MARS RECONNAISSANCE ORBITER HIRISE IMAGES
September 16, 2015

o Western Medusa Fossae Formation: Dust and Dunes
  http://hirise.lpl.arizona.edu/ESP_041864_1745

  The bluish sand in this image is thought to originate 
  from the bedrock that lies beneath the dust.

o Possible Sulfates in the Northeast Syrtis Major Region        
  http://hirise.lpl.arizona.edu/ESP_041893_1975

  This particular region has been studied intensely due to the 
  presence of volcanics from Syrtis Major and impact ejecta 
  from the Isidis Basin.

o Which Came First?     
  http://hirise.lpl.arizona.edu/ESP_042040_1275

  Let's untangle the history of certain formations in this image 
  of sand dunes trapped inside an unnamed crater in southern 
  Terra Cimmeria.

o Bizarre TARs  
  http://hirise.lpl.arizona.edu/ESP_042124_1665

  Unlike other transverse aeolian ridges on Mars, these TARs have 
  blunt edges and serrated ridges. Why?

All of the HiRISE images are archived here:

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

Information about the Mars Reconnaissance Orbiter is 
online at http://www.nasa.gov/mro. The mission is 
managed by NASA's Jet Propulsion Laboratory, a division 
of the California Institute of Technology, for the NASA 
Science Mission Directorate, Washington, D.C. Lockheed 
Martin Space Systems, of Denver, is the prime contractor 
and built the spacecraft. HiRISE is operated by the 
University of Arizona. Ball Aerospace and Technologies 
Corp., of Boulder, Colo., built the HiRISE instrument.

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