Vredefort crater

From Wikipedia, the free encyclopedia
  (Redirected from Vredefort Dome)
Jump to: navigation, search
Vredefort Dome *
The multi-ringed Vredefort crater
Country South Africa
Type Natural
Criteria viii
Reference 1162
Region ** Africa
Inscription history
Inscription 2005 (29th Session)
* Name as inscribed on World Heritage List
** Region as classified by UNESCO

Vredefort crater is the largest verified impact crater on Earth.[1][2] It is located in the Free State Province of South Africa and named after the town of Vredefort, which is situated near its centre. The site is also known as the Vredefort dome or Vredefort impact structure. In 2005, the Vredefort Dome was added to the list of UNESCO World Heritage Sites for its geologic interest.

Contents

[edit] Formation and structure

The asteroid that hit Vredefort is estimated to have been one of the largest ever to strike Earth (at least since the Hadean eon some four billion years ago). The asteroid is thought to have been approximately 5–10 km (3.1–6.2 mi) in diameter.[3]

The crater has a diameter of roughly 250–300 km (160–190 mi),[2] larger than the 200 km (120 mi) Sudbury Basin and the 170 km (110 mi) Chicxulub crater. This makes Vredefort the largest known impact structure on Earth. If the Wilkes Land crater in Antarctica is an impact crater then it is the largest known at 500 km (310 mi) diameter. The Vredefort crater's age is estimated to be 2,023 ± 4 million years which places it in the Paleoproterozoic era. It is the second-oldest known crater on Earth, a little less than 300 million years younger than the Suavjärvi crater in Russia.

It was originally thought that the dome in the center of the crater was formed by a volcanic explosion, but in the mid 1990s evidence revealed that it was the site of a huge bolide impact, as telltale shatter cones were discovered in the bed of the nearby Vaal River.

The Vredefort crater site is one of the few multi-ringed impact craters on Earth, although they are more common elsewhere in the Solar System. Perhaps the best-known example is Valhalla crater on Jupiter's moon Callisto, although Earth's Moon has a number as well. Geological processes, such as erosion and plate tectonics, have destroyed most multi-ring craters on Earth.

The nearby Bushveld Igneous Complex (BIC) and Witwatersrand Basin were created during this same period, leading to speculation that the Vredefort bolide's mass and kinetics were of sufficient magnitude to induce regional volcanism. The BIC is the location of most of the world's known reserves of platinum group metals (PGMs), while the Witwatersrand basin holds most of the known reserves of gold.

[edit] Conservation

Monochrome satellite view of the crater

The Vredefort Dome World Heritage Site is currently subject to property development and local owners have expressed concern regarding sewage dumping into the Vaal River and the crater site.[4] The granting of prospecting rights around the edges of the crater has led environmental interests to express fear of destructive mining.

[edit] Community

The Vredefort dome in the center of the crater is home to three towns namely Parys, Vredefort and Koppies. With Parys as the largest and tourist hub, both Vredefort and Koppies is mainly agricultural-dependent for economy.

On 19 December 2011 an broadcasting license was granted by ICASA to a community radio station to broadcast for the Afrikaans and English speaking members of the communities within the Vredefort dome.

The Afrikaans name Koepel Stereo refer to the dome and announces its broadcast as KSFM. The station broadcast on 94.9 MHz FM


[edit] References

[edit] External links

Coordinates: 27°0′S 27°30′E / 27°S 27.5°E / -27; 27.5

Personal tools
Namespaces
Variants
Actions
Navigation
Interaction
Toolbox
Print/export
Languages