The Purloined Lunar Crater
The Moon is our inconstant companion; always changing its face,
always changing its position in the sky. But to be fair it’s always
there, somewhere, and always predictable.
Or is it? While reading up on a small (180 meter, or 200 yard diameter) crater on the Moon’s far side, I got quite a surprise. I bet you will too.
First, here’s the crater in question:
Lovely, isn’t it? The shot was taken by the Lunar Reconnaissance
Orbiter when it was directly over the crater. Not only that, the Sun was
almost directly overhead. That means there are no shadows, so the
crater itself looks soft and difficult to see. The rough surface in the
middle is studded with boulders, some as big as cars or small trucks.
The ejecta blanket — the dust and rock thrown out by the blast of the
impact — is quite bright and obvious. This means the crater is young; lunar dust darkens over time from the erosive effects of the Sun and micrometeorite impacts. Why, it may only be a few million years old!
That high Sun angle makes the ejecta even more obvious, too, because
it highlights brightness changes in the surface. Dust with a higher
albedo (the fraction of sunlight it reflects) is easier to spot, and the
newer dust is more reflective than the older surface.
But there’s something else going on here as well. Because there are no shadows, changes in topography — hills and dips — are more
difficult to see, hiding some features. Don’t believe me? Then check
out this next LRO picture taken of the same spot, but when the Sun was
at a much lower angle:
Yes, that’s really the same spot! I scaled and cropped the picture to
roughly match the one above; if you look carefully you can match up
some smaller craters around the edges. As you can see, there’s a second
crater about the same size as the first one that’s almost completely
hidden in the first picture.
Now that you know it’s there, you can see hints of it in the first shot; the ejecta rays (plumes of material that collapsed down into long, linear features) curve when they cross the hidden crater. Other than that, though, you’d be forgiven for saying it’s not there at all. It helps that the crater is clearly (well, in the second picture) much older; the very slow erosion process on the Moon has softened its features; it may be billions of years old.
Now that you know it’s there, you can see hints of it in the first shot; the ejecta rays (plumes of material that collapsed down into long, linear features) curve when they cross the hidden crater. Other than that, though, you’d be forgiven for saying it’s not there at all. It helps that the crater is clearly (well, in the second picture) much older; the very slow erosion process on the Moon has softened its features; it may be billions of years old.
Amazing. An ancient crater, hidden on the Moon in plain sight.
Obviously, if you want to study the Moon, you can’t just take a picture
and think you’re seeing the whole thing. It’s critical to wait a while
and look again. The Moon may be an inconstant companion, but perhaps
that’s not such a bad thing if you want to learn more about it.
[Note: While poking around for this article, I found one I wrote back in 2006 titled “The Purloined Crater”;
this was about an impact crater hidden in plain sight… on Earth! And
not-too-coincidentally, it too was spotted in images taken by an
orbiting camera.]
0 Comments:
Post a Comment
<< Home