Tens of thousands of lava - like stream dot the surface of Mars , but a fresh work suggest   not all of   them   are in reality lava . Instead , some   are   mud volcanoes .

Mars has the tallest mountain in the Solar System , a vent called Olympus Mons that ’s three times the size of Everest . This is just one of many examples of volcanism on the Red Planet . Yet despite chiliad of lava - lilke flow , some do n’t expose any other signs of   volcanism . The squad discovered they are potential   sedimentary deposits , mayhap constitute   after catastrophic floods .   Water then ooze into the soil and finally remerged as mud volcanoes .

dry land has mud volcanoes so their establishment is   certainly possible . However , Mars is   colder and has   a abject atmospheric pressure than Earth . To essay   their surmise , the team recreated the   clay volcanoes in a   lab .   Using a vacuum sleeping room , they made mud flow   at a fraction of Earth ’s normal pressing and at a temperature well below zero . The results are published inNature Geoscience .

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" We suggest that mud volcanism can explain the shaping of some lava - like flow morphologies on Mars and that similar processes may apply to volcanic eruption of mud on icy bodies in the outer Solar System , like on Ceres , " lead source Dr Petr Brož , from the Institute of Geophysics of the Czech Academy of Sciences , said in astatement .

Under Martian conditions , the pee begin   to roil   and evaporate due to the low pressure . The   surface of the mud then freeze   due to the low temperature , which lead to the geological formation of   form similar topahoehoe , the rippled structure imprint by cooling lava picture typically in Hawaii .

The team consider the same cognitive operation would be even more good ondwarf planet Ceresdue to the lack of atmosphere and cold temperature on the aerofoil . It ’s also possible the process   happens on other moons and nanus planets in the solar system .

The authors conclude : " Our results show that it is critical to consider the upshot of the differing environmental conditions on other world surface when compare analogue landofrms observed on Earth with apparently alike gushing morphologies on other bodies . "