Difference between revisions of "October 24, 2004"

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=A Long, Cold Mare=
 
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    <tr><td><div align="center" class="main_sm">Image Credit: [mailto:kcpaulhk@yahoo.com.hk KC Pau]</p>
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<p align="center"><b>A Long, Cold Mare</b></p>
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<p align="center"><b>A Long, Cold Mare</b></p>
<p align="left">Maria seem to come in all shapes and [http://cwm.lpod.org/DataStuff/MareAreas.htm  sizes] - from the large, near circular Mare Imbrium to the small Mare Anguis (which I always think of as anguishing over its impudence in being a mare rather than a lacus). But the strangest mare of all is Frigoris, which stretches about 1600 km from east to west, but only 200 or so km from north to south. Frigoris clearly does not fill a circular impact basin, and the best that can be said is that its mare lavas occupy a concentric depression around Imbrium, just as do Mare Vaporum and Sinus Aestuum. The Frigoris lavas seem to be of somewhat diverse ages and compositions. KC's image illustrates that large parts of the mare are lighter than other parts, partially because it is crossed by some bright [http://www.lpod.org/archive/2004/05/LPOD-2004-05-14.htm rays]. But part of the light hue is due to a difference in composition - the Galileo multi-spectral [http://www.lpod.org/archive/2004/05/LPOD-2004-05-10.htm image] shows that most of Frigoris is gold-hued, but the western part is blue. And gold = titanium-poor, and blue = intermediate titanium lavas. Crater counts indicate that most Imbrium lavas are Imbrium in age, but the darker patches north of Plato and the broad region around Harpalus are [http://www.lpod.org/archive/2004/02/LPOD-2004-02-23.htm Eratosthenian].
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<p align="left">Maria seem to come in all shapes and [http://cwm.lpod.org/DataStuff/MareAreas.htm  sizes] - from the large, near circular Mare Imbrium to the small Mare Anguis (which I always think of as anguishing over its impudence in being a mare rather than a lacus). But the strangest mare of all is Frigoris, which stretches about 1600 km from east to west, but only 200 or so km from north to south. Frigoris clearly does not fill a circular impact basin, and the best that can be said is that its mare lavas occupy a concentric depression around Imbrium, just as do Mare Vaporum and Sinus Aestuum. The Frigoris lavas seem to be of somewhat diverse ages and compositions. KC's image illustrates that large parts of the mare are lighter than other parts, partially because it is crossed by some bright [http://www.lpod.org/archive/2004/05/LPOD-2004-05-14.htm rays]. But part of the light hue is due to a difference in composition - the Galileo multi-spectral [http://www.lpod.org/archive/2004/05/LPOD-2004-05-10.htm image] shows that most of Frigoris is gold-hued, but the western part is blue. And gold = titanium-poor, and blue = intermediate titanium lavas. Crater counts indicate that most Imbrium lavas are Imbrium in age, but the darker patches north of Plato and the broad region around Harpalus are [http://www.lpod.org/archive/2004/02/LPOD-2004-02-23.htm Eratosthenian].
 
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<blockquote><p align="right">&#8212; [mailto:chuck@observingthesky.org Chuck Wood]</blockquote>
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<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>
 
September 26, 2004, a mosaic of 4 images using a 10" Newtonian and a webcam. CAW has enhanced the image using the Photoshop unsharp mask filter.</p>
 
September 26, 2004, a mosaic of 4 images using a 10" Newtonian and a webcam. CAW has enhanced the image using the Photoshop unsharp mask filter.</p>
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<br>Rukl <i>Atlas of the Moon,</i> Sheets 2, 3 & 4
 
<br>Rukl <i>Atlas of the Moon,</i> Sheets 2, 3 & 4
 
<p align="left"><b>Tomorrow's LPOD: </b> Modeling Domes</p>
 
<p align="left"><b>Tomorrow's LPOD: </b> Modeling Domes</p>
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<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
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<p align="center" class="main_titles"><b>Author &amp; Editor:</b><br>  
[mailto:chuck@observingthesky.org Charles A. Wood]</p>
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[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>
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<p align="center" class="main_titles"><b>Contact Translator:</b><br>
[mailto:pablolonnie@yahoo.com.mx" class="one Pablo Lonnie Pacheco Railey]  (Es)<br>
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[mailto:pablolonnie@yahoo.com.mx" class="one Pablo Lonnie Pacheco Railey]  (Es)<br>
[mailto:chlegrand@free.fr" class="one Christian Legrand] (Fr)</p>
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[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 18:26, 4 January 2015

A Long, Cold Mare

<nobr>A Long, Cold Mare</nobr>

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Image Credit: KC Pau


A Long, Cold Mare

Maria seem to come in all shapes and sizes - from the large, near circular Mare Imbrium to the small Mare Anguis (which I always think of as anguishing over its impudence in being a mare rather than a lacus). But the strangest mare of all is Frigoris, which stretches about 1600 km from east to west, but only 200 or so km from north to south. Frigoris clearly does not fill a circular impact basin, and the best that can be said is that its mare lavas occupy a concentric depression around Imbrium, just as do Mare Vaporum and Sinus Aestuum. The Frigoris lavas seem to be of somewhat diverse ages and compositions. KC's image illustrates that large parts of the mare are lighter than other parts, partially because it is crossed by some bright rays. But part of the light hue is due to a difference in composition - the Galileo multi-spectral image shows that most of Frigoris is gold-hued, but the western part is blue. And gold = titanium-poor, and blue = intermediate titanium lavas. Crater counts indicate that most Imbrium lavas are Imbrium in age, but the darker patches north of Plato and the broad region around Harpalus are Eratosthenian.

Chuck Wood

Technical Details:
September 26, 2004, a mosaic of 4 images using a 10" Newtonian and a webcam. CAW has enhanced the image using the Photoshop unsharp mask filter.

Related Links:
Ages of Mare Basalts...
Rukl Atlas of the Moon, Sheets 2, 3 & 4

Tomorrow's LPOD: Modeling Domes



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.