It is thought that at one point during its history Mars did house liquid oceans, and did resemble an Earth-like appearance on the surface, with large bodies of water, land continents and rivers. The majority of water that has been discovered to be now existing on Mars is in the form of ice and water vapor (sublimation dominates most state transitions). Mars does have a very thin atmosphere, which houses the vapor, while the ice is massed mostly at the poles and has actually been discovered scattered throughout the surface and has been confirmed by NASA's Phoenix Mars Lander to be water ice, which was melted by the lander. As for liquid water, in the last several years NASA has found evidence that there may be some below the surface of Mars. The evidence astronomers are looking at is the periodic deposits of new sediment to the surface terrain (see Image 1 Mars, below), that appear to have been brought to the surface by liquid water, indicating that liquid water may indeed be able to exist briefly and periodically on the surface, and these brief appearances may be sourced by underground liquid reservoirs. Beyond these deposits astronomers have observed other geological disturbances to the surface of Mars that could likely have been caused by liquid water, such as gullies formed near faults (see Image 2 Mars, below), which is consistent with an occurrence on Earth where springs tend to pop up near faults; these disturbances are relatively recent as well, within the time since Mars has generally become a "dry planet."

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