Monger Gold Limited announced assay results from follow-up rock-chip sampling on tenements P26/4106 and P26/4106, located within the 17.7km2 Mt Monger South Project. This campaign was designed to follow up MMG's 2022 rock chip sampling with anomalous rock chip samples from a gossanous sediment adjacent to a basalt. Twenty-four additional samples were taken from the same stratigraphic horizon west along strike, extending the anomaly to over 150m with one additional anomalous sample a further 180 west.

The samples were found to be higher in zinc compare to the eastern samples with 8 samples above 0.1% zinc. MMG is planning a geochemical soil sampling program in June 2022 and a second stage geological mapping program, focusing on building a structural geological model (specialist structural geologists at Model Earth Pty Ltd) in July. Samples from the geochemical program will utilise the Ultrafine+ fraction soil. A FLEM geophysics program is planned for July.

Regionally, the Mt Monger South Project (MSP) tenement package is positioned within the Eastern Goldfields Province of the Achaean Norseman-Wiluna Greenstone Belt. The greenstone belt has been subdivided into a number of geological terranes which are separated by regional scale faults. The NNW trending, east/northeast dipping Mt Monger Fault, located to the south and west of MSP, separates the Kurnalpi Terrane in the east from the Kalgoorlie Terrane to the west.

The Mt Monger Shear hosts the Daisy Milano gold mineralisation 5km to the northwest of MSP. A fault separates the Gindalbie and Bulong Domains within the Kurnalpi Terrane. MSP is in the Bulong Domain which consists of a discontinuous lower basalt then a lower intermediate to felsic volcanic sequence with associated volcanoclastic and conglomerate overlain by thick ultramafic to mafic successions known as the Bulong Complex (Daisy Milano Komatiite, Wombola Dolerite and Mt Monger mafic sills and basalts.

Both sequences have been folded into a broad, north-south plunging anticline known as the Bulong Anticline. The MSP is situated in the southern hinge of the anticline. On the eastern side of the Mirror Shear lithological and structural trends show a marked change to predominantly east-west orientations.

The Mt Monger Shear dips southwest into the Mt Monger Fault with bedding and layering dipping in the same direction. Younging is generally towards the south into the Mt Monger Fault. There have been seven major periods of VMS formation, typically corresponding to periods of ocean-closing and terrane accretion.

In geological time the two oldest of these are in the Mid Achaean (around 3200Mya) and the Late Achaean (2700Mya). The Ben Nevis VMS Prospect coincides with the Late Archean time period.