Vredefort crater

Vredefort crater is the largest "verified" impact crater on Earth. That means we know for certain it was caused by an asteroid or meteorite strike. The crater is in the Free State Province of South Africa. 
In 2005, the Vredefort Dome was added to the list of UNESCO World Heritage Sites as a natural site of geologic interest.
Formation and structure.
The asteroid that hit Vredefort was one of the largest ever to strike Earth since the Hadean eon. The Vredefort hit was some two billion years ago. The bolide is thought to have been about 5–10 km (3–6 miles) in diameter. 
The crater has a diameter of roughly , larger than the Sudbury Basin and the 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 diameter.
The Vredefort crater's age is about two billion (109) years old, which puts it in the Palaeoproterozoic era. It is the second-oldest known crater on Earth, a little less than 300 million years younger than the Suavjärvi crater in Russia. In comparison, it is about 10% older than the Sudbury Basin impact (at 1.849 billion years).
It was originally thought that the crater was formed by a volcanic explosion, but in the mid 1990s evidence showed that it was the site of a huge bolide impact. 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 removed 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 bolide was big and fast enough to cause local volcanism. The BIC is where most of the world's known reserves of platinum group metals (PGMs) are found, while the Witwatersrand basin holds most of the known reserves of gold.
The Vredefort dome in the center of the crater is home to three towns: Parys, Vredefort and Koppies.