However, this is not the case. Small craters are predominantly located on peeks and ridges. It is quite common to see them on the edge of older, bigger craters, or lined up neatly along a ridge.
Electrical cratering on exposed edges
All of this indicate some sort of continuous process in which craters are excavated slowly over time.
The prime suspect in this case would be ion winds. Charged particles move along the surface of our Moon until they find a suitable escape point, usually on a ridge or other high point. They spiral around the escape point a few times before leaving the surface.
Over time, craters appear, evenly spaced out, themselves forming a spiralling pattern.
Lunar north pole
By NASA/GSFC/Arizona State University -
http://wms.lroc.asu.edu/lroc_browse/view/npole (see also
http://photojournal.jpl.nasa.gov/catalog/PIA14024), Public Domain,
https://commons.wikimedia.org/w/index.php?curid=31697472
The craters on the Moon are not proof of a violent past, but mostly the result of dust and other particles fluttering along its surface.
Impact craters are relatively rare in comparison to electrically excavated craters.
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