Klaproth (crater)
The outer rim of Klaproth has been deeply eroded, incised, and reshaped by a long history of bombardment. The rim to the north and east remains relatively circular, but the original rim along the western face has been overlain by satellite craters Klaproth G and Klaproth H, and other impacts. To the south the crater Casatus significantly intrudes into the interior floor. The remaining floor has been resurfaced by some material in the past, possibly fluidized ejecta or lava, leaving a level and nearly featureless surface that is marked only by a multitude of tiny craterlets. If this walled-plain once possessed a central peak, it no longer exists.
The crater was named after Martin Heinrich Klaproth, the German chemist and discoverer of Uranium.
Satellite craters
By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Klaproth.
| Klaproth | Latitude | Longitude | Diameter |
|---|---|---|---|
| A | 68.2° S | 21.6° W | 30 km |
| B | 72.0° S | 24.7° W | 11 km |
| C | 69.1° S | 19.5° W | 8 km |
| D | 70.2° S | 20.4° W | 8 km |
| G | 68.6° S | 31.2° W | 30 km |
| H | 69.4° S | 33.1° W | 41 km |
| L | 70.1° S | 36.5° W | 11 km |
References
- Wood, Chuck (2006-08-05). "Unknown Klaproth". Lunar Photo of the Day. Archived from the original on 2007-09-27. Retrieved 2006-08-05.
- Andersson, L. E.; Whitaker, E. A. (1982). NASA Catalogue of Lunar Nomenclature. NASA RP-1097.
- Blue, Jennifer (July 25, 2007). "Gazetteer of Planetary Nomenclature". USGS. Retrieved 2007-08-05.
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