Lukedu (moon)
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| Orbital characteristics | ||
| Mass (Kg) | 1.07E+23 | |
| Radius (Km) | 1,567 | |
| Solar Day (h) | 27.9 | |
| Orbital Period (days) | 4.45 | |
| Semi-Major Axis (Km) | 716,855(km) | |
| Periapsis (AU) | .004 | |
| Apoapsis (AU) | .005 | |
| Albedo | .44 | |
| Surface Temperature (K) | 166 | |
| Surface Gravity (m/s^2) | 2.91 | |
| Axial Tile (degrees) | .9 | |
| Inclination (degrees) | 0 | |
| Orbital Speed (Km/s) | 29 | |
| Satellites | None | |
Lukedu is the second of the three known moons of Chrysos.
North Polar Regions
The North Polar Regions of Lukedu are dominated by a broad cap of bright polar ice laid across rugged, dark underlying terrain. The northern ice sheet extends continuously across the highest latitudes, but its margins are deeply broken by scarps, fractures, embayed recesses, and steep-walled troughs. Along the edge of the cap, the frozen cover gives way to dark plains, cratered uplands, and volcanic terrain extending into the middle latitudes. In the northwestern quarter, the rough and heavily reworked terrain known as the Marches of Delkar marks one of the clearest transitions between bright ice and older dark crust. Farther east, the broad circular volcanic rise called the Conflux Crown stands out as one of the most prominent northern constructions on the moon, while the broken northern approaches to the central volcanic province are threaded by the Corridor of Symphonara, a dark transitional belt leading from the ice margin toward the equatorial plains.
Beneath the polar cover, the northern hemisphere preserves an older and heavily reworked crust. Large impact craters, degraded basin rims, and rough uplands remain visible along the ice margin, while darker volcanic plains occupy much of the lower polar belt. The boundary between ice and exposed ground is sharp in some sectors and diffuse in others, with frost spreading into colder depressions and along shaded slopes. This pattern is especially evident west of the Crown around the basin called Nexus of Vireon, where darker lowland material is ringed by lighter deposits, and farther east toward the pale volcanic uplands surrounding Aurex Basin and the boundary zone known as the Verge of Aethros. Together, these named northern regions define the meeting point of permanent ice, dark volcanic terrain, and the first major routes into Lukedu’s equatorial province.
The north is therefore defined by the meeting of permanent ice and dark volcanic terrain. The most extensive frozen deposits are concentrated at the highest latitudes, while exposed rock, ash-darkened plains, cratered basins, and volcanic rises dominate the transition into the equatorial regions. The Marches of Delkar, Conflux Crown, Corridor of Symphonara, Nexus of Vireon, Aurex Basin, and Verge of Aethros give the northern hemisphere a more localized structure within Lukedu’s broader polar geology.
Equatorial Regions
The Equatorial Regions of Lukedu are dominated by volcanic plains, caldera complexes, ash-darkened lowlands, and broad fields of yellow-grey surface deposits. Much of the equatorial belt is organized around large volcanic centers surrounded by darker lava plains and mantled in places by lighter ash, sulfurous material, ejecta, or wind-reworked deposits. Several major volcanic constructs rise prominently above the surrounding terrain, each marked by deep summit craters and broad radial aprons. The broad central volcanic province is now commonly designated the Lukedion Expanse, a name applied to the wide dark equatorial belt tying together the moon’s most prominent volcanic rises, ash-darkened lowlands, and pale depositional fields.
The largest of these volcanic provinces lies across the central and eastern equatorial belt, where multiple calderas, cone clusters, and overlapping lava fields occupy a wide continuous zone. Dark plains cover most of the lowlands, while lighter material spreads outward in broad patches and halos around the principal vents. Narrow channels and irregular lowland corridors cut through some of the darker terrain, separating major volcanic rises from surrounding plains. At the heart of this region, the Conflux Crown dominates the western side of the central volcanic province, while the large caldera and associated pale apron of Patera Confluxis help define the eastern side of the same system. Between them, the Via Constellis marks one of the clearest east-west corridors of connected lowland flow, while the more sheltered interior tract known as the Hall of Measured Flow occupies a calmer and more enclosed portion of the southern equatorial volcanic belt.
The equatorial zone is also broken into distinct secondary regions. West of the central province, the canyoned terrain of Chasma Interlinka cuts through older volcanic ground, while the southern interior basin known as the Exchange Basin of Kalyx gathers lighter deposits and low-relief terrain at the foot of the main volcanic zone. In the south-central equatorial belt, the more enclosed tract called the Sanctum of Passage lies between darker plains and broken pale deposits, while farther southeast the branching route system known as the Route of the Twin Paths divides the lower volcanic terrain into multiple channels and low ridges. The eastern margin of the main volcanic province is bounded by the Verge of Aethros, beyond which the equatorial surface becomes more broken and irregular.
Later research and continued observation placed the most likely approximate source region of the radio anomaly detected in 35.19 PSSC within this broad equatorial volcanic province, most likely in the central-to-eastern equatorial belt where several of the largest calderas and associated deposits are concentrated. In the context of the mapped regions, that approximate source area aligns most closely with the Lukedion Expanse between Patera Confluxis, Aurex Basin, Via Constellis, and the surrounding clustered vents and pale ejecta fields. The signal itself was originally reported only from the immediate vicinity of Lukedu, so this location is best treated as an approximate source area rather than a confirmed site.
Southern Polar Regions
The Southern Polar Regions of Lukedu are covered by an extensive ice mass broken by dark rocky uplands, broad frozen basins, and belts of fractured terrain. The southern cap is less uniform than the northern one, with large sections of roughened ice, broken shelves, embedded rocky masses, and irregular margins where the frozen cover extends into lower terrain. In several sectors, darker land rises through the ice as exposed ridges, crater rims, and isolated uplands. The broad southern ice margin is best expressed in the zone called the Terminal Confluence Shelf, where the frozen cap spreads in apron-like form across low terrain and merges with darker volcanic and sediment-darkened ground. At the far southeastern edge, the broken margin known as the Outer Passage Scarp marks one of the clearest escarpments along the southern transition from exposed volcanic terrain into the heavier polar ice.
The southern transition zone is especially complex. Ice fills enclosed basins, spreads through low channels, and gathers in broad apron-like deposits around rough high ground. Nearby volcanic and tectonic terrain remains partly exposed, producing strong contrast between bright frozen surfaces and dark ash-rich or lava-darkened ground. Smaller vents and heated areas in the southern mid-latitudes contribute to this broken pattern, especially where pale deposits surround cratered or elevated terrain. This is most apparent in the southwestern heated tract called the Fumaroles Transitus, in the southern lowland system of the Exchange Basin of Kalyx, and along the pale connected channels of the Route of the Twin Paths, which lead toward the southern shelf.
The south combines extensive permanent ice with volcanic and impact-marked terrain beneath and around the frozen cover. Large parts of the polar region are stable and heavily glaciated, while the lower southern latitudes retain a more varied surface of exposed rock, fractured plains, localized vents, and connected passage corridors. In this sense, the Terminal Confluence Shelf, Outer Passage Scarp, Fumaroles Transitus, Exchange Basin of Kalyx, and Route of the Twin Paths define the southern hemisphere as the zone where Lukedu’s frozen cap and volcanic underworld meet most visibly.
Unusual Qualities
Lukedu is associated with intermittent electromagnetic disturbances centered in the central-to-eastern equatorial volcanic belt, the same broad region later linked by observation to the approximate source area of the unexplained radio signals first detected in 35.19 PSSC. The most widely accepted scientific explanation attributes these emissions to conductive mineral layers, magma-heated fracture networks, and piezoelectric discharge generated by tectonic stress beneath the major caldera fields. More speculative interpretations persist, especially among religious observers, who sometimes describe the signals as patterned rather than incidental.
Radio Anomolies
In 35.19 PSSC, researchers working for the New Zimian Space Exploration and Settlement Agency reported the detection of unusual radio signals from the immediate vicinity of Lukedu. Since the initial detection, the signals have been documented by researchers elsewhere and remain unexplained.
Subsequent analysis and continued observation roughly associated the signal with the moon’s central-to-eastern equatorial volcanic belt, especially the broad province containing the largest calderas, clustered vents, and surrounding deposits. That identification remains approximate, but it provides the clearest regional source area currently associated with the anomaly.
