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Posted Tuesday February 26, 2008, 2:08 pm, Over one day old
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daily pictures of Earth's moon
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The LPOD software is too slow to use today - please go back HERE, to the Moon-Wiki site for Wednesday’s LPOD of a historic image. Chuck
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I want to use it for LPOD so I’ll have to find something new to say… Wait, what is that thin line near top right between the west end of the Straight Range and the isolated peak? The upper part of the chain, near shore, is definitely a secondary crater chain cluster.
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Read A NARROW THRILL (Links)
Visit LPOD at a temporary home until I can repair the normal LPOD software.
Read LPOD IS BROKEN (Links)
image from JAXA, Japan, and Lunar Orbiter IV added by C. Wood Selene and the other lunar orbiters will do much more than capture images of the Moon’s surface. The highest parts of the Cordillera Mountains - the outer prominent Orientale ring - are 5 km above the average radius.
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Read HOW HIGH THE MOON (AND LOW TOO)? (Links)
Did erosion remove the sea sides of lunar bays? Looking at a beautiful bay in Hong Kong caused us to consider how bays form on Earth and Moon, and even though there are few similarities in the processes, the thinking has been informative.
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Read APPLES AND ORANGES (Links)
image by Paolo R. Lazzarotti, Massa, Italy. The southern part of the floor is lighter hued, more cratered and slightly more elevated than the northern half. There are a dozen or more craters that have been covered entirely or partially filled by the smooth fill on the northern floor.
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Read A SMOOTHER DEPRESSION (Links)
Read CRYSTAL SKYRING (Links)
image by Oliver Pettenpaul Mare Humorum and Orientale are such compelling targets that the region between is often overlooked. At bottom right is a pond of lava captured between the Humorum mare-edge ring (diameter 425 km according to Paul Spudis) and the next one out.
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Read MERSENIUS WEST (Links)
The thing that jumped out immediately to me was the broad very low dome near the middle of Agatharchides at the bottom of the image. Another interesting feature at the top left is a elongated oval swell cut down the middle by a curved depression.
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Read INCONSPICUOUS VOLCANICS (Links)
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