Phi Phraya: Difference between revisions
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{{BorealisUniverse}}{{Infobox:_Moon|title1 = '''{{PAGENAME}}'''|code = 47 Ursae Majoris d I|parent_planet = [[ |
{{BorealisUniverse}}{{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]] |
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* [[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 [[ |
* [[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. |
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=='''History'''== |
=='''History'''== |
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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. |
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. |
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[[Category: Moons]] |
[[Category: Moons]] |
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[[Category:Ocean Moons]] |
[[Category:Ocean Moons]] |
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[[Category: |
[[Category:Milky Way]] |
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[[Category:Human Colonies]] |
[[Category:Human Colonies]] |
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[[Category:Unfinished]] |
[[Category:Unfinished]] |
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[[Category:Chalawan System]] |
[[Category:Chalawan System]] |
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[[Category:*Scope: Borealis Universe]][[Category: No Longer In Active Development]] |
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[[Category:*Ocean World]] |
[[Category:*Ocean World]] |
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Revision as of 17:37, September 26, 2024
Template:Infobox: MoonPhi Phraya is an O-Class moon orbiting the planet Krathong in the 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 FUSS, only losing to Andeshölm in 10th 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.