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SRK Consu Bosl/Brac Figure 4- lting: 453803: A 4 Geologic Arnot to Gumen cal map sho i High Voltage L owing Strati Lines-Stage 1 U graphy in re Undermining Stu elation to pr udy (Interim) roposed rou 453803_Ar utes not_Gumeni Underm mining Study_Stage1 _InterimFinal_20121 1107.docx Page November 201 e 7 12
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4 Geologic al map showing Stratigraphy in relation to ...€¦ · 4.5 Regional and Structural Geology The 1: 500 000 geological map for the area (Geological Series) shows that the

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Page 1: 4 Geologic al map showing Stratigraphy in relation to ...€¦ · 4.5 Regional and Structural Geology The 1: 500 000 geological map for the area (Geological Series) shows that the

SRK Consu

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not_Gumeni Undermmining Study_Stage1_InterimFinal_201211107.docx

Page

November 201

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Page 2: 4 Geologic al map showing Stratigraphy in relation to ...€¦ · 4.5 Regional and Structural Geology The 1: 500 000 geological map for the area (Geological Series) shows that the

SRK Consu

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not_Gumeni Undermmining Study_Stage1_InterimFinal_201211107.docx

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November 201

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Page 3: 4 Geologic al map showing Stratigraphy in relation to ...€¦ · 4.5 Regional and Structural Geology The 1: 500 000 geological map for the area (Geological Series) shows that the

SRK Consulting: 453803: Arnot to Gumeni High Voltage Lines-Stage 1 Undermining Study (Interim) Page 9

Bosl/Brac 453803_Arnot_Gumeni Undermining Study_Stage1_InterimFinal_20121107.docx November 2012

The general locality, topography, geology and slope classification maps covering the study area are

provided in Figures 4-2 to 4-5 below.

4.2 General Mining Activities in the Study Area The study area falls within a region of South Africa notorious for its coal deposits. Other mining and

quarrying activities are also present in the general Mpumalanga area, however coal mining has been

identified as the main mining activity with the relevant study area.

The coal deposits in the study area are exploited by various separate small to large scale

mines/collieries.

The largest operational mine in the area is Arnot, which is owned by Exxaro Resources Pty (Ltd)

(Exxaro), this mine extracts coal using both underground and opencast operations and produces

5Mtpa of power station coal. Arnot uses mechanised mining methods and continuous mining

processes.

Other operation also under Exxaro’s control includes the Glisa and Strathrea collieries. The Glisa

colliery employs both opencast and underground mining methods whereas at Strathrea Colliery only

surface mining methods are utilised. The visual surface extent of the Glisa Colliery falls outside of

the study area; however the exact areas affected by underground workings could not be determined

during this desktop study.

The Belfast Colliery, in close proximity to Glisa has been decommissioned according to the

Department of Resources (DMR), this colliery however falls outside of the study area.

Two relatively small areas were identified in Google Earth where evidence of mining activities was

noted. However the operators of these pits could not be identified. It is suspected that these areas

may form part of Arnot’s mining lease and are being mined as part of the Arnot operation, however

no confirmation of this could be obtained as yet.

The approximate location and surface extent of current mining activities identified within and in close

proximity to the study area have been outlined and are illustrated in Figure 4-2 to Figure 4-5 above.

The areas indicated in Figure 4-6 below show the small scale mining activities noted of unidentified

operators within the study area.

4.3 Sourcing Information from current mining operations As indicated by the DMR, government departments only keep records of decommissioned

operations. As the operations that will potentially influence the proposed routes under investigation

are currently in operation, the relevant information needs to be directly sourced from these

companies.

During the Stage 1 investigation various officials from the Exxaro operations were contacted to try

and source the relevant information; however to date this information has not yet been made

available to SRK to utilise. The mining operations requested that a formal request be made to them

by ESKOM before releasing any information.

After further discussion with the business unit manager of the Arnot mining operation, Mr Chris

Ballot, the following was indicated:

Arnot mine is willing to provide SRK with the relevant detailed information of the mining

areas under their control coinciding with the proposed routes,

They will only be able to provide this information at a later stage due to unavailability of key

personnel that would need to assist in this regard.

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SRK Consulting: 453803: Arnot to Gumeni High Voltage Lines-Stage 1 Undermining Study (Interim) Page 11

Bosl/Brac 453803_Arnot_Gumeni Undermining Study_Stage1_InterimFinal_20121107.docx November 2012

affected negatively by underground activities is not yet confirmed as detailed information is still to be

sourced from the respective operations.

4.3.3 Mining Activities interaction with Route 5

It is believed that sections along the first few kilometres of the route from the Arnot substation

traverse areas falling within the Arnot colliery mining lease area. The extent of areas affected by

underground activities is not yet confirmed.

A small opencast mining area was noted along this route. Further investigation into the owner of this

mining operation and planned future extensions will need to be investigated.

4.4 Potential Future mining development From internet research it has come to light that the Glencore group recently acquired some of the

main coal mining operations in the area including the Klippan and Grootpan collieries situated to the

west of the study area. A planned colliery named Wonderfontein is due to start operations in 2013.

From discussion with relevant persons from the DMR and also local mining operators it is possible

that this future operation may be situated within the study area. No concrete information confirming

the location of this new mining development could however be sources.

The location of the new Wonderfontein mine will be confirmed and included in an update of this Stage 1 report.

4.5 Regional and Structural Geology The 1: 500 000 geological map for the area (Geological Series) shows that the study area is

predominately underlain by sedimentary rocks such as sandstones and shale of the

Madzaringwe/Vryheid Formation which is part of the Ecca Group forming part of the Karoo

Supergroup. The Dwyka group is also present within the study area. Small portions of the study

area are underlain by rocks from the Transvaal Supergroup generally comprising meta-sedimentary

rocks from the Pretoria Group. Some intrusive Karoo Dolerite is also mapped in the area as well as

intrusive rocks forming part of the Rustenburg layered suite.

Mapped faults are shown traversing the study area in the most eastern regions and intersect Route 1

and Route 5 once. Two fault lines intersecting Route 3.

Figure 4-4 and Figure 4-5 above illustrates the site location in relation to the main geological data

available for the study area as described above.

The current mining activities identified are all located in areas underlain by rocks from the Karoo

Supergroup as coal deposits tend to be concentrated in rocks from the Karoo Supergroup. It is

therefore safe to assume that other areas associated with this geological unit, not yet mined, may be

associated with exploration and mining activities in future.

4.5.1 Predominant Geology - Route 1

The geology traversed by Route 1 is dominated by the Karoo Supergroup sediments with

approximately 35% of the route underlain by lithologies belonging to this Supergroup. Other

lithologies include rocks from the Pretoria Group and some intrusive dolerite. These lithologies

comprise the remaining 65% of the route ranging between 1.5% to 18% respectively.

4.5.2 Predominant Geology - Route 3

The geology traversed by Route 3 is dominated by the Karoo Supergroup sediments with

approximately 74% of the route underlain by lithologies belonging to this Supergroup. Other

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Bosl/Brac 453803_Arnot_Gumeni Undermining Study_Stage1_InterimFinal_20121107.docx November 2012

lithologies include rocks from the Pretoria Group and some intrusive dolerite. These lithologies

comprise the remaining 26% of the route ranging between 1.75% to 10.5% respectively.

4.5.3 Predominant Geology - Route 5

The geology traversed by Route 5 is dominated by the Karoo Supergroup sediments with

approximately 75% of the route underlain by lithologies belonging to this Supergroup. Other

lithologies include rocks from the Pretoria Group and some intrusive dolerite. These lithologies

comprise the remaining 25% of the route ranging between 2.3% to 7% respectively.

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Bosl/Brac 453803_Arnot_Gumeni Undermining Study_Stage1_InterimFinal_20121107.docx November 2012

5 Conclusions and Recommendations

5.1 General Routes 3 and Route 5 are most likely to be subject to future interactions with new mining operations

as the underlying geology dominating these routes are usually associated with containing mineable

coal reserves.

5.2 General undermining risk areas identified From the limited freely available information that could be gathered for the relevant study area the

following can be concluded regarding undermining risk:

Route 1, 3 and 5 potentially have low to high risk interaction with surface and undermining

associated with the Arnot mining operation. The extent of this interaction is believed to be

limited within the extent of the route traversing the Arnot mine lease area.

In addition to above Route 3 may have low to high risk interaction with undermining

associated the Glisa mining operation. The extent of this interaction is believed to be limited

within the extent of the route traversing the Glisa mine lease area.

In addition to above Route 1 may have low risk interaction with open cast mining associated

with the Strathrea opencast mining operation, should future mining be planned to extend in a

southerly direction. The extent of this interaction is believed to be limited within the extent of

the route traversing the respective mine lease area.

In addition to above Route 5 may have low to high risk interaction with opencast mining

associated with the unidentified mining operation found approximately 14km along the route

from the Arnot substation.

5.3 Further detail investigation required The investigation summarised in this report was completed to gain a general overview of the site

only and forms Stage 1 of the investigation process. The following additional work is recommended:

Obtain the general information from the relevant mining operators and future operators to

confirm the exact zones of potential interaction between the mining activities and the

proposed routes. This information can be evaluated and summarised in an update to this

interim Stage 1 report.

Further desk study will be required to identify details of the undermining at the identified

interaction zones. This will aid in identifying high risk areas requiring further detail analysis.

Further desk study to review available geological information in the vicinity of the delineated

interaction areas to confirm and assess geotechnical stability.

Where deemed required, further intrusive investigation to determine the geotechnical

parameters relevant to the specific location and design of the powerline structures and

infrastructure once such details are more fully known.

From the above work final risk ratings, monitoring and mitigation measures can be

formulated as part of a Stage 2 detailed assessment.

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6 Selected Bibliography

Brink A.B.A., (1979). Engineering Geology of Southern Africa. Volume 3: The Karoo Sequence, Chapter 7-8, pp 177-233.

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