Oblique view of Mandel'shtam Q crater, southwest of <a href="https://en.wikipedia.org/wiki/Mandel%27shtam_(crater)" class="extiw" title="en:Mandel'shtam (crater)">Mandel'shtam</a>, on the far side of the moon.  This is Figure 237 of <i>Apollo Over the Moon</i> (NASA SP-362, 1978), which has the following caption:<br>
A view looking south into a small 19-km diameter crater southwest of <a href="https://en.wikipedia.org/wiki/Mandel%27shtam_(crater)" class="extiw" title="en:Mandel'shtam (crater)">Mandel'shtam</a> on the lunar far side. The crater has a floor that is heavily lineated and grooved, but this structure is subdued rather than sharp and is contained wholly within the crater. The cracked floor is typical of a variety of craters that occur in the highlands away from the mare basins. They differ from cracked floor craters, such as <a href="https://en.wikipedia.org/wiki/Humboldt_(crater)" class="extiw" title="en:Humboldt (crater)">Humboldt</a>, and rilled craters, such as <a href="https://en.wikipedia.org/wiki/Goclenius_(crater)" class="extiw" title="en:Goclenius (crater)">Goclenius</a>; their origin is unknown.- J.W.H. (<i><a href="https://en.wikipedia.org/wiki/James_W._Head" class="extiw" title="en:James W. Head">James W. Head III</a></i>)
NASA image<br>
<p>Transferred from <span class="plainlinks"><a class="external text" href="https://en.wikipedia.org">en.wikipedia</a></span> to Commons.
(<span lang="en" dir="ltr">Original text: <i><bdi lang=""><a href="https://en.wikipedia.org/wiki/Apollo_16" class="extiw" title="en:Apollo 16">Apollo 16</a> Panoramic camera image AS16-P-4151.<br></bdi></i></span></p><i>
<b>Immediate source</b>: NASA History Program Office, <a rel="nofollow" class="external text" href="http://history.nasa.gov/SP-362/contents.htm">Apollo Over the Moon</a>, A view from orbit (NASA SP-362, 1978)<br>Figure 237 <a rel="nofollow" class="external text" href="http://history.nasa.gov/SP-362/hrp222.jpg">hrp222</a></i>)