Difference between revisions of "Vall"
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According to former developer NovaSilisko, Vall was planned to be made more like [[Eeloo]], with cracks in the ice and a more chaotic surface than in 0.20.2.<ref>[http://forum.kerbalspaceprogram.com/threads/29807-Planet-Ideas-And-Names-For-The-Future-Of-Kerbal-Space-Program?p=447959&viewfull=1#post447959 Post in the forum] by NovaSilisko</ref> | According to former developer NovaSilisko, Vall was planned to be made more like [[Eeloo]], with cracks in the ice and a more chaotic surface than in 0.20.2.<ref>[http://forum.kerbalspaceprogram.com/threads/29807-Planet-Ideas-And-Names-For-The-Future-Of-Kerbal-Space-Program?p=447959&viewfull=1#post447959 Post in the forum] by NovaSilisko</ref> | ||
| − | == Description == | + | == In-game Description == |
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Revision as of 13:22, 29 March 2014
Vall is one of the five natural satellites of Jool. Like the other large Joolian moons, Vall is tidally locked. Synchronous orbits around Vall are not possible, as they would lie outside of its SOI, at a radius of 3,893,254 meters.
Vall is KSP's analog to Jupiter's moon Europa.
Though the bodies have topical similarities, landing on Vall and returning is significantly more challenging than a landing on the Mün, due to the former's higher gravity and more uneven terrain.
According to former developer NovaSilisko, Vall was planned to be made more like Eeloo, with cracks in the ice and a more chaotic surface than in 0.20.2.[1]
In-game Description
| “ | Vall was one of the last Moons of Jool to be discovered. Frustrated scientists kept trying to wipe it off the lenses of their telescopes. Eventually after a rash of returned telescopes, Advanced Optics Co. finally decided to just tell them it was an actual object in the sky. — Kerbal Astronomical Society |
” |
Topology
Vall has an icy surface which is dominated by hilly lowland areas separated by mountain ridges, and ranges in elevation from 0 to 7976 m. There are almost no completely level areas, making it hard to find good landing spots.
Vall has some circular mountain ridges which could be remnants of impact craters, but they are heavily eroded, hinting that Vall has some geological activity, presumably in the form of cryovolcanism.
The surface color ranges between white and light blue. When terrain scatters are activated, large boulders with contrast-rich black and white surface patterns can be found on the surface.
Reference Frames
| Time warp | Minimum Altitude |
|---|---|
| 1× | Any |
| 5× | 24 500 m |
| 10× | 24 500 m |
| 50× | 24 500 m |
| 100× | 40 000 m |
| 1 000× | 60 000 m |
| 10 000× | 80 000 m |
| 100 000× | 100 000 m |
Gallery
A small user-created probe in low orbit around Vall. Jool and Laythe have risen in the background.
A crew of Kerbonauts enjoying the view over Vall's landscape.
One of the rocks which can be found on Vall.
A topographic map of Vall made with the ISA MapSat plugin.
A bump map in approximate natural colors.
The surface of Vall with Jool, Laythe and Tylo in the background. Bop is also on this picture but far too small to recognise.
A topographic height map of Vall made with the ISA MapSat plugin
Picture of Vall visible from Laythe
A small probe in a high orbit over Vall
- 2013-08-19 00005.jpg
A crew of kerbonauts, a lander, and a rover on the surface of Vall.
Trivia
- According to the Tracking Station information of Vall, it was one of the last moons of Jool to be discovered. This was because the Kerbal astronomers mistook the icy moon for a smudge. After multiple failed attempts to get rid of the "smudge", they figured out it was, in fact, a moon.
Changes
- Initial Release
Notes
- ↑ Post in the forum by NovaSilisko
