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13626 results for: ‘仿风车IM即时通讯/群聊/邀请码注册/免短信/去后门/市面好版本✅项目合作 二开均可 TG:saolei44✅.cnyVJVWLDnhKJPj’

  • 14th October 2013 Sol 424

    Posted by jbridges in Mars Science Laboratory Blog on October 14, 2013 The noon to pre-dawn temperature variation at Gale Crater can be up to 90 degrees centigrade.   This MastCam image shows the effects of this extreme temperature variation.

  • 25th November 2014 Sol 819

    Posted by jbridges in Mars Science Laboratory Blog on November 25, 2014 We are continuing our detailed traverse around the Pahrump area. I will be Geo ScienceTheme Lead tomorrow and we aim to do more contact science.  The MastCam image is of Book Cliffs.

  • 11th March 2016 Sol 1278

    Posted by jbridges in Mars Science Laboratory Blog on March 11, 2016 In the last few days we have been finding these rounded cm-sized nodules on eroded faces of the underlying Stimson sandstone.

  • 4th September 2015 Sol 1094

    Posted by jbridges in Mars Science Laboratory Blog on September 4, 2015 This NavCam mosaic shows the Williams outcrop in front of us, which is part of the Stimson unit.

  • 16th August 2016 Sol 1432

    Posted by jbridges in Mars Science Laboratory Blog on August 16, 2016 The Veins of Mars The Veins of Mars Dr Samuel Illingworth of Manchester Metropolitan University has written a poem about the sulphate veins on Mars that we have just published about in Meteoritics and...

  • 13th June 2016 Sol 1370

    Posted by jbridges in Mars Science Laboratory Blog on June 13, 2016 Here is the Oudam drillhole and the nearby dump piles for material that has been analysed by CheMin.

  • MA Museum Studies Placement in Special Collections, Weeks 7-8

    Posted by Sarah Wood in Library Special Collections on September 5, 2018 Guest post from Yineng Zhu, Andrew Permain and Joe Searle, MA Museum Studies students working with the Archives & Special Collections team.

  • 19th January 2014 Sol 517

    Posted by jbridges in Mars Science Laboratory Blog on January 19, 2014 On Earth rocks that are as ancient as those we are studying on Mars have been destroyed by the tectonic recycling process or heavily metamorphosed.

  • 18th July 2013 Sol 337

    Posted by jbridges in Mars Science Laboratory Blog on July 18, 2013 We are getting into the new routine of driving e.g. 30 or 40 m per day together with science observations, in particular from the mast instruments.

  • 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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