Vredefort Dome (26° 52’ to 26° 56’S and 27° 11’ to 27° 26’E) is a World Heritage Site. The site straddles the Vaal river which forms the administrative boundary of the Northwest Province and the Free State Province in the nomination area. It is about 120 km southwest of Johannesburg, between the towns of Parys and Potchefstroom.
Core zone: 30,111 hectares (ha) which includes three nearby 1-ha outcrop satellite sites: the Stromatolite Basal Fault, Pseudotachylite (Quarry) and Chocolate Tablet, sites. It has a planned buffer zone of 14,422 ha.
1,300 m to 1,692.7 m.
Vredefort Dome, some 120 km southwest of Johannesburg and covering 30,111 ha, is a representative part of a larger meteorite impact structure (or astrobleme), which has a radius of impact of 190 km. The eastern boundary of the distorted north easterly trending oval shaped nominated area is found 5 km from the town of Parys, with its western boundary located some 19 km from the town. The southern boundary of the nominated area lies about 6 km to the north of the town of Vredefort, and the northern boundary is about 26 km to the north of the town.
The Vredefort Dome is one of about 200 meteorite impact structures currently known. Its structure is the oldest (2,023 million years) and largest (radius 190 km) so far found on earth. It is one of only three meteorite impact structures known with a diameter greater than 150 km. It is also the most deeply eroded impact structure known, with current levels of exhumation of about 38 km. The nominated area includes part of the ring structure and a cross-section of the geological formations and structures that provide evidence for the impact. On the ground, the magnitude of the diameter of the multi-ring structure and of the forces which contributed to forming the overturned, steeply dipping and highly faulted hills of the Vredefort Dome can best appreciated at a landscape scale from vantage points within the nominated area. The steepest gradient of the Vaal River is found where it courses through the Vredefort Dome hills giving rise to rapids, irregular stream patterns and islands and a range of riverine habitats. Short, sharp streams have formed steep gullies and valleys that have cut into these hills.T he nominated area, delimited by secondary roads, contains the most visible part of the dome’s structure. This comprises part of the central granite core in the rolling relatively flat cropland to the south, dotted with kopjes, and the first concentric rings to the northwest in the Vredefort Hills, which are bisected by the Vaalriver. This landscape is partly grazed hillsides with scattered farms, but the quartzite hills, upturned by the impact, have steep northern slopes and both U- and V-shaped valleys which make for handsome scenery. The gradient of the river cutting through the hills has created many rapids, braids and islands, resulting in a variety of habitats.
The area has a climate of high seasonal and diurnal temperature variation. The summers are hot, wet and average between 15°C and 30°C. Winters are cold and dry with frosts, averaging between -10°C and 18°C. The average rainfall is 625 mm of which 500 mm falls in summer, often in thunderstorms. The prevailing winds are northerly.
In spite of the extensive grazing and cultivation of lower areas of the site, the vegetation is well conserved in some areas and is varied owing to the topographic and geological diversity of the land. Floral mapping of the nominated area recognizes 5 broad communities including the dolomite grassland, andesite mountain bushveld, witwatersrand mountain bushveld, VD granite grassland and the riverine bushland. The dominant vegetation types are, in the north, rocky high veld grassland and banken veld (open grassland of wiry grasses) with hookthorn Acacia caffra. The south is basically grassland. This includes typical bush veld species such as grass veld sugarbush Protea caffra and false hookthorn Acacia hereroensis; also bush willow Combretum spp and red ivory Berchemia zeyheri, which are commoner hundreds of kilometres away. Kopjes hold thick stands of wild sweet olive trees Olea europaea ssp.africana. In between there is riverine bush and various types of hillside vegetation with the hardy deciduous Drege’s tree fern Cyathea dregei in ravines. Lower down are unspoilt well watered wooded valleys containing a variety of microhabitats and trees such as white stinkwood Celtis africana, wild peach Kiggelaria africana, tree fuchsiaHalleria lucida, sagewood Buddleja salvifolia and orange thorn Cassinopsis ilicifolia. At least 99 plant species have been recorded for a part of the area. The following distinct tree and shrub communities have been described; Protea caffra; Acacia hereroensis; Olea europaea ssp africana - Pavetta zeyheri; Combretum molle; Buddleja saligna – Rhoicissus tridentata; Salix capensis; Diospyros lycioidis – Rhus pyroides and Acacia karoo – Protasparagus suaveolens.
Farming extirpated many large animals native to the area though some are being re-introduced on game farms. The area however is very rich for some native species. especially butterflies, and includes many native birds, mammal species and other fauna. Some medium sized animals remain, such as the Cape baboon Papio ursinus, brown hyaena Hyaena brunnea, black-backed jackal Canis mesomelas, serval Felis serval and steenbuck Raphicerus campestris. 50 species of small mammals are still found, among them the spotted-necked otter Lutra maculicollis (VU) and the white-tailed rat Mystromus albicaudatis (EN). The variety of habitats is reflected in the 200 bird species observed which include Cape vulture Gyps coprotheres (VU) and lesser kestrel Falco naumanni (VU), and the area’s listing as an Important Bird Area. Over 70 butterfly species have also been recorded.
Stone Age caves with skulls and tools have been found; and at askoppies (ash middens) in Tygerfontein and Buffelshoek there are late Iron Age settlements with extensive walls which contain deep deposits of cultural material. There is some rock art of the Khoi-San bushmen who once lived there and the ruined kraals of later Sotho and Tswana cultures. There are also remnants of battlefields and 19th century settlements such as the old mining village of Venterskroon, and of gold-mining which continued for 30 years round the turn of the 20th century.
Local Human Population
The site is shared between 149 farms growing predominantly maize in the flatter land over the core of the dome in the south, and in the hills, pastureland with scattered cultivation in valleys. The average property size is about 175 ha but only about half the farms are permanently occupied. Much of the land, except along the river, is marginal for agriculture, and in Northwest province on the north side of the river, grazing is fast declining in favor of game farms and tourism, based on the beauty and variety of the scenery and its proximity to the Gauteng metropolitan area. The idea of nature conservancy has been less developed by the Free State landowners.
Visitors and Visitor Facilities
The countryside of the Dome is beautiful and bio diverse, rich in archaeological remains and easily accessible from Johannesburg. As a focus, the nearby structure of the Dome to the north is very recognizable. Youth camps, hiking and bird-watching clubs already use the area. The potentials for summer tourism, recreation, education and research are high and are beginning to be developed by local landowners as an economic alternative to farming. Seventeen landowners in the hills have game-fenced their farms and begun to re-introduce some of the large game animals formerly existing in the area. Canoeing, rafting and fishing, camping, riding, hiking, mountain-biking and rock-climbing are all pursued on site. There is hotel, guest house and resort accommodation in the nearby towns of Parys and Potchefstroom and in game farms and corporate convention centres on site. In 2001 there was said to be well over 60,000 overnight visitors to the nominated area. .
Scientific Research and Facilities
The Vredefort Dome exposures of formations associated with the meteorite impact are of high quality and the area is of considerable scientific interest. Since it was first recognized in 1937, writing about the dome has been voluminous: at least 750 publications have been listed and researches continue into every aspect of the area. Intensive exploration by hundreds of bore holes of the gold-bearing strata in the northern folds have led to a deep understanding of the structure of the dome. Recently, international workshops held nearby in 1987 and 1999 on explosion structures and on the dome focussed attention on the area. A study of its cultural aspects in preparation for the development of management plans has also recently been completed.
Vredefort Dome is the oldest, largest, and most deeply eroded meteorite impact structure in the world. It is the site of the world’s greatest single, known energy release event. It contains high quality and accessible geological (outcrop) sites which demonstrate a range of geological evidences of a complex meteorite impact structure. The rural and natural landscapes of the serial property help portray the magnitude of the ring structures resulting from the impact. The serial nomination is considered to be a representative sample of this meteorite impact structure. A comprehensive comparative analysis with other complex meteorite impact structures demonstrated that it is the oldest, the largest and the only example on earth providing a full geological profile of an astrobleme below the crater floor, thereby enabling research into the genesis and development of an astrobleme immediately post impact.
The land within the nominated property is predominantly agricultural, has freehold status, and is subject to national, provincial and district statutory regulations. The following national legislation is applicable: The World Heritage Convention Act 49 of 1999; the National Heritage Resources Act 25 of 1999; the National Environmental Managements Act 107 of 1998 and the Physical Planning Act 88 of 1967. At the Provincial level, the Northwest and Free State Provinces have applicable nature conservation ordinances regulating environmental aspects of the area. At the local level, the nominated property falls within the District Municipalities of Northern Free State and Southern District North West, and the Local Municipal areas of Potchefstroom (Northwest Province) and Parys (Free State Province), and their environmental regulations.
In December 2002, the South African National Heritage Resources Agency decided, in principle, to declare the nominated property a National Heritage Site under the provisions of the National Heritage Resources Act 25 of 1999 subject to a Cultural Heritage Survey and Management Plan being completed. This document was completed by February 2005 although no advice of the formal declaration of the National Heritage Site had been received as of March 2005.
In 2004, interim government management structures and actions were put in place in recognition of the potential World Heritage status of the nominated property. They include: The Vredefort Dome Inter-provincial Task Team which provides interim technical and administrative management until a Management Authority is appointed under the World Heritage Convention Act, 1999. The Inter-provincial Task Team is commissioned to develop an Integrated Management Plan for the serial property in accordance with the Act. Part of this process includes preparation by Northwest Province of a Development Plan to include a Strategic Environmental Assessment of the area and a Management (zoning) Plan. This work aims to enhance the stature of the Vredefort Dome as a National Heritage site. A Vredefort Dome Steering Committee, involving district and local municipalities, provincial, and national government representatives, was established to oversee the process of obtaining World Heritage status and the appointment of a Management Authority. A Vredefort Dome Stakeholder Forum was established for public participation and awareness raising about World Heritage status and the establishment of a Management Authority.The area was considered for a National Park but the extent of private ownership made this potentially too expensive.
A Vredefort Dome Bergland Conservancy has been established by private landowners in the Northwest Province as a Section 21 Company. Its main objectives are to convert the private properties of the area into a voluntary nature reserve, and to conserve its unique aspects. The Conservancy has prepared a management plan to facilitate these objectives. It will be represented in the Stakeholder Forum, and it plays an important role in the facilitation of private landowner’s involvement in the nominated property. A Vredefort Dome Conservancy has also been established in the Free State Province by private landowners following the IUCN field mission.
Little threatens the integrity of the area at present, but the anticipated increase in tourist numbers and facilities serving tourism will need regulation.. Gold exists in small quantities but its mining is not seen as a threat by geological experts, and stone quarrying is closely regulated. There is some danger of pollution of the Vaal river by various effluents from the farmland, industry and metropolis upstream which have led to infestation by algae and water hyacinth Eichhornia crassipes. The Vaal valley has also been invaded by the alien water-demanding blue gum Eucalyptus globulus. Prickly pear Opuntia spp, has also spread over the drier land. There has been some erosion on slopes. Future monitoring will concentrate on these potential threats. The amount of land in private ownership may be a source of difficulty
Comparison with Similar Sites
The multi-ring complex meteorite impact structure centered on the Vredefort Dome represents the oldest meteorite impact structure known on earth. The catastrophic, short duration impact that created this feature was the single greatest energy release event ever known to have affected earth. Of the three largest meteorite impact structures, Vredefort Dome is not only the largest (380 km diameter) and oldest, but it has better exposures of impact evidences than either Sudbury in Canada (250 km in diameter, 1,800 million years old) or Chicxulub in Yucatan, Mexica (170 km in diameter, 60 million years old, and also famous for its links to the demise of the dinosaurs at the end of Cretaceous). Field inspections at Vredefort Dome clearly demonstrated the outstanding quality of the meteorite impact geological evidence.
The property’s structure provides the only structurally intact exposure of the basement, below the crater floor of a very large astrobleme. This is unique for the planet. It shows a geological section that reaches from the rocks which once covered the crater floor, through the floor, and down into the basement of the structure. The central cone of the crater rose (rebound) by approximately 38 km to provide a surface outcrop equivalent of mantle rocks. These mantle rocks also show a type of metamorphism found only in conditions of very high energy release. This characteristic may be unique to the nominated property. It is not found at Sudbury and Chicxulub. The energy released created chocolate tablet boudinage in cherts, and their association with distally situated ring thrusts is also thought to be unique. The impact forces overturned 17 km (true thickness) of strata to dip towards the center of the structure. No other similar terrestrial phenomenon of this nature, of a comparable magnitude has (probably) been observed. Like other complex impact structures, Vredefort Dome includes examples of shatter cones, planar deformation features in minerals, high pressure mineral polymorphs. It does not include evidences of impact melts. In conclusion, the nominated property, has high quality exposures of a complex meteorite impact event that are readily accessible. It is a high quality representative example of a meteorite impact structure and has special significance given its status as evidence of the world’s greatest single event release of energy. It is the world’s only structurally intact exposure of the basement, below the crater floor, of a very large astrobleme. It provides the only mappable and restorable profile that illustrates the genesis and development of an astrobleme during the very short time after impact.