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  • 5th December 2013 Sol 474

    Posted by jbridges in Mars Science Laboratory Blog on December 5, 2013 We have paused to do some contact science, using the robotic arm to use APXS on the local rocks.

  • March 3rd 2013 Sol 206

    Posted by jbridges in Mars Science Laboratory Blog on March 5, 2013 No new data or images over the last few sols.

  • 28th May 2013 Sol 288

    Posted by jbridges in Mars Science Laboratory Blog on May 28, 2013 We are holding a ChemCam meeting at the Cite de Espace, Toulouse.  The Cite de Espace hosts an exhibition about Mars Science Laboratory and ChemCam.

  • 26th June 2013 Sol 316

    Posted by jbridges in Mars Science Laboratory Blog on June 26, 2013 Curiosity Inspecting Shaler. This HazCam image shows our location at Shaler and the tracks left as we have manoeuvred along the outcrop to look at the planar and cross bedding structures.

  • 21st December 2016 Sol 1556

    Posted by jbridges in Mars Science Laboratory Blog on December 21, 2016 I am Geo-Min Science theme lead for todays plan.  As usual after 4 years of operations we are doing 3 sols of planning at one go.

  • 19th January 2017 Sol 1584

    Posted by jbridges in Mars Science Laboratory Blog on January 19, 2017 We have found another (the 4th) meteorite.  The fist sized sample called Ames_Knob – which was analysed by ChemCam – turns out to be composed of Fe and Ni metal.

  • 17th April 2016 Sol 1315

    Posted by jbridges in Mars Science Laboratory Blog on April 17, 2016 Here is a NavCam mosaic of the Naukluft Plateau.  We are looking around us for the next drill target. A particular feature is searching for, and trying to understand, silica enrichments.

  • 6th February 2017 Sol 1602

    Posted by jbridges in Mars Science Laboratory Blog on February 6, 2017 We have started the second part of the Bagnold Dunes campaign. This NavCam image shows Bagnold dunes in front of Ireson Hill. This first in the current dunes campaign is Called Mapleton.

  • February 2nd 2013 Sol 176

    Posted by jbridges in Mars Science Laboratory Blog on February 2, 2013 The rover planners are testing the drill by touching 4 points around the chosen drill site and testing the drill action, but not with the full force that the final drill action will use.

  • 1st November 2013 Sol 439

    Posted by jbridges in Mars Science Laboratory Blog on November 1, 2013 We have driven right up to the Cooperstown outcrop.  The rdige (a few tens of cm high) is composed of a resistant layer of sedimentary rock.

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