Amplats’ Mineral Resources of Platinum Group Metals (PGM) occur exclusively within southern Africa and are hosted by two distinct layered intrusions: the Bushveld Complex in South Africa and the Great Dyke in Zimbabwe.

Formed over 2 billion years ago from multiple injections of magma into the earth’s crust many kilometres below the surface, the Bushveld Complex is geologically unique due to its size, uniformity of its layering and extent of known mineral content. This saucer-shaped intrusion is over 350km wide, 250km long and up to 12km thick. Over time, the rim of the intrusion has been exposed by erosion, revealing three separate main segments known as the Western, Eastern and Northern Limbs. The Western Limb is split into two lobes (north-western and south- western) by the Pilanesberg complex, a remnant of an alkaline volcanic plug intruded into the Bushveld Complex about 1,250 million years ago. The Eastern Limb is split into two lobes (north-eastern and south-eastern) by the north- east trending Steelpoort fault. The exposed segments exhibit layering of pyroxenites, norites, gabbros, anorthosites and chromitites and this layering occurs across the entire extent of the complex. Within the layers, mineralisation is found in specific horizons containing chromium, iron, titanium, vanadium, nickel, copper and PGM.

The Bushveld Complex comprises three main suites, namely the Rooiberg Group, Lebowa Granite Suite and Rustenburg Layered Suite. The Rustenburg Layered Suite comprises four major subdivisions: the Upper Zone, Main Zone, Critical Zone and Lower Zone. Economic concentrations of PGMs occur mainly in three distinct units within the Critical Zone: Merensky Reef; Upper Group 2 (UG2) chromitite; and Platreef. The Merensky Reef and UG2 Reef occur around the Eastern and Western Limbs of the complex, while the Platreef is found only along the eastern edge of the Northern Limb.

The UG2 Reef, which is consistently developed throughout the EL and WL, is rich in chromitite, but with lower gold and base metal content compared to Merensky Reef. In the WL, the UG2 Reef occurs between 12m and 150m vertically below the Merensky Reef and dips at 18º to 27º in a south-easterly direction. In the EL, the reef occurs between 120m and 400m vertically below the Merensky Reef and dips at 8º to 18º in a south-westerly direction.

UG2 Reef is exploited at Kroondal operations, which consists of two chromite rich horizons hosting PGM minerals, separated by a pyroxenite, parting forming the mineable horizon. The reef dips at ~9º towards the northeast. The two chromitite horizons, termed the UG2 leader seam and the UG2 main seam, are about 20cm and 70cm thick respectively, and the pyroxenite parting has a variable thickness of up to 4m, but is typically <1.5m. The mining cut typically includes both the seams, and the minimum mining width is 200cm and the maximum is 270cm, which includes the internal pyroxenite. The orebody is tabular, laterally continuous with relatively long-range grade consistency and predictability. Reef disruptions in the form of potholing, faulting, IRUP and dykes occur throughout the orebody, resulting in an average geological loss of ~15%, except for Bambanani Shaft which is about 30%.

Kroondal consists of established shallow, mechanised PGM operations in the Western Limb of the BIC.

The UG2 Reef is exploited and the deposit is accessed from surface using decline systems and mined via bord and pillar method. Mining takes place at depths between 250m and 550m below surface.

Kroondal is a large, established operation with all the necessary surface infrastructure to support mining operations. Apart from the five operating shafts, Kwezi, K6, Kopaneng, Simunye and Bambanani, it hosts five shafts under care and maintenance.

ROM ore is treated via two concentrator processing plants (K1 and K2) and there is spare processing capacity at a third concentrator plant, which is currently under care and maintenance (Marikana plant). The concentrate is sold to RPM, a wholly owned subsidiary of Anglo American Platinum, under an off-take agreement.

Currently ore from Kwezi, Simunye and Bambanani shafts is processed at K2 plant. Ore from K6 and Kopaneng shafts is processed at K1 plant.

Three TSFs currently cater for the 600ktpm depositional requirements. Although the current available capacity is not sufficient to cater for the LoM Mineral Reserves, studies are being conducted to assess additional storage facilities in redundant, worked-out opencast and there is a reasonable and realistic chance of this being feasible.

K1 TSF receives tailings from K1 concentrator plant. K150 TSF receives tailings from K1 and K2 concentrator plants (portion of K1). K2 TSF receives tailings from K2 con ........