|Moho as seen from orbit.|
|Planet of Kerbol|
|Semi-major axis||5 263 138 304 m [Note 1]|
|Apoapsis||6 315 765 980 m [Note 1]|
|Periapsis||4 210 510 628 m [Note 1]|
|Orbital inclination||7.0 °|
|Argument of periapsis||15 °|
|Longitude of the ascending node||70 °|
|Mean anomaly||3.14 rad (at 0s UT)|
|Sidereal orbital period||2 215 754 s|
|102 d 3 h 29 m 14.2 s|
|Synodic orbital period||2918346.4 s|
|Orbital Velocity||12 186 to 18 279 m/s|
|Equatorial radius||250 000 m|
|Surface area||7.8539816×1011 m2|
|Standard gravitational parameter||1.6860938×1011 m3/s2|
|Density||38 599.963 kg/m3|
|Surface gravity||2.70 m/s2 (0.275 g)|
|Escape velocity||1 161.41 m/s|
|Sidereal rotation period||1 210 000.0 s|
|56 d 0 h 6 m 40 s|
|Solar day||2 665 723.4 s|
|123 d 2 h 28 m 43.4 s|
|Sidereal rotational velocity||1.2982 m/s|
|Synchronous orbit||18 173.17 km|
|Sphere of influence||9 646 663.0 m[Note 1]|
|Atmosphere present||× No|
|“|| Moho figures in Kerbal mythology as a fiery place with oceans of flowing lava. In reality, however, it's much less interesting.
Scientists speculate about possible ways to make it awesome like in the stories. Some of those ideas have led to new breakthroughs in aerospace technology.
Moho gets its name from the Mohorovičić discontinuity; the boundary between the Earth's crust and mantle.
Moho's surface ranges from light brown highlands to dark brown basins, possibly the product of volcanism. Its highest point is in its northern hemisphere at an altitude of 6817 m. Moho's heavy cratering suggests erosion. Tidal friction with Kerbol most likely causes airless Moho's erosion by inducing volcanic periods that fill craters.
Moho has a very deep well at its geographic north pole, called the Mohole by fans in reference to Project Mohole, and the Northern Sinkhole by scientific instruments. Despite, according to the Map View, the apparent existence of another hole at the geographic south pole, one does not exist. The Mohole is about 4.6 kilometers deep. The hole is a glitch in the procedural generation of terrain; many other bodies with land at the north pole have similar bugs.
The Mohole can destroy craft and Kerbals that fall into it.
Mohosynchronous and semi-synchronous orbits are impossible — they would require altitudes of 18 182.00 km and 11 361.44 km respectively, both of which are beyond Moho's sphere of influence.
|5×||10 000 m|
|10×||10 000 m|
|50×||30 000 m|
|100×||50 000 m|
|1 000×||100 000 m|
|10 000×||200 000 m|
|100 000×||300 000 m|
Solar System Counterpart
Moho is the apparent Kerbol System analog of the planet Mercury. Both share a similar cratered landscape, like most bodies with little to no atmosphere. Due to the lack of an atmosphere to retain heat, Moho and Mercury are freezing on the night side and, relative to Earth, extremely hot on the day side. Both planets are the closest to their respective stars and lack natural satellites.
However, Moho has a brown surface, while Mercury has a dark grey surface. In addition, Mercury has a tenuous atmosphere of about 10⁻¹³ kPa while Moho has no atmosphere; although, a pressure of 10⁻¹³ kPa (≃ 10⁻¹⁵ atm) would be rendered "unmeasurable" by the PresMat Barometer and register in KSP as a vacuum.
Bill Kerman having the time of his life wedged in the Northern Mohole.
Hanny Kerman wedged in the Northern Mohole sideways. Lots of orientation jittering was observed.
- Added biomes
- New, procedurally generated, textures added, with higher detail craters.
- Entirely changed more cratered surface.
- Color changed from red to brown.
- No more superheated atmosphere.
- No longer tidally locked.
- Mass reduced.
- Initial Release