Difference between revisions of "May 27, 2005"

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=Is It Love or a Sinus Infection?=
 
=Is It Love or a Sinus Infection?=
 
 
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    <tr><td><div align="center" class="main_sm">Image Credit: [mailto:paololazzarotti@astromeccanica.it Paolo Lazzarotti]</p>
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<tr><td><div align="center" class="main_sm">Image Credit: [mailto:paololazzarotti@astromeccanica.it Paolo Lazzarotti]</p>
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<p align="center"><b>Is It Love or a Sinus Infection?</b></p>
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<p align="center"><b>Is It Love or a Sinus Infection?</b></p>
<p align="left">I thought I knew the Moon until I saw this image. The right side, showing Cauchy and nearby fault, rille and domes is familiar, of course. The left side reveals features in the Bay of Love (Sinus Amoris) that I never knew existed. This little nook of the Moon is a hidden treasure trove of geologic delights. Lets start on the far left (north) and work southward. From Franck (diameter 12 km) toward the word Sinus (see mouseover) the mare has a linear roughness that looks like lava flow margins. Of course this does not showup in the higher sun view of the Lunar Orbiter IV (plate 73-H3), so this may be the discovery image for these features. Maraldi Mountain (MM) looks jagged in this low sun, but higher illumination shows it to be a very odd, pancake like elevation - I wonder if it is volcanic? Inside the big nearly buried ring, Maraldi D are two hills that may be remnant central peaks, a pitted dome, and a straight, sharp-edged ridge. Mt. Esam (why was this minor hill named?) is about in the middle of a line of domes; three tiny ones are below Esam and a large pitted dome is just above it. Three more apparent small domes extend this line to the right (south) of Lucian. These 7 domes make up the longest line of domes I know of on the Moon, and strongly suggest they all erupted from a fissure. A shorter line of 3 larger domes (1, 2, 3 in mouseover) occurs north of Lucian. The low lighting near Cauchy reveals many mare ridges (as well as domes). Interestingly, many of the ridges stop at the fault, rather than continuing on the other side. This is peculiar. Finally did you notice the rimless pits (Cauchy A and Lyell A are the biggest but there are others)? Paolo’s image establishes the Amoris-Cauchy area as one of the leading volcanic concentrations on the Moon. Why here? </p>
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<p align="left">I thought I knew the Moon until I saw this image. The right side, showing Cauchy and nearby fault, rille and domes is familiar, of course. The left side reveals features in the Bay of Love (Sinus Amoris) that I never knew existed. This little nook of the Moon is a hidden treasure trove of geologic delights. Lets start on the far left (north) and work southward. From Franck (diameter 12 km) toward the word Sinus (see mouseover) the mare has a linear roughness that looks like lava flow margins. Of course this does not showup in the higher sun view of the Lunar Orbiter IV (plate 73-H3), so this may be the discovery image for these features. Maraldi Mountain (MM) looks jagged in this low sun, but higher illumination shows it to be a very odd, pancake like elevation - I wonder if it is volcanic? Inside the big nearly buried ring, Maraldi D are two hills that may be remnant central peaks, a pitted dome, and a straight, sharp-edged ridge. Mt. Esam (why was this minor hill named?) is about in the middle of a line of domes; three tiny ones are below Esam and a large pitted dome is just above it. Three more apparent small domes extend this line to the right (south) of Lucian. These 7 domes make up the longest line of domes I know of on the Moon, and strongly suggest they all erupted from a fissure. A shorter line of 3 larger domes (1, 2, 3 in mouseover) occurs north of Lucian. The low lighting near Cauchy reveals many mare ridges (as well as domes). Interestingly, many of the ridges stop at the fault, rather than continuing on the other side. This is peculiar. Finally did you notice the rimless pits (Cauchy A and Lyell A are the biggest but there are others)? Paolo’s image establishes the Amoris-Cauchy area as one of the leading volcanic concentrations on the Moon. Why here? </p>
<blockquote><p align="right">&#8212; [mailto:tychocrater@yahoo.com Chuck Wood]</blockquote>
+
<blockquote><p align="right">&#8212; [mailto:tychocrater@yahoo.com Chuck Wood]</blockquote>
 
<p align="left"><p><b>Technical Details:</b><br>
 
<p align="left"><p><b>Technical Details:</b><br>
 
April 13, 2005. Planewton DL-252 telescope + Lumenera LU075 M camera + Edmund Optics R+IR filter; 300 of 4000 frames.</p>
 
April 13, 2005. Planewton DL-252 telescope + Lumenera LU075 M camera + Edmund Optics R+IR filter; 300 of 4000 frames.</p>
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Rukl Plates 25 & 36
 
Rukl Plates 25 & 36
 
<p align="left"><b>Tomorrow's LPOD: </b> Down the Rille</p>
 
<p align="left"><b>Tomorrow's LPOD: </b> Down the Rille</p>
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<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
+
<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
[mailto:chuck@observingthesky.org Charles A. Wood]</p>
+
[mailto:tychocrater@yahoo.com Charles A. Wood]</p>
<p align="center" class="main_titles"><b>Technical Consultant:</b><br>
+
<p align="center" class="main_titles"><b>Technical Consultant:</b><br>
[mailto:anthony@perseus.gr Anthony Ayiomamitis]</p>
+
[mailto:anthony@perseus.gr Anthony Ayiomamitis]</p>
<p align="center" class="main_titles"><b>Contact Translator:</b><br>
+
<p align="center" class="main_titles"><b>Contact Translator:</b><br>
[mailto:pablolonnie@yahoo.com.mx" class="one Pablo Lonnie Pacheco Railey]  (Es)<br>
+
[mailto:pablolonnie@yahoo.com.mx" class="one Pablo Lonnie Pacheco Railey]  (Es)<br>
[mailto:chlegrand@free.fr" class="one Christian Legrand] (Fr)</p>
+
[mailto:chlegrand@free.fr" class="one Christian Legrand] (Fr)</p>
<p align="center" class="main_titles"><b>[mailto:webuser@observingthesky.org Contact Webmaster]</b></p>
+
<p align="center" class="main_titles"><b>[mailto:webuser@observingthesky.org Contact Webmaster]</b></p>
<p align="center" class="main_titles"><b>A service of:</b><br>
+
<p align="center" class="main_titles"><b>A service of:</b><br>
[http://www.observingthesky.org/" class="one ObservingTheSky.Org]</p>
+
[http://www.observingthesky.org/" class="one ObservingTheSky.Org]</p>
<p align="center" class="main_titles"><b>Visit these other PODs:</b> <br>
+
<p align="center" class="main_titles"><b>Visit these other PODs:</b> <br>
[http://antwrp.gsfc.nasa.gov/apod/astropix.html" class="one Astronomy] | [http://www.msss.com/" class="one Mars] | [http://epod.usra.edu/" class="one Earth]</p>
+
[http://antwrp.gsfc.nasa.gov/apod/astropix.html" class="one Astronomy] | [http://www.msss.com/" class="one Mars] | [http://epod.usra.edu/" class="one Earth]</p>
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<p>&nbsp;</p>
 
<p>&nbsp;</p>
 
 
 
 
 
----
 
----
 
===COMMENTS?===  
 
===COMMENTS?===  
 
Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.
 
Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.

Revision as of 18:33, 4 January 2015

Is It Love or a Sinus Infection?

<nobr>Is It Love or a Sinus Infection?</nobr>

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Image Credit: Paolo Lazzarotti


Is It Love or a Sinus Infection?

I thought I knew the Moon until I saw this image. The right side, showing Cauchy and nearby fault, rille and domes is familiar, of course. The left side reveals features in the Bay of Love (Sinus Amoris) that I never knew existed. This little nook of the Moon is a hidden treasure trove of geologic delights. Lets start on the far left (north) and work southward. From Franck (diameter 12 km) toward the word Sinus (see mouseover) the mare has a linear roughness that looks like lava flow margins. Of course this does not showup in the higher sun view of the Lunar Orbiter IV (plate 73-H3), so this may be the discovery image for these features. Maraldi Mountain (MM) looks jagged in this low sun, but higher illumination shows it to be a very odd, pancake like elevation - I wonder if it is volcanic? Inside the big nearly buried ring, Maraldi D are two hills that may be remnant central peaks, a pitted dome, and a straight, sharp-edged ridge. Mt. Esam (why was this minor hill named?) is about in the middle of a line of domes; three tiny ones are below Esam and a large pitted dome is just above it. Three more apparent small domes extend this line to the right (south) of Lucian. These 7 domes make up the longest line of domes I know of on the Moon, and strongly suggest they all erupted from a fissure. A shorter line of 3 larger domes (1, 2, 3 in mouseover) occurs north of Lucian. The low lighting near Cauchy reveals many mare ridges (as well as domes). Interestingly, many of the ridges stop at the fault, rather than continuing on the other side. This is peculiar. Finally did you notice the rimless pits (Cauchy A and Lyell A are the biggest but there are others)? Paolo’s image establishes the Amoris-Cauchy area as one of the leading volcanic concentrations on the Moon. Why here?

Chuck Wood

Technical Details:
April 13, 2005. Planewton DL-252 telescope + Lumenera LU075 M camera + Edmund Optics R+IR filter; 300 of 4000 frames.

Related Links:
Rukl Plates 25 & 36

Tomorrow's LPOD: Down the Rille



Author & Editor:
Charles A. Wood

Technical Consultant:
Anthony Ayiomamitis

Contact Translator:
" class="one Pablo Lonnie Pacheco Railey (Es)
" class="one Christian Legrand (Fr)

Contact Webmaster

A service of:
" class="one ObservingTheSky.Org

Visit these other PODs:
" class="one Astronomy | " class="one Mars | " class="one Earth

 


COMMENTS?

Click on this icon File:PostIcon.jpg at the upper right to post a comment.