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The largest structure on the Moon listed officially as a crater is
Hertzsprung, diameter 591 km, which lies on the farside of the
Moon and so is permanently invisible from Earth. It is a multi-
ringed impact feature. Similar impact structures on the nearside
of the Moon became flooded with lava which solidified into
dark rock. These features are now named as maria (seas) rather
than craters. Such volcanic flooding did not occur on the lunar
farside. As a result, there are many more very large impact
structures on the farside that are described as 'craters' compared
with the nearside. They include Apollo (537 km), Birkhoff (345
km), Korolev (437 km), Mendeleev (313 km), Planck (314 km)
and Schroedinger (312 km).
The largest crater on the nearside of the Moon is Bailly, diameter
287 km (not to be confused with Baily, which is a different
crater). The largest impact basin of any kind identified on the
Moon is the South Pole-Aitken Basin, which is 2,500 km across
and stretches almost a quarter the way round the Moon.
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