Difference between revisions of "O'Day"

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(Created page with "<div id="content_view" class="wiki" style="display: block"> =O'Day= {| class="wiki_table" | Lat: 30.62°S, Long: 157.5°E, Diam: 72.66 km, Depth: 5.6 km, Rükl: ''(farside...")
 
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Lat: 30.62°S, Long: 157.5°E, Diam: 72.66 km, Depth: 5.6 km, Rükl: ''(farside)'', [http://the-moon.wikispaces.com/Stratigraphy Copernican]<br />
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Lat: 30.62°S, Long: 157.5°E, Diam: 72.66 km, Depth: 5.6 km, Rükl: ''(farside)'', [http://the-moon.us/wiki/Stratigraphy Copernican]<br />
 
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[http://www.lpod.org/coppermine/thumbnails.php?album=search&type=full&search=O%27Day LPOD Photo Gallery] [http://www.lpi.usra.edu/resources/lunar_orbiter/bin/srch_nam.shtml?O%27Day%7C0 Lunar Orbiter Images] [http://www.lpi.usra.edu/resources/apollo/search/feature/?feature=O%27Day Apollo Images]<br /> [http://www.lpi.usra.edu/resources/lunarorbiter/images/preview/2075_h3.jpg LO-II 075 h3] is a HiRes scan of Lunar Orbiter II's detailed photograph of '''O'Day''' (upper part of photograph, south up), with a curious elongated depression near the photograph's lower left corner (called '''Barbier K''')(according to LAC 103 in the ''Clementine Atlas of the Moon'').<br />  Additional research: Danny Caes<br /> <br />  
 
[http://www.lpod.org/coppermine/thumbnails.php?album=search&type=full&search=O%27Day LPOD Photo Gallery] [http://www.lpi.usra.edu/resources/lunar_orbiter/bin/srch_nam.shtml?O%27Day%7C0 Lunar Orbiter Images] [http://www.lpi.usra.edu/resources/apollo/search/feature/?feature=O%27Day Apollo Images]<br /> [http://www.lpi.usra.edu/resources/lunarorbiter/images/preview/2075_h3.jpg LO-II 075 h3] is a HiRes scan of Lunar Orbiter II's detailed photograph of '''O'Day''' (upper part of photograph, south up), with a curious elongated depression near the photograph's lower left corner (called '''Barbier K''')(according to LAC 103 in the ''Clementine Atlas of the Moon'').<br />  Additional research: Danny Caes<br /> <br />  
 
==Maps==
 
==Maps==
''([http://the-moon.wikispaces.com/LAC%20zone LAC zone] 103D3)'' [http://www.lpi.usra.edu/resources/mapcatalog/LM/lm103/ LM map]<br /> <br />  
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''([http://the-moon.us/wiki/LAC%20zone LAC zone] 103D3)'' [http://www.lpi.usra.edu/resources/mapcatalog/LM/lm103/ LM map]<br /> <br />  
 
==Description==
 
==Description==
 
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* Originally mapped as Copernican because it has rays but these are compositional rays (highlands material) thatt have reached full optical maturity and thus are older than Copernicus; O'Day is Eratosthenian age. (Hawke et al: Composition and origin of Copernican Rays… Mappers Conference 2005).
 
* Originally mapped as Copernican because it has rays but these are compositional rays (highlands material) thatt have reached full optical maturity and thus are older than Copernicus; O'Day is Eratosthenian age. (Hawke et al: Composition and origin of Copernican Rays… Mappers Conference 2005).
 
* Maximum depth read from LM map; seems too deep.
 
* Maximum depth read from LM map; seems too deep.
* [http://the-moon.wikispaces.com/Central%20peak%20composition Central peak composition]: A, GNTA1 & GNTA2 ([http://the-moon.wikispaces.com/Tompkins%20%26%20Pieters%2C%201999 Tompkins & Pieters, 1999])
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* [http://the-moon.us/wiki/Central%20peak%20composition Central peak composition]: A, GNTA1 & GNTA2 ([http://the-moon.us/wiki/Tompkins%20%26%20Pieters%2C%201999 Tompkins & Pieters, 1999])
* Exterior impact melt deposits most extensive to ESE, max of ~30 km beyond rim. Most extensive ejecta, rays and secondary craters to the SE, with max wall slumping on W side of crater, and topographically lowest rim crest to SE ([http://the-moon.wikispaces.com/Hawke%20and%20Head%2C%201977 Hawke and Head, 1977]).
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* Exterior impact melt deposits most extensive to ESE, max of ~30 km beyond rim. Most extensive ejecta, rays and secondary craters to the SE, with max wall slumping on W side of crater, and topographically lowest rim crest to SE ([http://the-moon.us/wiki/Hawke%20and%20Head%2C%201977 Hawke and Head, 1977]).
 
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==Nomenclature==
 
==Nomenclature==
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<br /> <br />
 
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[http://the-moon.wikispaces.com/Alphabetical%20Index Named Features] -- Prev: [http://the-moon.wikispaces.com/Obruchev Obruchev] -- Next: [http://the-moon.wikispaces.com/Lacus%20Odii Lacus Odii]<br />
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[http://the-moon.us/wiki/Alphabetical%20Index Named Features] -- Prev: [http://the-moon.us/wiki/Obruchev Obruchev] -- Next: [http://the-moon.us/wiki/Lacus%20Odii Lacus Odii]<br />
 
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Revision as of 20:26, 11 April 2018

O'Day

Lat: 30.62°S, Long: 157.5°E, Diam: 72.66 km, Depth: 5.6 km, Rükl: (farside), Copernican

Table of Contents

[#O'Day O'Day]
[#O'Day-Images Images]
[#O'Day-Maps Maps]
[#O'Day-Description Description]
[#O'Day-Description-Wikipedia Wikipedia]
[#O'Day-Additional Information Additional Information]
[#O'Day-Nomenclature Nomenclature]
[#O'Day-LPOD Articles LPOD Articles]
[#O'Day-Bibliography Bibliography]
external image normal_oday.jpg
LROC image WAC No. M118823820ME. Calibrated by LROC_WAC_Previewer.

Images

LPOD Photo Gallery Lunar Orbiter Images Apollo Images
LO-II 075 h3 is a HiRes scan of Lunar Orbiter II's detailed photograph of O'Day (upper part of photograph, south up), with a curious elongated depression near the photograph's lower left corner (called Barbier K)(according to LAC 103 in the Clementine Atlas of the Moon).
Additional research: Danny Caes

Maps

(LAC zone 103D3) LM map

Description


Wikipedia

O'Day

Additional Information

  • IAU page: O'Day
  • Originally mapped as Copernican because it has rays but these are compositional rays (highlands material) thatt have reached full optical maturity and thus are older than Copernicus; O'Day is Eratosthenian age. (Hawke et al: Composition and origin of Copernican Rays… Mappers Conference 2005).
  • Maximum depth read from LM map; seems too deep.
  • Central peak composition: A, GNTA1 & GNTA2 (Tompkins & Pieters, 1999)
  • Exterior impact melt deposits most extensive to ESE, max of ~30 km beyond rim. Most extensive ejecta, rays and secondary craters to the SE, with max wall slumping on W side of crater, and topographically lowest rim crest to SE (Hawke and Head, 1977).


Nomenclature

Marcus Driver O'Day (1897 – 1961) was an American physicist. In 1946 and 1947 he guided a team that worked to launch scientific payloads into the ionosphere using V-2 rockets. He would theorize in 1958 that solar power could be used to sustain a colony on the Moon, and hypothesized that there may be water under the lunar surface.

LPOD Articles


Bibliography




Named Features -- Prev: Obruchev -- Next: Lacus Odii


This page has been edited 1 times. The last modification was made by - tychocrater tychocrater on Jun 13, 2009 3:24 pm - afx3u3