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Orientation: Between Delareyville and Bloemhof
Location:
Project Areas: Delareyville area and Bloemhof area
Licence Type: Prospecting Right
Development Status: Pre Exploration
Licence Area: 444.53 km²
Licence Expiry Date: 20 June 2008 (some licences pending renewal)

 
           

 

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Delareyville area | Bloemhof area

 

 

The Bloemhof Project comprises four groups of farms situated in the North West Province of South Africa between Delareyville and Bloemhof and have been grouped into two areas, namely: -
• Delareyville Area, comprising the Bergspruit and Wolmaransstad West Blocks; and
• Bloemhof Area, comprising the Palmietfontein North and Zoutpan North Blocks.

 
 

History
Diamond diggers first located the diamondiferous alluvial gravels of the Vaal River in the vicinity of Christiana and Bloemhof in the mid 1880’s, and from there, progressively extended their prospecting activities north and north-eastward. By 1912, the rich diggings on Mooifontein and London, south of Schweizer Reneke, had been discovered, as had the equally rich deposits to the southwest of Wolmaransstad.

The bulk of the production from the field took place in the 1920’s, although digging activities on a smaller scale have been more or less continuous since then. A total production of 2,117,380cts has been recorded from 226 farms in the diamond-field, up to the end of 1989, 12 of the farms having recorded over 50,000cts each.

 
 

 

 
 

Local Geology
Ventersdorp lavas or Karoo Shale broadly underlies the diamond fields of the area. The surface on which the gravels are deposited is crudely planar, with a shallow southwesterly dipping slope. The planar surface of the lavas generally exhibits a weathering pattern similar to that of the dolomites, with gullies and potholes eroded into structural trends and intersections, but, in contrast to the dolomite, these surfaces are smoothly rounded. The topographic lows are the trap sites for the alluvial deposits.

The area was the subject of a doctoral thesis by T. R. Marshall, which concentrated mainly on palaeo-geomorphology and structural controls on the fossilised and present drainage systems. The table below outlines the types of gravels described in the thesis: -

 
 

NAME

DESCRIPTION OF GRAVELS

 

Older (A1) Alluvial Gravels

• Oldest gravels;
• Occur 30-50m above present stream systems;
• Possibly underlain by even older unit;
• “Channels” up to 15m in width;
• Vary in thickness, averaging 2m;
• Often overlain by layer of hardpan calcrete up to 2m thick;
• Comprise granule – cobble sized, clast supported, variably calcretised conglomerates;
• Made up of rounded quartzites, vein-quartz, quartz amygdales, jasper and banded iron
..formation (“BIF”), Ventersdorp lavas and Karoo shale; and
• Matrix contains kimberlitic garnets and Ilmenites.

Older (D1) Derived Gravels

• Formed subsequently to the calcretisation of the A1 gravels;
• Solution of the calcrete led to development of typical Rooikoppie-type residual gravel,
..with a yellowish-red fine sandy matrix;
• Rooikoppie is often overlain by a thin(<1m) colluvial gravel;
• Clasts are predominantly siliceous, with minor lava showing advanced calcretisation; and
• Gravels are diamondiferous.

Younger (A2) Terrace Gravels

• Occur 3-8m below present surface;
• Comprises a thin (<5cm) layer of basal sands, overlain by a granule-course cobble
..conglomerate (0.5-2.0m);
• Clast composition similar to A1 Gravels;
• Gravel is poorly sorted and matrix supported with crude horizontal layering;
• Usually overlain by alluvial sands and muds;
• Sequence is either oxidised or reduced, dependent on position of water table; and
• Gravels are diamondiferous.

Youngest (A3) River Gravels

• Only occur in present bed of the Vaal River; and
• The gravels are not relevant to the PDF properties.

Source: TR Marchall (1990)

 
 

The Delareyville Area lies approximately 8km south of Delareyville and 40km northwest of the town of Wolmaransstad and is loosely broken into three different blocks.

The Bergspruit Block comprises seven farms or portions thereof, including Hartsrivierdiamant 363 IO, Goedgevonden 366 IO, Brodricks Valley 386 IO, Bossieslaagte 369 IO, Simonsvallei 382 IO, Vlakpan 381 IO and Oshoek 367 IO.

The Wolmaransstad West Block lies just west of the town of Wolmaransstad. It comprises six farms or portions thereof, including Wolmaransstad 184 HO, De Put 180 HO, Tweeloop 160 HO, Weltevreden 161 HO, Uitkyk 156 HO and Bosrand 158 HO.

Access and Infrastructure
Access to the prospect area is via either the main R47 tarred road running between the towns of Delareyville and Vryburg, or two secondary roads, the 506 and the 507, running from Delareyville to Schweizer-Reneke and Ottosdal respectively. The Harts River runs between the Migdol and Bergspruit Blocks.

Access to the properties is via good secondary roads that branch off the main N12 Highway that runs between Johannesburg and Kimberly. Only one annual stream occurs on any one of the farms and, as the area is semi-arid, water would have to be sourced from boreholes if mining had to commence.

Recent Exploration
Apart from available data compilation and target generation, limited RC drilling has been completed to identify the extent of the gravel runs.

Future Exploration
Boreholes have been sited on alluvial diamond targets identified, it is envisaged that drilling will continue during 2008.

Management & Staff
An on-site geologist is responsible for all exploration activities. Contracting companies will be used for the drilling and bulk sampling exercises.

 
 

The Bloemhof area comprises two relatively large blocks of farms that lie to the north of the Vaal River and to the west of the town of Bloemhof. The Palmietfontein North Block comprises portions of four farms, including Zendelingsfontein 294 HO, Sterkfontein 271 HO, Palmietfonetin 294 HO and Holfontein 276 HO.

The Zoutpan North Block comprises portions of four farms, including Gezicht 265 HO, Kafferpan 273 HO, Blaauwboschpan 293 HO and Holwater 302 HO.

Access and Infrastructure
Access to the prospect area is via either the main R47 tarred road running between the towns of Delareyville and Vryburg, or two secondary roads, the 506 and the 507, running from Delareyville to Schweizer-Reneke and Ottosdal respectively. The Harts River runs between the Migdol and Bergspruit Blocks.

Access to the properties is via good secondary roads that branch off the main N12 Highway that runs between Johannesburg and Kimberly. Only one annual stream occurs on any one of the farms and, as the area is semi-arid, water would have to be sourced from boreholes if mining had to commence.

Recent Exploration
Available data compilation and target generation has been completed.  Limited drilling has shown the presence of an extensive gravel run beneath a calcrete cover on Zoutpan North.

Future Exploration
Boreholes have been sited on alluvial diamond targets identified, it is envisaged that drilling will continue in 2008.

Management & Staff
An on-site geologist is responsible for all exploration activities. Contracting companies will be used for the drilling and bulk sampling exercises.

 
 

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