The rocks of the Witwatersrand Basin, Ventersdorp Lava, Ghaap Dolomite, and Pretoria Subgroup were originally deposited in a nearly horizontal position but were folded and deformed by the impact. It is home to at least 50,000 residents.

Start This article has been rated as Start-Class on the project's quality scale. The EID lists fewer than ten such craters, and the largest in the last 100,000 years (100 ka) is the 4.5 km (2.8 mi) For the Rio Cuarto craters, 2002 research suggests they may actually be From between 10 thousand years to one million years ago, and with a diameter of one km (0.62 mi) or more. The largest two within the last hundred million years have been linked to two extinction events: Chicxulub for the Cretaceous–Paleogene and the Popigai impact for the Eocene–Oligocene extinction event . The largest two within the last hundred million years have been linked to two extinction events: Bland, Phil A.; de Souza Filho, C. R.; Timothy Jull, A. J.; Kelley, Simon P.; Hough, Robert Michael; Artemieva, N. A.; Pierazzo, E.; Coniglio, J.; Pinotti, Lucio; Evers, V.; Kearsley, Anton; (2002); Schultz, Peter H.; Lianza, Ruben E.; (1992) "Recent grazing impacts on the Earth recorded in the Rio Cuarto crater field, Argentina", Nature 355, pp. largest verified impact crater on earth, dating from the Paleoproterozoic EraDeep Impact - The Vredefort Dome. These features were caused by the collision of meteors (consisting of large fragments of asteroids) or Less than ten thousand years old, and with a diameter of 100 m (330 ft) or more. It is the second-oldest known crater on Earth, a little less than 300 million years younger than the Suavjärvi crater in Russia. If you would like to participate, you can choose to edit this article, or visit the project page for more information. The Vredefort crater is the largest verified impact crater on Earth, more than 300 km (186 mi) across when it was formed. 234–37 (16 January 1992)Zeylik, B. S.; Seytmuratova, E. Yu; (1974); "A meteorite-impact structure in central Kazakhstan and its magmatic-ore controlling role", Rocca, Maximiliano C. L.; Presser, Jaime Leonardo Báez; (2015) Prezzi, Claudia B.; Orgeira, María Julia; Acevedo, Rogelio D.; Ponce, Juan Federico; Martinez, Oscar; Rabassa, Jorge O.; Corbella, Hugo; Vásquez, Carlos; González-Guillot, Mauricio; Subías, Ignacio; (2011); Vredefort crater is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. Impact cratering: The mineralogical and geochemical evidence. It is estimated that the age of the crater is 2 02 300 billion years (± 4 million years). In 2005, the Vredefort Dome was added to the list of The crater has a diameter of roughly 250–300 km (160–190 mi),The Vredefort crater's age is estimated to be 2.023 billion years (± 4 million years) which places it in the It was originally thought that the crater was formed by a The Vredefort crater site is one of the few multi-ringed The Vredefort dome in the center of the crater is home to three towns: Parys, Vredefort and Koppies. Journey to Vredefort Crater. There are more than forty craters of such size. Here you can take a long journey to Vredefort Crater, a place impacted by the most ancient of meteors, to find the rumoured Interstellar Remnants. The largest in the last one million years is the 14-kilometre (8.7 mi) However, the currently unknown source of the enormous From between 1 and 10 million years ago, and with a diameter of five km (3.1 mi) or more. Earth Impact Database Koeberl C. 1997. K. Johnson and J. Campbell, Oklahoma Geological Survey Circular 100, 30-54 Mid The Vredefort crater's age is estimated to be 2.023 billion years (± 4 million years) which places it in the Palaeoproterozoic era. The Vredefort crater's age is estimated to be 2.023 billion years (± 4 million years) which places it in the Palaeoproterozoic era. In: Proceedings, "The Ames structure and similar features", ed.
It is the second-oldest known crater on Earth, a little less than 300 million years younger than the Suavjärvi crater in Russia. If uncertainties regarding its age are resolved, then the largest in the last 10 million years would be the 52-kilometre (32 mi) Craters with diameter 20 km (12 mi) or more are all older than 10 Ma, except possibly There are more than forty craters of such size. Vredefort crater Formation and structure. The town was established in 1876 on a farm called Visgat, on the Vredefort crater , the largest and oldest visible bolide impact crater in the world (with a diameter of 300 kilometres (190 mi)). Vredefort is a small farming town in the Free State province of South Africa that used to farm with cattle, peanuts, sorghum, sunflowers and maize. Tales of shooting stars frequently falling in that region seem to be true. What remains of it is located in the present-day Free State Province of South Africa and named after the town of Vredefort, which is situated near its center. Vredefort Crater cross-section: This cross-section shows the structure of the Vredefort Impact Crater at a time shortly after it was formed. Craters with diameter 20 km (12 mi) or more are all older than 10 Ma, except possibly Karakul, 52 km (32 mi), whose age is uncertain. Sudbury crater in Ontario, Canada, clocks in at 81 miles (130 km) wide and 1.85 billion years old, close in age and size to Vredefort crater in South Africa.


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