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Grootegeluk mine

GROOTEGELUK MINE

Grootegeluk overview

Grootegeluk mine is on the southern margin of the Waterberg coalfield, south of the Daarby fault on the shallow opencast portion of the coalfield. The mine is 25km west of the town of Lephalale in the Lephalale magisterial district of Limpopo, South Africa. Grootegeluk can be reached from Lephalale via the hard-topped Nelson Mandela Drive, which is linked to the R510 road connecting Lephalale to the town of Vaalwater to the south and the Stockpoort border post between South Africa and Botswana to the north.

The mine is linked to the suburb of Onverwacht, the town of Lephalale and neighbouring towns, as well as nearby border posts with Botswana via the R510 road.

Grootegeluk comprises of one open-pit mine, which includes two overburden benches, nine RoM benches and three interburden benches. A series of parallel benches are advanced progressively across the deposit via a process of drilling, blasting, loading and hauling with truck-and-shovel fleets. RoM is transported to the Grootegeluk beneficiation complex via haul trucks and in-pit crushing and conveying systems.

Coal is beneficiated via eight different plants that produce power station coal (thermal coal) at 35% ash, variously sized metallurgical coal products at different quality specifications and semi-soft coking coal. Thermal coal is sold to Eskom in terms of long-term coal supply agreements to supply feed coal to the Matimba and Medupi power stations via conveyor belts. Various sized metallurgical coal products at 15% ash and 11.25% ash, semi-soft coking coal at 10.3% ash, as well as steam coal at 12.5% ash are railed to various customers and shipped to international clients via an export harbour. A small portion of the total product is sold on-site to smaller customers and dispatched by road. Beneficiation plant discard is backfilled into the mined-out portion of the open pit while slimes are pumped to a specially designed cyclic pond system from where it is later reclaimed and blended in small quantities with the power station coal produced.

A portion of the mine's product is railed from site to a range of customers by a single-gauge railway line that extends southward to Thabazimbi where it links into the main railway network. Most coal exports are shipped via Richards Bay Coal Terminal (710km south-east of Grootegeluk) and the rest from the Durban harbour (760km south-east of Grootegeluk).

Power supply to the mine is obtained directly from the power station via two 132kV lines that supply the mine's three 840 megavolt amperes (MVA) transformers, which in turn distribute 33 kilovolts (kV) through 12 (20MVA) transformers to the plant and mining operations. Raw water is delivered to the mine and to a water-treatment plant on the farm Zeeland by the 700mm-diameter Hans Strijdom pipeline. The pipeline originates at the Mokolo Dam, in the Waterberg mountains, 39km south-east of Grootegeluk. Potable water from the Zeeland water-treatment plant (11km south-south-east of Grootegeluk) is in turn routed to the mine and local communities.

Figure 11: Grootegeluk mine

Grootegeluk mine
Grootegeluk history

Table 20: Grootegeluk operation history

Date range Company Material notes
1960s to 1980 Yskor – Iscor – Iscor Mining – Kumba Drilling exploration holes before mine commissioning took place (221 boreholes drilled)
1980 to 2020 Kumba – Kumba Coal – Exxaro Resources Continued exploration drilling post mine commissioning (1 247 boreholes drilled)

Since beginning exploration activities at Grootegeluk, the company has changed its name and/or unbundled several times without selling the asset to new owners. Through all these changes, exploration drilling continued in the same way.

Small-diameter boreholes (HQ/TNW size core) were drilled on a 500m x 500m grid when the initial exploration project at Grootegeluk started. The suite of analyses performed at that time was analysed only per coal sample and the amount of core obtained from the boreholes was adequate for all the required analysis. Over time, gradual subdivision of coal zones into smaller units or "samples", as well as added relative density fractions to the suite of analysis, resulted in insufficient sample material in some samples and some relative density fractions for the required suite of analyses.

To accommodate the new sample subdivision and in order to have sufficient material available from each sample for the required suite of analyses to relative densities of 2.20 grams per cubic centimetre (g/cc), it was decided to change the size of exploration boreholes from small to large-diameter: 123 millimetres (mm)-diameter drill core. The large-diameter boreholes were drilled in between the existing 500m x 500m grid of small-diameter boreholes. The reason for this placement of large-diameter boreholes was that analysis of samples from the large-diameter boreholes could be used to supplement analysis of existing small-diameter boreholes where samples and density fractions were absent.

Grootegeluk executes its exploration strategy across the Coal Resource. Boreholes furthest from the open pit are spaced 3 000m x 3 000m and, closer to the pit, infill holes are drilled to reduce borehole spacing to 1 000m x 1 000m. For the area in front of the open pit (10 years ahead of planned pit-advance direction), drilled boreholes form a grid of 500m x 500m. In addition, infill holes are also drilled on a 350m x 350m spacing to cover the area that will be mined in the next five years and percussion boreholes are drilled in geologically complex areas to complement the structural interpretation.

Grootegeluk geology

Regionally, Grootegeluk is in the southern portion of the Limpopo depression, a relatively small corridor between the Limpopo River in the west and the Palala-Pietersburg plateau in the east. Fundamentally, it is a re-exposed post-Waterberg topographical feature on which Karoo sediments were deposited, followed by tectonic activity, which was the primary element responsible for the development of the depression.

The Zoetfontein fault forms the boundary of the Waterberg coalfield in the north while the Eenzaamheid fault forms the boundary in the south. The Daarby fault, with a throw of some 350m, divides the coalfield into a deep north-eastern portion and a shallow south-western portion. The first fresh coal in the shallow south-western portion is on average 20m below surface. The lowermost coal seam (Zone 1) occurs at a depth of about 130m in the shallow portion of the coalfield but this may vary depending on the local structure (Figure 16). The predominantly horizontal coal-bearing formations have a very gentle dip to the south-east near Grootegeluk. Only a few dolerite dykes outcrop in the south-eastern portion of the Waterberg coalfield and no sills have been encountered in any exploration boreholes drilled in the mine right area to date.

The upper part of the coal deposit, the Volksrust formation (approximately 60m thick), comprises intercalated mudstone or carbonaceous shale and bright coal layers. It displays such a well-developed repetition of coal-shale assemblages that it can be subdivided into seven discrete sedimentary cycles or zones (Zone 11 to Zone 5). Smaller subcycles (samples) were chosen within these zones and sampled individually in the exploration phase. This subdivision of coal seams into smaller lithological units is necessary to cater for numerous mining bench definitions and/or product specifications. The terms "zone" and "sample" are used at Grootegeluk instead of "seam" and "ply" due to the site-specific intercalated nature of the coal and shale. The Volksrust formation is classified as a thick interbedded seam deposit type.

The Volksrust formation zones typically start with bright coal at the base. The ratio of coal to shale decreases from the base of each zone upwards. The basal zone (Zone 5) is an exception because of a more homogeneous distribution of coal and shale throughout this zone. The Volksrust formation shale shows an increase in carbon content with depth and varies from a massive bluish-grey mudstone to carbonaceous shale towards the base. Although the thickness and coal quality of the Volksrust formation are reasonably constant across the coal field, a large variation in the yield of semi-soft coking coal and total sulphur content occurs vertically in the coal succession.

The Vryheid formation (approximately 55m thick) forms the lower part of the coal deposit and comprises carbonaceous shale and sandstone with interbedded dull coal seams varying in thickness from 1.5m to 9m. It is therefore classified as a multiple-seam deposit type.

There are five coal zones that consist of predominantly dull coal with some bright coal developed at the base of zones 2, 3 and 4 in the Vryheid formation. Due to lateral facies changes and variations in the depositional environment, these zones are characterised by a large variation in thickness and quality. It is noted in the mine lease area that these zones depreciate in development and coal quality in a westward direction due to sedimentological facies changes. Zone 3 is the best-developed dull coal zone in the mine lease area and reaches a maximum thickness of 8.9m. The basal portion of this zone yields some semi-soft coking coal. Zone 2, on average 4m thick, reaches a maximum thickness of 6m in the mine lease area. The basal portion of this zone also exhibits semi-soft coking coal properties. Zone 2 exhibits the most consistent thickness of all the Vryheid coal zones across the entire Waterberg coalfield. Zone 1, the basal Vryheid coal zone, has an average thickness of 1.38m. Zone 1 contains the best-quality metallurgical coal at Grootegeluk and is suitable to produce char but is not included in the mine plan due to the high-stripping ratio given a 12m thick overlying interburden sandstone seam. Due to previous mining activity, over 5Mt of high-quality low-phosphorous content metallurgical coal from Zone 1 has been sterilised to date by the pit backfill operation.

Grootegeluk Resource evaluation

All exploration boreholes are logged and sampled by experienced on-site geologists, aligned and in compliance with logging and sampling standards, and standard operating procedures. Samples are selected according to seam coal and shale contacts, visual variation in the vitrinite content, assisted by a suite of downhole geophysical logs, and non-coal material present in the seam boundaries. Large-diameter core (123mm) boreholes are drilled for Coal Resource purposes.

Core loss for coal seam intersections is recorded and a recovery of <95% through coal (by volume) is deemed unsatisfactory. Anomalies were investigated and redrilled if required. Logging is conducted by recording lithology down to centimetre scale according to the classification of the various coal "lithofacies"/coal types (shale-coaly, coal-shaly, coal dull, coal mixed/mainly dull, coal mixed, coal mixed/mainly bright and coal bright) based on the discernible lithofacies change and identified marker horizons, particularly through coal zones.

Sampling of boreholes is only conducted after the stratigraphy has been correlated. The geologist in charge supervises all borehole drilling, and is responsible for logging and sampling. Each sample submitted to the laboratory is accompanied by a unique sample number for validation and tracking, as well as a submission list that serves as a sample advice sheet with instructions for analysis. The delivery or turnaround time is calculated as the time from which the laboratory receives the samples to the time when the last batch of analysis is reported. Once the laboratory has received and signed the dispatch sheet, the safekeeping and storage of that batch of samples lies with the laboratory.

Grootegeluk uses Bureau Veritas laboratory for its exploration borehole sample analyses. Bureau Veritas acquired Advanced Coal Technology in 2013, which performed Grootegeluk's analysis of exploration borehole samples since the early 1960s. Advanced Coal Technology was an outsourced company formed from the old Iscor pilot plant laboratories and has been a continuation of services previously provided by Iscor.

The only form of subsampling conducted at Grootegeluk is the separate sampling of coal and shale layers of the Volksrust formation sample units for analyses. The coal and shale samples per sample interval are weighed to determine the samples' relative densities and percentage core recovery. Relative density measurements are carried out at Grootegeluk using the "mass in air versus mass in water" method.

Figure 12: Grootegeluk mine and the adjacent Thabametsi project area


Current sample intervals as per exploration borehole are, in certain cases, subintervals of historical sample intervals. For instance, samples 22A, 22B, 22C, 22D and 22E are subdivisions of sample 22 as it was sampled in historical boreholes hence the nomenclature. When compositing these relevant subintervals, it is fully representative and can be used in conjunction with historical boreholes to describe the same geological unit.

The laboratory follows one of four standard suites of analysis for each sample from Grootegeluk, namely Volksrust formation coal, Volksrust formation shale, Vryheid formation coal and Vryheid formation shale. Coal samples are analysed before shale samples because of potential changes that could take place in the characteristics of the coal due to exposure to the atmosphere.

The analyses performed on the borehole core samples include proximate analysis, ash composition analysis, ash fusion temperature analysis and petrography. Analyses are performed separately on the coal and shale samples after float-and-sink analyses have been performed to obtain fractional analysis for the range of densities. All data received from Bureau Veritas is in digital format and checked against the original request list to ensure the required analyses were conducted and results were recorded appropriately. The digital data is then imported into the same database in which the core log data has been captured (acQuire) and subsequent validation procedures are conducted. This serves to verify laboratory accuracy and it is performed during the data-importation stage.

The Coal Resource classification methodology for both formations is fundamentally based on SANS 10320:2004 and considers borehole spacing, type of boreholes and structural complexity of the Resource. Additional exploration efforts are employed to provide for areas with perceived geological risk.

The classification method is the same for the overlying Volksrust and underlying Vryheid formations Coal Resources for practical considerations. The classification methodology is reviewed each year and reconciliation for that year is used to test the classification criteria. The review addresses specific geological risks expected in the Resource, including increased variability in certain coal qualities, thinning of certain benches by weathering in the Volksrust formation, deterioration of coal formation in certain benches and a gradual increase in the average total sulphur content in general. Only cored boreholes with applicable coal quality data are used and structurally complex areas must be complemented by additional geophysically logged open (percussion drilled) boreholes. Aspects relating to guidelines of the new SANS 10320:2020, specifically regarding the resource classification of the Volksrust and Vryheid formations, are currently under review.

Figure 13: Typical north-south section through Grootegeluk geological model showing the various benches and zones

Grootegeluk mine

Table 21: Grootegeluk Coal Resource reporting criteria

Thickness cut-off (thickness and extraction height considerations) Quality cut-offs (adb) Geological loss (%)
<0.5m Ash content of >65% Variable per bench, calculated each year considering geological model estimation error and physical geological loss

Table 22: Grootegeluk Coal Resource estimation criteria

Item

 

Description

 
Database Borehole database   acQuire  
Data datum LO27 WGS 84
Number of boreholes used for Resource estimation 1 083
Validation Conducted using queries in acQuire and Excel
Data compositing and weighting Coal analyses and beneficiation (CAB) module in Sable Data Warehouse
Model Previous model date   2016  
Last model update 2020 updated
Geological modelling software Geovia MinexTM
Estimation technique Growth algorithm
Grid mesh size 20m x 20m
Scan distance 2 000m
Data boundary 200m
Model build limits Upper: limit of weathering and topography/collar
Lower: Zone 1 floor
Model outputs Roof, floor and thickness grids generated for structure.
  Coal-washability quality grids
Changes to modelling process Definition of Bench 9A to exclude sample 25 and 25S from RoM bench

Table 23: Grootegeluk Coal Resource classification criteria

Resource category Type of boreholes Borehole spacing
(Volksrust and
Vryheid formations)
Structurally complex areas Borehole/ha
Measured Cored boreholes with applicable coal qualities ≤500m Matrix (additional geophysically logged boreholes needed) 0.1
Indicated Cored boreholes with applicable coal qualities >500m and ≤1 000m Matrix (additional geophysically logged boreholes needed) 0.03
Inferred Cored boreholes with applicable coal qualities >1 000m and ≤3 000m Matrix (additional geophysically logged boreholes needed) 0.03

Table 24: Grootegeluk Resource and Reserve statement

Category 2020  
(Mt)
2019 
(Mt)
Difference 
in tonnes 
(Mt)
Difference 
(%)
Reason for change
Measured 2 532  2 786  (254) (9) The decrease is primarily the result of new information (11Mt), reclassification (~151Mt), mining (58Mt) and sterilisation due to the change in LoM plan (56Mt)
Indicated 1 422  1 017  405  40  The change is the result of new information (~255Mt) and reclassification (~151Mt Measured to Indicated)
Inferred 338  653  (315) (48) The change is the result of new information (~325Mt) and the inclusion of a small amount of Resource located in the adjacent Thabametsi mining right
Total Coal Resources 4 291  4 455  (164) (4)
Proved 1 730  2 520  (789) (31) The decrease is primarily the result of mining depletion (56Mt), new pit layout (480Mt) and changes in the Resource base (253Mt)
Probable 898   645  253  39  The increase is the result of changes within the Resource categories (253Mt)
Total Coal Reserves 2 628  3 165  (536) (17) The change is primarily due to the implementation of a new mine plan

Notes:

  • Rounding of figures may cause computational discrepancies.
  • All changes more than 10% are explained.
  • Mining method: OC.
  • Figures are reported at 100% irrespective of percentage attributable to Exxaro.
  • Tonnages are quoted in metric tonnes and million tonnes (Mt). Coal Resources are quoted as MTIS and refer to remaining Resources after 31 December 2020 and 31 December 2019.
  • Coal Resources are reported on MTIS basis.
  • Cut-offs applied as per Resource reporting criteria table.
  • Coal Resources are quoted inclusive of Coal Resources converted to Coal Reserves.
Grootegeluk Reserve estimation

The LoM plan for Grootegeluk was revised in 2020 and the change in the pit layout, mining sequence and LoM schedule are reflected in the 2020 Reserve Statement. All modifying factors were considered and downgraded, where applicable, to the Coal Reserves in the various categories.

RPM Global's XPAC mine-scheduling software is used to derive the remaining saleable Reserves from RoM Reserves in the approved pit layout. After converting the geological model's grids to the appropriate format, the floor, roof and thickness data as well as quality data for each bench is imported into the XPAC model. In this model, validations are performed to evaluate the data for possible discrepancies, such as incremental yields anomalies for each bench, thus ensuring they rise with increases in the relative float densities. The Resource category areas are also loaded into the XPAC model for Reserve categorisation purposes.

The XPAC model integrates new geometallurgical principles into the LoM planning process and scheduling model to better predict as-mined plant performance. This is an all-inclusive model that can simulate all the plants in the Grootegeluk complex from one integrated flow sheet. The key improvement is that the model provides:

  • Combined washability data for all material fed to a specific plant
  • The data is combined for each relative density
  • The impact on plant yield performance, due to the RoM feed consisting of coal from various benches, is modelled

A number of audits have been conducted, in conjunction with the mine, to ensure the process applied is well understood, documented and that predicted product volumes are realistic and transparent.

Item

Criteria

Considered

Comment

Geological data Data has been validated and signed off by competent person Yes Geological structures, seam thickness ≥0.5m, ash content <65%. Coal qualities reported on an air-dry basis
Geological model Geological model was considered and signed off Yes 2020
Structural model Structural model was considered and signed off Yes 2019
Mining Mining assumptions considered and defined Yes Opencast
Assurance Minimum tier 1 assurance (Exxaro governance) Yes Resource and LoM done in 2018
Economic evaluation A concept-level exploitation with economic and mining assumptions, including geotechnical and geohydrological assumptions Yes Exploitation strategy over mining right
Environmental Reasonable demonstration that environmental approvals can be obtained within the context of local, regional and national governmental legislation Yes Current required approvals in place
Tenure Formal tenure must be demonstrated with reasonable demonstration that a mining right approval can be obtained within the context of local, regional and national governmental legislation Yes Mining right (21 years) with reasonable expectation that right will be renewed
Infrastructure Assumptions used should be reasonable and within known/assumed tolerances or have examples of precedence Yes Existing infrastructure adequate or can be upgraded. New required infrastructure under construction
Market A potential market for the product with a reasonable assumption that this market is sustainable Yes Current coal supply agreements for local and export markets

The washability tables for each blast block are imported into the geometallurgical model (XPAC). The geometallurgical schedule imitates reality at Grootegeluk as portions of a single blast block can be allocated to several beneficiation plants in a particular scheduling period. Once the production schedule has run, a blend of blast blocks from different benches is allocated to each plant for each scheduling period. A new composite wash table is then derived for each plant for each scheduling period, which represents the blend of material fed from the mine to that plant. This composite wash table is then used to derive the specific products required to be produced by that plant for that period. A set of calibrated plant factors is applied per plant to adjust theoretical product yields to practical expected levels. It is thus not assumed that a block in its entirety is allocated to one plant only, as this does not represent reality at Grootegeluk. The scheduled mining blocks are of the same size as current actual blast blocks in the mine. The fact that material from different benches is combined and beneficiated simultaneously creates difficulty in reporting saleable product tonnages per bench. The preferred reporting practice at Grootegeluk is therefore RoM tonnes per bench and saleable product tonnes per beneficiation plant.

Indicated Resources are generally converted to Probable Reserves and Measured Resources to Proved Reserves after consideration of all applicable modifying factors. If one or more of the modifying factors have not been fulfilled, Measured Resource is either not converted or the Measured Resource is converted but downgraded to Probable and the associated risk is clearly stated. Inferred Resources are not converted to Coal Reserves.

Some 137Mt of Inferred Resources are included in the LoM plan, representing 5.2% of the LoM plan, and are not considered material. The impact of the Inferred Resources are known, with the majority thereof occurring at the tail end of the LoM plan and are addressed by an integrated exploration plan that is reviewed every year.

Table 26: Grootegeluk production figures

Actual
2019
FC
2020
Actual
2020
FC
2021
FC
2022
RoM (Mt) 56.2 59.8 54.6 61.9 68.4

Table 27: Grootegeluk modifying factors considered in converting Coal Resources to Coal Reserves

Modifying factors Value
Geological loss (varies per bench) 0 to 0.75% for Proved Reserves
0 to 1.5% for Probable Reserves
Thickness cut-off ≥0.5m
Quality cut-offs ≤65% ash content (raw in situ coal)
Mining loss 0 due to the fact that all mining boundaries are reached, no pillars are left
Boundary pillar N/A
Dilution Applied to in situ mineable Reserves due to the inter-layered composition of the deposit
Contamination (varies per bench) 0 to 0.75m applied to interburden seams
Mining recovery efficiency (varies per bench) 0 to 0.75m depending on bench height
Planned average slope angles <61.7 degrees
Practical plant yield Considered in the reserving process as per wash table information per combination of blocks per planning increment and the empirically determined practical yield adjustment factor
Strip ratio cut-off Energy strip ratio >7GJ/ex-pit tonne
Environmentally sensitive areas Areas underlying wetlands and other eco-sensitive areas are excluded from the Reserves with a 100m or 100-year floodline cut-off applied
Legal The layout is within the mining right boundary and not closer than 15m
Social There are no known socially sensitive areas in the pit layout (for example, graveyards and dwellings)
Geohydrological Areas identified are flagged and excluded or reclassified in the reserving process
Grootegeluk known risks

We do not know of any pertinent risks or other material conditions that may impact on the company's ability to mine or explore including technical, environmental, social, economic, political and other key risks.

There are a number of low risks addressed by continuous actions at the operation:

  • Geological structure accuracy: The structure interpretation (fault positions) is based on current points of observation. Additional percussion boreholes are required in structurally complex areas to finalise the position and characteristics of faults. This risk was illustrated by the reclassification of approximately 151Mt of Measured Resources to the Indicated category this year. Our improved structural interpretation of the position and orientation of the interpreted fault positions in the northern pit changed meaningfully enough to warrant a reclassification. When reviewing the supporting borehole information in the area, it was evident that the boreholes within each of the newly interpreted faulted blocks occur in single lines. This presents a challenge when trying to access the orientation and extent of seam development as well as the boundaries of the faulted resource block. Focused drilling will be conducted to outline the fault orientations.
  • Thinning of upper benches: Bench 2 and bench 3 are thinning, and are not present in certain areas of the Coal Resource due to weathering with only a small portion of bench 2 remaining in the next few years. This information has been incorporated in the mine's production schedules. Large portions of bench 2 and bench 3 are still available in the planned pit layout further away from the current production face
  • Increasing total sulphur content in semi-soft coking coal: A trend of increasing sulphur content in the benches used to produce semi-soft coking coal (benches 2, 3 and 4) is observed in the geological model. Coal sulphur content is known to be highly variable, which makes it difficult to estimate accurately. The variability was considered during the revision of the 2020 pit and LoM plan
  • Phosphorus content in semi-coke feed coal: The phosphorous content of bench 11 poses a risk to the production of semi-coke. Bench 11 and Zone 1 are the sources of relatively low phosphorus content coal but bench 11 shows a continual increase in phosphorus content. Studies conducted show that most of the phosphorous content of bench 11 is in the uppermost portion of the bench and can be removed separately to mitigate the risk. In addition, Zone 1 (bench 13) is currently omitted from the mine plan due to its high-stripping ratio but can be used as a sweetener if it is blended with bench 11
  • Resources within the Thabametsi mining right: Approximately 58Mt is included in the Grootegeluk LoM. Both mining rights are held by Exxaro and the risk is therefore deemed low
Grootegeluk excellence

The implementation of the short-term geological model proofs to be a significant valuable instrument for medium and shor- term mine planning. The development of an online geographic information system (GIS) tool to manage pit survey, mining development surfaces as well as COVID-19 management is an exceptional development for the operation.

At the beginning of 2020, the new optimised exploitation strategies were finalised and approved for the various business units in Exxaro. To ensure accurate execution and control, the plans were embedded in Exxaro's business processes through incorporation in the LoM plans and the business plans and budgets. These strategies have been included into the LoM plan for Grootegeluk. This strategy entails a pit-shell redesign to exclude high stripping and low-quality areas and to target high-value areas in the LoM plan.

GG6 expansion project is an expansion of the existing Grootegeluk 2 plant and aims to enable additional production of semi-soft coking coal. First production is expected during 1Q2021.

The new rapid load out station project delivered a rail siding equipped with a load out facility for Grootegeluk. It is a state-of-the art facility and is equipped with a telescopic chute that enables continuous loading of different mix product wagon trains. The development will enhance the infrastructure expansion of the Grootegeluk mining complex significantly.

Grootegeluk mine