Tilted bedrock in the walls of the main crater Kaali is a group of nine in the village of on the island of. Most recent estimates put its formation shortly after 1530–1450 BC (3237+/-10 14C yr BP).

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It was created by an and is one of the few impact events that has occurred in a populated area (other ones are: and ). Before the 1930s there were several hypotheses about the origin of the crater, including theories involving and processes. Its meteoritic origins were first conclusively demonstrated by Ivan Reinvald in 1928, 1933 and 1937.