- A gravity survey and a new model of the Steinheim crater
- Morphology and geology
- No Steinheim basin suevite
- “The Steinheim impact crater (Germany) – where is the ejecta blanket?” – Comment on the Buchner & Schmieder paper
- Impact rocks – impactites
The 15 Ma Steinheim basin, very probably a companion to the Ries impact structure, is a typical complex impact structure with a distinct 1,000 m-diameter central uplift (Fig. 1) as also shown by topographical profiles, in a relief map and on the geological map. Commonly, a diameter of about 3.7 km is quoted, but there is evidence that the structure is much larger (see gravity survey).
Fig. 1. Steinheim basin impact structure; view to the north. Source: Google Earth. Typical example of a complex impact crater exhibiting a central uplift (in the middle of the image) that formed in the final phase of impact cratering in the modification stage.