Kurato: Difference between revisions
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| mean_radius = {{convert|24.966|km|mi|comma=gaps|abbr=on}} | | mean_radius = {{convert|24.966|km|mi|comma=gaps|abbr=on}} | ||
| surface_area = 15,865,000km<sup>2</sup><br>(6,125,000 mi<sup>2</sup>) | | surface_area = 15,865,000km<sup>2</sup><br>(6,125,000 mi<sup>2</sup>) | ||
| volume = 65,180.972 km<sup>3</sup> | | volume = 65,180.972 <sup>km</sup><sup>3</sup> | ||
| mass = 1.195 × 10<sup>15</sup> kg | | mass = 1.195 × 10<sup>15</sup> kg | ||
| density = 1.834 g/cm<sup>3</sup> | | density = 1.834 g/cm<sup>3</sup> | ||
Revision as of 17:37, 14 May 2023
_mathilde_crop.jpg) | |||||||||||||
| Orbital characteristics | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Epoch A2000 | |||||||||||||
| Aphelion | 244410 km (151870 mi) | ||||||||||||
| Perihelion | 219360 km (136300 mi) | ||||||||||||
| 231887 km (144088 mi) | |||||||||||||
| Eccentricity | ~0.054021 | ||||||||||||
| 13.4711 d (323.31 h) | |||||||||||||
Average orbital speed | 1.249 km/s (0.776 mi/s) | ||||||||||||
| Inclination | 10.3670° (to Stratos's equator) 1.3524° (to the ecliptic) | ||||||||||||
| Satellite of | Stratos | ||||||||||||
| Physical characteristics | |||||||||||||
| 15,865,000km2 (6,125,000 mi2) | |||||||||||||
| Volume | 65,180.972 km3 | ||||||||||||
| Mass | 1.195 × 1015 kg | ||||||||||||
Mean density | 1.834 g/cm3 | ||||||||||||
| 1.2059 m/s2 | |||||||||||||
| 1.646 km/s (1.023 mi/s) | |||||||||||||
Sidereal rotation period | synchronous | ||||||||||||
| 2.02° | |||||||||||||
| Albedo | 0.234 Bond | ||||||||||||
| |||||||||||||
Kurato, or Stratos II, is the larger of the two significant moons of Stratos, with an orbital period of just shorter than 13 and a half days around the planet.
Formation
Kurato is thought to have originated as a small planetoid within the inner Tendor System, likely at around a distance of 2-2.1 AU. It is believed that the migration of Aurious towards the inner system would have disturbed its previously circular orbit and shifted it into a more elliptical orbit, which after a few million years landed it within the influence of Stratos, henceforth capturing it as a moon.
The hypothesis came to be given the fact that the moon has an inclination more similar to that of the ecliptic than that of Stratos and Loftuslo, a composition comparatively dissimilar with Stratos and Loftuslo, and that the hypothesis explains the distinct lack of planets in between Anteria and Stratos.
Physical Characteristics
WIP
Surface Geology
WIP
Orbit and Rotation
Kurato is tidally locked to Stratos, similar to that of Loftuslo, and completes an orbit around the planet about every 13.5 days. Curiously, the moon has a relatively large axial tilt for a tidally locked moon, even moreso than the Moon, making for slight variations in which portions of the moon's surface can be seen on the Stratoshian surface.
Habitability
WIP
