.
Enter the email you signed up with and we'll email it to you.
Location: 5 km SW from Mankessim, Ghana
Level 17, Angel Place 123 Pitt StreetSydneyNew South Wales, Australia2000
Stay on top of the latest gold discoveries. Examine the latest updates on drilling outcomes spanning various commodities.
Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
Shaft depth, mining scale, backfill type and mill throughput data.Full profiles of select mines and projects.
Equipment type, model, size and quantity.Full profiles of select mines and projects.
Camp size, mine location and contacts.Full profiles of select mines and projects.
Elevra has completed Stage 2 of its investment in the Project, entling Elevra to an inial 22.5% interest of Atlantic Lithium Ltd.'s Project ownership. From 1 October 2025, Elevra reduced its funding to 22.5%, with all costs currently being funded by the Company (77.5%) and Elevra (22.5%).
- subscription is required.
Pegmatite-hosted lithium deposits are the target for exploration. This style of mineralisation typically forms as dykes and sills intruding or in proximity to granite source rocks. The Ewoyaa pegmatites contain relatively consistent amounts of spodumene (within the mineralised zones), quartz, albite, potassic feldspar (“k-feldspar”) and muscovite mica, along with numerous other minerals in relatively minor amounts.The Ewoyaa Project area has two clearly defined material types of spodumene bearing lithium mineralisation. The Company has termed these material types as Pegmatite Type 1 (“P1”) and Pegmatite Type 2 (“P2”). P1 material is characterised by coarse grained spodumene bearing pegmatite which exhibits very coarse to pegmatoidal, euhedral to subhedral spodumene crystals. P2 material consists of medium grained spodumene, euhedral to subhedral in shape and can compose up to 50% of the rock. The two material types have different metallurgical recoveries.In general, the Ewoyaa Project area is largely underlain by rocks of the Birimian Supergroup, dominated by volcano-sedimentary lithologies of the Cape Coast Basin, situated on the southeast margin of the extensive Cape Coast Granitoid. Three forms of schist are developed in the area; mica schist, staurolite schist and garnet schist; all of which are a blue-grey colour when fresh, with weathering to a brown colour. All of the schist appears to be quartz-biotite rich and well-foliated. The staurolite occurs as 2mm to 20mm porphyroblasts, while the garnets are generally small 1 to 2mm and could be almandine or possibly spessartine within the quartz-mica schist.Several, presumably Eburnean-aged, granitoids intrude the basin metasediments as small bosses and plugs. These granitoids range in composition from intermediate granodiorite (often medium-grained) to felsic leucogranites (coarse to pegmatoidal grain size), both sometimes in close association with pegmatite veins and bodies.Several roughly north-south trending dolerite dykes cut through the Birimian schist and the later granitic and pegmatite intrusions and are presumably of Miocene age. The dolerite dykes are some 5 to 30m wide and are easily mapped using the airborne magnetic data and also outcrop in places as rounded float and boulders. A single dolerite dyke cuts through the Abonko area, skirting the east side of the aggregate quarry. In the extreme west of the tenement area, a number of subparallel dolerite dykes extend from the coast northwards through and past the large Afrangwa granitic boss. This north-south trending structural corridor of parallel dolerite dykes appears to host roughly north-south trending elongate granitic intrusive bodies and pegmatites as well as the dolerite dykes.DimensionsThe Project Mineral Resource area extends over a north-south strike length of 4,390m (from 577,380mN – 581,770mN), and includes the 360m vertical interval from 80mRL to -280mRL.
Success!