It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
The crater is 35 kilometres wide and has a maximum depth of approximately 2 kilometres beneath the crater rim. The circular patch of bright material located at the centre of the crater is residual water ice.
It cannot be frozen carbon dioxide since carbon dioxide ice had already disappeared from the north polar cap at the time the image was taken (late summer in the Martian northern hemisphere).
Methane sublimates at much lower temperatures than water does. Pretty certain to be water ice and not much reason to think otherwise. The 2005 article:
im going to go ahead and say its methane ice and not 'water' ice on mars.
This white patch is present all year round, as the temperature and pressure conditions do not favour the sublimation of water ice. It cannot be frozen carbon dioxide since carbon dioxide ice had already disappeared from the north polar cap at the time the image was taken (late summer in the Martian northern hemisphere).
originally posted by: Phage
a reply to: odzeandennz
Methane sublimates at much lower temperatures than water does. Pretty certain to be water ice and not much reason to think otherwise. The 2005 article:
im going to go ahead and say its methane ice and not 'water' ice on mars.
This white patch is present all year round, as the temperature and pressure conditions do not favour the sublimation of water ice. It cannot be frozen carbon dioxide since carbon dioxide ice had already disappeared from the north polar cap at the time the image was taken (late summer in the Martian northern hemisphere).
www.esa.int...
originally posted by: LookingAtMars
It does not say where the water ice came from. Rain? Snow? Ground Water? Any ideas where the water came from?
originally posted by: LookingAtMars
a reply to: wildespace
Thanks for the HiRise image. That seems to be a lot of water ice to be from condensation. Could it have been a frozen lake that has sublimed away over eons and now that is all that is left?
originally posted by: 0bserver1
What's the dark pluim of smoke doing there at the bottom?
Some readers have asked, how do we know the white substance is not frozen CO2 (dry ice) instead of frozen water? Answer: Phoenix's landing site is too warm for dry ice. The average daily temperature is about -70 F while dry ice requires temperatures lower than about -109 F.
Finding water was one of the key goals of the Phoenix mission. Although H2O has trouble flowing as a liquid on the surface of Mars, it may be able to liquify, from time to time, just below the surface, providing a habitat for martian microbes. Exciting stuff! Stay tuned as the digging continues.