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Europa, an icy little moon that circles the giant planet Jupiter, probably sustains a global ocean of liquid water beneath a tortured, shattered icy crust. For a long time, weird and jumbled regions of ice disruption, called "chaos terrains", were seen only on Europa, and their origins remained cloaked in mystery. But astronomers now think that the "chaos terrains" formed as the result of a subsurface liquid saltwater lake, equal to all of the Great Lakes on Earth combined. Hidden about 1.9 miles beneath Europa's cracked eggshell-like frozen crust, the ice-embedded lake may be one of the latest potentially habitable environments discovered so far in our Solar System.
and here is another
In July 2017, a team of astronomers announced that they had used satellite data to find--for the first time--signs of widespread water hidden beneath ancient volcanic material on Earth's Moon. The scientists' discovery suggests that the interior of our Moon holds large quantities of indigenous water. This plentiful, but well-hidden water, reveals its secret presence in numerous volcanic deposits, that had been explosively distributed across our Moon's surface when ancient lunar volcanoes erupted. These primordial deposits contain unusually large amounts of imprisoned water compared with nearby terrains. The detection of water within these lunar deposits, is believed to be made up of glass beads that formed as a result of the explosive fiery eruption of magma, hurled out from deep within our Moon. This finding supports the theory that the lunar mantle is surprisingly soggy.
In dramatic contrast, the inner region of our Solar System, where our Earth dwells--along with Mercury, Venus, and Mars--is relatively barren of moons. Mercury and Venus have no moons, and Mars is orbited by a small duo of deformed moons, Phobos and Deimos, that are probably asteroids that escaped from the Main Asteroid Belt between Mars and Jupiter billions of years ago--only to be captured by the Red Planet's powerful gravitational embrace. Our Earth is the only inner planet that possesses an impressively large, spherical Moon.
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The two scientists found clear evidence of water in nearly all of the large pyroclastic deposits that had been mapped earlier across our Moon's surface, including deposits near the Apollo 15 and 17 landing sites where the water-bearing glass bead samples were collected.
Astronomers have for years contemplated two competing hypotheses explaining the origin of the Martian moons. The first proposes that Phobos and Deimos are, indeed, escapees from the Main Asteroid Belt. Alas, this viewpoint begs the question of why they should have been so cruelly captured by their adopted parent-planet in the first place. An alternative theory points to the possibility that the moons were born from the debris left by a violent collision between Mars and a primordial protoplanet--a baby planet still under construction. However, this theory also suffers from uncertainty because it does not explain precisely how this particular tragic mechanism gave rise to Phobos and Deimos.
Dr. Jacobson believes that this new study showing a later lunar birthday means that our planet's impact history was more turbulent than earlier thought. The alteration in Earth's bombardment rate, he suggests, also means an alteration in the quantity of energy that went into our planet's oceans and atmosphere. It also has implications for the history of our planet's surface temperature--which is important because liquid water could not exist until the surface had cooled off sufficiently.