Puiseux (crater)
Encyclopedia
Puiseux is the remnant of a lunar
Moon
The Moon is Earth's only known natural satellite,There are a number of near-Earth asteroids including 3753 Cruithne that are co-orbital with Earth: their orbits bring them close to Earth for periods of time but then alter in the long term . These are quasi-satellites and not true moons. For more...

 crater
Impact crater
In the broadest sense, the term impact crater can be applied to any depression, natural or manmade, resulting from the high velocity impact of a projectile with a larger body...

 that has been almost completely submerged by lava
Lava
Lava refers both to molten rock expelled by a volcano during an eruption and the resulting rock after solidification and cooling. This molten rock is formed in the interior of some planets, including Earth, and some of their satellites. When first erupted from a volcanic vent, lava is a liquid at...

. It is located near the southern end of Mare Humorum
Mare Humorum
Mare Humorum is a lunar mare. The impact basin it is located in is 825 kilometers across. It was not sampled by the Apollo program, so a precise age has not been determined. However, geological mapping indicates that it is intermediate in age between the Imbrium and Nectaris Basins, suggesting an...

, to the north east of the ruined crater Doppelmayer
Doppelmayer (crater)
Doppelmayer is the remains of a lunar crater that lies on the southwest edge of Mare Humorum. To the south-southeast is another flooded crater designated Lee, and to the southeast is Vitello. Just to the east-northeast of Doppelmayer lies the nearly submerged crater Puiseux.The rim of Doppelmayer...

. To the south-southeast is Vitello
Vitello (crater)
Vitello is a lunar crater that lies along the southern edge of the small Mare Humorum, in the southwest part of the Moon's near side. It lies just to the east of the lava-flooded crater Lee. To the northeast along the edge of the lunar mare is the Rupes Kelvin, an irregular fault line.This crater...

. Of the original structure of Puiseux, only the upper part of the rim remains above the mare
Lunar mare
The lunar maria are large, dark, basaltic plains on Earth's Moon, formed by ancient volcanic eruptions. They were dubbed maria, Latin for "seas", by early astronomers who mistook them for actual seas. They are less reflective than the "highlands" as a result of their iron-rich compositions, and...

surface. There are some small craterlets within the interior floor.

Satellite craters

By convention these features are identified on lunar maps by placing the letter on the side of the crater mid-point that is closest to Puiseux.
Puiseux Latitude Longitude Diameter
A 26.5° S 39.7° W 3 km
B 25.7° S 38.8° W 4 km
C 24.7° S 37.8° W 3 km
D 25.7° S 36.1° W 7 km
F 23.4° S 38.8° W 4 km
G 28.2° S 37.8° W 3 km
H 27.4° S 37.0° W 3 km
The source of this article is wikipedia, the free encyclopedia.  The text of this article is licensed under the GFDL.
 
x
OK