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The rim of this crater retains much of its original structure, although the features have become softened and worn in comparison to the younger Hale.
The rim has a polygonal appearance along most of the perimeter, and traces of terraces can still be seen along sections of the inner wall.
There is a small crater across the northwest rim, but otherwise the formation is not significantly marked by impacts.
The interior floor is relatively flat and level, with a central peak near the midpoint.
There is the ghostly remnant of a crater to the northeast of the middle peak.

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