Amundsen is a crater — a circular depression, almost always an impact scar — on The Moon, 103 km across, centred at 84.4° S, 83.1° E in the Amundsen quadrangle. It is the 338th largest named feature on The Moon and the 182nd largest of its class there.
Roald Engelbregt Gravning; Norwegian explorer (1872-1928). The International Astronomical Union approved the name in 1964, under the theme it applies to every crater on The Moon. Of the 1615 features of this class catalogued on The Moon, the naming categories run Germany (234), American (229), France (163), Great Britain (160).
The Moon scores 29.1 as a world. That number is the same for every square metre of it — but sunlight, water, radiation and the ground under your feet are not. This is the same question asked at 84.4° S, 83.1° E.
What this spot has going for it is water — inside the polar zone where The Moon keeps its ice. What works against it is sunlight — 10% of the sunlight the sunniest latitude on The Moon gets.
Computed from Amundsen's catalogued latitude, longitude and feature class — 84% of the model's weight had a basis here, and one axis was dropped as not applicable to The Moon (radiation geometry). Gravity, pressure, delta-v and distance from the Sun are the same everywhere on The Moon and are already counted in the world's own index, not again here.
What this cannot see: elevation. Slope, local shadowing and the polar “peaks of eternal light” — ridge tops near the poles of a barely tilted world that catch sun almost continuously while a crater floor kilometres away never does — need a terrain model this does not have. Where a real mission targets a pole, that is usually why.
The IAU names smaller craters around a major one by letter. Amundsen has 1, and each shares the parent's namesake rather than carrying one of its own.
All 1,615 craters on The Moon — mapped together, with the naming theme and the size distribution.