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| '''Otaared Planitia''' is a smooth plain on ]. It was named for the Arabic word for the planet Mercury, in 2017 by the ].<ref>, Gazetteer of Planetary Nomenclature, International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)</ref> The plain is approximately 470 |
'''Otaared Planitia''' is a smooth plain on ]. It was named for the Arabic word for the planet Mercury, in 2017 by the ].<ref>, Gazetteer of Planetary Nomenclature, International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)</ref> The plain is approximately {{cvt|470|km}} in diameter. | ||
| There are no named craters within the plain, but the small crater ] is just south of it. | There are no named craters within the plain, but the small crater ] is just south of it. | ||
| Otaared Planitia is at the center of an ancient impact basin now known as Calder-Hodgkins.<ref>Denevi, B. W., Ernst, C. M., Prockter, L. M., and Robinson, M. S., 2018. The Geologic History of Mercury. In ''Mercury: The View After ]'' edited by Sean C. Solomon, Larry R. Nittler, and Brian J. Anderson. Cambridge Planetary Science. Chapter 6.</ref> The scarps include the highest point on the planet.<ref>Becker, K. J., Robinson, M. S., Becker, T. L., Weller, L. A., Edmundson, K. L., Neumann, G. A., Perry, M. E., and Solomon, S. C. (2016). First global digital elevation model of Mercury. ''Lunar Planet Sci.'', 47, abstract 2959.</ref> The basin was originally identified as ''b30''.<ref name=Fassett_2012>{{cite journal | |||
| |author=Fassett C. I. |author2=Head J. W. |author3=Baker D. M. H. |display-authors=etal | |||
| |date=2012 | |||
| |title=Large impact basins on Mercury: Global distribution, characteristics, and modification history from MESSENGER orbital data | |||
| |journal=Journal of Geophysical Research | |||
| |volume=117 | |||
| |issue=E12 | |||
| |doi=10.1029/2012JE004154 | |||
| |bibcode=2012JGRE..117.0L08F | |||
| |url=http://www.planetary.brown.edu/pdfs/4324.pdf | |||
| |archiveurl=https://web.archive.org/web/20130129075452/http://www.planetary.brown.edu/pdfs/4324.pdf | |||
| |archivedate=2013-01-29 | |||
| }}</ref> The basin is named after ] crater near the south rim, and ] crater near the north rim. It is about {{cvt|1460|km}} in diameter. | |||
| ==References== | ==References== | ||
Revision as of 20:12, 13 December 2024
Geologic basin on Mercury| Location | Derain quadrangle, Mercury |
|---|---|
| Coordinates | 18°16′N 337°37′W / 18.26°N 337.61°W / 18.26; -337.61 |
| Eponym | Arabic word for Mercury |
Otaared Planitia is a smooth plain on Mercury. It was named for the Arabic word for the planet Mercury, in 2017 by the IAU. The plain is approximately 470 km (290 mi) in diameter.
There are no named craters within the plain, but the small crater Petipa is just south of it.
Otaared Planitia is at the center of an ancient impact basin now known as Calder-Hodgkins. The scarps include the highest point on the planet. The basin was originally identified as b30. The basin is named after Calder crater near the south rim, and Hodgkins crater near the north rim. It is about 1,460 km (910 mi) in diameter.
References
- Otaared Planitia, Gazetteer of Planetary Nomenclature, International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)
- Denevi, B. W., Ernst, C. M., Prockter, L. M., and Robinson, M. S., 2018. The Geologic History of Mercury. In Mercury: The View After MESSENGER edited by Sean C. Solomon, Larry R. Nittler, and Brian J. Anderson. Cambridge Planetary Science. Chapter 6.
- Becker, K. J., Robinson, M. S., Becker, T. L., Weller, L. A., Edmundson, K. L., Neumann, G. A., Perry, M. E., and Solomon, S. C. (2016). First global digital elevation model of Mercury. Lunar Planet Sci., 47, abstract 2959.
- Fassett C. I.; Head J. W.; Baker D. M. H.; et al. (2012). "Large impact basins on Mercury: Global distribution, characteristics, and modification history from MESSENGER orbital data" (PDF). Journal of Geophysical Research. 117 (E12). Bibcode:2012JGRE..117.0L08F. doi:10.1029/2012JE004154. Archived from the original (PDF) on 2013-01-29.
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