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                                  What material could be shooting into the Martian air? Could it be dark sand? What impells it to such heights? Or... is there anything happening here at all?  Other possible geysers are visible in the image at right.    Click the image to go to the next page of Geysers on Mars Commentary by Nick Hoffman, Geophysicist Extraordinaire, regarding the phenomenon below... It is well known that C02 changes phase from solid to   vapour at relatively low temperatures at the low martian   ambient pressure. The corollory of this is that if you   can heat it above that temperature, it will develop a   substantial pressure (if you confine it). For instance,   at -57 C the solid has an equilibrium vapour pressure of   5 bars which is enough to physically lift a lid of 100m   of solid CO2 ice or ~ 75 metres of regolith.    The polar icepack is only a few metres thick, so   pressures of ~ 0.1 bars will suffice to blow through the   "roof" and erupt as a geyser. This equates to a   temperature of 170K (~24 K warmer than the main snowpack   which condenses in equilibrium with the ~6.5 millibar   atmosphere). Carbon dioxide has a very steep ramp of   equilibrium vapour pressure with temperature whicj makes   effects like this very powerful. It also has low specific   heat capacity which makes it easy to warm (unlike water)   and low latent heat capacity which makes it easy to   melt/vaporise (unlike water).    This is NOT a sign of internal volcanic heat, but simply   a consequence of spring sunshine shining down through   relatively transparent CO2 snow and block ice and warming   the surface of dark dune material underneath, like Earth   sunshine melting snow on a black bitumen sidewalk from   the bottom up.    What we observe is not so much the active geyser, as the   trail of fine dust that has been jetted out of the   orifice and spread downwind. If the wind direction   changes, so does the streak direction so on different   days you get different trails, or sometimes the winds   swirl noticeably acroll the length of a frame and show   varying orientations - a dead giveaway for wind streaks   rather than shadows.    There are a couple of scientific papers published already   that discuss this phenomenon.      
  Another Viewpoint: "Annual Punctuated C02 Slab-Ice and Jets On Mars" by H.H. Kieffer of the USGS -- Adobe Acrobat reader required  |