The Jovian moon Io is noted for being the only other place that Earth   in the Solar System to have active volcanism . But another feature has been intriguing scientists for a long time : How do its   lone mountains build ?

The peck are not assort with vent , but they are colligate with crust and mantle   fundamental interaction . As the magma flows out from the core , it set the surface under pressure , build stress into the crust . This is liberate as a dowry of the crust shoot up , forming the inscrutable mountains .

This solvent was obtained by two American researcher , Michael   Bland and William McKinnon from Washington University , with the help of a computer simulation . The numeric experiment demo   that as the interior of Io is squeeze , the song localise in a undivided fracture that   propagates upward , break the aerofoil and forming the mountains .

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" The compressive effect late in the encrustation are incredibly high , " McKinnon said in astatement .   " When these faults breach the Earth’s surface , those forces are released , and the entire stress surround around the fault change , providing a pathway for magma to erupt . "

This result , bring out inNature Geoscience , clearly excuse why the mountains incline to be relate with patera   –   shallow depressions   scattered across the surface of Io .

The numerical simulation register that as the cracking propagate upwards , it creates a mountain as well as magma lakes call off patera .   Bland & Mckinnon

Volcanos and mountains are anti - correlate on Io . Volcanos carry heat and press away from the crust , but when volcanism slows down , thermic emphasis increment , which lead to more peck contain   shape .

The mountains have an average height of 6 km ( 3.7   miles ) , with the tall one reaching 17.5 kilometers ( 10.9 mil )   –   huge in comparison to the modest size of the orbiter .

" It ’s a fresh batch - forming mechanism that we do n’t see elsewhere in the Solar System , " added McKinnon .

On Earth , mountains imprint   when continental plates interact , raising one on top of the other . But McKinnon does n’t except that this other mechanism was in play when our planet was new . He really suggest that if the primordial Earth was underwrite by a shallow sea , this is how the first dry land might have emerged .

mayhap by studying Io , we can learn something about how our planet looked billions of years ago .