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Phi Phraya: Difference between revisions

From Amaranth Legacy, available at amaranth-legacy.community
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Delete this, i am reworking on every article of mine.
{{Infobox:_Moon|title1 = '''{{PAGENAME}}'''|code = 47 Ursae Majoris d I|parent_planet = [[Krathong]]|image1 = Scr01001.jpg|mass = 0.920507 M<sub>[[Earth]]</sub>|diameter = 13,734.42 km|rotation_period = Tidally locked|average_tempreature = -194 °C|atmospheric_pressure = 49.8 atm|age = 5.3 billion years|under_control_of = [[Confederacy of Borealis]]
* [[Federations of United Star Systems]]|additonal_notes = Has an atmosphere made of 100% oxygen, and liquid oxygen seas}}'''{{PAGENAME}}''' is an [[Planet Class|O-Class]] moon orbiting the planet [[Krathong]] in the [[Chalawan|Chalawan System]], 46 light-years from [[Earth]]. It is famous across the [[Milky Way]] for its liquid oxygen oceans, which are sometimes misrepresented as liquid water by this moon's visitors. Phi Phraya is as unique as its sister-moon [[Keriyn]], ranked as one of the top 20 most popular touristic attractions within the [[Federations of United Star Systems|FUSS]], only losing to [[Andeshölm]] in 10<sup>th</sup> place.
=='''History'''==
Although not much is known about the moon, Phi Phraya is theorized to have been an ice world that formed when several icy asteroids present in Krathong's ring system clumped together, following that, the new “asteroid merger” gained a gravitational field, attracting even more ring debris. Eventually, the gravity became so strong that tens of asteroid moons went into Phi Phraya and crashed into it, heating up the surface and creating an atmosphere. The ice surface would later melt and become the liquid oxygen superocean that we see today.
[[Category:Exomoon]]
[[Category:Exomoon]]
[[Category:Ocean Moons]]
[[Category:Ocean Moons]]
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[[Category:Unfinished]]
[[Category:Unfinished]]
[[Category:Chalawan System]]
[[Category:Chalawan System]]
[[Category:Candidates for Deletion]]

Revision as of 11:37, August 2, 2020

Delete this, i am reworking on every article of mine.