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Look at the maria with a telescope, and you can see that they're flat plains that appear to fill low-lying areas.And most of those low-lying areas are circular basins rimmed by mountainous ridges.

Rolf Hempel took advantage of this "Supermoon" apparition and clear skies over Germany to capture this spectacularly detailed portrait.Here is a lovely view from Lunar Reconnaissance Orbiter.Orientale is the youngest large impact basin on the Moon and is about 960 kilometers across.That's how old geology on the Moon is -- it's almost inverted from Earth, where most of the geology that we can see in rocks around us happened in the last few hundred million years. Rocks returned by the Apollo astronauts that were thought to come from Nectaris are only 70 million years older than the dates we get for Imbrium. If Nectaris really is only 70 million years older than Imbrium, that tells a shocking story: that half of the Moon's biggest basins happened in a really short time, geologically speaking, an event that's sometimes called the "lunar cataclysm" or "late heavy bombardment." But what if the age for Nectaris is wrong?When you're talking about things that happened nearly 4000 million years ago, 70 million is virtually an eyeblink. It could be; the compositions of lunar rocks read from orbit suggest that Apollo astronauts might just have been sampling Imbrium-related rocks over and over and over again, and that we don't actually know how old Nectaris is.

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The big basins are old, so a lot has happened to them since they formed.

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