Difference between revisions of "Vall"
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Landing on Vall and returning is significantly more challenging than the [[Mün]]. It lacks atmosphere but has a higher gravity and more uneven terrain, so a larger rocket is required. | Landing on Vall and returning is significantly more challenging than the [[Mün]]. It lacks atmosphere but has a higher gravity and more uneven terrain, so a larger rocket is required. | ||
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+ | == Topology == | ||
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+ | Valls topology is dominated by hilly lowland areas separated by mountain ridges. There are almost no completely level areas, making it hard to find good landing spots. | ||
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+ | 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, pressumably in form of cryovulkanism. | ||
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+ | 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 == | == Reference Frames == |
Revision as of 17:15, 25 March 2013
Vall is one of the five natural satellites of Jool. It has an icy surface which is somewhat hilly, ranging in elevation from 0 m to 7976 m. Like the other large Joolian moons, Vall is tidally locked. Synchronus orbits around Vall are not possible, as they would lie outside of its SOI, at a radius of 3,893,254 meters.
Landing on Vall and returning is significantly more challenging than the Mün. It lacks atmosphere but has a higher gravity and more uneven terrain, so a larger rocket is required.
Contents
Topology
Valls topology is dominated by hilly lowland areas separated by mountain ridges. 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, pressumably in form of cryovulkanism.
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
Gallery
Changes
- Initial Release