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Like Earth's own large Moon, Triton is locked in synchronous rotation with its planet--one side always faces Neptune. However, because of Neptune's odd orbital inclination, both of the moon's polar regions take turns facing the Sun. Spacecraft images of Triton reveal mounds and round pits formed from icy lava flows (cryovolanism), as well as smooth volcanic plains. The surface of the moon is only sparsely cratered, indicating that its surface is new--that is, it is constantly being resurfaced, probably by the "lava" flow from icy volcanoes. Triton is very bright--its fresh, sparkling, new ice-coating is believed to cover a heart of metal and rock. Triton's high density suggests that it contains more rock in its interior than the icy moons of Saturn and Uranus.



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Dr. Alice Le Gall commented in the same JPL Press Release that "Before Cassini, we expected to find that Ligeia Mare would be mostly made up of ethane, which is produced in abundance in the atmosphere when sunlight breaks methane molecules apart. Instead, this sea is predominantly made of pure methane." Dr. Le Gall, a Cassini radar team associate, is of the French research laboratory LATMOS, in Paris, and lead author of the new study.



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There are ongoing studies assessing the past habitability potential of the Red Planet, as well as the possibility of life.

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The birthday of Earth's Moon came about 95 million years after the formation of the Solar System itself, according to the new calculations. This means that our planet's nearest neighbor in Space is approximately 60 million years younger than earlier estimates indicated.



This revised birth date for the Moon comes from a new study that takes a detour from the long-standing debate about its true age, and is basically in agreement with those planetary scientists who suggest a late-forming Moon. The new method that the scientists used to arrive at their conclusion eliminates numerous problems with traditional methods for calculating the Moon's age.



"Our model explains the diversity of these ice-rich moons and the evidence for their very active geology and dynamics. It also explains a puzzling fact about Titan, in that a giant impact would give it a high orbital eccentricity," Asphaug continued to explain to the press on October 18, 2012.