Search results
Results From The WOW.Com Content Network
The lunar south pole is the southernmost point on the Moon. ... The south pole temperature averages approximately 260 K (−13 °C; 8 °F). ... Formula Composition ...
The longitude gives the position east or west of the Moon's prime meridian, which is the line passing from the lunar north pole through the point on the lunar surface directly facing Earth to the lunar south pole. (See also Earth's prime meridian.) This can be thought of as the midpoint of the visible Moon as seen from the Earth.
Shackleton is an impact crater that lies at the lunar south pole. The peaks along the crater's rim are exposed to almost continual sunlight, while the interior is perpetually in shadow. The low-temperature interior of this crater functions as a cold trap that may capture and freeze volatiles shed during comet impacts on the Moon.
For example, there are two peaks near Shackleton Crater that are illuminated a combined ~94% of a lunar year. [19] Permanently shadowed regions have a stable surface temperature. On the Moon, the temperature hovers somewhere at or below 50 K (−223.2 °C; −369.7 °F). [20]
Due to Haworth's position near the lunar south pole, large amounts of the crater are permanently shadowed regions.These regions are very cold; many are believed to never reach temperatures above 40 Kelvin, making Haworth colder than nearby craters such as Shackleton and Faustini. [4]
Luna 25 and India’s Chandrayaan-3 mission, which launched in mid-July, are both expected to land at the lunar south pole on August 23, and it’s a race to see which country will land first ...
Malapert is a lunar impact crater that lies near the south pole of the Moon, named for 17th century astronomer Charles Malapert. [2] From the Earth this formation is viewed from the side, limiting the amount of detail that can be seen. The crater is also illuminated at very low angles, so that parts of the interior remain in almost constant ...
The lunar south pole features a region with crater rims exposed to near constant solar illumination, where the craters' interior are permanently shaded from sunlight, allowing for natural trapping and collection of water ice that could be mined in the future. Water molecules (H 2 O) can be broken down to form molecular hydrogen (H