C. Mayer (crater)
![]() View from Lunar Orbiter 4 | |
| Coordinates | 63°12′N 17°18′E / 63.2°N 17.3°E |
|---|---|
| Diameter | 37.54 km (23.33 mi)[1] |
| Depth | 3.24 km (2.01 mi)[2] |
| Colongitude | 343° at sunrise |
| Eponym | Christian Mayer |


C. Mayer is a lunar impact crater that is located at the northern edge of the Mare Frigoris.[3] It is at the western end of the Montes Carpatus range,[4] and due north of the prominent crater Aristoteles. Also to the south, but only a third as distant, is the smaller crater Sheepshanks. Due east of C. Mayer is the flooded crater Kane.[5]
C. Mayer is a relatively young formation, with a sharp-edged and well-defined outer rim. The rim is not quite circular, and appears somewhat polygonal-shaped with outward bulges along the edge, most notably to the west. The inner walls have a terrace system and the interior is somewhat rough and irregular. The central peak lies just to the north of the midpoint, and extends in a northerly direction.
The lava-flooded formation C. Mayer D is attached to the southeastern rim of the crater, and a gap in the southeastern rim joins it to the Mare Frigoris. Thus the lunar mare extends up to the outer rampart of C. Mayer.[6]: 13
This crater is named after the Moravian astronomer and teacher Christian Mayer (1719-1783).[1] His name was added to lunar nomenclature by German astronomer Johann H. Schröter in 1791.[7] Its designation was adopted by the International Astronomical Union in 1935.[1]
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 C. Mayer.[8] (See the C Mayer D crater that is very similar in shape to the map of Brazil). >> [(pt:C. Mayer D (Cratera) )]
| C. Mayer[6]: 294 | Latitude | Longitude | Diameter |
|---|---|---|---|
| B | 60.2° N | 15.6° E | 36 km |
| D | 62.1° N | 18.6° E | 66 km |
| E | 61.1° N | 16.0° E | 12 km |
| F | 62.0° N | 19.5° E | 7 km |
| H | 64.1° N | 14.7° E | 43 km |
The satellite features F and H include permanently shadowed regions where the sunlight never reaches.[9]
References
- 1 2 3 "C. Mayer". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
- ↑ Joshi, Maitri P. (February 2017). "Physical properties of lunar craters". Research in Astronomy and Astrophysics. 17 (3). id. 24. Bibcode:2017RAA....17...24J. doi:10.1088/1674-4527/17/3/24.
- ↑ Moore, Patrick (2001). On the Moon. Sterling Publishing Co. pp. 172–173. ISBN 978-0-304-35469-6.
- ↑ Grego, Peter (2005). The Moon and How to Observe It. Astronomers' Observing Guides Series. London: Springer-Verlag. p. 152. ISBN 1-85233-748-6.
- ↑ "LAC 13" (PDF). Gazeteer of Planetary Nomenclature. Retrieved 2026-06-20.
- 1 2 Bussey, B.; Spudis, P. (2004). The Clementine Atlas of the Moon. New York: Cambridge University Press. ISBN 978-0-521-81528-4.
- ↑ Whitaker, Ewen A. (1999). Mapping and Naming the Moon. Cambridge University Press. pp. 101, 218. ISBN 978-0-521-62248-6.
- ↑ Grego, P. (2015). "Satellite Crater". In Hargitai, H.; Kereszturi, Á. (eds.). Encyclopedia of Planetary Landforms. New York, NY: Springer. doi:10.1007/978-1-4614-3134-3_328.
- ↑ McGovern, J. Andrew; et al. (March 2013). "Mapping and characterization of non-polar permanent shadows on the lunar surface". Icarus. 223 (1): 566–581. Bibcode:2013Icar..223..566M. doi:10.1016/j.icarus.2012.10.018.
Sources
- Price, Fred W. (1988). The Moon Observer's Handbook. Cambridge University Press. ISBN 978-0-521-33500-3.
- Rükl, Antonín (1990). Atlas of the Moon. Kalmbach Books. ISBN 978-0-913135-17-4.
- Wlasuk, Peter T. (2000). Observing the Moon. Springer. ISBN 978-1-85233-193-1.

