|
[2004-07-30]
¥dùºû´µ§C¦a
Caloris Planitia
| ¤ÑÅé |
¤ô¬P |
| ½n«× |
30.5N |
| ¸g«× |
189.8W |
| ¦WºÙÄݦa |
©Ô¤B |
| ±Ä¥Î¦~¥÷ |
1976 |
| ¦WºÙ°O¸ü |
Lists
of names for Mercury nomenclature, provided by David Morrison |
| ¦WºÙ¥Ñ¨Ó |
"ª¢¼öªº¥ì"¡A³oùØªí±·Å«×³Ì°ª |
¥dùºû´µ§C¦a Caloris
Planitia
Credit :: JPL
[PIA03102] |
¤ô¬P¤W³ÌµÛ¦Wªº¬O¦ì©ó¥dùºû´µ§C¦a(Caloris
Planitia¡A«UºÙ Caloris Basin)¤Wª½®|¹F1300kmªº¥¨¤j¹k¥Û§|¡A³o¹k¥Û§|ªºª½®|¹F¤ô¬P¦Û¨ª½®|ªº1/4¡C³o¹k¥Û§|¥]³òªº¦a¤è´N¬O¥dùºû´µ§C¦a¡A¥~³òªº¬O¥dùºû´µ¤s(Caloris
Montes)¡C¥Ñ©ó¨ü¨ì«D±`¥¨¤jªº¼²À»¡A¦b¤ô¬Pªí±¤W§Î¦¨¥dùºû´µ¹k¥Û§|¡A¤£³æ¦p¦¹¡A¥dùºû´µ¼²À»ªº¼vÅTÁÙ¬ï¹L¤ô¬Pªº®Ö¤ß¡A¼²À»ªº½ÄÀ»ªi³z¹L¤ô¬Pªí±©M¦a®Öªº¶Ç¼½¨ì¹F¥dùºû´µªº¹ï·¥¡A¥O¨º¨àªº¦a´ß¬ð°_¨Ó¡A§Î¦¨¤F«Ü¦h¤s»P¤Î½u±øª¬ªº¦a§Î¡C(³oºØ¦a§Î¤£¦s¦b©ó¤ô¬Pªº¨ä¥L¦a¤è)¹³³o¼Ëªº¦]¥¨¤j¼²À»¦Ó¦¨ªº¹ï·¥¦a§Î¡A©ó¤ë²y©M¤ì½Ã¥|¥d¥§´µ¦«¤]¦³µo²{¡C
¥dùºû´µ¬O©Ô¤B¤å¡u¼ö¡vªº·N«ä¡A¨ä¹ê¨CÓ¬P²y¤Wªº¦a§Î¯S¼x³£¦³¬J©wªº©R¦W¤èªk¡A¥H¤ô¬P¬°¨Ò¡A¥ì·|¥Î¡u¤ô¬P¡vªº¤£¦P»y¨¥¨Ó©R¦W¡A¹k¥Û§|·|¤Þ¥ÎµÛ¦WªºÃÀ³N®a¡Bµ¼Ö®a¡Bµe®a¡B§@®aªº¦W¦r¡C¥dùºû´µ¦ì©ó¤ô¬Pªº¡u¼ö·¥¡v(hot
pole)¤W¡A¨C·í¤ô¬P¹Lªñ¤éÂI®É¡A¤Ó¶§´N·|ªø®É¶¡°±¯d·Ó®g©ó¥dùºû´µ¤§¤W¡A´N¹³¤@Ó¨`¼ö¦aº»¡A¥dùºû´µ¤]¦]¦Ó±o¦W¡C¦æ¬PÀô¶¤Ó¶§¤½Âà³t«×ªº§ÖºC¡A¥Ñ¸Ó¦æ¬PÂ÷¤Ó¶§ªº¦ì¸m»·ªñ¦Ó©w¡A´Nºâ¬O¦P¤@Áû¦æ¬P¡A¤½Â઺³t«×¤]®É§Ö®ÉºC¡A©óªñ¤éÂI§Ö¡A»·¤éÂIºC¡C¥Ñ©ó¤ô¬P«Ü±µªñ¤Ó¶§¡A¹Lªñ¤éÂI®Éªº¤½Âà³t«×§Ö±o¶W¹L¤F¤ô¬P¥»¨ªº¦ÛÂà³t«×¡AP¨Ï¥X²{¤@Ó©_©Çªº²{¶H¡AYªG¦³¤H¯¸¦b¥dùºû´µ¤W¬ÝµÛ¤Ó¶§¦b¤Ñ¤Wªº²¾°Ê¡A·|¬Ý¨£¤Ó¶§º¥ý°±¤î²¾°Ê¡AµM«á§ó¦V¬Û¤Ï¤è¦V°f¦æ¡Aµ¥¤ô¬P»·Â÷ªñ¤éÂI¤~¦^´_¥¿±`¡C
| Object |
Mercury |
| Lat |
30.5N |
| Long |
189.8W |
| Ethnic
group |
Latin |
| Year
adopted |
1976 |
| Name
source |
Lists
of names for Mercury nomenclature, provided by David Morrison |
| Name
origin |
"Hot
plain"; surface temperature hottest near this position |
The
most famous feature on Mercury is the 1300km diameter impact crater
located at Caloris Planitia (or informally Caloris Basin), where its
size is as large as 1/4 of Mercury's diameter. The crater floor is Caloris
Planitia and surounded by Caloris Montes. This crater was formed during
a very large impact 3.6 billion years ago, shockwaves of this impact
even travelled through Mercury's surface and core, created hilly and
lineated terrain on its antipode. This unique features only exist on
Caloris and its antipode. While this kind of landscape formed during
huge impact can also be found on the Moon and Callisto, the Jovian moon.
Calois
is the word "hot" in Latin. We name this planitia as Caloris
as it is located at Mercury's "hot pole", our Sun would directly
shine on Caloris when Mercury is at perihelion. At perihelion, Mercury
moves so swiftly that, its self rotation slower than its orbital speed,
therefore from the vantage of someone on the surface, the sun would
appear to stop in the sky and go backward - until the planet's rotation
catches up and makes the sun go forward again.
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