Posidonius (crater)

Posidonius is a lunar impact crater that is located on the north-eastern edge of Mare Serenitatis, to the south of Lacus Somniorum. It was named after ancient Greek philosopher and geographer Posidonius of Apamea.[1] The crater Chacornac is attached to the southeast rim, and to the north is Daniell.

Oblique view of Posidonius from Apollo 17. Note that the lava which flooded the crater reached its rim and is clearly above the mare plain to the west (left).
The hill Posidonius γ with the craterlet Posidonius Y (LRO image).
Posidonius
Coordinates31.88°N 29.99°E / 31.88; 29.99
Diameter95 km
Depth2.3 km
Colongitude343° at sunrise
EponymPosidonius
Oblique view of Posidonius from Apollo 15. A tightly convoluted sinuous rille crosses the raised floor of the crater, turns back, and follows the rim to a low point in the western rim.
Part of the sinuous rille in Posidonius (LRO image).

Description

The rim of Posidonius is shallow and obscured, especially on the western edge, and the interior has been overlain by a lava flow in the past. The crater ramparts can still be observed to the south and east of the crater rim, and to a lesser degree to the north.

There is a smaller, semi-circular rim of a concentric, flooded crater within the main rim, offset towards the eastern edge. There is no central peak, but the floor is hilly and laced with a rille system named the Rimae Posidonius. The floor is also slightly bulged due to the past lava uplift, which also likely produced the complex of rilles. The northeast rim is interrupted by the smaller crater Posidonius B. Within the crater rim, offset just to the west of center is another smaller crater Posidonius A.

On the Mare Serenitatis surface near Posidonius is a notable system of wrinkle ridges that parallel the nearby shore. These are designated the Dorsa Smirnov. At the peak of these ridges is a small craterlet (Posidonius Y) with a diameter of 2 km. This craterlet is surrounded by a patch of high-albedo material, and is an example of a lunar bright spot. This peak was formerly designated Posidonius Gamma (γ).

Posidonius Gamma was first observed by the lunar cartographer Julius Schmidt in 1867, who noted the similarity to the bright patch surrounding the crater Linné.[2]

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 Posidonius.

Posidonius Coordinates Diameter, km
A 31.69°N 29.52°E / 31.69; 29.52 (Posidonius A) 11.1
B 33.16°N 31.02°E / 33.16; 31.02 (Posidonius B) 14.1
C 31.13°N 29.69°E / 31.13; 29.69 (Posidonius C) 3.5
E 30.55°N 19.7°E / 30.55; 19.7 (Posidonius E) 3.1
F 32.82°N 27.13°E / 32.82; 27.13 (Posidonius F) 6.0
G 34.79°N 27.23°E / 34.79; 27.23 (Posidonius G) 4.8
J 33.8°N 30.79°E / 33.8; 30.79 (Posidonius J) 22.0
M 34.36°N 30.01°E / 34.36; 30.01 (Posidonius M) 9.3
N 29.7°N 21.04°E / 29.7; 21.04 (Posidonius N) 6.2
P 33.6°N 27.58°E / 33.6; 27.58 (Posidonius P) 14.7
W 31.65°N 20.13°E / 31.65; 20.13 (Posidonius W) 3.0
Y 30.03°N 24.91°E / 30.03; 24.91 (Posidonius Y) 2.0
Z 30.75°N 22.95°E / 30.75; 22.95 (Posidonius Z) 5.9

References

  1. "Posidonius (crater)". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  2. Elger T. G. (1895). The Moon. A Full Description and Map of its Principal Physical Features. London: Georg Philip & Son. p. 160. (In this book, east on the Moon is called "west" according to terminology of that time).
  • Lunar Reconnaissance Orbiter pages with images:
    • Plescia J. (2013-02-05). "Meanders in Posidonius". NASA/GSFC/LROC, School of Earth and Space Exploration, Arizona State University. Archived from the original on 2018-01-30. - especially on the rille Rimae Posidonius
    • Braden S. (2011-10-25). "Posidonius Y". NASA/GSFC/LROC, School of Earth and Space Exploration, Arizona State University. Archived from the original on 2017-10-05.
    • Ostrach L. (2010-12-01). "Rimae Posidonius". NASA/GSFC/LROC, School of Earth and Space Exploration, Arizona State University. Archived from the original on 2018-05-31.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.