Difference between revisions of "March 22, 2004"
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=Double Planet= | =Double Planet= | ||
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| − | + | [[File:LPOD-2004-03-22.gif|LPOD-2004-03-22.gif]]</div> | |
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| − | + | <td><div align="center"><p>Image Credit: [http://www2.jpl.nasa.gov/galileo/earthmo2.html Galileo Mission]</p></div></td> | |
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| − | + | <p class="story" align="center"><b>Double Planet </b></p> | |
| − | + | <p class="story" align="left"> | |
| − | + | The origin of the Moon was long a mystery. Most scientists now accept the giant impact | |
| − | + | [[March_12,_2004|model]] but one of the earlier ideas was that the Earth and Moon formed at the | |
| − | + | same time from the same region of the solar nebula. However, this sister planet or double planet theory could not | |
| − | + | explain why, if the two worlds formed of the same material, the Earth has a massive iron core and a density of | |
| − | + | 5.5 g/cc while the Moon has only a small amount of iron and a resulting density of only 3.3 g/cc. The double | |
| − | + | planet theory is dead, but the Earth-Moon system does look like a double planet because the Moon is relatively | |
| − | + | large compared to the Earth: their diameters are 3,476 km and 12,756 km. And like a contrasting double star pair, | |
| − | + | the colors of our two worlds are strikingly different - we must be one of the most wonderful sights in the solar | |
| − | + | system! </p> | |
| − | + | <p><b>Technical Details:</b><br> | |
| − | + | The Galileo spacecraft took this image in 1992 while swinging close to Earth for a gravitational | |
| − | + | push towards Jupiter. The Moon is actually in the foreground moving from left to right around the | |
| − | + | Earth. The JPL web site says that contrast and color of both Earth and Moon were enhanced, but | |
| − | + | the Moon looks yellower to me than it actually is. However, the image was taken not through a green | |
| − | + | filter that mimics our eyes sensitivity, but with violet, red and infrared filters and may be | |
| − | + | correct for this combination. </p> | |
| − | + | <p class="story"><b>Related Links:</b><br> | |
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[http://www2.jpl.nasa.gov/galileo/mission_end.html Galileo mission overview]<br> | [http://www2.jpl.nasa.gov/galileo/mission_end.html Galileo mission overview]<br> | ||
[http://www.lpl.arizona.edu/outreach/origin/ The Origin of the Moon]</p> | [http://www.lpl.arizona.edu/outreach/origin/ The Origin of the Moon]</p> | ||
| − | + | <p><b>Yesterday's LPOD:</b> [[March 21, 2004|Fold a Moon]] </p> | |
| − | + | <p><b>Tomorrow's LPOD:</b> [[March 23, 2004|Magnificent Moon!]] </p> | |
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| − | + | <p align="center" class="main_titles"><b>Author & Editor:</b><br> | |
| − | + | [mailto:tychocrater@yahoo.com Charles A. Wood]</p> | |
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Latest revision as of 18:14, 7 February 2015
Double Planet
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Image Credit: Galileo Mission |
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Double Planet The origin of the Moon was long a mystery. Most scientists now accept the giant impact model but one of the earlier ideas was that the Earth and Moon formed at the same time from the same region of the solar nebula. However, this sister planet or double planet theory could not explain why, if the two worlds formed of the same material, the Earth has a massive iron core and a density of 5.5 g/cc while the Moon has only a small amount of iron and a resulting density of only 3.3 g/cc. The double planet theory is dead, but the Earth-Moon system does look like a double planet because the Moon is relatively large compared to the Earth: their diameters are 3,476 km and 12,756 km. And like a contrasting double star pair, the colors of our two worlds are strikingly different - we must be one of the most wonderful sights in the solar system! Technical Details: Related Links: Yesterday's LPOD: Fold a Moon Tomorrow's LPOD: Magnificent Moon! |
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Author & Editor: |
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