Difference between revisions of "Vall"

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File:Vall_800_map.gif                |A topographic height map of Vall made with the ISA MapSat plugin
 
File:Vall_800_map.gif                |A topographic height map of Vall made with the ISA MapSat plugin
 
File:VallFromLaythe.png | Picture of Vall visible from Laythe
 
File:VallFromLaythe.png | Picture of Vall visible from Laythe
File:Screenshot62.png |A small probe in a high orbit over Vall
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File:Probe high above Vall.png |A small probe in a high orbit over Vall
 
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File:Landing party on Vall.jpg| A crew of kerbonauts, a lander, and a rover on the surface of Vall.
2013-08-19_00005.jpg| A crew of kerbonauts, a lander, and a rover on the surface of Vall.
 
 
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Revision as of 11:38, 17 April 2014

Vall/Data

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
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

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

0.17
  • Initial Release

Notes

  1. Post in the forum by NovaSilisko