Meteoritics & Planetary Science 38, Nr 11, 1551–1578 (2003) Abstract available online at http://meteoritics.org The shape and appearance of craters formed by oblique impact on the Moon and Venus Robert R. HERRICK 1* and Nancy K. FORSBERG-TAYLOR 2† 1Lunar and Planetary Institute, 3600 Bay Area Boulevard, Houston, Texas 77058, USA 2Department of Geology, Hofstra University, Hempstead, New York 11550, USA †Present Address: Department of Earth and Planetary Sciences, Washington University in St. Louis, One Brookings Drive, Campus Box 1169, St. Louis, Missouri 63130, USA *Corresponding author. E-mail:
[email protected] (Received 23 August 2002; revision accepted 12 November 2003) Abstract–We surveyed the impact crater populations of Venus and the Moon, dry targets with and without an atmosphere, to characterize how the 3-dimensional shape of a crater and the appearance of the ejecta blanket varies with impact angle. An empirical estimate of the impact angle below which particular phenomena occur was inferred from the cumulative percentage of impact craters exhibiting different traits. The results of the surveys were mostly consistent with predictions from experimental work. Assuming a sin 2Q dependence for the cumulative fraction of craters forming below angle Q, on the Moon, the following transitions occur: <~45 degrees, the ejecta blanket becomes asymmetric; <~25 degrees, a forbidden zone develops in the uprange portion of the ejecta blanket, and the crater rim is depressed in that direction; <~15 degrees, the rim becomes saddle-shaped; <~10 degrees, the rim becomes elongated in the direction of impact and the ejecta forms a “butterfly” pattern. On Venus, the atmosphere causes asymmetries in the ejecta blanket to occur at higher impact angles.