Recent results from Global Surveyor corroborate the hypothesis that episodes of outburst flooding produced ponded water and climate change on Mars. This hypothesis colligates diverse facts concerning the Martian landscape and its history into a unified genetic system.


    Access

    Access via TIB

    Check availability in my library


    Export, share and cite



    Title :

    Mars' Oceanus Borealis, Ancient Glaciers, and the MEGAOUTFLO Hypothesis


    Contributors:
    Baker, V. R. (author) / Strom, R. G. (author) / Dohm, J. M. (author) / Gulick, V. C. (author) / Kargel, J. S. (author) / Komatsu, G. (author) / Ori, G. G. (author) / Rice, J. W., Jr. (author)


    Publication date :

    2000-03-01


    Type of media :

    Conference paper


    Type of material :

    No indication


    Language :

    English




    Oceanus NF4 concept overview

    Elliott, John | NTRS | 2017


    The Borealis Basin of Mars

    Wilhelms, D. E. / Squyres, S. W. | NTRS | 1984



    Evidence for Pre-Nectarian Impact Basin in Northwestern Oceanus Procellarum

    McEwen, A. / Davis, P. / Howington-Kraus, A. et al. | British Library Conference Proceedings | 1994


    Mare-Highland Mixing Relationships Along the Southwestern Shores of Oceanus Procellarum

    Mustard, J. F. / Head, J. W. / Antenenko, I. et al. | British Library Conference Proceedings | 1994