Difference between revisions of "Apolda"
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m (Kongsberg was renamed to Thuringia in 4.90.2 Patch 2. System related links fixed here. Category: Rheinland added) |
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| house = {{House Link | Rheinland}} | | house = {{House Link | Rheinland}} | ||
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The moon once served as a water source for [[Deuterium]] fuel production during the 80-Years War, leaving traces of exploitation on the surface and the remains of mining machinery locked in the ice. Geologically fragile due to its internal structure, Lozten's crust and mantle mainly consists of frozen water and sedimentary rock. Its non-metallic core solidified millions of years ago. | The moon once served as a water source for [[Deuterium]] fuel production during the 80-Years War, leaving traces of exploitation on the surface and the remains of mining machinery locked in the ice. Geologically fragile due to its internal structure, Lozten's crust and mantle mainly consists of frozen water and sedimentary rock. Its non-metallic core solidified millions of years ago. | ||
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| + | [[Category: Rheinland]] | ||
Revision as of 17:40, 18 July 2018
v4.90.2
)This article has not been verified to be up to date for the latest version of the Discovery mod. The last edit was made on 18.07.2018 (DD/MM/YYYY). You may help by updating it, often by using the code generator.
| Lotzen | |
| Owner | unknown |
| Location | 5F, Thuringia Rheinland
|
| Technical information | |
| Population | unknown |
| Docking | N/A |
| Terrain | N/A |
| Diameter | N/A |
| Mass | N/A |
| Temperature | N/A |
| Escape velocity | N/A |
Lozten is a small ice moon with a thin atmosphere orbiting Planet Rossel. Its surface is covered by a thin layer of iron oxide dust with huge cracks in the crust that let ice shine through. Lozten is the largest and brightest object in Rossel's orbit and its trailing ice fragments form a small ring whose shards sparkle in Rossel's night sky.
The moon once served as a water source for Deuterium fuel production during the 80-Years War, leaving traces of exploitation on the surface and the remains of mining machinery locked in the ice. Geologically fragile due to its internal structure, Lozten's crust and mantle mainly consists of frozen water and sedimentary rock. Its non-metallic core solidified millions of years ago.
