The ore deposit in Malmberget includes 21 ore bodies of various size and shape. They are spread out over an area of 5 kilometers in the W-E direction and 2,5 kilometers in the N-S direction. The ore bodies in the western field inherit 90-95% magnetite and 5-10% hematite while the ore bodies in the eastern field is constituted of almost 100% magnetite (International Mining, 2014).

The most frequently occurring polluting minerals are apatite, amphibolite, pyroxene and biotite and the ore bodies are commonly surrounded by breccia or skarn breccia types. The host rocks inherits a felsic to mafic composition and are usually called leptites in the Malmberget area. The Malmberget deposit is stronger metamorphosed and deformed than the Kiirunavaara deposit and has been exposed to ductile deformations (Martinsson, 2004). Granite veins often intrude the ore (Hedstrom et al., 2001). The dip of the ore bodies varies from 45° to 70° and the iron content varies from 54 to 63% (Hedstrom et al., 2001).

The mine is divided into two parts: the western and eastern fields. The ore bodies in the eastern fields are composed of massive magnetite ores with a current known depth of 1600m and provide 80% of the total production (Lund, 2013). The western fields consist of small magnetite-hematite deposits with a current known depth of 950m (Lund, 2013). The ore bodies in the eastern field are Alliansen (Al), Fabian (Fa), Kapten (Ka), Dennewitz (De), Parta (Pa), Printzsköld (Pr), Ö ........

The Malmberget mine has scattered ore bodies with varying mine design parameters.

The mine design and layout at the Malmberget mine vary from one ore body to another. The Malmberget mine uses both transverse and longitudinal layouts for production, depending on the width of the ore body. This provides the mine with the flexibility to employ different mine layouts to reduce ore loss. The layout at one level can be longitudinal and the level below can be transverse, making the layout more complicated than a typical SLC operation. In most cases, levels up to 780m (below surface) have a longitudinal SLC layout, while levels from 805m and below have a transverse layout (Kristina Jonsson, personal communications, 2015).

A drift´s orientation is guided by ore geometry and ore geology. The production drifts are planned to avoid weak zones and zones with major waste intrusions (Sven-Erik Wennebjörk, personal communications, 2015). Longitudinal SLC accounts for 10% of the production and transverse SLC accounts for 90% (Sven-Erik Wennebjörk, Personal communications, 2016). The sublevel interval varies from 20 to 30m (floor to floor) depending on the ore body. The drift spacing stays constant at 22.5m (centre to centre) for all ore bodies. The overall orientation of the production drifts is optimized to minimize ore loss, as the ore body shape and size varies. But this variation results in a complex network of production drifts, and drifts at the upper levels are no ........

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