Difference between revisions of "August 25, 2010"

From LPOD
Jump to: navigation, search
Line 3: Line 3:
 
<!-- ws:start:WikiTextHeadingRule:1:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextHeadingRule:1:&lt;h1&gt; -->
 
<!-- ws:start:WikiTextLocalImageRule:16:&lt;img src=&quot;/file/view/LPOD-Aug25-10.jpg/158173079/LPOD-Aug25-10.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Aug25-10.jpg|LPOD-Aug25-10.jpg]]<!-- ws:end:WikiTextLocalImageRule:16 --><br />
 
<!-- ws:start:WikiTextLocalImageRule:16:&lt;img src=&quot;/file/view/LPOD-Aug25-10.jpg/158173079/LPOD-Aug25-10.jpg&quot; alt=&quot;&quot; title=&quot;&quot; /&gt; -->[[File:LPOD-Aug25-10.jpg|LPOD-Aug25-10.jpg]]<!-- ws:end:WikiTextLocalImageRule:16 --><br />
<em>image by [mailto:stefanoderosa66@gmail.com" rel="nofollow Stefano De Rosa]</em><br />
+
<em>image by [mailto:stefanoderosa66@gmail.com Stefano De Rosa]</em><br />
 
<br />
 
<br />
 
Stefano and his daughter are big fans of the full Moon. The Moon itself has been considered a daughter of the Earth. In the 1960s, before Apollo began to provide other evidence, a major theory was that the Moon broke off the Earth, with the early Earth's rapid rotation oozing off crustal material that the Moon formed from. In this model, the Moon was made of terrestrial mantle material, an offspring of Mother Earth. But Apollo showed that Moon rocks were strongly depleted in volatiles, inconsistent with the traditional fission model of its formation. Elements of the daughter model survive in the current Big Splash theory, with the kick start (and a free parameter) of a giant impact providing the heat to eliminate volatiles.  <br />
 
Stefano and his daughter are big fans of the full Moon. The Moon itself has been considered a daughter of the Earth. In the 1960s, before Apollo began to provide other evidence, a major theory was that the Moon broke off the Earth, with the early Earth's rapid rotation oozing off crustal material that the Moon formed from. In this model, the Moon was made of terrestrial mantle material, an offspring of Mother Earth. But Apollo showed that Moon rocks were strongly depleted in volatiles, inconsistent with the traditional fission model of its formation. Elements of the daughter model survive in the current Big Splash theory, with the kick start (and a free parameter) of a giant impact providing the heat to eliminate volatiles.  <br />
 
<br />
 
<br />
<em>[mailto:tychocrater@yahoo.com" rel="nofollow Chuck Wood]</em><br />
+
<em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br />
 
<br />
 
<br />
 
<strong>Technical Details</strong><br />
 
<strong>Technical Details</strong><br />
Line 13: Line 13:
 
<br />
 
<br />
 
<hr />
 
<hr />
<div>You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591" rel="nofollow LPOD!]<br />
+
<div>You can support LPOD when you buy any book from Amazon thru [http://www.lpod.org/?page_id=591 LPOD!]<br />
 
</div>
 
</div>
 
----
 
----
 
===COMMENTS?===  
 
===COMMENTS?===  
Click on this icon [[image:PostIcon.jpg]] at the upper right to post a comment.
+
Register, and click on the <b>Discussion</b> tab at the top of the page.

Revision as of 17:23, 11 January 2015

Daughter Moon

LPOD-Aug25-10.jpg
image by Stefano De Rosa

Stefano and his daughter are big fans of the full Moon. The Moon itself has been considered a daughter of the Earth. In the 1960s, before Apollo began to provide other evidence, a major theory was that the Moon broke off the Earth, with the early Earth's rapid rotation oozing off crustal material that the Moon formed from. In this model, the Moon was made of terrestrial mantle material, an offspring of Mother Earth. But Apollo showed that Moon rocks were strongly depleted in volatiles, inconsistent with the traditional fission model of its formation. Elements of the daughter model survive in the current Big Splash theory, with the kick start (and a free parameter) of a giant impact providing the heat to eliminate volatiles.

Chuck Wood

Technical Details
August 24, 2010 at 11.46 p.m. (local time). Canon Eos 1000d; Exp: 10 seconds; F/5.6; ISO 100; focal lenght: 18mm, from Isola d' Elba (Italy)


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.