Difference between revisions of "June 15, 2009"
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<em>image by [mailto:ferreira1@llnl.gov Jim Ferreira], Livermore, California</em><br /> | <em>image by [mailto:ferreira1@llnl.gov Jim Ferreira], Livermore, California</em><br /> | ||
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| − | Just south of Petavius is the Snellius Valley, which here can been seen stretching its entire 600 km toward the limb. Further south is the Rheita Valley, and [[July_22,_2004|many]] less conspicuous linear features are in between. All of these are generally [http://lpod. | + | Just south of Petavius is the Snellius Valley, which here can been seen stretching its entire 600 km toward the limb. Further south is the Rheita Valley, and [[July_22,_2004|many]] less conspicuous linear features are in between. All of these are generally [http://www2.lpod.org/wiki/July_23,_2008 radial] to the center of the Nectaris impact basin. The two named valleys are giant secondary crater chains, and most of the other radials are probably due to crustal fracturing associated with the impact. The amazing thing is the such features are clustered here to the southeast of the basin and a few more are toward the south. There could have been similar radials in areas covered by maria, but there aren't any to the west where ancient crust remains. The USGS also [http://www.lpi.usra.edu/resources/mapcatalog/usgs/I703/ mapped] most of the Nectaris Basin ejecta in this direction. I propose that basin secondary chains are the megascale equivalent of crater rays, and that these suggest that Nectaris was an oblique impact with the projectile coming from the north-northwest.<br /> |
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<em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | ||
Latest revision as of 07:30, 28 October 2018
Convergence
image by Jim Ferreira, Livermore, California
Just south of Petavius is the Snellius Valley, which here can been seen stretching its entire 600 km toward the limb. Further south is the Rheita Valley, and many less conspicuous linear features are in between. All of these are generally radial to the center of the Nectaris impact basin. The two named valleys are giant secondary crater chains, and most of the other radials are probably due to crustal fracturing associated with the impact. The amazing thing is the such features are clustered here to the southeast of the basin and a few more are toward the south. There could have been similar radials in areas covered by maria, but there aren't any to the west where ancient crust remains. The USGS also mapped most of the Nectaris Basin ejecta in this direction. I propose that basin secondary chains are the megascale equivalent of crater rays, and that these suggest that Nectaris was an oblique impact with the projectile coming from the north-northwest.
Chuck Wood
Technical Details
C9.25 @ f/10 and DMK21.
Related Links
Rükl plates 68 & 69
Jim's entire mosaic
Yesterday's LPOD: Neison Reborn
Tomorrow's LPOD: Out On a Gaussian Limb
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