Ivory: Difference between revisions
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[[File:IvoryLabelled2026.jpeg|200px|thumb|left|A labelled map of the surface of ivory.]] | [[File:IvoryLabelled2026.jpeg|200px|thumb|left|A labelled map of the surface of ivory.]] | ||
[[File:Ivory2026Skin.jpeg|200px|thumb|left|The surface of Ivory, unlabelled.]] | [[File:Ivory2026Skin.jpeg|200px|thumb|left|The surface of Ivory, unlabelled.]] | ||
The | The North Polar Regions of Ivory are defined by dark, elevated terrain broken by extensive crater fields, wind-scoured ridges, and scattered patches of frost along the highest latitudes. The far northwestern uplands, collectively referred to as the '''Zephyron Marches''', form a harsh and exposed region shaped by persistent high-altitude winds and minimal atmospheric buffering. To the east of this, the large enclosed depression known as the '''Basin of Clear Silence''' occupies one of the most visually distinct northern basins, its subdued tone and relative smoothness contrasting with the surrounding fractured highlands. Rising prominently nearby, the elevated massif called the '''Crown of Lucent Stone''' marks one of the clearest highland structures in the northern hemisphere, its lighter tone and broad uplift suggesting a region of exposed, weathered bedrock. | ||
Further east, the terrain transitions into the broken uplands of the '''High Aetheric Rise''', a region of steep slopes, cratered ridges, and uneven elevation. Along the northeastern boundary, the fractured edge known as the '''Haifan Verge''' forms a transition into more heavily disrupted terrain. Across these northern zones, the surface is characterized by long-term erosion, impact scarring, and wind-driven redistribution of fine material, producing a landscape that appears both ancient and sharply defined. The northern hemisphere is therefore dominated by exposed stone, elevated ridges, and cratered basins, with the Zephyron Marches, Basin of Clear Silence, Crown of Lucent Stone, High Aetheric Rise, and Haifan Verge providing a more localized geography within Ivory’s broader austere polar environment. | |||
==Equatorial Regions== | ==Equatorial Regions== | ||
Revision as of 02:36, 15 April 2026
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| Orbital characteristics | ||
| Mass (Kg) | 7.99E+18 | |
| Radius (Km) | 77.1 | |
| Solar Day (h) | 9.29 | |
| Orbital Period (days) | .71 | |
| Semi-Major Axis (Km) | 1.78E+04 | |
| Periapsis (AU) | 15,793(km) | |
| Apoapsis (AU) | 19,881(km) | |
| Albedo | .09 | |
| Surface Temperature (K) | 182 | |
| Surface Gravity (m/s^2) | .08 | |
| Axial Tile (degrees) | 3.05 | |
| Inclination (degrees) | 2.04 | |
| Orbital Speed (Km/s) | 23 | |
| Satellites | None | |
North Polar Regions
The North Polar Regions of Ivory are defined by dark, elevated terrain broken by extensive crater fields, wind-scoured ridges, and scattered patches of frost along the highest latitudes. The far northwestern uplands, collectively referred to as the Zephyron Marches, form a harsh and exposed region shaped by persistent high-altitude winds and minimal atmospheric buffering. To the east of this, the large enclosed depression known as the Basin of Clear Silence occupies one of the most visually distinct northern basins, its subdued tone and relative smoothness contrasting with the surrounding fractured highlands. Rising prominently nearby, the elevated massif called the Crown of Lucent Stone marks one of the clearest highland structures in the northern hemisphere, its lighter tone and broad uplift suggesting a region of exposed, weathered bedrock.
Further east, the terrain transitions into the broken uplands of the High Aetheric Rise, a region of steep slopes, cratered ridges, and uneven elevation. Along the northeastern boundary, the fractured edge known as the Haifan Verge forms a transition into more heavily disrupted terrain. Across these northern zones, the surface is characterized by long-term erosion, impact scarring, and wind-driven redistribution of fine material, producing a landscape that appears both ancient and sharply defined. The northern hemisphere is therefore dominated by exposed stone, elevated ridges, and cratered basins, with the Zephyron Marches, Basin of Clear Silence, Crown of Lucent Stone, High Aetheric Rise, and Haifan Verge providing a more localized geography within Ivory’s broader austere polar environment.
Equatorial Regions
The Equatorial Regions of Ivory are dominated by dark cratered plains, immense impact basins, and broad stretches of exposed rocky ground. Several very large circular basins define the equatorial belt, many with smoother, darker floors set inside sharply preserved rims. Between them lie dense fields of smaller craters, overlapping ejecta blankets, and rough highland belts broken by fractures and degraded escarpments.
This is the most varied part of the moon’s surface. Some sectors consist of relatively smooth plains marked by later impacts, while others are more broken and uneven, with clustered craters and irregular ridges cutting across older basin margins. The equatorial terrain is dry, airless, and geologically inert at the surface, with its present form set by repeated bombardment and long preservation under cold conditions. The low reflectivity of Ivory is especially evident here, where darker regolith and shadowed basin floors dominate much of the landscape.
Southern Polar Regions
The Southern Polar Regions of Ivory are brighter than much of the equator, with frost and ice spread more broadly across the highest latitudes and along cold-trapping depressions. A pale southern cap extends over the polar margin, collecting in crater floors, low basins, and sheltered hollows. Even with this brighter cover, the underlying terrain remains clearly visible, including large worn craters, rough basin edges, and broken upland surfaces.
The south preserves the same ancient impact-scarred character seen elsewhere on the moon, but with a stronger contrast between dark exposed ground and lighter frost deposits. Large circular depressions remain common, and several broad basins continue across the lower southern latitudes before merging into the frost-brightened polar zone. The result is a cold and stable southern hemisphere shaped by cratering, regolith accumulation, and persistent polar frost rather than by active surface change.
