Reiner Gamma
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Reiner Gamma (γ) is a geographical feature of the Moon known as a lunar swirl. It is one of the most visible lunar swirls from Earth, visible from most telescopes.Template:R It was originally thought to be a lunar highland, but scientists eventually realized that it cast no shadow on the moon.Template:R
Origin
The origin of Reiner GammaTemplate:Mdashlike other lunar swirlsTemplate:Mdashis not completely understood. It is associated with a localized magnetic field, but not with any particular irregularities in the surface. Similar features have been discovered in Mare Ingenii and Mare Marginis by orbiting spacecraft.[1] The feature on Mare Ingenii is located at the lunar opposite point from the center of Mare Imbrium. Likewise the feature on Mare Marginis is opposite the midpoint of Mare Orientale. Thus one hypothesis is that the feature resulted from seismic energies generated by the impacts that created these maria.Script error: No such module "Unsubst". However, no such lunar mare formation is on the opposite side of the Moon from Reiner Gamma.
Location and Features
Reiner Gamma is located on the Oceanus Procellarum, west of the crater Reiner. Its center is located at selenographic coordinates Template:Coords. It has an overall length of about 70 kilometres. The feature has a higher albedo than the relatively dark mare surface, with a diffuse appearance and a distinctive swirling, concentric oval shape. Related albedo features continue across the surface to the east and southwest, forming loop-like patterns over the mare.
The central feature of Reiner Gamma resembles the dipolar formation created by iron filings on a surface with a bar magnet on the underside. Low-orbiting spacecraft have observed a relatively strong magnetic field associated with each of these albedo markings. Some have speculated that this magnetic field and the patterns were created by cometary impacts. However the true cause remains uncertain.
Reiner Gamma's magnetic field strength is approximately Script error: No such module "val"., measured from an altitude of Script error: No such module "val".. This is one of the strongest localized magnetic anomalies on the Moon.[2] The surface field strength of this feature is sufficient to form a mini-magnetosphere that spans Script error: No such module "val". at the surface, forming a Script error: No such module "val". thick region of enhanced plasma where the solar wind flows around the field.[3] As the particles in the solar wind are known to darken the lunar surface, the magnetic field at this site may account for the survival of this albedo feature.[4]
In early lunar maps by Francesco Maria Grimaldi, this feature was incorrectly identified as a crater. His colleague Giovanni Riccioli then named it Galilaeus, after Galileo Galilei. The name was later transferred northwest to the current crater Galilaei.
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References
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Other references
- Ewen A. Whitaker, Mapping and Naming the Moon: A History of Lunar Cartography and Nomenclature, Cambridge University Press, 1999, Template:ISBN.
External links
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- Overexposed 35mm Nikon camera image of Reiner Gamma from Apollo 17: AS17-158-23895
- Lunar Orbiter 4 image showing Reiner Gamma in upper left: IV-157-H1
