Middle Crescent (crater)
{{Short description|Crater on the Moon}}
{{Infobox Lunar crater
| image = File:Middle Crescent crater M114104917RC.jpg
| caption = LRO Narrow Angle Camera image
| coordinates = {{coord|3.00|S|23.44|W|globe:moon_type:landmark|display=inline,title}}
| diameter = 360 m[http://planetarynames.wr.usgs.gov/Feature/3885 Middle Crescent], Gazetteer of Planetary Nomenclature, International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)
| depth =
| colong =
| eponym = Astronaut-named feature
}}
Middle Crescent crater is a small crater in Oceanus Procellarum on the Moon. The name of the crater was formally adopted by the IAU in 1973.
Apollo 12 astronauts Pete Conrad and Alan Bean landed the Lunar Module (LM) Intrepid east of Middle Crescent crater on November 19, 1969. To the southeast of Middle Crescent is Head crater. Middle Crescent is the largest crater visited by the Apollo 12 astronauts.
File:Middle Crescent crater AS12-46-6837-6839-6841-6844.jpg
The crater was described in the Apollo 12 Preliminary Science Report:Apollo 12 Preliminary Science Report, NASA Special Publi PDFcation 235, 1970. [https://ntrs.nasa.gov/api/citations/19700025955/downloads/19700025955.pdf PDF]
:Northwest of the LM is the largest crater visited, the 400-m-diameter Middle Crescent Crater. On looking down into the crater, the astronauts noticed huge blocks on the crater wall, which were probably derived from the local bedrock. Large rock fragments in this crater probably have been exposed since the crater was formed and probably represent the deepest layers excavated at the Apollo 12 landing site.
{{Clear}}
Samples
Lunar sample 12004, an olivine basalt, was collected at the rim of Middle Crescent.[https://www.lpi.usra.edu/lunar/samples/atlas/compendium/12004.pdf 12004], Lunar Samples, Lunar and Planetary Institute Samples 12014, 12015, and 12016 were probably collected there, but the provenance is less certain. 12014 is also an olivine basalt.[https://www.lpi.usra.edu/lunar/samples/atlas/compendium/12014.pdf 12014], Lunar Samples, Lunar and Planetary Institute 12015 is an olivine vitrophyre.[https://www.lpi.usra.edu/lunar/samples/atlas/compendium/12015.pdf 12015], Lunar Samples, Lunar and Planetary Institute 12016 is an ilmenite basalt.[https://www.lpi.usra.edu/lunar/samples/atlas/compendium/12016.pdf 12016], Lunar Samples, Lunar and Planetary Institute
File:AS12-47-6936 (21633565836).jpg|Sample 12004 is at center
External links
- Lunar Orbiter 3 image [http://www.lpi.usra.edu/resources/lunarorbiter/images/print/3154_h2.jpg 154 H2], used for planning the mission (landing site is left of center).
- Lunar Orbiter 1 sequence of images [https://www.lpi.usra.edu/resources/lunarorbiter/frame/?1157 157], [https://www.lpi.usra.edu/resources/lunarorbiter/frame/?1158 158], and [https://www.lpi.usra.edu/resources/lunarorbiter/frame/?1159 159], showing the Apollo 12 landing site and vicinity