Lebowakgomo sits south east of Polokwane on Transvaal Supergroup and Bushveld margin ground, below the Strydpoort mountains.
Quartzite and shale with Bushveld rock nearby, so yields vary with which unit sits beneath the property.
What Is Under Lebowakgomo
The formations below are what a rig actually meets on a Lebowakgomo property, and between them they govern the depth, the casing requirement and what the hole will realistically give you.
| Formation | Where it sits | What it means for drilling |
|---|---|---|
| Malmani Subgroup dolomite | The eastern Sekhukhune margin toward Abel Erasmus Pass and the Echo Caves | Karstic and by far the best aquifer in the district: around half of boreholes exceed 5 litres per second, and in one eastern dataset only three of 84 holes were dry. |
| Pretoria Group quartzite, shale and andesite, and Rooiberg felsite | Much of the district around Lebowakgomo and Jane Furse | Combined intergranular and fractured, with dominant yields of a tenth to five litres per second. The purely fractured portion medians only a tenth to half a litre. |
| Marble Hall Fragment, and Olifants river alluvium | Around Marble Hall, and along the Olifants and Elands channels | The Marble Hall carbonate was metamorphosed by the Bushveld intrusion to marble and calc-silicate and has lost much of its karst permeability. The river alluvium, by contrast, seldom gives under 5 litres per second. |
Send your street and what the water is for, and get an itemised quote for Lebowakgomo.
Get a Lebowakgomo Borehole QuoteWhat That Means for Your Borehole
- Dolomite needs a different drilling protocol, because cavities cause loss of circulation and sudden rod drops. Casing through the overburden and any cavity zone is essential, and this is the formation associated with sinkhole risk nationally.
- The name Marble Hall is misleading about the water. The carbonate there is metamorphosed marble rather than fresh Malmani dolomite, so it does not deliver karst yields. Do not budget on the strength of the town's name.
- Karst water is excellent and extremely vulnerable, with chloride, sulphate and nitrate varying so widely in dolomite analyses that the water department reads it as a contamination signature. Conduits move surface contamination fast.
Where We Work Around Lebowakgomo
- Lebowakgomo zones and the central area
- The legislature and government precinct
- The Strydpoort mountain footslopes
- Zebediela and Chuenespoort approaches
- Schools, clinics and institutional facilities
- Surrounding villages and settlements
What to Watch For Here
Footslope positions below the Strydpoort recharge better than the flats and are generally the stronger prospect.
The mixed geology means neighbour results are a weak guide, because two properties nearby can sit on quite different rock.
What the Water Is Used For
- Household supply where the analysis allows it
- Garden, vegetable patch and fruit trees
- Standby supply through municipal interruptions
- Stock and poultry watering on larger plots
- Reducing a monthly municipal water account
Wellpoint or Borehole?
Yes on the Olifants river alluvium around Marble Hall and Groblersdal, where yields seldom fall below 5 litres per second and quality is good. Not on the dolomite, the Pretoria Group or the Bushveld rock. One trap worth knowing: the general authorisation excludes alluvial aquifers directly connected to a stream from the definition of a groundwater resource, and abstraction within 100 metres of a watercourse's riparian edge needs a licence regardless of volume. A shallow hole or a wellpoint in live river sand is therefore a licence question, not a registration one, even at modest volumes.
Water Quality in Lebowakgomo
Dolomite water averages around 63 millisiemens per metre with nitrate and fluoride within limits, but the variability is the story: coefficients of variation above 200 per cent for chloride, sulphate and nitrate are read as a contamination signature in karst. At catchment scale the issues are secondary salinisation from irrigation return flows in the Loskop scheme, pesticide residues including elevated DDT at several sites, and phosphate from non-compliant wastewater works. Acid mine drainage in the Olifants is confined to the upper Mpumalanga reaches, not here.
A water analysis is what turns that from a general expectation into a number for your specific hole, and treatment should be specified against the result rather than against the area's reputation.
Registration and Abstraction
Registration for water use in Limpopo sits with the Department of Water and Sanitation through its national registration system, not with the municipality. We could not find a published municipal borehole by-law anywhere in the province, so we do not claim one exists. What municipalities do enforce is the prohibition on cross-connecting a borehole to the municipal reticulation, and their ordinary building and planning rules. Separately, the National Water Act governs how much you may abstract. Reasonable domestic use and small-scale garden watering generally fall under Schedule 1 and need no licence or registration, but taking more than 10 cubic metres a day from groundwater on a property must be registered, and irrigation or commercial volumes usually require registration or a water use authorisation from the Department of Water and Sanitation.
Related Services
For the drilling process itself, the geology across the rest of the country and how a quote is put together, see Borehole Installers South Africa.
Borehole Prices in Lebowakgomo
Drilling is charged per metre, so depth drives the total. The ranges below are framed for local ground conditions and access.
| Item | Indicative range | What moves it locally |
|---|---|---|
| Drilling, per metre | R500 - R1,250 /m | Dolomite drills quickly until it does not: cavities cause circulation loss and rod drops, which is time and risk rather than metres. |
| uPVC casing, installed, per metre | R450 - R850 /m | On dolomite this is the critical item. Casing through overburden and any cavity zone is what keeps the hole from becoming a ground-stability problem. |
| Mobilisation and site establishment | R3,000 - R15,000 | Access, distance and site conditions move this; a site visit settles it before quoting. |
| Water survey | R5,000 - R12,000 | Targets structure rather than depth. Worth most where yield is fracture-dependent. |
| Yield testing | R3,500 - R15,000 | Establishes the sustainable rate that pump selection depends on. |
| Pump, supplied and installed | R15,000 - R45,000 | Greater depth means more head, which means a larger pump and heavier cable. |
| Storage and booster | R12,000 - R35,000 | Needed wherever peak demand exceeds the borehole's sustainable rate. |
| Typical complete project | R75,000 - R215,000+ | Everything above, excluding treatment, which depends entirely on the water analysis. |
These are indicative ranges, not a quotation. They are compiled from published South African supplier and contractor pricing to give you a starting point for budgeting. They are not our rate card, and no figure here is a commitment.
Treat them as a broad guide only. Published borehole pricing in South Africa varies enormously - different 2026 guides quote per-metre drilling rates for the same province that differ by a factor of three - because depth, geology, access, specification, distance and fuel costs all move the number. Depth in particular is not known until the hole is finished. Figures generally exclude VAT unless noted, and change over time. Only an itemised written quote against your actual site means anything.
Lebowakgomo Borehole FAQs
What is under Lebowakgomo?
Transvaal Supergroup quartzite and shale with Bushveld rock nearby, which is a more mixed picture than the uniform basement further north.
That mix is why a site assessment carries more weight here than an area average does.
Can government offices here run on boreholes?
Partly, for grounds irrigation, washdown and non-potable use. A full potable supply for a large facility is a bigger project.
It starts from total daily demand and tested combined yield, then storage sized to cover a day.
Is there dolomite under Lebowakgomo?
Real Malmani dolomite sits along the eastern margin of this district, toward Abel Erasmus Pass and the Echo Caves, and where it is present it is the best aquifer around: about half of boreholes exceed 5 litres per second.
Around Marble Hall itself the carbonate is a Transvaal inlier that the Bushveld intrusion metamorphosed to marble and calc-silicate, and it has lost much of its karst permeability. The town's name is not a promise of yield.
Why does dolomite need special care?
Because it dissolves along fractures over geological time, leaving cavities and variable ground. Drilling into that without assessing it first risks losing circulation, dropping rods, or creating a stability problem at surface.
It is also the formation associated with sinkhole risk in South Africa. The ground assessment and a proper casing and sealing specification are what make it safe, and a quote that ignores them is worth questioning.
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