The heavily eroded outer rim of Goldschmidt is rugged and irregular, with an inner wall that is incised in several locations by small impacts. Much of the western rim no longer exists, due to the overlapping Anaxagoras and the smaller 'Anaxagoras A' craters, and the ejecta from these formations covers the western third of the interior floor. The remaining floor is nearly level and flat, most likely due to having been resurfaced by lava flows. However the surface is now pock-marked by a multitude of tiny craterlets, the most prominent being the small 'Goldschmidt A'.
| Goldschmidt | Latitude | Longitude | Diameter |
|---|---|---|---|
| A | 72.5° N | 2.5° W | 7 km |
| B | 70.6° N | 6.7° W | 10 km |
| C | 71.1° N | 6.0° W | 7 km |
| D | 75.3° N | 7.7° W | 14 km |