Difference between revisions of "August 21, 2011"
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Circular maria don’t have corners, but sometimes there are edges that get overlooked. In the case of Mare Serenitatis, there is much to see at Posidonius and along the albdeo boundary of the northern and eastern shores. But stuck away in the odd semi-circular southern extension of Serenitatis (a smaller, older basin?) is a short segment of a rille named after the nearby Calippus crater. This rille is unusual for it has two or three short tributaries near its southern/western end - I assume that it originally flowed to the north/east but I don’t have topography to check. Tributaries occur for terrestrial rivers that have multiple source areas - rain. The Calippus Rille is not quite a sinuous rille but I’d guess it formed by flowing lava, and most sinuous rilles have one lava source which is where they start. So this is strange. Another reason for thinking it is a volcanically-formed feature is the small dark patch that surrounds its middle. This looks like a tiny exposure of pyroclastic material, but it wasn’t mapped as such by the USGS Lunar Pyroclastic Volcanism Project. The small mare ridge south of the rille is dusted by a ray - an interesting chance convergence of volcanic and impact features. Finally, it seems mandatory to mention that the large broken crater (with secondary crater chains from Eudoxus) to the north is Alexander (a name that seems to deserve a more splendid memorial), and the steep walled pit with a little bit of swirl on its floor is Calippus itself.<br /> | Circular maria don’t have corners, but sometimes there are edges that get overlooked. In the case of Mare Serenitatis, there is much to see at Posidonius and along the albdeo boundary of the northern and eastern shores. But stuck away in the odd semi-circular southern extension of Serenitatis (a smaller, older basin?) is a short segment of a rille named after the nearby Calippus crater. This rille is unusual for it has two or three short tributaries near its southern/western end - I assume that it originally flowed to the north/east but I don’t have topography to check. Tributaries occur for terrestrial rivers that have multiple source areas - rain. The Calippus Rille is not quite a sinuous rille but I’d guess it formed by flowing lava, and most sinuous rilles have one lava source which is where they start. So this is strange. Another reason for thinking it is a volcanically-formed feature is the small dark patch that surrounds its middle. This looks like a tiny exposure of pyroclastic material, but it wasn’t mapped as such by the USGS Lunar Pyroclastic Volcanism Project. The small mare ridge south of the rille is dusted by a ray - an interesting chance convergence of volcanic and impact features. Finally, it seems mandatory to mention that the large broken crater (with secondary crater chains from Eudoxus) to the north is Alexander (a name that seems to deserve a more splendid memorial), and the steep walled pit with a little bit of swirl on its floor is Calippus itself.<br /> | ||
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| − | <em>[mailto:tychocrater@yahoo.com | + | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> |
| − | A normally 60 minute car trip coming back from taking our son to college took 3.5 hrs due to a ten plus mile detour at an average speed of about 5 mph. So I am lucky to have so many classic LPOD, such as [http://www.lpod.org/?m=20070821 | + | A normally 60 minute car trip coming back from taking our son to college took 3.5 hrs due to a ten plus mile detour at an average speed of about 5 mph. So I am lucky to have so many classic LPOD, such as [http://www.lpod.org/?m=20070821 this] from 4 years ago today, to draw upon for times such as this!<br /> |
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<strong>Technical Details</strong><br /> | <strong>Technical Details</strong><br /> | ||
Revision as of 16:38, 11 January 2015
Tributaries?
image by Jérôme Grenier, Paris, France
Circular maria don’t have corners, but sometimes there are edges that get overlooked. In the case of Mare Serenitatis, there is much to see at Posidonius and along the albdeo boundary of the northern and eastern shores. But stuck away in the odd semi-circular southern extension of Serenitatis (a smaller, older basin?) is a short segment of a rille named after the nearby Calippus crater. This rille is unusual for it has two or three short tributaries near its southern/western end - I assume that it originally flowed to the north/east but I don’t have topography to check. Tributaries occur for terrestrial rivers that have multiple source areas - rain. The Calippus Rille is not quite a sinuous rille but I’d guess it formed by flowing lava, and most sinuous rilles have one lava source which is where they start. So this is strange. Another reason for thinking it is a volcanically-formed feature is the small dark patch that surrounds its middle. This looks like a tiny exposure of pyroclastic material, but it wasn’t mapped as such by the USGS Lunar Pyroclastic Volcanism Project. The small mare ridge south of the rille is dusted by a ray - an interesting chance convergence of volcanic and impact features. Finally, it seems mandatory to mention that the large broken crater (with secondary crater chains from Eudoxus) to the north is Alexander (a name that seems to deserve a more splendid memorial), and the steep walled pit with a little bit of swirl on its floor is Calippus itself.
Chuck Wood
A normally 60 minute car trip coming back from taking our son to college took 3.5 hrs due to a ten plus mile detour at an average speed of about 5 mph. So I am lucky to have so many classic LPOD, such as this from 4 years ago today, to draw upon for times such as this!
Technical Details
4 Aug, 2007, 05h20m in good seeing. Orion Optics (UK) OMC 12″ + barlow 2x + red 23a filter + DMK 31AF03; 500 frames stacked in Registax.
Related Links
Rükl plate 13
