that similar styled copper-silver mineralization is observed within northern Montana, near the Montana - Idaho border, termed the western Montana Copper Belt.

This belt is host to several large sediment-hosted stratabound copper-silver deposits within quartzites of the Proterozoic (1.47 - 1.40 Ma) ReveW Formation. Three significant deposits have been documented - Rock Creek, Montanore and Spar Lake: Rock Creek contains an inferred resource of100 Mt of 0.7% Cu and 1.5 oz/ton. Montanore contains an inferred resource of 112 Mt of 0.7% Cu and 1.6 oz/ton Ag.

Spar Lake contains 81 Mt of 0.63% Cu. Hayes et al. (2010) describes sediment-hosted stratabound copper deposits as characterized by their copper mineralization, exhibiting extensive lateral zonation from chalcopyrite through to chalcocite and bornite within sedimentary or metasedimentary hosts.

These deposits are categorized into three types based on host lithology and reduced mineraliza'on environment responsible for precipitating copper sulfides from oxidized sedimentary brines: Reduced-facies type in organic-rich shale and mudstone. Sandstone-type in petroleum-associated sandstone/quartzite. Red-bed type in fluvial sandstone with carbonized plant matter.

The Revett, or sandstone subtype, is associated with nearshore marine and beach sand- stones and fluvial and aeolian environments. These deposits are typically situated within the topset beds of deltaic sedimentary packages, characterized by their geological setting that facilitate the stratiform distribution of copper minerals. The Revett subtype is characterized by diffuse reductant distribution in the sedimentary matrix, which is crucial for the mineralization process.

The dimensions and mineral content of sediment-hosted stratabound copper deposits vary by type, with reduced-facies and sandstone deposits achieving notable copper grades and tonnage in contrast to red-bed types. Morphologically, these deposits range from sheet-like to lens-shaped bodies, covering vast lateral extents of mineraliza'on. These deposits also stand out as vital sources of gold and silver, with their distinct mineral zonation setting them apart from other sedimentary copper deposits.

A previous exploration program at Monument Peak undertaken by DGC in 2021, included the collection of 557 soil and 13 rock samples to assess mineralized strike potential. Project highlights follow (from North to South): Highlights of Soil Sampling and Geological Reconnaissance: Rock samples ranged up to 5.61% Cu, 175 g/t Ag, 17.6 g/t Au; the samples returned an arithmetic average of 2.18% Cu, 63 g/t Ag, 3.65 g/t Au, Soil samples show strong geochemical (Cu, Ag, Au) anomalies along the known mineralized trend, which extends for 3,200+ metres, A mineralized pit in the south part of the property was identified 200 metres due east of previous known mineralization. A newly identified historical trench between the south and central showings confirms continuity of mineralization, and Workings, outcrops, and soil geochemistry imply the mineralized system could be continuous over its entire known strike length of 3,200+ metres.