Difference between revisions of "February 4, 2009"
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| − | <em>left: Lunar Orbiter IV -162 h2 image from the [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?4162 | + | <em>left: Lunar Orbiter IV -162 h2 image from the [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?4162 LPI Lunar Orbiter Photo Gallery] and right: Lunar Orbiter III image 3214 Medium also from [http://www.lpi.usra.edu/resources/lunarorbiter/frame/?3214 LPI Lunar Orbiter Photo Gallery]</em><br /> |
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| − | Did you notice the low ridges near the horizon of [http://lpod.wikispaces.com/February+3%2C+2009 yesterday's] LPOD? That was almost a surface view of the fronts of a series of parallel mare ridges. Repeated from yesterday is the same LO 3 image, seen a little closer, with a LO 4 view to show the same area from overhead. The ridges (unnamed as are many in Procellarum) extend to the northwest from Galilaei A (bottom right of left image and right-center of right image). The steepness of the mare ridges is indicated by the small shadows they cast. This illustrates that mare ridges are not simply very low angle swells. Many mare ridges have two components - a broad gentle swell and a narrow, steeper rope-like ridge crest. Mare ridges are now known to be low angle thrust faults - meaning that one slab of mare lava rides up over what it used to be adjacent to. I don't know if the rope is simply the edge of the tilted slab or if there is a more complex origin. By the way, there is a higher res, closer [http://www.lpi.usra.edu/resources/lunarorbiter/images/preview/3214_h3.jpg | + | Did you notice the low ridges near the horizon of [http://lpod.wikispaces.com/February+3%2C+2009 yesterday's] LPOD? That was almost a surface view of the fronts of a series of parallel mare ridges. Repeated from yesterday is the same LO 3 image, seen a little closer, with a LO 4 view to show the same area from overhead. The ridges (unnamed as are many in Procellarum) extend to the northwest from Galilaei A (bottom right of left image and right-center of right image). The steepness of the mare ridges is indicated by the small shadows they cast. This illustrates that mare ridges are not simply very low angle swells. Many mare ridges have two components - a broad gentle swell and a narrow, steeper rope-like ridge crest. Mare ridges are now known to be low angle thrust faults - meaning that one slab of mare lava rides up over what it used to be adjacent to. I don't know if the rope is simply the edge of the tilted slab or if there is a more complex origin. By the way, there is a higher res, closer [http://www.lpi.usra.edu/resources/lunarorbiter/images/preview/3214_h3.jpg view] of these ridges (but it is uglier). And I was forced to use the LO 4 view because there seems to be no wonderful low Sun amateur image. Who says everything on the Moon is already imaged?<br /> |
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| − | <em>[mailto:tychocrater@yahoo.com | + | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> |
<!-- ws:start:WikiTextHeadingRule:4:<h2> --><h2 id="toc1"><!-- ws:end:WikiTextHeadingRule:4 -->UPDATE</h2> | <!-- ws:start:WikiTextHeadingRule:4:<h2> --><h2 id="toc1"><!-- ws:end:WikiTextHeadingRule:4 -->UPDATE</h2> | ||
| − | BBC now has [http://www.bbc.co.uk/worldservice/programmes/discovery.shtml | + | BBC now has [http://www.bbc.co.uk/worldservice/programmes/discovery.shtml two programs] about the Moon, with some of my comments in both. Programme 2 is an updated version of the one on Lunar Transient Phenomena including a new quote from me near the end. <br /> |
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<strong>Related Links</strong><br /> | <strong>Related Links</strong><br /> | ||
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| − | You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 | + | You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 LPOD!]<br /> |
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===COMMENTS?=== | ===COMMENTS?=== | ||
| − | + | Register, and click on the <b>Discussion</b> tab at the top of the page. | |
Revision as of 17:09, 11 January 2015
The Great Wall of Procellarum
left: Lunar Orbiter IV -162 h2 image from the LPI Lunar Orbiter Photo Gallery and right: Lunar Orbiter III image 3214 Medium also from LPI Lunar Orbiter Photo Gallery
Did you notice the low ridges near the horizon of yesterday's LPOD? That was almost a surface view of the fronts of a series of parallel mare ridges. Repeated from yesterday is the same LO 3 image, seen a little closer, with a LO 4 view to show the same area from overhead. The ridges (unnamed as are many in Procellarum) extend to the northwest from Galilaei A (bottom right of left image and right-center of right image). The steepness of the mare ridges is indicated by the small shadows they cast. This illustrates that mare ridges are not simply very low angle swells. Many mare ridges have two components - a broad gentle swell and a narrow, steeper rope-like ridge crest. Mare ridges are now known to be low angle thrust faults - meaning that one slab of mare lava rides up over what it used to be adjacent to. I don't know if the rope is simply the edge of the tilted slab or if there is a more complex origin. By the way, there is a higher res, closer view of these ridges (but it is uglier). And I was forced to use the LO 4 view because there seems to be no wonderful low Sun amateur image. Who says everything on the Moon is already imaged?
Chuck Wood
UPDATE
BBC now has two programs about the Moon, with some of my comments in both. Programme 2 is an updated version of the one on Lunar Transient Phenomena including a new quote from me near the end.
Related Links
Rükl plate 28
COMMENTS?
Click the Discussion tab above.
You can support LPOD when you buy any book from Amazon thru LPOD!
COMMENTS?
Register, and click on the Discussion tab at the top of the page.
