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A little interesting about space life.
Triton is one of the coldest bodies in our Solar System. In fact, it is so cold that most of its nitrogen atmosphere is condensed as frost, giving its surface a very bright, mirror-like surface, that reflects about 70% of the sunlight that reaches it.
and here is another
Again, they pour and throw water; only this time not over one another (so you must not worry, we will stay dry) out of earthen pots (atar pots) they have bought earlier (at the full moon of Kason they can buy them literally at every pagoda corner) but over a tree (or its roots) of the genus 'Ficus' that belongs to the family of 'Moraceae' and is classified as 'Ficus religiosa'. This tree is commonly known as 'Banyan tree', 'Bo tree' or 'Bodhi tree' and is a fig tree, more precisely the 'Indian fig' tree. Especially on the full-moon day of Kason this sacred tree is of great significance to Burmese Buddhists as it is closely related to Gautama Buddha. In order to understand why this is so, we have to travel some 2,500 years back in time.
For a long time, planetary scientists thought that in the aftermath of the Moon-forming collision, hydrogen dissociated from water molecules. According to this scenario, both water and other elements that have low boiling temperatures (volatile elements), escaped from the disk and were lost forever to space. This model would form a volatile-element-depleted and bone-dry Moon. At the time, this scenario seemed to be consistent with earlier analyses of lunar samples.
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The vanished, ill-fated, large moon could have been a few hundred kilometers in diameter. The large moon would also have allowed a handful of other smaller moons to form--including the duo of small, shapeless ones that survive today. However, this large inner moon would have been born close to or within the Roche limit. This is why it is likely that it crashed into Mars as a result of tidal forces within several million years--and the collection of other small moons followed their leader. Only Phobos and Deimos kept their distance.
Earlier research had determined the quantity of material accreted onto the ancient Earth following the Moon-forming collision. These previous calculations were based on how the siderophile or "iron-loving" elements such as platinum and iridium show a strong tendency to wander down into our planet's core. Following each giant impact that the primordial Earth experienced, these elements would have leached from Earth's mantle and bonded with iron-rich, heavy material that was destined to travel down, down, down into our planet's heart.
Our Earth basks comfortably in the sunny, warmer, inner regions of our Solar System, and our Moon is the largest one of its kind, in this region, relatively close to our Star. Of the four rocky, terrestrial planets--of which our Earth is a member--Mercury and Venus are moonless, and Mars sports two small, misshapen little rocky moons, Phobos and Deimos, that are likely captured refugees from the main asteroid belt that circles our Sun between the orbits of Mars and Jupiter.