Miranda (moon)

From Wikipedia, the free encyclopedia

Jump to: navigation, search
Miranda
Miranda
Discovery
Discovered by: Gerard P. Kuiper
Discovery date: February 16, 1948
Orbital characteristics
Semi-major axis: 129,390 km
Eccentricity: 0.0013
Orbital period: 1.413479 d
Inclination: 4.232° (to Uranus' equator)
Satellite of: Uranus
Physical characteristics
Dimensions: 480×468.4×465.8 km
Mean radius: 235.8 km (0.03697 Earths)
Surface area: 700,000 km2
Volume: 54,835,000 km3
Mass: 6.59×1019 kg (1.103×10-5 Earths)
Mean density: 1.20 g/cm3
Equatorial surface gravity: 0.079 m/s2
Escape velocity: 0.19 km/s
Rotation period: synchronous
Axial tilt: zero
Albedo: 0.32
Surface temp.:
   Kelvin
min mean max
  ~59 K 86 K

Miranda (pronounced /mɨˈrændə/ mə-ran'-də) is the smallest and innermost of Uranus' five major moons.

It was discovered by Gerard Kuiper on 1948-02-16 at McDonald Observatory. It was named after Prospero's daughter in William Shakespeare's play The Tempest by Kuiper in his report of the discovery.[1] The adjectival form of the name is Mirandan. It is also designated Uranus V.

So far the only close-up images of Miranda are from the Voyager 2 probe, which made observations of the moon during its Uranus flyby in January, 1986. During the flyby the southern hemisphere of the moon was pointed towards the Sun so only that part was studied. It is geologically the most active body in the Uranian system.

Contents

Close-up view of Verona Rupes, a large fault scarp on Miranda; possibly 5 km (3 miles) high.
Close-up view of Verona Rupes, a large fault scarp on Miranda; possibly 5 km (3 miles) high.[2][3]

Miranda's surface may be mostly water ice, with the low density body also likely containing silicate rock and organic compounds in its interior.

Miranda's surface has patchwork regions of broken terrain indicating intense geological activity in the moon's past, and is criss-crossed by huge canyons. Large grooved structures, called coronae, may be diapirs, or upwellings of warm ice. The grooves probably represent cryovolcanic ridges formed by fissure eruptions of icy magma. The canyons probably represent grabens formed by extensional faulting. The diapirs may have changed the density distribution within the moon, which could have caused Miranda to reorient itself,[4] an event similar to what is believed to have occurred on Saturn's geologically active moon Enceladus. Miranda is one of the few bodies in the solar system in which the equatorial circumference is shorter than the pole-to-pole circumference, likely a consequence of the diapir activity.

Miranda's past geological activity is believed to have been driven by tidal heating at a time when its orbit was more eccentric than currently. Early in its history, Miranda was apparently captured in a 3:1 orbital resonance with Umbriel, from which it subsequently escaped.[5] The resonance would have increased orbital eccentricity; resulting tidal friction due to time-varying tidal forces from Uranus would have caused warming of the moon's interior. In the Uranus system, due to the planet's lesser degree of oblateness, and the larger relative size of its satellites, escape from a mean motion resonance is much easier than for satellites of Jupiter or Saturn. Miranda's orbital inclination (4.34°) is unusually high for a body so close to the planet. Miranda probably escaped from its resonance with Umbriel via a secondary resonance, and the mechanism of this escape is believed to explain why its orbital inclination is more than 10 times those of the other large Uranian moons (see Uranus' natural satellites).[6][7]

An earlier theory, proposed shortly after the Voyager 2 flyby and now out of favor, was that a previous incarnation of Miranda was shattered by a massive impact, with the fragments reassembling into the current strange pattern.[3]

Scientists recognize the following geological features on Miranda:

  • Astronomy Domine, a song by Pink Floyd, refers to Miranda as well as Oberon and Titania.
  • In the fictional Star Trek universe, the crystalline mineral dilithium was first discovered on Miranda in the mid-21st century. The moon said to be the only naturally occurring source of dilithium in the Sol system. This mineral was, a short time later, used to facilitate warp drive propulsion systems which allowed spacecraft to achieve faster-than-light travel.
  • In Kim Stanley Robinson's Mars Trilogy the moon is visited by the characters Ann Clayborne and Zo Boone.

  1. ^ G. P. Kuiper, The Fifth Satellite of Uranus, Publications of the Astronomical Society of the Pacific, Vol. 61, No. 360, p. 129, June 1949
  2. ^ PIA00044: Miranda high resolution of large fault. JPL, NASA. Retrieved on 2007-07-23.
  3. ^ a b Chaikin, Andrew (2001-10-16). Birth of Uranus' provocative moon still puzzles scientists. space.com. Imaginova Corp.. Retrieved on 2007-07-23.
  4. ^ R., Pappalardo; Greeley, R. (1993). "Structural evidence for reorientation of Miranda about a paleo-pole". In Lunar and Planetary Inst., Twenty-Fourth Lunar and Planetary Science Conference. Part 3: N-Z: 1111–1112. Retrieved on 2006-08-05. 
  5. ^ Tittemore, William C.; Jack Wisdom (June 1990). "Tidal evolution of the Uranian satellites III. Evolution through the Miranda-Umbriel 3:1, Miranda-Ariel 5:3, and Ariel-Umbriel 2:1 mean-motion commensurabilities". Icarus 85 (2): 394–443. Elsevier Science. doi:10.1016/0019-1035(90)90125-S. 
  6. ^ W. C. Tittemore, J. Wisdom (1989). "Tidal Evolution of the Uranian Satellites II. An Explanation of the Anomalously High Orbital Inclination of Miranda". Icarus 78: 63-89. doi:10.1016/0019-1035(89)90070-5. 
  7. ^ R. Malhotra, S. F. Dermott (1990). "The Role of Secondary Resonances in the Orbital History of Miranda". Icarus 85: 444-480. doi:10.1016/0019-1035(90)90126-T. 

Advanced Search
Included Web Search Engines


Safe Search

close

Top Matching Results

Occasionally Search.com will highlight specialized results that are based on the context of your query. Examples of specialized results include specific links to news, images, or video.

Top Matching Results may highlight information from other Search.com pages, content from the CNET Network of sites, or third party content. The listings are based purely on relevance. Search.com does not receive payment for listings in this section but our partners that provide this data may get paid for listing these products.

Sponsored Links

This section contains paid listings which have been purchased by companies that want to have their sites appear for specific search terms and related content. These listings are administered, sorted and maintained by a third party and are not endorsed by Search.com.

Search Results

Search.com sends your search query to several search engines at one time and integrates the results into one list which has been sorted by relevance using Search.com's proprietary algorithm. You can customize the list of search engines included in your metasearch from the preferences.

The search engines that are used in your metasearch may allow companies to pay to have their Web sites included within the results. To view the Paid Inclusion policy for a specific search engine, please visit their Web site. Search.com does not accept payment or share revenue with any search engine partner for listings in this section.