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Ribbed terrain Small cracks become larger and larger because the more surface area the more sublimation. Source: http://hirise.lpl.arizona.edu/ESP_028339_2245 Lat: 44° N Long: 26.2°E Image credit: NASA/JPL/University of Arizona
 
 
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== Summary ==
== Summary ==
Ribbed terrain  
 
Ribbed terrain, as seen by HiRISE under HiWish program
 
Small cracks become larger and larger because the more surface area the more sublimation.
Small cracks become larger and larger because the more surface area the more sublimation.


Source: http://hirise.lpl.arizona.edu/ESP_028339_2245
Source: http://hirise.lpl.arizona.edu/ESP_028339_2245
Lat: 44° N Long: 26.2°E  
Lat: 44° N Long: 26.2°E  
Image credit: NASA/JPL/University of Arizona
Image credit: NASA/JPL/University of Arizona


== Licensing ==
== Licensing ==
{{PD}}
{{PD}}

Latest revision as of 19:35, 27 February 2020

Summary

Ribbed terrain, as seen by HiRISE under HiWish program

Small cracks become larger and larger because the more surface area the more sublimation.

Source: http://hirise.lpl.arizona.edu/ESP_028339_2245

Lat: 44° N Long: 26.2°E

Image credit: NASA/JPL/University of Arizona

Licensing

Public domain images are available for anybody to use without any licenses, royalties, or special permissions.

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current19:05, 27 February 2020Thumbnail for version as of 19:05, 27 February 2020800 × 359 (50 KB)Suitupandshowup (talk | contribs)Ribbed terrain Small cracks become larger and larger because the more surface area the more sublimation. Source: http://hirise.lpl.arizona.edu/ESP_028339_2245 Lat: 44° N Long: 26.2°E Image credit: NASA/JPL/University of Arizona

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