The narrow-angle camera (LROC NAC) aboard NASA’s Lunar Reconnaissance Orbiter (LRO) has photographed a large percentage of the moon’s surface multiple times. By looking for differences between earlier and later images, the LROC team has found over 200 new craters large enough for the camera to see (at least 5 meters in diameter), as well as thousands of what they call splotches, many of which are likely caused by smaller craters.
In a paper in the Oct. 13, 2016, issue of Nature, Emerson Speyerer and his coauthors divide the crater ejecta into four zones that differ in brightness and distance from the crater, and they explain the processes involved in the formation of each zone. They also use the number of craters and splotches to infer the gardening rate, the rate at which the top few centimeters of regolith is churned and replaced by impacts. Their conclusion is that this is happening over 100 times faster than previously thought.
The visualization simulates the formation of one of the craters featured in the paper. We first see a flash, then zoom all the way to the surface, where the animation blinks between the actual before and after LROC NAC images (M1105837846R and M1121160416R) that were used to detect this new 12-meter crater. Finally, we see the ratio of the two images, which very clearly shows both the new crater and the radial pattern of ejecta.
Note: Video is silent/no audio.
Credits: NASA’s Goddard Space Flight Center/Ernie Wright, Data Visualizer/Katrina Jackson, Producer
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