MARS RECONNAISSANCE ORBITER HIRISE IMAGES
January 28, 2015

o Gullies Old and New Near the Argyre Region    
  http://hirise.lpl.arizona.edu/ESP_038931_1355

  As gullies form on slopes, sediment can become deposited 
  to form lobe-shaped fans.

o Higher Terrain between Sinai and Solis Plana  
  http://hirise.lpl.arizona.edu/ESP_038932_1635

  The area is riddled with faults and ridges that look like 
  uncovered magma dikes.

o Filled Crater and Scallops    
  http://hirise.lpl.arizona.edu/ESP_038967_1230

  These scallop formations might be possibly due to ground ice 
  sublimation.

o Pits in Hale Crater Ejecta    
  http://hirise.lpl.arizona.edu/ESP_039524_1445

  The pits visible here aren't impact craters. The material 
  they're embedded into is ejecta from a large crater called Hale.


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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