The focus of this image just pops out at you as soon as you look at it. It’s the figure-8 shaped crater, Hainzel (roughly near the center the image composed of 3 different overlapping impacts. The northernmost crater, last formed and thus the sharpest and less eroded one, is Hainzel A (diameter 55 km) a rather young crater by lunar standards only 1.1-3.2 billion years old, formed in the Eratosthean period. This crater sits to the north on top of a much older crater Hainzel, from the Nectarian period (3.85-3.9 b.y.o.) that is larger at 71km dia. Then east of a line between the centers of these last two is a third crater, Hainzel C (28x19km in size) formed in the Imbriam period (3.2-3.85 b.y.o.).
South and west (lower left) of Hainzel is the large, badly eroded crater Mee (136km) of Pre-Nectarian age (3.92-4.55 b.y.o.). The eastern wall of this crater seems to combine with other material to form a large mountain ridge that runs south. The south wall of Mee seems to be ejecta splattered further to the south. Northeast of Hainzel is a small winding flat mare-like area, Lacus Timoris that winds its way from Hainzel to Haidinger (22km) that has to smaller craters next to it to the northeast and southeast, Haidinger A (9km) and Haidinger B (10km) respectively. Another such mare-like area like L. Timoris can be seen in the upper left corner of this image deep in shadow. This is Lacus Excellentiae. Where Lacus Timoris intersects Hainzel a couple thin rimae can be seen heading north from Hainzel. These are the southern terminus of the Rimae Ramsden that begin in and near the crater Ramsden just off the upper edge of this image.
We end with the large crater on the right edge of this image. This is Wilhelm (111km) as old as Mee but in much better shape with less overlain recent impacts and ejecta infill. Note the interesting striations on the floor of Wilhelm. So as you can see from this, Hainzel sits at the center of much of the selenographical features of this region but is a Figure-8 landmark that is easy to spot!
