Random bombardment by comets, asteroids and associated fragments form and alter the lunar regolith and other rocky surfaces. The accumulation of impact craters over time is of fundamental use in evaluating the relative ages of geologic units. Crater counts and radiometric ages from returned samples provide constraints with which to derive absolute model ages for unsampled units on the Moon and other Solar System objects1,2,3,4. However, although studies of existing craters and returned samples offer insight into the process of crater formation and the past cratering rate, questions still remain about the present rate of crater production, the effect of early-stage jetting during impacts and the influence that distal ejecta have on the regolith. Here we use Lunar Reconnaissance Orbiter Camera (LROC) Narrow Angle Camera (NAC) temporal (‘before and after’) image pairs to quantify the contemporary rate of crater production on the Moon, to reveal previously unknown details of impact-induced jetting, and to identify a secondary impact process that is rapidly churning the regolith. From this temporal dataset, we detected 222 new impact craters and found 33 per cent more craters (with diameters of at least ten metres) than predicted by the standard Neukum production and chronology functions for the Moon2. We identified broad reflectance zones associated with the new craters that we interpret as evidence of a surface-bound jetting process. We also observe a secondary cratering process that we estimate churns the top two centimetres of regolith on a timescale of 81,000 years—more than a hundred times faster than previous models estimated from meteoritic impacts (ten million years)5.
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We acknowledge the engineers and technical support team at NASA Goddard Space Flight Center and Arizona State University who enable the collection of a vast image archive of the lunar surface that will be used for decades to come. This work is supported by the Lunar Reconnaissance Orbiter (LRO) Project and the Arizona State University LROC contract.
The authors declare no competing financial interests.
Reviewer Information Nature thanks M. Cintala, B. Ivanov and the other anonymous reviewer(s) for their contribution to the peer review of this work.
Extended data figures and tables
Histogram of reflectance changes associated with low-reflectance (top; n = 18,756) and high-reflectance (bottom; n = 1,757) splotches.
Image footprints colour-coded by the number of days between the before and after observations (June 2009 to May 2015). The size of image footprints are exaggerated for display clarity.
Left, distribution of the area covered by individual temporal pairs versus the temporal spacing between the corresponding observations. Right, histogram of the ground sampling distance for each after image of the NAC temporal pair.
a–d, Examples of a temporal ratio image with decreasing pixel offsets (ratio of NAC frames M188678240LR/M1180548227LR): 10-pixel offset (7.8-m offset; a); 5-pixel offset (3.9-m offset; b); 3-pixel offset (2.3-m offset; c); and <1-pixel offset (<0.8-m offset; d). The larger offsets in a–c make the identification of the new impact crater impossible.
Relative crater frequency R of the 222 new impact craters identified with temporal imaging. For reference, a 1-yr isochron (grey line) derived from the NPF is overlaid for diameters of ≥10 m. Error bars are estimated on the basis of Poisson statistics of counts.
Temporal ratio image of the 17 March 2013 impact site surrounded by four distinct reflectance zones (ratio of NAC frames M1129645568L/M183689789L).
Maximum zone distance versus crater diameter for each of the four reflectance zones observed around new impacts. Craters smaller than 3 m in diameter were excluded from the least-squares fit.
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Speyerer, E., Povilaitis, R., Robinson, M. et al. Quantifying crater production and regolith overturn on the Moon with temporal imaging. Nature 538, 215–218 (2016). https://doi.org/10.1038/nature19829
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