It is 3.8 km in diameter and the age is estimated to be about 14.3 million years (Miocene). The crater is exposed at the surface. It had previously been thought that the two craters formed simultaneously by the impact of a double asteroid 14.8 million years ago, but a study published in 2020 suggests that Steinheim could actually be about 500,000 years younger than Nördlinger Ries.[5][6]
J. Baier, V. J. Sach: Shatter-Cones aus den Impaktkratern Nördlinger Ries und Steinheimer Becken. In: Fossilien, 35(2), Wiebelsheim 2018.
V. J. Sach & J. Baier: Neue Untersuchungen an Strahlenkalken und Shatter-Cones in Sediment- und Kristallingesteinen (Ries-Impakt und Steinheim-Impakt, Deutschland). Pfeil-Verlag, München 2017. ISBN978-3-89937-229-8.