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 = [[Krathon[[Category:*Scope: Borealis Universe - Milky Way]]]|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 [[Krathon[[Category:*Scope: Borealis Universe - Milky Way]]] in the [[Chalawan|Chalawan System]], 46 light-years from [[Earth]]. It is famous across the [[Milky Wa[[Category:*Scope: Borealis Universe - 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:Milky Way]] |
[[Category:Milky Wa[[Category:*Scope: Borealis Universe - 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 |
[[Category:*Scope: Borealis Univers[[Category:*Scope: Borealis Universe - Milky Way]]][[Category: No Longer In Active Developmen[[Category:*Scope: Borealis Universe - Milky Way]]] |
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[[Category:*Ocean World]] |
[[Category:*Ocean World]] |
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Revision as of 20:58, September 21, 2024
{{Infobox:_Moon|title1 = Phi Phraya|code = 47 Ursae Majoris d I|parent_planet = [[Krathon]|image1 = Scr01001.jpg|mass = 0.920507 MEarth|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}}Phi Phraya is an O-Class moon orbiting the planet [[Krathon] in the Chalawan System, 46 light-years from Earth. It is famous across the [[Milky Wa] 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. [[Category:Milky Wa] [[Category:*Scope: Borealis Univers][[Category: No Longer In Active Developmen]