 |
|
 |
Main belt | A Wisdom Archive on Main belt |  | Main belt A selection of articles related to Main belt |  |
|
More material related to Main Belt can be found here:
|
|
|  | |
Main belt
|  | | » Page 1 « Page 2 |  |
 | |
|
ARTICLES RELATED TO Main belt | |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
 |  |  | Main belt: Encyclopedia II - Minor planet - The main asteroid beltThe overwhelming majority of asteroids have orbits lying between the orbits of Mars and Jupiter, roughly between 2 to 4 AU. These couldn't form a planet due to the gravitational influence of Jupiter. Jupiter's gravitational influence, through orbital resonance, clears Kirkwood gaps in the asteroid belt, first recognised by Daniel Kirkwood in 1874.
The region with the densest concentration (lying between the Kirkwood gaps at 2.06 and 3.27 AU, with eccentricities below about 0.3, and inclinations smaller than 30°) is often called the M ...
See also:Minor planet, Minor planet - Groups out to the orbit of Earth, Minor planet - Groups out to the orbit of Mars, Minor planet - The main asteroid belt, Minor planet - Families within the main asteroid belt, Minor planet - Other groups out to the orbit of Jupiter, Minor planet - Groups beyond the orbit of Jupiter, Minor planet - Quasi-satellites and horseshoe objects Read more here: » Minor planet: Encyclopedia II - Minor planet - The main asteroid belt |
|  |
|
 |  |  | Main belt: Encyclopedia II - 243 Ida - MoonIda has a small moon, Dactyl, which was discovered by Galileo mission member Ann Harch, while examining the delayed image downloads, discovered on February 17, 1994. The moon was given the provisory designation S/1993 (243) 1 and later named (243) Ida I Dactyl. The discovery images were taken on 28 August 1993, hence the provisory designation. The satellite was reported on 12 March 1994.
Dactyl is only 1.4 km in diameter. Some researchers believe that Dactyl formed from debris ejected from Ida by cratering, while ...
See also:243 Ida, 243 Ida - Discovery and name, 243 Ida - Moon, 243 Ida - Physical characteristics, 243 Ida - Ida, 243 Ida - Dactyl Read more here: » 243 Ida: Encyclopedia II - 243 Ida - Moon |
|  |
|
 |  |  | Main belt: Encyclopedia II - 6 Hebe - Physical characteristicsLightcurve analysis suggests that Hebe has a rather angular shape, which may be due to several large impact craters [4]. Hebe rotates in a prograde direction, with the north pole pointing towards ecliptic coordinates (β, λ) = (45°, 339°) with a 10° uncertainty [4]. This gives an axial tilt of 42°.
It has a bright surface and, if its identification as the parent body of the H chondrites is correct, a surface composition of silicate chondritic rocks mixed with pieces of nickel-iron metal. A likely scenario fo ...
See also:6 Hebe, 6 Hebe - Discovery, 6 Hebe - Major meteorite source, 6 Hebe - Physical characteristics, 6 Hebe - Jebe, 6 Hebe - Aspects Read more here: » 6 Hebe: Encyclopedia II - 6 Hebe - Physical characteristics |
|  |
|
|
|
 | | » Page 1 « Page 2 |  |
 | |
|
|
More material related to Main Belt can be found here:
|
|
|
 | |