Amazing facts and figures highlight the scientific debates

 

 

 

 

 

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YOUR HOSTS

Graeme Addison

science writer

I'm a writer of popular science and technology books and articles, a former Professor of Communication whose hobby is now "backyard astronomy" with history thrown in!  I'm a keen mountain-biker and kayaker, so the Dome and Vaal River are my playground.

Karen Addison

researcher

I'm a former teacher who has worked with Graeme on many aspects of science & local history research, and I have got to know the Dome by preparing the maps and data used in our various presentations. My passions are mountain running and education. I manage Otters' Haunt.

 
 

 

This is in many ways the most scientifically controversial of South Africa’s WHS’s. It is not absolutely certain that it is  an impact crater although the evidence is almost overwhelming.

 

INTRODUCTION

A VERY OLD CRATER

Scientific debates continue to swirl around Vredefort Dome

The pages in this section may repeat what appears elsewhere on the website but in more detail and with greater emphasis on the scientific facts and debates.

Some 2.03 billion years ago, something blew a huge hole in the Earth’s surface near the present-dayA visiting scientist studies pseudotachylite,displayed in a rock pavement in the Otavi quarry near Parys town of Vredefort in central South Africa. Three crater rings were formed, the outer one being being the edge of the Witwatersrand and Free State goldfields (from Johannesburg through Klerksdorp to Welkom) some 300-odd km across. The middle one is marked by the Gatsrand, a wide ridge of hills stretching from Potchefstroom in a northeasterly direction, and it can be seen at the Grasmere tollgate on the N1. What remains in the middle is the semicircle of the Dome Bergland, the so-called collar of the Dome core. This collar consists ofmountains formed by Witwatersrand rock strata that were capsized by the blast.

This is the world’s largest known blast crater and the oldest known to exist, the Earth itself being about 4.5 billion years old. Despite its size and the fact that it has been intensively studied, the crater remains controversial in all sorts of ways. For example, reasons for the concentration of gold in the Witwatersrand, encircling the Vredefort Dome in the north and west in a so-called Arc of Gold, remain a subject of scientific dispute. Even the size of the crater is not widely agreed. The Unesco Declaration that identified the Vredefort Dome in 2005 gave its diameter as 190km. This may represent the Dome's eroded surface today, but some scientists say it is 250km across and the original surface of the crater could have been as much as 360km across.

Controversy does not stop with the science. Historically, this area has seen more chaos and carnage than most other parts of South Africa because it lies at the heart of South Africa and thus attracts racial and cultural disagreement over who did what to whom and how history should be interpreted. Sharpeville, for instance, the scene of a passbook protest in 1960 which resulted in the massacre of PAC supporters, lies near the Vaal River outside Vereeniging. The name of the city means “unity” referring to the settlement between white Afrikaners and the English-speakers who formed the white-dominated Union of South Africa in 1910. About the only thing everyone agrees on is that the uniquely beautiful and meaningful natural environment should be conserved.

Blast or Belch?

Scientists differ about the cause and consequences of the blast.

  • The overwhelming consensus today is that it occurred when a wandering asteroid struck the Earth. This lump of space rock could have been the size of Table Mountain or larger, some 11-15km across, travelling at 20-30km a second. It exploded with the force of trillions of H-bombs and immediately melted the crust of the Earth down to about 50km. The hole spat meteorites into space and scattered debris over the earth, darkening the atmosphere for years. Molten rock ballooned upwards from within the crust and this upheaval dome, together with infalling debris, plugged the hole. This is the origin of the “dome” of granite that exists in the centre of the blast zone, now some 30-60km across in parts.

  • Another theory is that the crater was caused by a blast from inside the Earth itself. For most of the 20th century this was the explanation offered for the existence of the Vredefort Dome. But it was always controversial. Recently, researchers have suggested that some large craters – and Vredefort could be one of them – were caused by “Verneshots” as the Earth exhaled a mix of gases, spitting rock into space. Like the meteorite hypothesis, this explanation may account for the strange signatures in the rock – pseudotachylite seams shatter cones (or triangular shards of rock like broken glass from a car’s windscreen), and shock metamorphosis (or tiny markings in quartzite indicating that the rock has been shocked).

World Heritage Site

In 2005 the Vredefort Dome World Heritage Site (WHS) was designated by Unesco.The Dome was previously listed as a National Heritage and it includes several National Monuments such as the Wild Olive Tree Forest at Koppieskraal, and Liebenbergskop where a family of Voortrekkers died at the hands of the Matabele. Vredefort Dome was declared primarily for its geological interest but its ecological, archaeological and historical features add to its value. And its source of main appeal to the general public tend to be the activities, from outdoor adventure to antiques and  artwork.

UNESCO DECLARATION, 2005, Durban

The Vredefort Dome, approximately 120km to the south and west of Johannesburg, is a representative part of a larger meteorite impact structure, or astrobleme. Dating back 2,023 million years, it is the oldest astrobleme found on earth so far. With a radius of 190km, it is also the largest and the most deeply eroded. Vredefort Dome bears witness to the world’s greatest single known energy release event, which caused devastating global change, including, according to some scientists, major evolutionary changes. It provides critical evidence of the Earth’s geological history and is crucial to our understanding of the evolution of the planet. Meteorite impact has played a significant part in the geological history of the Earth, but geological activity on the Earth’s surface has led to the disappearance of evidence from most impact sites. Vredefort’s structure provides the only structurally intact exposure of the basement below the crater floor and is, in this regard, unique.

 

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