Lunar Reconnaissance Orbiter Wide Angle Camera image of Reiner Gamma
Lunar Reconnaissance Orbiter Wide Angle Camera image of Reiner Gamma
Another view of Reiner Gamma swirls
Another view of Reiner Gamma swirls
Mare Ingenii
Mare Ingenii
Swirls east of Firsov crater, from Apollo 10
Swirls east of Firsov crater, from Apollo 10

Lunar swirls are enigmatic features found across the Moon's surface, which are characterized by having a high albedo, appearing optically immature (i.e. having the optical characteristics of a relatively young regolith), and (often) having a sinuous shape. Their curvilinear shape is often accentuated by low albedo regions that wind between the bright swirls. They appear to overlay the lunar surface, superposed on top of craters and ejecta deposits, but impart no observable topography. Swirls have been identified on the lunar maria and highlands - they are not associated with a specific lithologic composition. Swirls on the maria are characterized by strong albedo contrasts and complex, sinuous morphology, whereas those on highland terrain appear less prominent and exhibit simpler shapes, such as single loops or diffuse bright spots.

Association with magnetic anomalies

The lunar swirls are coincident with regions of the magnetic field of the Moon with relatively high strength on a planetary body that lacks, and may never have had, an active core dynamo with which to generate its own magnetic field. Every swirl has an associated magnetic anomaly, but not every magnetic anomaly has an identifiable swirl. Orbital magnetic field mapping by the Apollo 15 and 16 sub-satellites, Lunar Prospector, and Kaguya show regions with a local magnetic field. Because the Moon has no currently active global magnetic field, these regional anomalies are regions of remnant magnetism; their origin remains controversial.

Formation models

There are three leading models for swirl formation. Each model must address two characteristics of lunar swirls formation:

  1. The lunar swirls are optically immature.
  2. The lunar swirls are associated with magnetic anomalies.

Models for creation of the magnetic anomalies associated with lunar swirls point to the observation that several of the magnetic anomalies are antipodal to the younger, large impact basins on the Moon.[1]

Cometary impact model

This theory argues that the high albedo of the swirls is the result of an impact with a comet. The impact would cause scouring of the top-most surface regolith by the coma's turbulent flow of gas and dust, which exposed fresh material and redeposited the fine, scoured material in discrete deposits.[2] According to this model, the associated strong magnetic anomalies are the result of magnetization of near-surface materials heated above the Curie temperature through hyper-velocity gas collisions and micro-impacts as the coma impacted the surface. Proponents of the cometary impact model consider the occurrence of many swirls antipodal the major basins to be coincidental or the result of incomplete mapping of swirl locations.[3][4]

Solar wind shielding model

This theory suggests that the swirls are formed because the lighter-colored regolith is protected from the solar wind, due to a magnetic anomaly.[5] The swirls represent exposed silicate materials whose albedos have been selectively preserved over time from the effects of space weathering via deflection of solar wind ion bombardment. According to this model, optical maturation of exposed silicate surfaces is a result of solar wind ion bombardment. This model suggests that swirl formation is a continuing process, which began after creation of the magnetic anomaly.

Mathematical simulations conducted in 2018 showed that lava tubes could have become magnetic as they cooled, which would provide a magnetic field consistent with the observations near the lunar swirls.[6]

Dust transport model

The dust transport model proposes that weak electric fields created by interaction between the crustal magnetic anomalies and the solar wind plasma could attract or repel electrically charged fine dust. High albedo, feldspathic material is the dominant component of the finest particles of lunar soil. Electrostatic movement of dust lofted above the surface during terminator crossings could cause this material to preferentially accumulate and form the bright, looping swirl patterns.[7][8]

Satellite measurements

Direct magnetic observations of the lunar swirls have been conducted by many lunar spacecraft, including Clementine and Lunar Prospector. The results of these observations are inconsistent with the Cometary impact model.[9] Further observations by the Lunar Reconnaissance Orbiter support the theory that solar wind is being deflected by a magnetic field.

Spectral observations by the Moon Mineralogy Mapper instrument on board Chandrayaan-1 confirmed that the lighter-colored regions are deficient in hydroxide, which also supports the hypothesis that solar wind is being deflected in the pale areas.[10]

As of 2018, a CubeSat mission concept is under study at NASA, with the goal of understanding the formation of the lunar swirls. The proposed Bi-sat Observations of the Lunar Atmosphere above Swirls, or BOLAS mission would involve two small satellites connected with a 25 km (16 mi) space tether. The lower CubeSat would orbit at an altitude of six miles above the surface.[11][12]

See also


  1. ^ L. L. Hood; P. J. Coleman & D. E. Wilhelms (1979). "The Moon: Sources of the crustal magnetic anomalies". Science. 204 (4388): 53–57. Bibcode:1979Sci...204...53H. doi:10.1126/science.204.4388.53. PMID 17816737. S2CID 9385779.
  2. ^ P. C. Pinet; V. V. Shevchenko; S. D. Chevrel; Y. Daydou & C. Rosemberg (2000). "Local and regional lunar regolith characteristics at Reiner Gamma Formation: Optical and spectroscopic properties from Clementine and Earth-based data". Journal of Geophysical Research. 105 (E4): 9457–9476. Bibcode:2000JGR...105.9457P. doi:10.1029/1999JE001086.
  3. ^ P. H. Schultz & L. J. Srnka (1980). "Cometary collisions on the Moon and Mercury". Nature. 284 (5751): 22–26. Bibcode:1980Natur.284...22S. doi:10.1038/284022a0. S2CID 4241425.
  4. ^ "Crashing Comets May Explain Mysterious Lunar Swirls - SpaceRef". 1 June 2015. Retrieved 10 September 2018.
  5. ^ L. L. Hood & G. Schubert (1980). "The Moon: Lunar magnetic anomalies and surface optical properties". Science. 208 (4439): 49–51. Bibcode:1980Sci...208...49H. doi:10.1126/science.208.4439.49. PMID 17731569. S2CID 42500916.
  6. ^ "Lunar Swirls Point to the Moon's Volcanic Magnetic Past - SpaceRef". 6 September 2018.
  7. ^ Garrick-Bethell, Ian; et al. (2011). "Spectral properties, magnetic fields, and dust transport at lunar swirls". Icarus. 212 (2): 480–492. Bibcode:2011Icar..212..480G. doi:10.1016/j.icarus.2010.11.036.
  8. ^ Steigerwald, Bill (28 April 2016). "Lunar Tattoos: New Clues". NASA. Retrieved 10 September 2018.
  9. ^ Blewett, David T.; Coman, Ecaterina I.; Hawke, B. Ray; et al. (3 February 2011). "Lunar swirls: Examining crustal magnetic anomalies and space weathering trends". Journal of Geophysical Research. 116 (E2): E02002. Bibcode:2011JGRE..116.2002B. doi:10.1029/2010JE003656.
  10. ^ Kramer, Georgiana Y.; Besse, Sebastien; Dhingra, Deepak; et al. (9 September 2011). "M spectral analysis of lunar swirls and the link between optical maturation and surface hydroxyl formation at magnetic anomalies". Journal of Geophysical Research. 116: E00G18. Bibcode:2011JGRE..116.0G18K. doi:10.1029/2010JE003729.
  11. ^ Jenner, Lynn (8 August 2017). "NASA Studies Tethered CubeSat Mission to Study Lunar Swirls". NASA. Retrieved 10 September 2018.
  12. ^ Bi-Sat Observations of the Lunar Atmosphere Above Swirls (BOLAS): Tethered SmallSat Investigation of Hydration and Space Weathering Processes at the Moon. (PDF) Stubbs, T. J.; Malphrus, B. K.; Hoyt, R., etal. 49th Lunar and Planetary Science Conference; 19–23 March 2018 at The Woodlands, Texa, USA.

See also