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Permanently shadowed crater

Permanently shadowed region of a body in the Solar System


Permanently shadowed region of a body in the Solar System

A **permanently shadowed crater ** is a depression on a body in the Solar System within which lies a point that is always in darkness. As of 2019, there are 324 known permanently shadowed regions on the Moon. Such regions also exist on Mercury and Ceres.

Location

Cabeus

Such a crater must be located at high latitude (close to a pole) and be on a body with very small axial tilt. The Moon has an axial tilt of about 1.5°; Mercury, 0.03°; and Ceres, about 4°. On the Moon, permanent shadow can exist at latitudes as low as 58°; approximately 50 permanently shadowed regions exist in the 58°- 65° latitude range for both lunar hemispheres. The cumulative area of permanently shadowed lunar regions is about 31 thousand km2; more than half of it is in the southern hemisphere.

Conditions inside craters

Craters of eternal darkness might be advantageous for space exploration and colonization, as they preserve sources of water ice that can be converted into drinkable water, breathable oxygen, and rocket propellant. Several of such craters show indications of water ice in their interiors, including Rozhdestvenskiy and Cabeus craters on the Moon, and Juling Crater on Ceres. Other volatiles besides water can also be trapped in such craters, such as mercury. The LCROSS mission additionally found native silver and gold in permanently shadowed craters on the Moon, probably brought there by electrostatic dust transport, and some inconclusive evidence for platinum. Gold was estimated to have a soil mass abundance of 0.52% in these craters from LCROSS data, and mercury 0.39%. This high mercury abundance has been noted as a possible health hazard of water derived from permanently shadowed craters. The craters may also contain unusually high concentrations of helium-3.

K}}.

Computer simulations show that powerful solar storms can charge up the soil in permanently shadowed regions near the lunar poles, and may possibly produce "sparks" that could vaporize and melt the soil. There are other unique challenges of such regions: dark environments that restrict the ability of rovers to perceive their surroundings, cryogenic regolith that could be hard to move on, and communication interruptions.

In some cases, peaks of eternal light are located nearby, that could be advantageous for solar power generation. For example, there are two peaks near Shackleton Crater that are illuminated a combined ~94% of a lunar year.

Utilization

A business case analysis indicates that mining of propellants in the craters could become a profitable commercial enterprise.

Planetary protection

In 2020, NASA assigned "sensitive location" status to the Moon's permanently shadowed regions to avoid their contamination. The SETI Institute has a contract to manage planetary protection measures for NASA.

List

Below is an incomplete list of such craters:

The Moon:

  • Shackleton
  • Shoemaker
  • Erlanger
  • Sylvester
  • Cabeus
  • Rozhdestvenskiy
  • Malapert
  • Marston

Mercury:

  • Chao Meng-Fu
  • Kandinsky
  • Petronius
  • Prokofiev
  • Tolkien

Ceres:

  • Juling

Research missions

Past

In 2009, LCROSS sent an impactor into a Cabeus crater, that resulted in detection of water in the ejected material.

In 2012, The Lyman Alpha Mapping Project aboard NASA's Lunar Reconnaissance Orbiter has found that the permanently shadowed regions have a porous, powdery surface, that indicates the presence of water ice.

In 2018, an analysis of the results of the Moon Mineralogy Mapper confirmed the existence of water ice deposits in permanently shadowed craters and crevices, with more abundance near the south pole.

In 2022, Lunar Flashlight was launched as a secondary payload for the Hakuto-R Mission 1 mission. The cubesat mission failed to go into orbit around the moon when debris blocked propellant lines for the spacecraft’s thrusters.

In 2025, the IM-2 lunar mission, conducted by Intuitive Machines for NASA's CLPS program, landed a Nova-C lunar lander. The lander carried a hopper named Grace, a drone equipped with a neutron spectrometer to explore the permanently shadowed region of the nearby Marston crater. The lander landed on its side and the hopper couldn't be deployed.

Current

A camera called ShadowCam has been built that is able to take high-resolution images of Permanently Shadowed Regions. It is a NASA instrument that flies on board the Korea Pathfinder Lunar Orbiter (KPLO) since 2022.

Planned

The proposed International Lunar Observatory mission involves a landing near the Malapert crater.

The Moonraker mission proposed by ESA will, if approved, use a LiDAR instrument to explore and map the permanently shadowed regions of the Moon.

References

References

  1. "LUNAR RECONNAISSANCE ORBITER: Permanently Shadowed Regions on the Moon". National Aeronautics and Space Administration.
  2. (6 March 2013). "GMS: The Moon's Permanently Shadowed Regions".
  3. "Permanently Shadowed Regions | Lunar Reconnaissance Orbiter Camera".
  4. "Permanently shadowed, radar-bright regions on Mercury".
  5. (2016). "The permanently shadowed regions of dwarf planet Ceres". Geophysical Research Letters.
  6. "Planetary Fact Sheets".
  7. (6 July 2016). "The permanently shadowed regions of dwarf planet Ceres". Geophysical Research Letters.
  8. (1 September 2012). "A Global Catalogue of Lunar Permanently Shadowed Regions". EPSC Abstracts.
  9. (2015). "Lunar Resources: A Review". Progress in Physical Geography.
  10. (21 August 2018). "Water Ice Confirmed on the Surface of the Moon for the 1st Time!".
  11. "Moon Mountain Seen as Prime Real Estate".
  12. (2017). "Investigations of Water-Bearing Environments on the Moon and Mars".
  13. "LCROSS Mission Finds Water - Planetary News | the Planetary Society".
  14. (14 March 2018). "NASA Dawn Reveals Recent Changes in Ceres' Surface".
  15. (1999). "Don't drink the water". Meteoritics & Planetary Science.
  16. (12 December 2013). "Prospecting for Native Metals in Lunar Polar Craters". 7th Symposium on Space Resource Utilization.
  17. Cocks, F. H.. (2010). "3He in permanently shadowed lunar polar surfaces". Icarus.
  18. "Eternal Darkness Near the North Pole".
  19. "Casting Light on Permanently Shadowed Regions | Lunar Reconnaissance Orbiter Camera".
  20. "Liquid Mirror Telescopes on the Moon | Science Mission Directorate".
  21. "Solar Storms Could Spark Soils at Moon's Poles | The Science Explorer".
  22. (2014). "Deep dielectric charging of regolith within the Moon's permanently shadowed regions". Journal of Geophysical Research: Planets.
  23. (4 December 2014). "Roving in the Permanently Shadowed Regions of Planetary Bodies".
  24. Bussey D. B. J., McGovern J. A., Spudis P. D., Neish C. D., Noda H., Ishihara Y., Sørensen S.-A.. (2010). "Illumination conditions of the south pole of the Moon derived using Kaguya topography". Icarus.
  25. (2019). "Ice Mining in Lunar Permanently Shadowed Regions". New Space.
  26. "NASA issues new guidelines to protect the Moon and Mars from Earth's germs | Business Insider India".
  27. "NASA Awards SETI Institute Contract for Planetary Protection Support - NASA".
  28. (2012). "Testing lunar permanently shadowed regions for water ice: LEND results from LRO". Journal of Geophysical Research: Planets.
  29. David, Leonard. (June 14, 2024). "Moon ice in the Artemis era: what we still don’t know".
  30. L. J. Harcke. (2001). "Radar Imaging of Mercury's North and South Poles at 3.5 cm Wavelength". Workshop on Mercury: Space Environment, Surface, and Interior.
  31. J. K. Harmon. (1994). "Radar mapping of Mercury's polar anomalies". Nature.
  32. "Ice on Mercury". [[NASA]].
  33. "NASA - Eternal Darkness of Petronius Crater".
  34. [https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2017GL074723 New evidence for surface water ice in small‐scale cold traps and in three large craters at the north polar region of Mercury from the Mercury Laser Altimeter], Ariel N. Deutsch, Gregory A. Neumann, [[James W. Head]]. 14 September 2017. ''Geophysical Research Letters'', Volume 44, Issue 18. [https://doi.org/10.1002/2017GL074723 doi.org/10.1002/2017GL074723]
  35. (15 November 2012). "Permanently Shaded Polar Craters". NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington/National Astronomy and Ionosphere Center, Arecibo Observatory.
  36. "Juling Crater's Shadow".
  37. (19 January 2012). "Shadows of the Moon Hide 'Fluffy' Dirt & Water Ice".
  38. (9 October 2014). "NASA is Studying How to Mine the Moon for Water".
  39. (17 July 2019). "NASA's large SLS rocket unlikely to fly before at least late 2021".
  40. (9 August 2023). "Clogged propellant lines doomed NASA lunar cubesat mission".
  41. David, Leonard. (12 September 2024). "Ice-hunting Lunar Trailblazer and IM-2 nearly ready for January 2025 launch". [[SpaceNews]].
  42. (7 January 2025). "Launch of Intuitive Machines' Athena lander is targeted for no earlier than late February".
  43. "IM-2".
  44. David, Leonard. (14 June 2024). "Moon ice in the Artemis era: what we still don't know".
  45. (3 November 2021). "NASA, Intuitive Machines Announce Landing Site Location for Lunar Drill".
  46. "Athena landed in a dark crater where the temperature was minus 280° F - Ars Technica".
  47. (12 August 2017). "International Lunar Observatory to offer a new astrophysical perspective".
  48. "Creating a Lidar-based Elevation Map of the Moon".
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