Larvotto Resources Limited announced encouraging nickel and associated chrome results from a recent geochemical soil survey undertaken at the Dickie Dyke prospect at the Company's 100%-owned Eyre Project, located 70km east of Norseman in the Eastern Goldfields, Western Australia. Larvotto's Eyre Project occurs on the mineralised Jimberlana Dyke, historically known to host base metal and platinum-group elements (PGE), recently highlighted by Galileo Mining Limited at its Calisto discovery. Soil Geochemistry: The Dickie Dyke prospect is located on the north-eastern end of the Larvotto tenement.

The majority of E63/1976 was covered by 240m by 180m geochemical soil sampling in late 2022. The sampling identified a strong nickel and chrome geochemical high. Geological mapping has identified that this is associated with the Jimberlana Dyke, an extensive intrusive rock unit noted for its nickel, copper and recently platinum-group elements (PGE) mineralisation.

Larvotto has some 40km of exposure to the Jimberlana Dyke within its 692km2 tenement package at Eyre and this is the third Ni anomaly identified, with the other two being located near Mt Norcott approximately 35km west of the Dickie Dyke prospect. The survey location is 70km east of Norseman in the Eastern Goldfields, WA. The area has historically been largely unexplored, but recently is becoming a focus for numerous companies after the discovery of nickel, lithium and PGEs in the region.

The Jimberlana Dyke is a large mafic intrusive body that is up to 2.5km in width and has been referred to as analogous to the Great Dyke in Rhodesia by Western Mining Corporation, who explored the area in the 1960s and early 1970s and again from 1985 to the late 1980s. Newmont also explored the Mt Norcott area and confirmed the concentration of Ni-Cu-PGE sulphides at the top of a norite rock unit within the Dyke. The main nickel geochemical high at Dickie Dyke is nearly 2km long and has a peak Ni value of 1010ppm Ni which is up to 20 times higher than background samples.

The soil anomaly aligns extremely well with the southern margin of the Jimberlana Dyke which is also forms a distinct airborne magnetic high. The high being represented by the white areas on the image. Government geological interpretive mapping defines the extent of the Jimberlana Dyke in the Dickie Dyke area.

The chrome geochemical high corresponds well with the nickel high above and the southern margin of the Jimberlana Dyke where it is in contact with a granite. Geochemical Survey: The geochemistry program collected near surface soil samples. Average sample collection depth was 15cm.

Samples were sieved to minus 1.6mm and compressed into pucks for analysis by SciAps Portable Xray fluorescence (pXRF). Standards, blanks and repeat samples were included for quality control. Sample spacing was on north - south orientated lines, nominally 240m apart with sample points every 180m along the lines.

Some lines were not sampled where obvious transported soils associated with creeks or flood areas were evident.