Khwezela Operation (Landau and Kleinkopje Collieries) consists of two sections, namely the Kromdraai Section and the Navigation Section (Navigation West extention).

The eMalahleni area is underlain by the Karoo supergroup. The Karoo Supergroup comprises mainly a sedimentary succession of sandstone, siltstone, shale, mudstone, coal, diamictite and tillite. The Karoo Supergroup is lithostratigraphically subdivided into the Dwyka, Ecca and Beaufort groups, succeeded by the Molteno, Elliot and Clarens formations and the Drakensburg Formation. The Ecca Group comprises successions of formations which consists of sandstone, shale and coal and were developed within the Karoo basin locally. A number of intrusive dykes are known to occur within the study area. The positions of the dykes have been interpreted from geophysical surveys, but have mostly been delineated through mapping when intersected in the underground workings (Groundwater Complete, 2013).

The thickest portions of the Ecca Group were deposited in the southern Karoo basin in contrast to the relatively thin sequence which is now preserved in the East Rand. This succession of sedimentary rocks generally overly the well-consolidated conglomerates/diamictites of the Dwyka Formation, but in places the Ecca Group rocks rest directly on the felsites and granites of the pre-Karoo Basement rocks. Igneous intrusions of late Karoo Supergroup age in the form of dolerite dykes and sills also occur through the sedimentary succession. The sills usually precede the dykes, with the latter being emplaced during a later period of tensional forces within the earth’s crust. Tectonically, the Karoo sediments are practically undisturbed. Faults are rare. However, fractures are common in competent rocks such as sandstone and coal.

The sediments of the Vryheid Formation overlie an uneven Dwyka floor, which is controlled by the topography of the pre-Karoo platform upon which the Karoo sediments were deposited. The Vryheid Formation is present throughout the Witbank Area. At their thickest these sediments attain some 120 – 140m and can contain a number of coal seams of which four are considered to have economic potential. This area is known as the Witbank Coal fields.

The Navigation West Section is situated in the northern part of the Witbank coalfield. The coal measured forms part of the Vryheid formation of the Ecca group. All five coal seams, common to the Witbank coalfield, are present in the Navigation West Section area. The No. 4 Seam is suitable for mining by opencast methods. The No. 2 Seam is mostly thin and of moderate to low quality, as are the remaining No. 3, 4U and 4A Seams. The No. 5 Seam ‘sub-outcrops’ near the eastern boundary of the proposed mining area, and although of good quality, is not laterally extensive enough over the Navigation West Section to include in the mining plan.

The No. 4 Seam dips predominantly to the east, but also to the west (in the extreme west) as it is draped over a regional Pre-Karoo basement high. It is over the western part of the area that the No. 4 Seam is completely weathered as a result of its close proximity to surface. This ‘no coal’ area forms a major indent into the South Block and had a defining influence on the mining layout possibilities. The topography to the west, influenced by the upper reaches of the Grootspruit valley, dips fairly steeply towards the west, resulting in a sub-outcrop of the No. 4 Seam. To the east, the various seams dip at about 30 minutes towards the Greenside Colliery underground reserves, where all of the major seams have been preserved and mined to some extent.

Borehole logs of the geological successions encountered in vicinity of the Navigation West indicate a lithology of:
- Unconsolidated material between 0- and 4mbgl.
- Loose and weathered sandstone between 4- and 9mbgl.
- Coal between 10- and 15 mbgl.
- Shale and or sandstone between 15- and 20mbgl.

Kleinkopje Colliery.
Five main seams that are numbered in order of deposition from No.1 seam to No. 5 seam are present at Kleinkopje Colliery, this being typical of the Witbank Coalfield1. The coal- seams are separated by sediments of shale, sandstone and siltstone. The coal reserves of the mine are predominantly found in the No. 1, 2 and 4 seams1. There are limited reserves in the No. 2 Lower and No. 5 seam.

Coal is mined at Landau Colliery from the No.1, 2, and 4 Seams of the Witbank Coal Field.

The Colliery consists of two distinct open cast operations, Khwezela North and Khwezela South. Current mining operations are focused on the Navigation area in Khwezela North. The Bokgoni pit in Khwezela South, is currently on care and maintenance. Mining utilises draglines, and truck and shovel equipment focusing on the extraction of the No. 2 seam on the property.

There are two plants at Navigation Section where coal can be processed and both will be utilised for the proposed Navigation West – South Block Extension Project. The Ngwenya Plant is located within the boundary of the Navigation West Mini pit on Portion 2 of the farm Elandfontein 309 JS. The other plant is the main Navigation Beneficiation Plant located on Portion 23 of the farm Blaauwkrans 323 JS near the old Navigation dump.

The washing plant is primarily subdivided into Wemco drum, cyclone and fines sections respectively. Feed from run of mine (ROM) is subjected to banana screening to separate at 12 mm cut size. The oversize is fed into a drum feed silo while the undersize reports to a different silo, from which it is fed into a DSM cyclone plant. The final product from the three sections is combined and sent to the rapid loading terminal (RLT) and railed to Richards Bay Coal Terminal (RBCT) at calorific value of 27.40 MJ/kg on air dry basis, top size of 50 mm and total ........