Difference between revisions of "Moho"
ChillMonkey (talk | contribs) (→Geographical Features) |
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− | '''Moho''' is the innermost planet of the [[Kerbol]] star system. It | + | '''Moho''' is the innermost planet of the [[Kerbol]] star system. It is the [[w:Mercury (planet)|Mercury]] analogue for Kerbal Space Program. It is similar to [[Dres]] and [[Eeloo]] in that it has no atmosphere and no natural satellites. |
== Topography == | == Topography == | ||
− | + | Moho's surface ranges from light brown highlands to dark brown Maria. It is heavily cratered, but less so than the moons of [[Kerbin]] and [[Jool]], suggesting erosion. Because of the lack of an atmosphere on Moho, the primary suspect of Moho's erosion is volcanism. It is probable that Moho under goes volcanic periods, induced by tidal friction with Kerbol. This would lead to the filling up of craters. | |
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− | + | Moho has two very deep wells at the geographic north and south pole of a, as yet, undetermined depth. <!-- Where? Is this referring to the old, pre-0.18 Moho, with two deep volcanoes? --> Current analysis and probes dropped into the crater at the north pole revealed it to be more than 5 km deep before the probe crashed into the ever narrowing canyon walls. It is possible that these are volcanic tubes that are as of this moment dormant. Further analysis of the canyon walls is needed before a definitive answer can be presented. | |
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== Orbital Statistics == | == Orbital Statistics == | ||
− | Geosynchronous orbit around Moho is not possible — it would require an altitude of {{OrbitAltitude | period_s= | + | Geosynchronous orbit around Moho is not possible — it would require an altitude of {{OrbitAltitude | period_s=2215754 | mass_kg=3.675e21 | radius_km=250 }}, outside of Moho's sphere of influence. |
For a semi synchronous orbit of ½ Moho day (307.75 hours or 1,107,882 seconds) an orbit of | For a semi synchronous orbit of ½ Moho day (307.75 hours or 1,107,882 seconds) an orbit of | ||
{{OrbitAltitude | period_s=1107882 | mass_kg=3.675e21 | radius_km=250 }} above Moho is needed with a velocity of | {{OrbitAltitude | period_s=1107882 | mass_kg=3.675e21 | radius_km=250 }} above Moho is needed with a velocity of | ||
{{OrbitVelocity | period_s=1107882 | mass_kg=3.675e21 | radius_km=250 }}. | {{OrbitVelocity | period_s=1107882 | mass_kg=3.675e21 | radius_km=250 }}. | ||
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== Reference Frames == | == Reference Frames == | ||
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Rotational/Inertial transition: ? m | Rotational/Inertial transition: ? m | ||
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== Gallery == | == Gallery == | ||
<gallery> | <gallery> | ||
− | + | Moho_800_map.gif | A topographic height map of Moho as at Version 0.18.2 made with the ISA MapSat plugin. | |
− | Moho_800_map.gif |A | + | Moho_landing.png | A successful landing at Moho pre-0.18. Note the engines still overheating. |
</gallery> | </gallery> | ||
== Changes == | == Changes == | ||
;{{Version|0.18|}} | ;{{Version|0.18|}} | ||
− | *Entirely changed more cratered surface. | + | * Entirely changed more cratered surface. |
− | *Color changed from red to brown. | + | * Color changed from red to brown. |
− | *No more superheated atmosphere. | + | * No more superheated atmosphere. |
;{{Version|0.17|}} | ;{{Version|0.17|}} | ||
* Initial Release | * Initial Release |
Revision as of 18:03, 7 January 2013
Moho is the innermost planet of the Kerbol star system. It is the Mercury analogue for Kerbal Space Program. It is similar to Dres and Eeloo in that it has no atmosphere and no natural satellites.
Topography
Moho's surface ranges from light brown highlands to dark brown Maria. It is heavily cratered, but less so than the moons of Kerbin and Jool, suggesting erosion. Because of the lack of an atmosphere on Moho, the primary suspect of Moho's erosion is volcanism. It is probable that Moho under goes volcanic periods, induced by tidal friction with Kerbol. This would lead to the filling up of craters.
Moho has two very deep wells at the geographic north and south pole of a, as yet, undetermined depth. Current analysis and probes dropped into the crater at the north pole revealed it to be more than 5 km deep before the probe crashed into the ever narrowing canyon walls. It is possible that these are volcanic tubes that are as of this moment dormant. Further analysis of the canyon walls is needed before a definitive answer can be presented.
Orbital Statistics
Geosynchronous orbit around Moho is not possible — it would require an altitude of 0.00 m, outside of Moho's sphere of influence.
For a semi synchronous orbit of ½ Moho day (307.75 hours or 1,107,882 seconds) an orbit of 0.00 m above Moho is needed with a velocity of 0.00 m/s.
Reference Frames
Rotational/Inertial transition: ? m
Warp | Minimum Altitude |
---|---|
5x | 10 km |
10x | 10 km |
50x | 30 km |
100x | 50 km |
1,000x | 100 km |
10,000x | 200 km |
100,000x | 300 km |
Gallery
Changes
- Entirely changed more cratered surface.
- Color changed from red to brown.
- No more superheated atmosphere.
- Initial Release
Notes