Io7 Brown Nebula hubble finds three giant exoplanets and several brown Io7 Brown Nebula

Io7 Brown Nebula hubble finds three giant exoplanets and several brown Io7 Brown Nebula

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A little interesting about space life.

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.

and here is another

Titan possesses a smooth, young surface, scarred by comparatively few impact craters. The climate of this frigid moon--including its fierce winds and showers of hydrocarbon rain--carves out surface features that bear an eerie resemblance to those on Earth, such as lakes, sand dunes, rivers, seas, and deltas. Indeed, planetary scientists propose that Titan bears a haunting resemblance to Earth, and is believed to be similar to the way our planet was before life had a chance to evolve out of non-living substances (prebiotic).

and finally

In the tragicomedy that characterizes human relationships, it has been said that the closer we get to someone, the weirder that person gets. Earth's Moon is our planet's closest neighbor in Space--mysterious, bewitching, bothersome, and bewildering, it has successfully hidden many of its secrets from the prying eyes of curious observers. In July 2017, using satellite data, a team of astronomers announced that they have, for the first time, detected widespread water hidden within ancient explosive volcanic material on Earth's nearest and dearest companion world. This discovery indicates that the interior of Earth's Moon contains large quantities of indigenous water that has finally been revealed in numerous volcanic deposits distributed across the lunar surface--and these ancient deposits contain unusually high amounts of imprisoned water compared with surrounding terrains. The discovery of water in these ancient lunar deposits, which are believed to be composed of glass beads created in the explosive fiery eruption of magma shooting out from the deep interior of the Moon, strengthens the theory that the lunar mantle is surprisingly water-rich.

Other facts:

Now we know that there are over 100 moons circling the eight major planets of our Sun's family. The majority of our Solar System's moons are icy, small, and frozen worlds that contain only small quantities of rocky material. The distant multitude of sparkling, icy moons in our Solar System are primarily in orbit around the four giant gaseous planets, Here, in this strange, frigid and dimly-lit realm, far from our Star's melting fires and brilliant light, these tiny frozen moons do their fabulous, lovely dance around their quartet of parent-planets. The giant, gaseous worlds that inhabit our Solar System's outer suburbs--Jupiter, Saturn, Uranus, and Neptune--are blanketed by heavy atmospheres of gas, and are accompanied, in their travels around our Star, by their orbiting retinue of many moons and sparkling, icy moonlets.

The new study was published in the April 3, 2014 issue of the journal Nature, and it may provide a solution to a long-standing mystery of lunar origins pertaining to why Earth and its lovely companion appear to sport virtually identical compositions.

According to the new theory, moon-formation starts at the very edge of a planetary ring, where a fragile baby moon can begin to emerge without the danger of being ripped apart by the fierce gravity of its parent planet. These dancing little moonlets, formed from ring-material, then travel outward. As the ring-system continually produces moonlet after moonlet after moonlet, the small icy worlds coalesce to form increasingly larger moons. The larger moons, in turn, may also merge together, as they dance outward from their parent planet.