Difference between revisions of "Bergstrand"
(Created page with "<div id="content_view" class="wiki" style="display: block"> =Bergstrand= {| class="wiki_table" | Lat: 18.8°S, Long: 176.3°E, Diam: 43 km, Depth: km, Rükl: ''(farside)''<...") |
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[[Image:bergstrand-color.jpg|bergstrand-color.jpg]]<br /> | [[Image:bergstrand-color.jpg|bergstrand-color.jpg]]<br /> | ||
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| − | '''Left:''' [http://www.lpi.usra.edu/resources/apollo/frame/?AS17-M-0478 AS17-M-0478] (Note, the image in link has North on right, West on top). '''Right:''' [http://planetarynames.wr.usgs.gov/images/Lunar/lac_104.pdf Color-coded LAC 104] from [ | + | '''Left:''' [http://www.lpi.usra.edu/resources/apollo/frame/?AS17-M-0478 AS17-M-0478] (Note, the image in link has North on right, West on top). '''Right:''' [http://planetarynames.wr.usgs.gov/images/Lunar/lac_104.pdf Color-coded LAC 104] from [[USGS%20Digital%20Atlas|USGS Digital Atlas]].<br /> <div id="toc"> |
=Table of Contents= | =Table of Contents= | ||
<div style="margin-left: 1em">[#Bergstrand Bergstrand]</div><div style="margin-left: 2em">[#Bergstrand-Images Images]</div><div style="margin-left: 2em">[#Bergstrand-Maps Maps]</div><div style="margin-left: 2em">[#Bergstrand-Description Description]</div><div style="margin-left: 2em">[#Bergstrand-Description: Wikipedia Description: Wikipedia]</div><div style="margin-left: 2em">[#Bergstrand-Additional Information Additional Information]</div><div style="margin-left: 2em">[#Bergstrand-Nomenclature Nomenclature]</div><div style="margin-left: 2em">[#Bergstrand-LPOD Articles LPOD Articles]</div><div style="margin-left: 2em">[#Bergstrand-Bibliography Bibliography]</div></div> | <div style="margin-left: 1em">[#Bergstrand Bergstrand]</div><div style="margin-left: 2em">[#Bergstrand-Images Images]</div><div style="margin-left: 2em">[#Bergstrand-Maps Maps]</div><div style="margin-left: 2em">[#Bergstrand-Description Description]</div><div style="margin-left: 2em">[#Bergstrand-Description: Wikipedia Description: Wikipedia]</div><div style="margin-left: 2em">[#Bergstrand-Additional Information Additional Information]</div><div style="margin-left: 2em">[#Bergstrand-Nomenclature Nomenclature]</div><div style="margin-left: 2em">[#Bergstrand-LPOD Articles LPOD Articles]</div><div style="margin-left: 2em">[#Bergstrand-Bibliography Bibliography]</div></div> | ||
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[http://www.lpod.org/coppermine/thumbnails.php?album=search&type=full&search=Bergstrand LPOD Photo Gallery] [http://www.lpi.usra.edu/resources/lunar_orbiter/bin/srch_nam.shtml?Bergstrand%7C0 Lunar Orbiter Images] [http://www.lpi.usra.edu/resources/apollo/search/feature/?feature=Bergstrand Apollo Images]<br /> [http://www.mentallandscape.com/C_Zond08_60.jpg Frame 60], made by ZOND 8, shows '''Bergstrand''' rightward of the frame's central cross. Research: Danny Caes<br /> <br /> | [http://www.lpod.org/coppermine/thumbnails.php?album=search&type=full&search=Bergstrand LPOD Photo Gallery] [http://www.lpi.usra.edu/resources/lunar_orbiter/bin/srch_nam.shtml?Bergstrand%7C0 Lunar Orbiter Images] [http://www.lpi.usra.edu/resources/apollo/search/feature/?feature=Bergstrand Apollo Images]<br /> [http://www.mentallandscape.com/C_Zond08_60.jpg Frame 60], made by ZOND 8, shows '''Bergstrand''' rightward of the frame's central cross. Research: Danny Caes<br /> <br /> | ||
==Maps== | ==Maps== | ||
| − | ''([ | + | ''([[LAC%20zone|LAC zone]] 104A2)'' [http://www.lpi.usra.edu/resources/mapcatalog/LM/lm104/ LM map]<br /> <br /> |
==Description== | ==Description== | ||
| − | '''Bergstrand''' has impacted close to [ | + | '''Bergstrand''' has impacted close to [[Aitken|Aitken]] crater in the north-west -- a crater of the [[Stratigraphy|Late (upper) Imbrium]] period (~ 3.85 to 3.8 bn years), which has itself formed on deposits of the huge [[South%20Pole-Aitken%20Basin|South Pole Aitken Basin]] -- a 2500 kilometre-wide basin of the [[Stratigraphy|pre-Nectarian]] period (~ 4.6 to 3.92 bn years) predominatly in the south-east. '''Bergstrand's''' rim is slighly oval-shaped in a north-south direction -- both cardinal extremes of which show signs of collapsed material in towards its <span style="font-family: Arial">pock-marked floor covered in hundreds of small craters. Is this collapsed inner-rim material a sign of the age of '''Bergstrand''', or is it due to the material make-up on which it formed (note how craters on this inner-rim material has less number of small craters than those showing on the floor)? <span class="membersnap">- [http://www.wikispaces.com/user/view/JohnMoore2 [[Image:JohnMoore2-lg.jpg|16px|JohnMoore2]]] [http://www.wikispaces.com/user/view/JohnMoore2 JohnMoore2]</span></span><br /> <br /> |
==Description: Wikipedia== | ==Description: Wikipedia== | ||
[http://en.wikipedia.org/wiki/Bergstrand_(crater) Bergstrand]<br /> <br /> | [http://en.wikipedia.org/wiki/Bergstrand_(crater) Bergstrand]<br /> <br /> | ||
Revision as of 14:41, 15 April 2018
Contents
Bergstrand
| Lat: 18.8°S, Long: 176.3°E, Diam: 43 km, Depth: km, Rükl: (farside) |
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Table of Contents
[#Bergstrand Bergstrand]
[#Bergstrand-Images Images]
[#Bergstrand-Maps Maps]
[#Bergstrand-Description Description]
[#Bergstrand-Description: Wikipedia Description: Wikipedia]
[#Bergstrand-Additional Information Additional Information]
[#Bergstrand-Nomenclature Nomenclature]
[#Bergstrand-LPOD Articles LPOD Articles]
[#Bergstrand-Bibliography Bibliography]
Images
LPOD Photo Gallery Lunar Orbiter Images Apollo Images
Frame 60, made by ZOND 8, shows Bergstrand rightward of the frame's central cross. Research: Danny Caes
Maps
Description
Bergstrand has impacted close to Aitken crater in the north-west -- a crater of the Late (upper) Imbrium period (~ 3.85 to 3.8 bn years), which has itself formed on deposits of the huge South Pole Aitken Basin -- a 2500 kilometre-wide basin of the pre-Nectarian period (~ 4.6 to 3.92 bn years) predominatly in the south-east. Bergstrand's rim is slighly oval-shaped in a north-south direction -- both cardinal extremes of which show signs of collapsed material in towards its pock-marked floor covered in hundreds of small craters. Is this collapsed inner-rim material a sign of the age of Bergstrand, or is it due to the material make-up on which it formed (note how craters on this inner-rim material has less number of small craters than those showing on the floor)? - JohnMoore2 JohnMoore2
Description: Wikipedia
Additional Information
Nomenclature
Carl Östen Emanuel; Swedish astronomer (1873-1948).
LPOD Articles
Bibliography
This page has been edited 1 times. The last modification was made by - tychocrater tychocrater on Jun 13, 2009 3:24 pm - afx3u2
