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  • 25th February 2015 Sol 908

    Posted by jbridges in Mars Science Laboratory Blog on February 25, 2015 Here is the latest, spectacular MAHLI selfie, made from a mosaic of the microscope imager pictures in January shortly befroe we drilled Mojave2.

  • Thursday 20th September Sol 44

    Posted by jbridges in Mars Science Laboratory Blog on September 20, 2012 The image shows the shadows of Curiosity’s robotic arm and mast approaching our calibration rock.

  • 13th November 2013 Sol 453

    Posted by jbridges in Mars Science Laboratory Blog on November 13, 2013 We have restarted science operations again after the software upload taking longer than expected.

  • 15th May 2014 Sol 630

    Posted by jbridges in Mars Science Laboratory Blog on May 15, 2014 As you can see from this NavCam image we are now driving away from Mt Remarkable.

  • 15th February 2016 Sol 1254

    Posted by jbridges in Mars Science Laboratory Blog on February 15, 2016 We have now started driving away from the main Namib dunes, and onto the Naukluft Plateau.

  • 9th May 2016 Sol 1336

    Posted by jbridges in Mars Science Laboratory Blog on May 9, 2016 We have followed up the Lubango drillhole quickly with another one at a nearby Stimson aeolian sandstone outcrop (Okoruso).  The idea is to compare unaltered sandstone (Okoruso) to altered Lubango.

  • New five-year plan set to boost Leicester’s creative economy

    A five-year strategy that aims to create thousands of new jobs in Leicester’s creative economy and engage hundreds more adults in the city’s arts and cultural offer has been backed by the University of Leicester.

  • Wednesday 14th Nov 2012 Sol 98

    Posted by jbridges in Mars Science Laboratory Blog on November 14, 2012 With its APXS (Alpha Particle X-ray Spectrometer) instrument on the robotic arm of Curiosity is measuring the composition of rocks and soil at Rocknest.

  • 25th March 2015 Sol 936

    Posted by jbridges in Mars Science Laboratory Blog on March 25, 2015 This MAHLI image (field of view about 20 cm) shows how water has travelled through the Garden City mudstone rock.  It has left trails in veins – probably of gypsum or a similar mineral.

  • 11th November 2014 Sol 806

    Posted by jbridges in Mars Science Laboratory Blog on November 11, 2014 Mars Science Laboratory has changed our view of Mars: following the 2 Viking landers of 1976 and the Pathfinder Lander in 1997 we had an idea that Mars was predominantly made of basaltic igneous rocks.

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