770:
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disruption event occurred. According to an analysis of Ida's cratering processes, its surface is more than a billion years old. However, this is inconsistent with the estimated age of the Ida–Dactyl system of less than 100 million years; it is unlikely that Dactyl, due to its small size, could have escaped being destroyed in a major collision for longer. The difference in age estimates may be explained by an increased rate of cratering from the debris of the
Koronis parent body's destruction.
978:
866:
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1023:. Although there are a few steep slopes tilting up to about 50° on Ida, the slope generally does not exceed 35°. Ida's irregular shape is responsible for the asteroid's very uneven gravitational field. The surface acceleration is lowest at the extremities because of their high rotational speed. It is also low near the "waist" because the mass of the asteroid is concentrated in the two halves, away from this location.
593:, creatures which inhabited Mount Ida in Greek mythology. Dactyl is only 1.4 kilometres (0.87 mi) in diameter, about 1/20 the size of Ida. Its orbit around Ida could not be determined with much accuracy, but the constraints of possible orbits allowed a rough determination of Ida's density and revealed that it is depleted of metallic minerals. Dactyl and Ida share many characteristics, suggesting a common origin.
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with all three abundant enough to be classified as potential ores. All three contain feldspar (an aluminosilicate of calcium, sodium, and potassium), pyroxene (silicates with one silicon atom for each atom of magnesium, iron, or calcium), olivine (silicates with two iron or magnesium atoms per silicon atom), metallic iron, and iron sulfide (the mineral
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diameter greater than 80 m (260 ft), indicating that the moon has suffered many collisions during its history. At least six craters form a linear chain, suggesting that it was caused by locally produced debris, possibly ejected from Ida. Dactyl's craters may contain central peaks, unlike those found on Ida. These features, and Dactyl's
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recently or uncovered by an impact event. Most of them are located within the craters
Lascaux and Mammoth, but they may not have been produced there. This area attracts debris due to Ida's irregular gravitational field. Some blocks may have been ejected from the young crater Azzurra on the opposite side of the asteroid.
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Ida's region 2 features several sets of grooves, most of which are 100 m (330 ft) wide or less and up to 4 km (2.5 mi) long. They are located near, but are not connected with, the craters
Mammoth, Lascaux, and Kartchner. Some grooves are related to major impact events, for example
745:
trajectory carried it into the asteroid belt twice on its way to
Jupiter. During its second crossing, it flew by Ida on 28 August 1993 at a speed of 12,400 m/s (41,000 ft/s) relative to the asteroid. The onboard imager observed Ida from a distance of 240,350 km (149,350 mi) to its
959:
Both of these discoveries—the space weathering effects and the low density—led to a new understanding about the relationship between S-type asteroids and OC meteorites. S-types are the most numerous kind of asteroid in the inner part of the asteroid belt. OC meteorites are, likewise, the most common
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was taking place on Ida, a process which causes older regions to become more red in color over time. The same process affects both Ida and its moon, although Dactyl shows a lesser change. The weathering of Ida's surface revealed another detail about its composition: the reflection spectra of freshly
581:
and
Jupiter, like all main-belt asteroids. Its orbital period is 4.84 years, and its rotation period is 4.63 hours. Ida has an average diameter of 31.4 km (19.5 mi). It is irregularly shaped and elongated, apparently composed of two large objects connected together. Its surface is one of
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The chondrites fall naturally into five composition classes, of which three have very similar mineral contents, but different proportions of metal and silicates. All three contain abundant iron in three different forms (ferrous iron oxide in silicates, metallic iron, and ferrous sulfide), usually
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Dactyl is an "egg-shaped" but "remarkably spherical" object measuring 1.6 by 1.4 by 1.2 kilometres (0.99 by 0.87 by 0.75 mi). It is oriented with its longest axis pointing towards Ida. Like Ida, Dactyl's surface exhibits saturation cratering. It is marked by more than a dozen craters with a
604:
flyby, many different theories had been proposed to explain their mineral composition. Determining their composition permits a correlation between meteorites falling to the Earth and their origin in the asteroid belt. Data returned from the flyby pointed to S-type asteroids as the source for the
2329:
Nearly a month after a successful photo session, the
Galileo spacecraft last week finished radioing to Earth a high-resolution portrait of the second asteroid ever to be imaged from space. Known as 243 Ida, the asteroid was photographed from an average distance of just 3,400 kilometers some 3.5
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Ida is one of the most densely cratered bodies yet explored in the Solar System, and impacts have been the primary process shaping its surface. Cratering has reached the saturation point, meaning that new impacts erase evidence of old ones, leaving the total crater count roughly the same. It is
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About 20 large (40–150 m across) ejecta blocks have been identified, embedded in Ida's regolith. Ejecta blocks constitute the largest pieces of the regolith. Because ejecta blocks are expected to break down quickly by impact events, those present on the surface must have been either formed
1326:
Ida originated in the breakup of the roughly 120 km (75 mi) diameter
Koronis parent body. The progenitor asteroid had partially differentiated, with heavier metals migrating to the core. Ida carried away insignificant amounts of this core material. It is uncertain how long ago the
1833:
Dactyl may have originated at the same time as Ida, from the disruption of the
Koronis parent body. However, it may have formed more recently, perhaps as ejecta from a large impact on Ida. It is extremely unlikely that it was captured by Ida. Dactyl may have suffered a major impact around
936:. Estimates of Ida's density are constrained to less than 3.2 g/cm by the long-term stability of Dactyl's orbit. This all but rules out a stony-iron composition; were Ida made of 5 g/cm iron- and nickel-rich material, it would have to contain more than 40% empty space.
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Ida is a distinctly elongated asteroid, with an irregular surface. Ida is 2.35 times as long as it is wide, and a "waist" separates it into two geologically dissimilar halves. This constricted shape is consistent with Ida being made of two large, solid components, with loose
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recorded 47 images of Dactyl over an observation period of 5.5 hours in August 1993. The spacecraft was 10,760 kilometres (6,690 mi) from Ida and 10,870 kilometres (6,750 mi) from Dactyl when the first image of the moon was captured, 14 minutes before
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parent body. The largest crater, Lascaux, is almost 12 km (7.5 mi) across. Region 2 contains nearly all of the craters larger than 6 km (3.7 mi) in diameter, but Region 1 has no large craters at all. Some craters are arranged in chains.
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and Ida were secondary to the
Jupiter mission. These were selected as targets in response to a new NASA policy directing mission planners to consider asteroid flybys for all spacecraft crossing the belt. No prior missions had attempted such a flyby.
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produces an acceleration of about 0.3 to 1.1 cm/s over its surface. This field is so weak that an astronaut standing on its surface could leap from one end of Ida to the other, and an object moving in excess of 20 m/s (70 ft/s) could
4648:
Greeley, Ronald; Sullivan, Robert J.; Pappalardo, R.; Head, J.; Veverka, Joseph; Thomas, Peter C.; Lee, P.; Belton, M.; Chapman, Clark R. (March 1994). "Morphology and
Geology of Asteroid Ida: Preliminary Galileo Imaging Observations".
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If in a circular orbit at the distance at which it was seen, Dactyl's orbital period would be about 20 hours. Its orbital speed is roughly 10 m/s (33 ft/s), "about the speed of a fast run or a slowly thrown baseball".
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must be more than about 65 km (40 mi) from Ida for it to remain in a stable orbit. The range of orbits generated by the simulations was narrowed down by the necessity of having the orbits pass through points at which
1200:
The craters are simple in structure: bowl-shaped with no flat bottoms and no central peaks. They are distributed evenly around Ida, except for a protrusion north of crater Choukoutien which is smoother and less cratered. The
1192:
variations across its surface. An exception to the crater morphology is the fresh, asymmetric Fingal, which has a sharp boundary between the floor and wall on one side. Another significant crater is Afon, which marks Ida's
1780:, after two of the mythological dactyls. Acmon is the largest crater in the above image, and Celmis is near the bottom of the image, mostly obscured in shadow. The craters are 300 and 200 meters in diameter, respectively.
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found minimal variations on the surface, and the asteroid's spin indicates a consistent density. Assuming that its composition is similar to OC meteorites, which range in density from 3.48 to 3.64 g/cm, Ida would have a
4327:
3293:
Archinal, B. A.; Acton, C. H.; A'Hearn, M. F.; Conrad, A.; Consolmagno, G. J.; Duxbury, T.; et al. (February 2018). "Report of the IAU Working Group on Cartographic Coordinates and Rotational Elements: 2015".
1047:
and mostly gray, although minor color variations mark newly formed or uncovered areas. Besides craters, other features are evident, such as grooves, ridges, and protrusions. Ida is covered by a thick layer of
1267:. The megaregolith layer of Ida extends between hundreds of meters below the surface to a few kilometers. Some rock in Ida's core may have been fractured below the large craters Mammoth, Lascaux, and Undara.
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spacecraft during its flyby in 1993. These images provided the first direct confirmation of an asteroid moon. At the time, it was separated from Ida by a distance of 90 kilometres (56 mi), moving in a
3142:
When Zeus was born, Rhea entrusted the guardianship of her son to the Dactyls of Ida, who are the same as those called Curetes. They came from Cretan Ida – Heracles, Paeonaeus, Epimedes, Iasius and
672:
and Edward F. Tedesco as part of the eight-color asteroid survey (ECAS). Its spectrum matched those of the asteroids in the S-type classification. Many observations of Ida were made in early 1993 by the
1314:
of a uniformly dense object the same shape as Ida coincides with the spin axis of the asteroid. This suggests that there are no major variations of density within the asteroid. Ida's axis of rotation
1648:. Dactyl is heavily cratered, like Ida, and consists of similar materials. Its origin is uncertain, but evidence from the flyby suggests that it originated as a fragment of the Koronis parent body.
746:
closest approach of 2,390 km (1,490 mi). Ida was the second asteroid, after Gaspra, to be imaged by a spacecraft. About 95% of Ida's surface came into view of the probe during the flyby.
2000:
Belton, M. J. S.; Chapman, C. R.; Thomas, P. C.; Davies, M. E.; Greenberg, R.; Klaasen, K.; et al. (1995). "Bulk density of asteroid 243 Ida from the orbit of its satellite Dactyl".
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179:
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Chapman, Clark R.; Belton, Michael J. S.; Veverka, Joseph; Neukum, G.; Head, J.; Greeley, Ronald; Klaasen, K.; Morrison, D. (March 1994). "First Galileo image of asteroid 243 Ida".
1188:. Azzurra seems to be the most recent major impact on Ida. The ejecta from this collision is distributed discontinuously over Ida and is responsible for the large-scale color and
3833:
Lee, Pascal; Veverka, Joseph; Thomas, Peter C.; Helfenstein, Paul; Belton, Michael J. S.; Chapman, Clark R.; Greeley, Ronald; Pappalardo, Robert T.; et al. (March 1996).
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are very similar. The small differences indicate that the space weathering process is less active on Dactyl. Its small size would make the formation of significant amounts of
1225:(OC) meteorites. The composition of the interior has not been directly analyzed, but is assumed to be similar to OC material based on observed surface color changes and Ida's
3707:
1158:
covered with craters of all sizes and stages of degradation, and ranging in age from fresh to as old as Ida itself. The oldest may have been formed during the breakup of the
960:
type of meteorite found on the Earth's surface. The reflection spectra measured by remote observations of S-type asteroids, however, did not match that of OC meteorites. The
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739:. Mission planners delayed the decision to attempt a flyby until they were certain that this would leave the spacecraft enough propellant to complete its Jupiter mission.
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shape, imply that the moon is gravitationally controlled despite its small size. Like Ida, its average temperature is about 200 K (−73 °C; −100 °F).
1821:
observed Ida for eight hours and was unable to spot Dactyl. It would have been able to observe it if it were more than about 700 km (430 mi) from Ida.
1843:
3591:
Chapman, Clark R.; Ryan, Eileen V.; Merline, William J.; Neukum, Gerhard; Wagner, Roland; Thomas, Peter C.; Veverka, Joseph; Sullivan, Robert J. (March 1996).
4248:
Berger, Peter (2003). "The Gildemeester Organisation for Assistance to Emigrants and the expulsion of Jews from Vienna, 1938–1942". In Gourvish, Terry (ed.).
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Belton, M. J. S.; Chapman, Clark R.; Klaasen, Kenneth P.; Harch, Ann P.; Thomas, Peter C.; Veverka, Joseph; McEwen, Alfred S.; Pappalardo, Robert T. (1996).
3726:
Geissler, Paul E.; Petit, Jean-Marc; Greenberg, Richard (1996). "Ejecta Reaccretion on Rapidly Rotating Asteroids: Implications for 243 Ida and 433 Eros".
4014:
Sullivan, Robert J.; Greeley, Ronald; Pappalardo, R.; Asphaug, E.; Moore, J. M.; Morrison, D.; Belton, Michael J. S.; Carr, M.; et al. (March 1996).
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Petit, Jean-Marc; Durda, Daniel D.; Greenberg, Richard; Hurford, Terry A.; Geissler, Paul E. (November 1997). "The Long-Term Dynamics of Dactyl's Orbit".
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372:
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Greenberg, Richard; Bottke, William F.; Nolan, Michael; Geissler, Paul E.; Petit, Jean-Marc; Durda, Daniel D.; Asphaug, Erik; Head, James (March 1996).
3562:
Chapman, Clark R. (October 1996). "S-Type Asteroids, Ordinary Chondrites, and Space Weathering: The Evidence from Galileo's Fly-bys of Gaspra and Ida".
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Monet, A. K. B.; Stone, R. C.; Monet, D. G.; Dahn, C. C.; Harris, H. C.; Leggett, S. K.; Pier, J. R.; Vrba, F. J.; Walker, R. L. (June 1994).
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Geissler, Paul E.; Petit, Jean-Marc; Durda, Daniel D.; Greenberg, Richard; Bottke, William F.; Nolan, Michael; Moore, Jeffrey (March 1996).
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observed Dactyl to be at 16:52:05 UT on 28 August 1993, about 90 km (56 mi) from Ida at longitude 85°. On 26 April 1994, the
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Thomas, Peter C.; Belton, Michael J. S.; Carcich, B.; Chapman, Clark R.; Davies, M. E.; Sullivan, Robert J.; Veverka, Joseph (1996).
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excavated by impacts is deposited differently on Ida than on planets because of its rapid rotation, low gravity and irregular shape.
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4789:
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761:. The remaining images were sent in February 1994, when the spacecraft's proximity to the Earth allowed higher speed transmissions.
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Zellner, Ben; Tholen, David J.; Tedesco, Edward F. (March 1985). "The eight-color asteroid survey: Results for 589 minor planets".
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based on the similarity of its reflectance spectra with similar asteroids. S-types may share their composition with stony-iron or
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of Dactyl's orbit when most of the images were taken, which made determining its exact orbit difficult. Dactyl orbits in the
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265:
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exposed parts of the surface resembled that of OC meteorites, but the older regions matched the spectra of S-type asteroids.
4739:
4015:
3834:
3622:
3520:
Chapman, Clark R.; Klaasen, K.; Belton, Michael J. S.; Veverka, Joseph (July 1994). "Asteroid 243 IDA and its satellite".
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settle asymmetrically around their craters, but fast-moving ejecta that escapes from the asteroid is permanently lost.
4383:
The Standard American Encyclopedia of Arts, Sciences, History, Biography, Geography, Statistics, and General Knowledge
2920:). These three classes, referred to collectively as the ordinary chondrites, contain quite different amounts of metal.
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with a period of 77 thousand years, due to the gravity of the Sun acting upon the nonspherical shape of the asteroid.
681:. These improved the measurement of Ida's orbit around the Sun and reduced the uncertainty of its position during the
4867:
3541:
Chapman, Clark R. (September 1995). "Galileo Observations of Gaspra, Ida, and Dactyl: Implications for Meteoritics".
1134:, connected by a "waist". This feature may have been filled in by debris, or blasted out of the asteroid by impacts.
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and the subsequent measurement of Ida's mass provided new insights into the geology of S-type asteroids. Before the
5193:
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Several major structures mark Ida's surface. The asteroid appears to be split into two halves, here referred to as
5208:
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85:
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flyby of Ida found that some S-types, particularly the Koronis family, could be the source of these meteorites.
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The Eos and Koronis families ... are entirely of type S, which is rare at their heliocentric distances ...
1399:
909:. Ida's relatively large surface exhibited a diverse range of geological features. The discovery of Ida's moon
111:
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asteroids. Ida orbits the Sun at an average distance of 2.862 AU (428.1 Gm), between the orbits of
1052:, loose debris that obscures the solid rock beneath. The largest, boulder-sized, debris fragments are called
4981:
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flybys, but was interpreted to be either of two minerals found in meteorites that had fallen to the Earth:
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1103:. Because of this process, older regolith appears more red in color compared to freshly exposed material.
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626:
564:, the most numerous type in the inner asteroid belt. On 28 August 1993, Ida was visited by the uncrewed
350:
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Region 1 of Ida contains two major structures. One is a prominent 40 km (25 mi) ridge named
574:. It was the second asteroid visited by a spacecraft and the first found to have a natural satellite.
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filling the gap between them. However, no such debris was seen in high-resolution images captured by
933:
913:, the first confirmed satellite of an asteroid, provided additional insights into Ida's composition.
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that stretches 150 degrees around Ida's surface. The other structure is a large indentation named
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the most heavily cratered in the Solar System, featuring a wide variety of crater sizes and ages.
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D'Amario, Louis A.; Bright, Larry E.; Wolf, Aron A. (May 1992). "Galileo trajectory design".
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direction and is inclined about 8° to Ida's equator. Based on computer simulations, Dactyl's
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on Earth. The crater Azzurra, for example, is named after a submerged cave on the island of
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Images from the flyby, starting 5.4 hours before closest approach and showing Ida's rotation
661:, who proposed in 1918 that the group comprised the remnants of a destroyed precursor body.
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753:. The first five images were received in September 1993. These comprised a high-resolution
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Transmission of many Ida images was delayed due to a permanent failure in the spacecraft's
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mission member Ann Harch, while examining delayed image downloads from the spacecraft.
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Ida's moon Dactyl was discovered by mission member Ann Harch in images returned from
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impossible. This contrasts with Ida, which is covered by a deep layer of regolith.
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Size comparison of Ida, several other asteroids, the dwarf planet Ceres, and Mars
4550:
Byrnes, Dennis V.; D'Amario, Louis A.; Galileo Navigation Team (December 1994).
3800:"Tidal Evolution by Elongated Primaries: Implications for the Ida/Dactyl System"
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is located on the right "tip" of the asteroid. The dot to the right is its moon
4750:
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trajectory to approach Ida required that it consume 34 kg (75 lb) of
17:
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Vokrouhlicky, David; Nesvorny, David; Bottke, William F. (11 September 2003).
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Ida's interior probably contains some amount of impact-fractured rock, called
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Cowen, Ron (2 October 1993). "Close-up of an asteroid: Galileo eyes Ida".
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Bottke, William F. Jr.; Cellino, A.; Paolicchi, P.; Binzel, R. P. (2002).
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of 2.27–3.10 g/cm. OC meteorites contain varying amounts of the silicates
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Asymmetric 1.5 km (0.93 mi) wide crater Fingal at 13.2°S, 39.9°E
877:
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4474:. Cambridge Planetary Science. Vol. 11. Cambridge University Press.
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3411:"Galileo's Encounter with 243 Ida: An Overview of the Imaging Experiment"
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4611:"Idiosyncrasies of Ida—asteroid 243 Ida's irregular gravitational field"
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3499:
Chapman, Clark R. (1994). "The Galileo Encounters with Gaspra and Ida".
4353:. Translated by Jones, W. H. S.; Omerod, H. A. Loeb Classical Library.
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1983:
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1249:. The mineral content appears to be homogeneous throughout its extent.
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3942:"The overlapping plates method applied to CCD observations of 243 Ida"
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The surface of Ida is covered in a blanket of pulverized rock, called
4329:
Mining the Sky: Untold Riches from the Asteroids, Comets, and Planets
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4705:"Discovery of Ida's Moon Indicates Possible "Families" of Asteroids"
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4740:"Johann Palisa, the most successful visual discoverer of asteroids"
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Britt, D. T.; Yeomans, D. K.; Housen, K.; Consolmagno, G. (2002).
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1165:
1030:
946:
831:
817:
758:
646:
642:
638:
4871:
2946:
2870:
2858:
2767:
2712:
2658:
2580:
2578:
2576:
2574:
2404:
2311:
2295:
2293:
2047:
2045:
2043:
2041:
2039:
1292:
1238:
1076:
and redistributed across Ida's surface by geological processes.
1002:
Ida's mass is between 3.65 and 4.99 × 10 kg. Its
650:
578:
548:. It was discovered on 29 September 1884 by Austrian astronomer
401:
5045:
617:
Ida was discovered on 29 September 1884 by Austrian astronomer
609:
meteorites, the most common type found on the Earth's surface.
1279:
Orbit and positions of Ida and five planets as of 9 March 2009
871:
Trajectory of Galileo from launch to Jupiter orbital insertion
199:
4405:"Catalogue of Minor Planet Names and Discovery Circumstances"
3364:"An Overview of the Asteroids: The Asteroids III Perspective"
1987:
4651:
Abstracts of the 25th Lunar and Planetary Science Conference
4577:
Abstracts of the 25th Lunar and Planetary Science Conference
4102:"The vector alignments of asteroid spins by thermal torques"
3907:"Astrometry for the Galileo mission. 1: Asteroid encounters"
3258:
2977:
2843:
2618:
1099:. Its appearance changes over time through a process called
3172:
3153:
3151:
2882:
2729:
2697:
2682:
2646:
2565:
2553:
1760:
1737:
1515:
1512:
202:
190:
139:
133:
4167:
Wilson, Lionel; Keil, Klaus; Love, Stanley J. (May 1999).
3270:
3246:
3234:
3222:
3210:
3065:
2541:
2440:
2389:
2067:
2051:
1719:
The two largest imaged craters on Dactyl were named Acmon
1113:
image of a 150 m (490 ft) block at 24.8°S, 2.8°E
2893:
2891:
2484:
2482:
2480:
2478:
2476:
2101:
2099:
2097:
2095:
1769:
1728:
1506:
1494:
1433:
1424:
3677:"Erosion and Ejecta Reaccretion on 243 Ida and Its Moon"
3323:
Asphaug, Erik; Ryan, Eileen V.; Zuber, Maria T. (2003).
1310:
of 4.63 hours (roughly 5 hours). The calculated maximum
905:
asteroid mission, permitted the first study of asteroid
30:
This article is about an asteroid. For other uses, see
2793:
2584:
2428:
2299:
2284:
2272:
2241:
1058:, several of which have been observed on the surface.
924:. The composition of S-types was uncertain before the
560:. Later telescopic observations categorized Ida as an
5106:
4463:
Thomas, Peter C.; Prockter, Louise M. (28 May 2004).
2778:
2776:
2330:
minutes before Galileo's closest approach on Aug. 28.
1772:
1757:
1740:
1731:
1518:
1497:
1445:
1427:
782:
trajectory from 19 October 1989 to 30 September 2003
205:
4513:
Belton, Michael J. S.; Carlson, R. (12 March 1994).
4169:"The internal structures and densities of asteroids"
3078:
3076:
3074:
2217:
2200:
2188:
1834:
100 million years ago, which reduced its size.
1763:
1509:
1503:
1491:
1436:
1430:
1421:
196:
136:
3798:Hurford, Terry A.; Greenberg, Richard (June 2000).
2756:
2416:
2370:
1766:
1754:
1734:
1725:
1704:Dactyl shares many characteristics with Ida. Their
1609:
1597:
1587:
1580:
1570:
1560:
1548:
1536:
1529:
1500:
1479:
1467:
1455:
1418:
1409:
1397:
1392:
1384:
1371:
1361:
1356:
1347:Highest-resolution image of Dactyl, recorded while
512:
498:
488:
476:
463:
448:
436:
423:
410:
400:
388:
378:
371:
360:
348:
336:
326:
314:
301:
289:
279:
263:
249:
235:
216:
193:
178:
162:
150:
130:
121:
109:
104:
96:
84:
72:
67:
4778:33rd Annual Lunar and Planetary Science Conference
4301:
3121:
3119:
3014:
2740:
2738:
2597:
2595:
2593:
2525:
2523:
2521:
2519:
2517:
2515:
2513:
2500:
2498:
2496:
2488:
2463:
2461:
2459:
2457:
2455:
2453:
2451:
2449:
2368:
2366:
2364:
2362:
2360:
2358:
2356:
2354:
2352:
2350:
2256:
2254:
2252:
2250:
2172:
2170:
2168:
1920:
1796:Dactyl's orbit around Ida is not precisely known.
939:The Galileo images also led to the discovery that
4442:(Thesis). Massachusetts Institute of Technology.
3835:"Ejecta Blocks on 243 Ida and on Other Asteroids"
1844:List of geological features on 243 Ida and Dactyl
1299:. Ida takes 4.84089 years to complete one orbit.
668:was measured on 16 September 1980 by astronomers
3157:
3092:
3090:
2989:
2854:
2852:
1792:Diagram of potential orbits of Dactyl around Ida
757:of the asteroid at a resolution of 31–38 m/
685:flyby from 78 to 60 km (48 to 37 mi).
4440:Spin-Axis Alignment of Koronis Family Asteroids
3886:Journal of the British Astronomical Association
3140:
2913:
2327:
2204:
2082:
2080:
2078:
2076:
1245:. Olivine and pyroxene were detected on Ida by
633:, a Viennese brewer and amateur astronomer. In
4552:"Solving for Dactyl's Orbit and Ida's Density"
3884:Mason, John W. (June 1994). "Ida's new moon".
2931:
2897:
2782:
2105:
1883:A Practical Dictionary of the English Language
1174:Ida's major craters are named after caves and
625:. It was his 45th asteroid discovery. Ida was
5057:
4872:National Aeronautics and Space Administration
4850:. Jet Propulsion Laboratory. 25 August 2008.
4308:. Cambridge, UK: Cambridge University Press.
4281:Carroll, Bradley W.; Ostlie, Dale A. (1996).
4254:. Cambridge, UK: Cambridge University Press.
3940:Owen, W. M. Jr.; Yeomans, D. K. (June 1994).
3082:
3001:
2831:
1973:
8:
4703:Holm, Jeanne (June 1994). Jones, Jan (ed.).
4300:Greeley, Ronald; Batson, Raymond M. (2001).
3728:Completing the Inventory of the Solar System
3107:
3105:
2631:
2629:
2627:
1335:
1039:3.5 minutes before its closest approach
37:
4769:Sárneczky, K; Kereszturi, Á. (March 2002).
4620:. Vol. 147, no. 15. p. 207.
4596:. Vol. 144, no. 14. p. 215.
3454:"Asteroid Density, Porosity, and Structure"
3296:Celestial Mechanics and Dynamical Astronomy
2229:
2156:
2154:
2152:
2150:
1639:. It was discovered in images taken by the
5064:
5050:
5042:
4985:
4892:"Gazetteer of Planetary Nomenclature: Ida"
4848:"JPL Small-Body Database Browser: 243 Ida"
4411:. IAU commission. Vol. 20. Springer.
4304:The Compact NASA Atlas of the Solar System
4251:Business and Politics in Europe, 1900–1970
3749:"Collisional and Dynamical History of Ida"
3137:
1904:
1902:
1900:
1898:
1896:
1894:
1892:
1890:
1866:
1864:
1351:was about 3,900 km away from the moon
1341:
43:
4747:Meeting on Asteroids and Comets in Europe
4666:Green, Daniel W. E. (26 September 1994).
4192:
4090:
3996:
3965:
3930:
3823:
3616:
3434:
1958:
1956:
1954:
1952:
1950:
3125:
2129:
2068:Vokrouhlicky, Nesvorny & Bottke 2003
1656:Dactyl was found on 17 February 1994 by
1105:
899:flybys of Gaspra and Ida, and the later
653:. Ida was recognized as a member of the
5234:Astronomical objects discovered in 1884
5189:Minor planet object articles (numbered)
5113:
4925:, Robert Johnston, johnstonsarchive.net
4810:"Reflections on the Geology of 243 Ida"
3049:"The Argonautica" of Apollonius Rhodius
2816:
2814:
2805:
2670:
2601:
2529:
2504:
2467:
2374:
2341:
2260:
2176:
2117:
1860:
4902:from the original on 23 September 2006
4868:"Images of Asteroids Ida & Dactyl"
4283:An Introduction to Modern Astrophysics
3486:from the original on 17 September 2003
2958:
2744:
2141:
1615:200 K (−73 °C; −100 °F)
1334:
36:
4668:"1993 (243) 1 = (243) Ida I (Dactyl)"
4438:Slivan, Stephen Michael (June 1995).
4367:from the original on 18 November 2019
4285:. Addison-Wesley Publishing Company.
3111:
3096:
2909:
2635:
2323:
577:Ida's orbit lies between the planets
339:Longitude of ascending node
7:
4795:from the original on 26 January 2005
4690:from the original on 1 February 2019
4537:from the original on 1 February 2019
3035:participating institution membership
2794:Geissler, Petit & Greenberg 1996
2585:Geissler, Petit & Greenberg 1996
2429:Geissler, Petit & Greenberg 1996
2160:
2087:Archinal, Acton, A'Hearn et al. 2018
1941:participating institution membership
1908:
1870:
5214:Minor planets visited by spacecraft
4990:
4173:Meteoritics & Planetary Science
3349:from the original on 30 August 2021
1962:
1635:named Dactyl, official designation
995:Successive images of a rotating Ida
4854:from the original on 7 August 2011
4817:Lunar and Planetary Science XXVIII
4771:"'Global' Tectonism on Asteroids?"
4194:10.1111/j.1945-5100.1999.tb01355.x
3713:from the original on 20 March 2009
3584:10.1111/j.1945-5100.1996.tb02107.x
2218:Zellner, Tholen & Tedesco 1985
2201:Zellner, Tholen & Tedesco 1985
2189:Zellner, Tholen & Tedesco 1985
1676:1993 (243) 1. It was named by the
1087:Ida's regolith is composed of the
711:. Its encounters of the asteroids
25:
4834:from the original on 4 March 2009
4425:from the original on 15 June 2024
4390:from the original on 15 June 2024
4268:from the original on 15 June 2024
3625:from the original on 11 June 2019
3396:from the original on 11 June 2019
675:US Naval Observatory in Flagstaff
5164:
5152:
5140:
5128:
5116:
4933:AstDyS-2, Asteroids—Dynamic Site
4874:. 23 August 2005. Archived from
4409:Dictionary of minor planet names
4154:from the original on 11 May 2008
3785:from the original on 5 June 2019
2820:
2300:D'Amario, Bright & Wolf 1992
2285:D'Amario, Bright & Wolf 1992
2273:D'Amario, Bright & Wolf 1992
2242:D'Amario, Bright & Wolf 1992
1750:
1721:
1678:International Astronomical Union
1487:
1414:
988:
976:
876:
864:
768:
186:
126:
4898:Astrogeology Research Program.
4896:United States Geological Survey
4332:. Reading, MA: Addison-Wesley.
2757:Sárneczky & Kereszturi 2002
720:was launched into orbit by the
701:Ida was visited in 1993 by the
297:1,767.644 days (4.83955 a)
3158:Asphaug, Ryan & Zuber 2003
1680:in 1994, for the mythological
1043:Ida's surface appears heavily
1:
1149:a set opposite Vienna Regio.
1035:Mosaic of images recorded by
731:on 18 October 1989. Changing
570:spacecraft while en route to
5199:Discoveries by Johann Palisa
4380:Ridpath, John Clark (1897).
4232:10.1016/0019-1035(85)90133-2
3804:Geophysical Research Letters
2990:Hurford & Greenberg 2000
2898:Wilson, Keil & Love 1999
2106:Wilson, Keil & Love 1999
1080:observed evidence of recent
558:a nymph from Greek mythology
4609:Cowen, Ron (1 April 1995).
4465:"Tectonics of Small Bodies"
4386:. Encyclopedia Publishing.
1669:made its closest approach.
1082:downslope regolith movement
895:The data returned from the
351:Argument of perihelion
59:
5250:
4403:Schmadel, Lutz D. (2003).
3501:Asteroids, Comets, Meteors
2932:Thomas & Prockter 2004
2783:Thomas & Prockter 2004
2489:Byrnes & D'Amario 1994
1624:
1544:90 km at time of discovery
922:spectroscopic measurements
613:Discovery and observations
384:59.8 × 25.4 × 18.6 km
165:Minor planet category
29:
5224:S-type asteroids (Tholen)
5079:
4923:Asteroids with Satellites
3316:10.1007/s10569-017-9805-5
3186:"Planetary Names: Dactyl"
3083:Belton & Carlson 1994
3022:Oxford English Dictionary
3002:Carroll & Ostlie 1996
2832:Greeley & Batson 2001
1928:Oxford English Dictionary
1619:
1551:Orbital period (sidereal)
1340:
1217:Ida was classified as an
596:The images returned from
589:. It was named after the
527:
444:4.63 hours (0.193 d)
292:Orbital period (sidereal)
223:
42:
5229:S-type asteroids (SMASS)
3946:The Astronomical Journal
3911:The Astronomical Journal
3047:Edward Coleridge (1990)
1692:Physical characteristics
1688:on the island of Crete.
1582:Physical characteristics
1470:Alternative designations
968:Physical characteristics
916:Ida is classified as an
515:Absolute magnitude
494:200 K (−73 °C)
373:Physical characteristics
5073:Minor planets navigator
4982:JPL Small-Body Database
4185:1999M&PS...34..479W
3576:1996M&PS...31..699C
3477:10.2307/j.ctv1v7zdn4.37
3027:Oxford University Press
2230:Owen & Yeomans 1994
1933:Oxford University Press
1600:Synodic rotation period
1531:Orbital characteristics
1283:Ida is a member of the
1011:the asteroid entirely.
951:Polished section of an
439:Synodic rotation period
218:Orbital characteristics
4946:Observation prediction
4808:Stooke, P. J. (1997).
4738:Raab, Herbert (2002).
4092:10.1006/icar.1996.0033
4043:10.1006/icar.1996.0041
4007:10.1006/icar.1997.5788
3862:10.1006/icar.1996.0039
3776:10.1006/icar.1996.0040
3704:10.1006/icar.1996.0042
3618:10.1006/icar.1996.0038
3436:10.1006/icar.1996.0032
3387:10.2307/j.ctv1v7zdn4.7
3145:
2922:
2332:
2208:
1819:Hubble Space Telescope
1793:
1280:
1171:
1114:
1040:
956:
920:based on ground-based
4731:6 August 2019 at the
4709:The Galileo Messenger
4556:The Galileo Messenger
4350:Description of Greece
3640:Space Science Reviews
3259:Greenberg et al. 1996
3188:. IAU. Archived from
3138:Pausanias & 5.7.6
2978:Greenberg et al. 1996
1849:List of minor planets
1791:
1672:Dactyl was initially
1278:
1169:
1109:
1034:
950:
679:Oak Ridge Observatory
406:4.2 ± 0.6 ×10 kg
4711:(34). Archived from
4558:(35). Archived from
4016:"Geology of 243 Ida"
3825:10.1029/1999GL010956
3325:"Asteroid Interiors"
2947:Sullivan et al. 1996
2883:Geissler et al. 1996
2871:Sullivan et al. 1996
2859:Sullivan et al. 1996
2768:Sullivan et al. 1996
2713:Sullivan et al. 1996
2698:Geissler et al. 1996
2554:Geissler et al. 1996
2312:Sullivan et al. 1996
1881:Noah Webster (1884)
1400:MPC designation
1304:retrograde direction
1182:, also known as the
427:surface gravity
271:2.861 AU (4.280
255:2.743 AU (4.103
241:2.979 AU (4.457
112:MPC designation
32:Ida (disambiguation)
5204:Named minor planets
5033:Physical parameters
4825:1997LPI....28.1385S
4786:2002LPI....33.1381S
4684:1994IAUC.6082....2G
4659:1994LPI....25..469G
4585:1994LPI....25..237C
4531:1994IAUC.5948....2B
4472:Planetary Tectonics
4224:1985Icar...61..355Z
4129:10.1038/nature01948
4121:2003Natur.425..147V
4083:1996Icar..120...20T
4035:1996Icar..120..119S
3989:1997Icar..130..177P
3958:1994AJ....107.2295O
3923:1994AJ....107.2290M
3898:1994JBAA..104..108M
3854:1996Icar..120...87L
3816:2000GeoRL..27.1595H
3768:1996Icar..120..106G
3740:1996ASPC..107...57G
3696:1996Icar..120..140G
3652:1992SSRv...60...23D
3609:1996Icar..120...77C
3555:1995Metic..30R.496C
3534:1994Metic..29..455C
3513:1994IAUS..160..357C
3469:2002aste.book..485B
3427:1996Icar..120....1B
3379:2002aste.book....3B
3340:2002aste.book..463A
3308:2018CeMDA.130...22A
3173:Chapman et al. 1994
3025:(Online ed.).
2659:Greeley et al. 1994
2441:Chapman et al. 1994
2405:Greeley et al. 1994
2390:Chapman et al. 1994
2191:, pp. 357, 373
2014:1995Natur.374..785B
1931:(Online ed.).
1385:Discovery date
1373:Discovery site
1337:
1302:Ida rotates in the
1004:gravitational field
705:-bound space probe
666:reflection spectrum
649:who raised the god
419:2.6 ± 0.5 g/cm
157:Ida (nurse of Zeus)
97:Discovery date
86:Discovery site
39:
4970:Observational info
4878:on 21 October 2008
4756:on 30 October 2008
4347:Pausanias (1916).
4067:"The shape of Ida"
3660:10.1007/BF00216849
3593:"Cratering on Ida"
2844:Bottke et al. 2002
2808:, pp. 707–708
2619:Bottke et al. 2002
2544:, pp. 179–180
2089:, p. 6, 15–16
2052:Thomas et al. 1996
1974:Belton et al. 1996
1794:
1637:(243) Ida I Dactyl
1556:prograde, ca. 20 h
1405:(243) Ida I Dactyl
1363:Discovered by
1281:
1271:Orbit and rotation
1223:ordinary chondrite
1172:
1115:
1041:
957:
953:ordinary chondrite
930:ordinary chondrite
659:Kiyotsugu Hirayama
623:Vienna Observatory
607:ordinary chondrite
554:Vienna Observatory
100:September 29, 1884
91:Vienna Observatory
74:Discovered by
54:image of 243 Ida.
27:Main-belt asteroid
5194:Koronis asteroids
5104:
5103:
4562:on 5 January 1997
4481:978-0-521-76573-2
4418:978-3-540-00238-3
4360:978-0-674-99104-0
4339:978-0-201-47959-1
4315:978-0-521-80633-6
4292:978-0-201-54730-6
4261:978-0-521-82344-9
4115:(6954): 147–151.
3810:(11): 1595–1598.
3271:Petit et al. 1997
3247:Petit et al. 1997
3235:Petit et al. 1997
3223:Petit et al. 1997
3211:Petit et al. 1997
3066:Petit et al. 1997
3033:(Subscription or
2542:Petit et al. 1997
2417:Monet et al. 1994
2008:(6525): 785–788.
1988:Britt et al. 2002
1939:(Subscription or
1623:
1622:
1572:Satellite of
1312:moment of inertia
751:high-gain antenna
631:Moriz von Kuffner
531:
530:
432:0.3–1.1 cm/s
16:(Redirected from
5241:
5209:Binary asteroids
5169:
5168:
5167:
5157:
5156:
5155:
5145:
5144:
5143:
5133:
5132:
5121:
5120:
5119:
5112:
5066:
5059:
5052:
5043:
5025:Orbital elements
4989:
4911:
4909:
4907:
4887:
4885:
4883:
4863:
4861:
4859:
4843:
4841:
4839:
4833:
4814:
4804:
4802:
4800:
4794:
4775:
4765:
4763:
4761:
4755:
4749:. Archived from
4744:
4724:
4722:
4720:
4699:
4697:
4695:
4662:
4644:
4642:
4640:
4635:on 27 March 2012
4634:
4628:. Archived from
4615:
4605:
4588:
4571:
4569:
4567:
4546:
4544:
4542:
4500:
4498:
4496:
4490:
4484:. Archived from
4469:
4459:
4434:
4432:
4430:
4399:
4397:
4395:
4376:
4374:
4372:
4343:
4319:
4307:
4296:
4277:
4275:
4273:
4235:
4206:
4196:
4163:
4161:
4159:
4153:
4106:
4096:
4094:
4061:
4059:
4057:
4051:
4045:. Archived from
4020:
4010:
4000:
3971:
3969:
3952:(6): 2295–2298.
3936:
3934:
3917:(6): 2290–2294.
3901:
3880:
3878:
3876:
3870:
3864:. Archived from
3839:
3829:
3827:
3794:
3792:
3790:
3784:
3753:
3743:
3722:
3720:
3718:
3712:
3681:
3671:
3634:
3632:
3630:
3620:
3587:
3558:
3537:
3516:
3495:
3493:
3491:
3485:
3458:
3448:
3438:
3405:
3403:
3401:
3395:
3368:
3358:
3356:
3354:
3348:
3329:
3319:
3286:Journal articles
3274:
3268:
3262:
3256:
3250:
3244:
3238:
3232:
3226:
3220:
3214:
3208:
3202:
3201:
3199:
3197:
3182:
3176:
3170:
3161:
3155:
3146:
3135:
3129:
3123:
3114:
3109:
3100:
3094:
3085:
3080:
3069:
3063:
3052:
3045:
3039:
3038:
3030:
3018:
3011:
3005:
2999:
2993:
2987:
2981:
2975:
2962:
2956:
2950:
2944:
2935:
2929:
2923:
2907:
2901:
2895:
2886:
2880:
2874:
2868:
2862:
2856:
2847:
2841:
2835:
2829:
2823:
2818:
2809:
2803:
2797:
2796:, pp. 57–58
2791:
2785:
2780:
2771:
2765:
2759:
2754:
2748:
2742:
2733:
2727:
2716:
2710:
2701:
2695:
2686:
2680:
2674:
2668:
2662:
2656:
2650:
2644:
2638:
2633:
2622:
2616:
2605:
2599:
2588:
2582:
2569:
2563:
2557:
2551:
2545:
2539:
2533:
2527:
2508:
2502:
2491:
2486:
2471:
2465:
2444:
2438:
2432:
2426:
2420:
2414:
2408:
2402:
2393:
2387:
2378:
2372:
2345:
2339:
2333:
2321:
2315:
2309:
2303:
2297:
2288:
2282:
2276:
2270:
2264:
2258:
2245:
2239:
2233:
2227:
2221:
2215:
2209:
2198:
2192:
2186:
2180:
2174:
2163:
2158:
2145:
2139:
2133:
2127:
2121:
2115:
2109:
2103:
2090:
2084:
2071:
2065:
2054:
2049:
2034:
2033:
2022:10.1038/374785a0
1997:
1991:
1985:
1976:
1971:
1965:
1960:
1945:
1944:
1936:
1924:
1917:
1911:
1906:
1885:
1879:
1873:
1868:
1779:
1778:
1775:
1774:
1771:
1768:
1765:
1762:
1759:
1756:
1747:
1746:
1743:
1742:
1739:
1736:
1733:
1730:
1727:
1525:
1524:
1521:
1520:
1517:
1514:
1511:
1508:
1505:
1502:
1499:
1496:
1493:
1448:
1443:
1442:
1439:
1438:
1435:
1432:
1429:
1426:
1423:
1420:
1388:17 February 1994
1345:
1338:
1101:space weathering
1027:Surface features
992:
980:
941:space weathering
880:
868:
859:
857:
848:
843:
834:
829:
820:
815:
806:
801:
792:
787:
781:
772:
556:and named after
479:Geometric albedo
465:North pole
455:
450:North pole
274:
258:
244:
212:
211:
208:
207:
204:
201:
198:
195:
192:
146:
145:
142:
141:
138:
135:
132:
47:
40:
21:
5249:
5248:
5244:
5243:
5242:
5240:
5239:
5238:
5219:Galileo program
5179:
5178:
5175:
5165:
5163:
5153:
5151:
5141:
5139:
5127:
5117:
5115:
5107:
5105:
5100:
5075:
5070:
4962:Proper elements
4919:
4914:
4905:
4903:
4890:
4881:
4879:
4866:
4857:
4855:
4846:
4837:
4835:
4831:
4812:
4807:
4798:
4796:
4792:
4773:
4768:
4759:
4757:
4753:
4742:
4737:
4733:Wayback Machine
4718:
4716:
4715:on 24 June 2010
4702:
4693:
4691:
4665:
4647:
4638:
4636:
4632:
4613:
4608:
4591:
4574:
4565:
4563:
4549:
4540:
4538:
4512:
4508:
4503:
4494:
4492:
4491:on 4 March 2009
4488:
4482:
4467:
4462:
4437:
4428:
4426:
4419:
4402:
4393:
4391:
4379:
4370:
4368:
4361:
4346:
4340:
4322:
4316:
4299:
4293:
4280:
4271:
4269:
4262:
4247:
4243:
4238:
4209:
4166:
4157:
4155:
4151:
4104:
4099:
4064:
4055:
4053:
4052:on 12 June 2016
4049:
4018:
4013:
3998:10.1.1.693.8814
3974:
3939:
3904:
3883:
3874:
3872:
3871:on 12 June 2016
3868:
3837:
3832:
3797:
3788:
3786:
3782:
3751:
3746:
3725:
3716:
3714:
3710:
3679:
3674:
3637:
3628:
3626:
3590:
3561:
3540:
3519:
3498:
3489:
3487:
3483:
3456:
3451:
3408:
3399:
3397:
3393:
3366:
3361:
3352:
3350:
3346:
3327:
3322:
3292:
3288:
3283:
3278:
3277:
3269:
3265:
3257:
3253:
3245:
3241:
3233:
3229:
3221:
3217:
3209:
3205:
3195:
3193:
3184:
3183:
3179:
3171:
3164:
3156:
3149:
3136:
3132:
3124:
3117:
3110:
3103:
3095:
3088:
3081:
3072:
3064:
3055:
3046:
3042:
3032:
3013:
3012:
3008:
3000:
2996:
2988:
2984:
2976:
2965:
2957:
2953:
2945:
2938:
2930:
2926:
2908:
2904:
2896:
2889:
2881:
2877:
2869:
2865:
2857:
2850:
2842:
2838:
2830:
2826:
2819:
2812:
2804:
2800:
2792:
2788:
2781:
2774:
2766:
2762:
2755:
2751:
2743:
2736:
2730:Lee et al. 1996
2728:
2719:
2711:
2704:
2696:
2689:
2683:Lee et al. 1996
2681:
2677:
2669:
2665:
2657:
2653:
2647:Lee et al. 1996
2645:
2641:
2634:
2625:
2617:
2608:
2600:
2591:
2583:
2572:
2566:Lee et al. 1996
2564:
2560:
2552:
2548:
2540:
2536:
2528:
2511:
2503:
2494:
2487:
2474:
2466:
2447:
2439:
2435:
2427:
2423:
2415:
2411:
2403:
2396:
2388:
2381:
2373:
2348:
2340:
2336:
2322:
2318:
2310:
2306:
2298:
2291:
2283:
2279:
2271:
2267:
2259:
2248:
2240:
2236:
2228:
2224:
2216:
2212:
2199:
2195:
2187:
2183:
2175:
2166:
2159:
2148:
2140:
2136:
2128:
2124:
2116:
2112:
2104:
2093:
2085:
2074:
2066:
2057:
2050:
2037:
1999:
1998:
1994:
1986:
1979:
1972:
1968:
1961:
1948:
1938:
1919:
1918:
1914:
1907:
1888:
1880:
1876:
1869:
1862:
1857:
1840:
1831:
1786:
1753:
1749:
1724:
1720:
1708:and reflection
1694:
1654:
1629:
1602:
1553:
1541:
1539:Semi-major axis
1490:
1486:
1472:
1458:
1446:
1417:
1413:
1402:
1352:
1333:
1324:
1308:rotation period
1273:
1219:S-type asteroid
1215:
1207:Ejecta blankets
1155:
1139:Townsend Dorsum
1124:
1064:
1029:
1000:
999:
998:
997:
996:
993:
985:
984:
981:
970:
918:S-type asteroid
893:
888:
887:
886:
885:
884:
881:
873:
872:
869:
861:
860:
855:
854:
841:
840:
827:
826:
813:
812:
799:
798:
785:
784:
783:
779:
773:
699:
691:
670:David J. Tholen
635:Greek mythology
615:
562:S-type asteroid
520:
503:
481:
469:
456:
453:right ascension
451:
441:
429:
416:
393:
353:
341:
319:
307:
294:
272:
268:
266:Semi-major axis
256:
242:
189:
185:
167:
153:
129:
125:
114:
63:
35:
28:
23:
22:
18:Celmis (crater)
15:
12:
11:
5:
5247:
5245:
5237:
5236:
5231:
5226:
5221:
5216:
5211:
5206:
5201:
5196:
5191:
5181:
5180:
5174:
5173:
5161:
5149:
5137:
5125:
5102:
5101:
5099:
5098:
5093:
5086:
5084:242 Kriemhild
5080:
5077:
5076:
5071:
5069:
5068:
5061:
5054:
5046:
5038:
5037:
5036:
5035:
4993:Close approach
4974:
4973:
4972:
4926:
4918:
4917:External links
4915:
4913:
4912:
4888:
4864:
4844:
4805:
4766:
4735:
4700:
4663:
4645:
4606:
4589:
4572:
4547:
4515:"1993 (243) 1"
4509:
4507:
4504:
4502:
4501:
4480:
4460:
4435:
4417:
4400:
4377:
4359:
4344:
4338:
4324:Lewis, John S.
4320:
4314:
4297:
4291:
4278:
4260:
4244:
4242:
4239:
4237:
4236:
4218:(3): 355–416.
4207:
4179:(3): 479–483.
4164:
4097:
4062:
4029:(1): 119–139.
4011:
3983:(1): 177–197.
3972:
3967:10.1086/117037
3937:
3932:10.1086/117036
3902:
3881:
3830:
3795:
3762:(1): 106–118.
3744:
3723:
3690:(1): 140–157.
3672:
3646:(1–4): 23–78.
3635:
3588:
3570:(6): 699–725.
3559:
3538:
3517:
3496:
3449:
3406:
3359:
3320:
3289:
3287:
3284:
3282:
3279:
3276:
3275:
3263:
3251:
3239:
3227:
3215:
3203:
3192:on 1 July 2015
3177:
3162:
3147:
3130:
3115:
3101:
3086:
3070:
3053:
3040:
3006:
2994:
2992:, p. 1595
2982:
2963:
2951:
2936:
2924:
2902:
2887:
2875:
2863:
2848:
2836:
2824:
2810:
2798:
2786:
2772:
2760:
2749:
2747:, p. 1385
2734:
2717:
2702:
2687:
2675:
2663:
2651:
2639:
2623:
2606:
2589:
2570:
2558:
2546:
2534:
2509:
2492:
2472:
2445:
2433:
2421:
2419:, p. 2293
2409:
2394:
2379:
2346:
2334:
2326:, p. 215
2316:
2304:
2289:
2277:
2265:
2246:
2234:
2232:, p. 2295
2222:
2210:
2203:, p. 404
2193:
2181:
2164:
2146:
2134:
2122:
2110:
2091:
2072:
2055:
2035:
1992:
1977:
1966:
1946:
1912:
1886:
1874:
1859:
1858:
1856:
1853:
1852:
1851:
1846:
1839:
1836:
1830:
1829:Age and origin
1827:
1785:
1782:
1693:
1690:
1684:who inhabited
1653:
1650:
1646:prograde orbit
1625:Main article:
1621:
1620:
1617:
1616:
1613:
1607:
1606:
1603:
1598:
1595:
1594:
1593:1.6×1.4×1.2 km
1591:
1585:
1584:
1578:
1577:
1574:
1568:
1567:
1564:
1558:
1557:
1554:
1549:
1546:
1545:
1542:
1537:
1534:
1533:
1527:
1526:
1483:
1477:
1476:
1473:
1468:
1465:
1464:
1459:
1456:
1453:
1452:
1411:
1407:
1406:
1403:
1398:
1395:
1394:
1390:
1389:
1386:
1382:
1381:
1375:
1369:
1368:
1365:
1359:
1358:
1354:
1353:
1346:
1332:
1329:
1323:
1320:
1285:Koronis family
1272:
1269:
1214:
1211:
1195:prime meridian
1160:Koronis family
1154:
1151:
1123:
1120:
1063:
1060:
1028:
1025:
994:
987:
986:
982:
975:
974:
973:
972:
971:
969:
966:
902:NEAR Shoemaker
892:
889:
882:
875:
874:
870:
863:
862:
774:
767:
766:
765:
764:
763:
722:Space Shuttle
698:
692:
690:
687:
655:Koronis family
614:
611:
542:Koronis family
529:
528:
525:
524:
521:
513:
510:
509:
504:
499:
496:
495:
492:
486:
485:
482:
477:
474:
473:
470:
464:
461:
460:
457:
449:
446:
445:
442:
437:
434:
433:
430:
424:
421:
420:
417:
411:
408:
407:
404:
398:
397:
394:
389:
386:
385:
382:
376:
375:
369:
368:
365:
358:
357:
354:
349:
346:
345:
342:
337:
334:
333:
330:
324:
323:
320:
315:
312:
311:
308:
302:
299:
298:
295:
290:
287:
286:
283:
277:
276:
269:
264:
261:
260:
253:
247:
246:
239:
233:
232:
227:31 July 2016 (
221:
220:
214:
213:
184:Idean (Idæan)
182:
176:
175:
172:Koronis family
168:
163:
160:
159:
154:
151:
148:
147:
123:
119:
118:
115:
110:
107:
106:
102:
101:
98:
94:
93:
88:
82:
81:
76:
70:
69:
65:
64:
48:
26:
24:
14:
13:
10:
9:
6:
4:
3:
2:
5246:
5235:
5232:
5230:
5227:
5225:
5222:
5220:
5217:
5215:
5212:
5210:
5207:
5205:
5202:
5200:
5197:
5195:
5192:
5190:
5187:
5186:
5184:
5177:
5172:
5162:
5160:
5150:
5148:
5138:
5136:
5131:
5126:
5124:
5114:
5110:
5097:
5094:
5092:
5091:
5087:
5085:
5082:
5081:
5078:
5074:
5067:
5062:
5060:
5055:
5053:
5048:
5047:
5044:
5040:
5034:
5030:
5026:
5022:
5018:
5017:Orbit diagram
5014:
5010:
5006:
5002:
4998:
4994:
4991:
4988:
4984:
4983:
4978:
4975:
4971:
4967:
4963:
4959:
4955:
4951:
4947:
4943:
4939:
4936:
4935:
4934:
4930:
4927:
4924:
4921:
4920:
4916:
4901:
4897:
4893:
4889:
4877:
4873:
4869:
4865:
4853:
4849:
4845:
4830:
4826:
4822:
4819:: 1385–1386.
4818:
4811:
4806:
4791:
4787:
4783:
4779:
4772:
4767:
4752:
4748:
4741:
4736:
4734:
4730:
4727:
4714:
4710:
4706:
4701:
4689:
4685:
4681:
4677:
4673:
4669:
4664:
4660:
4656:
4652:
4646:
4631:
4627:
4623:
4619:
4612:
4607:
4603:
4599:
4595:
4590:
4586:
4582:
4578:
4573:
4561:
4557:
4553:
4548:
4536:
4532:
4528:
4524:
4520:
4516:
4511:
4510:
4505:
4487:
4483:
4477:
4473:
4466:
4461:
4457:
4453:
4449:
4445:
4441:
4436:
4424:
4420:
4414:
4410:
4406:
4401:
4389:
4385:
4384:
4378:
4366:
4362:
4356:
4352:
4351:
4345:
4341:
4335:
4331:
4330:
4325:
4321:
4317:
4311:
4306:
4305:
4298:
4294:
4288:
4284:
4279:
4267:
4263:
4257:
4253:
4252:
4246:
4245:
4240:
4233:
4229:
4225:
4221:
4217:
4213:
4208:
4204:
4200:
4195:
4190:
4186:
4182:
4178:
4174:
4170:
4165:
4150:
4146:
4142:
4138:
4134:
4130:
4126:
4122:
4118:
4114:
4110:
4103:
4098:
4093:
4088:
4084:
4080:
4076:
4072:
4068:
4063:
4048:
4044:
4040:
4036:
4032:
4028:
4024:
4017:
4012:
4008:
4004:
3999:
3994:
3990:
3986:
3982:
3978:
3973:
3968:
3963:
3959:
3955:
3951:
3947:
3943:
3938:
3933:
3928:
3924:
3920:
3916:
3912:
3908:
3903:
3899:
3895:
3891:
3887:
3882:
3867:
3863:
3859:
3855:
3851:
3848:(1): 87–105.
3847:
3843:
3836:
3831:
3826:
3821:
3817:
3813:
3809:
3805:
3801:
3796:
3781:
3777:
3773:
3769:
3765:
3761:
3757:
3750:
3745:
3741:
3737:
3733:
3729:
3724:
3709:
3705:
3701:
3697:
3693:
3689:
3685:
3678:
3673:
3669:
3665:
3661:
3657:
3653:
3649:
3645:
3641:
3636:
3624:
3619:
3614:
3610:
3606:
3602:
3598:
3594:
3589:
3585:
3581:
3577:
3573:
3569:
3565:
3560:
3556:
3552:
3548:
3544:
3539:
3535:
3531:
3527:
3523:
3518:
3514:
3510:
3506:
3502:
3497:
3482:
3478:
3474:
3470:
3466:
3462:
3461:Asteroids III
3455:
3450:
3446:
3442:
3437:
3432:
3428:
3424:
3420:
3416:
3412:
3407:
3392:
3388:
3384:
3380:
3376:
3372:
3371:Asteroids III
3365:
3360:
3345:
3341:
3337:
3333:
3332:Asteroids III
3326:
3321:
3317:
3313:
3309:
3305:
3301:
3297:
3291:
3290:
3285:
3280:
3273:, p. 182
3272:
3267:
3264:
3261:, p. 116
3260:
3255:
3252:
3249:, p. 193
3248:
3243:
3240:
3237:, p. 188
3236:
3231:
3228:
3225:, p. 195
3224:
3219:
3216:
3213:, p. 179
3212:
3207:
3204:
3191:
3187:
3181:
3178:
3175:, p. 455
3174:
3169:
3167:
3163:
3160:, p. 463
3159:
3154:
3152:
3148:
3144:
3139:
3134:
3131:
3127:
3126:Schmadel 2003
3122:
3120:
3116:
3113:
3108:
3106:
3102:
3099:, p. 108
3098:
3093:
3091:
3087:
3084:
3079:
3077:
3075:
3071:
3068:, p. 177
3067:
3062:
3060:
3058:
3054:
3050:
3044:
3041:
3036:
3028:
3024:
3023:
3017:
3010:
3007:
3004:, p. 878
3003:
2998:
2995:
2991:
2986:
2983:
2980:, p. 117
2979:
2974:
2972:
2970:
2968:
2964:
2961:, p. 134
2960:
2955:
2952:
2949:, p. 135
2948:
2943:
2941:
2937:
2933:
2928:
2925:
2921:
2919:
2912:, p. 89
2911:
2906:
2903:
2900:, p. 480
2899:
2894:
2892:
2888:
2885:, p. 155
2884:
2879:
2876:
2873:, p. 128
2872:
2867:
2864:
2861:, p. 124
2860:
2855:
2853:
2849:
2845:
2840:
2837:
2834:, p. 393
2833:
2828:
2825:
2822:
2817:
2815:
2811:
2807:
2802:
2799:
2795:
2790:
2787:
2784:
2779:
2777:
2773:
2770:, p. 131
2769:
2764:
2761:
2758:
2753:
2750:
2746:
2741:
2739:
2735:
2731:
2726:
2724:
2722:
2718:
2715:, p. 132
2714:
2709:
2707:
2703:
2700:, p. 141
2699:
2694:
2692:
2688:
2684:
2679:
2676:
2673:, p. 701
2672:
2667:
2664:
2661:, p. 470
2660:
2655:
2652:
2648:
2643:
2640:
2637:
2632:
2630:
2628:
2624:
2620:
2615:
2613:
2611:
2607:
2604:, p. 363
2603:
2598:
2596:
2594:
2590:
2586:
2581:
2579:
2577:
2575:
2571:
2567:
2562:
2559:
2556:, p. 142
2555:
2550:
2547:
2543:
2538:
2535:
2532:, p. 496
2531:
2526:
2524:
2522:
2520:
2518:
2516:
2514:
2510:
2507:, p. 710
2506:
2501:
2499:
2497:
2493:
2490:
2485:
2483:
2481:
2479:
2477:
2473:
2470:, p. 709
2469:
2464:
2462:
2460:
2458:
2456:
2454:
2452:
2450:
2446:
2443:, p. 238
2442:
2437:
2434:
2430:
2425:
2422:
2418:
2413:
2410:
2407:, p. 469
2406:
2401:
2399:
2395:
2392:, p. 237
2391:
2386:
2384:
2380:
2377:, p. 707
2376:
2371:
2369:
2367:
2365:
2363:
2361:
2359:
2357:
2355:
2353:
2351:
2347:
2344:, p. 358
2343:
2338:
2335:
2331:
2325:
2320:
2317:
2314:, p. 120
2313:
2308:
2305:
2301:
2296:
2294:
2290:
2286:
2281:
2278:
2274:
2269:
2266:
2263:, p. 699
2262:
2257:
2255:
2253:
2251:
2247:
2243:
2238:
2235:
2231:
2226:
2223:
2220:, p. 410
2219:
2214:
2211:
2207:
2202:
2197:
2194:
2190:
2185:
2182:
2179:, p. 700
2178:
2173:
2171:
2169:
2165:
2162:
2157:
2155:
2153:
2151:
2147:
2144:, p. 241
2143:
2138:
2135:
2131:
2130:Schmadel 2003
2126:
2123:
2120:, p. 206
2119:
2114:
2111:
2108:, p. 479
2107:
2102:
2100:
2098:
2096:
2092:
2088:
2083:
2081:
2079:
2077:
2073:
2070:, p. 147
2069:
2064:
2062:
2060:
2056:
2053:
2048:
2046:
2044:
2042:
2040:
2036:
2031:
2027:
2023:
2019:
2015:
2011:
2007:
2003:
1996:
1993:
1990:, p. 486
1989:
1984:
1982:
1978:
1975:
1970:
1967:
1964:
1959:
1957:
1955:
1953:
1951:
1947:
1942:
1934:
1930:
1929:
1923:
1916:
1913:
1910:
1905:
1903:
1901:
1899:
1897:
1895:
1893:
1891:
1887:
1884:
1878:
1875:
1872:
1867:
1865:
1861:
1854:
1850:
1847:
1845:
1842:
1841:
1837:
1835:
1828:
1826:
1822:
1820:
1816:
1811:
1807:
1803:
1799:
1790:
1783:
1781:
1777:
1745:
1717:
1715:
1711:
1707:
1702:
1700:
1691:
1689:
1687:
1683:
1679:
1675:
1670:
1668:
1663:
1659:
1651:
1649:
1647:
1642:
1638:
1634:
1628:
1627:Dactyl (moon)
1618:
1614:
1612:
1608:
1604:
1601:
1596:
1592:
1590:
1586:
1583:
1579:
1575:
1573:
1569:
1565:
1563:
1559:
1555:
1552:
1547:
1543:
1540:
1535:
1532:
1528:
1523:
1484:
1482:
1478:
1474:
1471:
1466:
1463:
1460:
1454:
1451:
1450:
1441:
1412:
1410:Pronunciation
1408:
1404:
1401:
1396:
1391:
1387:
1383:
1379:
1376:
1374:
1370:
1366:
1364:
1360:
1355:
1350:
1344:
1339:
1330:
1328:
1321:
1319:
1317:
1313:
1309:
1305:
1300:
1298:
1294:
1290:
1289:asteroid-belt
1286:
1277:
1270:
1268:
1266:
1265:
1259:
1257:
1252:
1248:
1244:
1240:
1236:
1232:
1228:
1224:
1220:
1212:
1210:
1208:
1204:
1198:
1196:
1191:
1187:
1186:
1181:
1177:
1168:
1164:
1161:
1152:
1150:
1146:
1144:
1140:
1135:
1133:
1129:
1121:
1119:
1112:
1108:
1104:
1102:
1098:
1094:
1090:
1085:
1083:
1079:
1075:
1074:impact events
1071:
1070:
1061:
1059:
1057:
1056:
1055:ejecta blocks
1051:
1046:
1038:
1033:
1026:
1024:
1022:
1018:
1012:
1010:
1005:
991:
979:
967:
965:
963:
954:
949:
945:
942:
937:
935:
931:
927:
923:
919:
914:
912:
908:
904:
903:
898:
890:
879:
867:
858: 243 Ida
852:
847:
838:
833:
824:
819:
810:
805:
796:
791:
778:
775:Animation of
771:
762:
760:
756:
752:
747:
744:
740:
738:
734:
730:
726:
725:
719:
714:
710:
709:
704:
696:
693:
688:
686:
684:
680:
676:
671:
667:
662:
660:
656:
652:
648:
644:
640:
636:
632:
628:
624:
620:
619:Johann Palisa
612:
610:
608:
603:
599:
594:
592:
588:
583:
580:
575:
573:
569:
568:
563:
559:
555:
551:
550:Johann Palisa
547:
546:asteroid belt
543:
539:
535:
526:
522:
519:
518:
511:
508:
505:
502:
501:Spectral type
497:
493:
491:
487:
483:
480:
475:
471:
468:
462:
458:
454:
447:
443:
440:
435:
431:
428:
422:
418:
415:
409:
405:
403:
399:
395:
392:
387:
383:
381:
377:
374:
370:
366:
364:
359:
355:
352:
347:
343:
340:
335:
331:
329:
325:
321:
318:
313:
309:
306:
305:orbital speed
300:
296:
293:
288:
284:
282:
278:
270:
267:
262:
254:
252:
248:
240:
238:
234:
230:
226:
222:
219:
215:
210:
183:
181:
177:
173:
169:
166:
161:
158:
155:
149:
144:
124:
122:Pronunciation
120:
116:
113:
108:
103:
99:
95:
92:
89:
87:
83:
80:
79:Johann Palisa
77:
75:
71:
66:
61:
57:
53:
52:
46:
41:
33:
19:
5176:
5171:Solar System
5088:
5039:
5028:
5020:
5012:
5004:
4996:
4980:
4965:
4957:
4954:Orbital info
4949:
4941:
4932:
4904:. Retrieved
4880:. Retrieved
4876:the original
4856:. Retrieved
4836:. Retrieved
4816:
4797:. Retrieved
4777:
4758:. Retrieved
4751:the original
4746:
4717:. Retrieved
4713:the original
4708:
4692:. Retrieved
4675:
4672:IAU Circular
4671:
4650:
4637:. Retrieved
4630:the original
4618:Science News
4617:
4594:Science News
4593:
4576:
4564:. Retrieved
4560:the original
4555:
4539:. Retrieved
4522:
4519:IAU Circular
4518:
4493:. Retrieved
4486:the original
4471:
4448:1721.1/11867
4439:
4427:. Retrieved
4408:
4392:. Retrieved
4382:
4369:. Retrieved
4349:
4328:
4303:
4282:
4270:. Retrieved
4250:
4215:
4211:
4176:
4172:
4156:. Retrieved
4112:
4108:
4077:(1): 20–32.
4074:
4070:
4054:. Retrieved
4047:the original
4026:
4022:
3980:
3976:
3949:
3945:
3914:
3910:
3889:
3885:
3873:. Retrieved
3866:the original
3845:
3841:
3807:
3803:
3787:. Retrieved
3759:
3755:
3731:
3727:
3715:. Retrieved
3687:
3683:
3643:
3639:
3627:. Retrieved
3603:(1): 77–86.
3600:
3596:
3567:
3563:
3546:
3542:
3525:
3521:
3504:
3500:
3488:. Retrieved
3460:
3418:
3414:
3398:. Retrieved
3370:
3351:. Retrieved
3331:
3299:
3295:
3266:
3254:
3242:
3230:
3218:
3206:
3194:. Retrieved
3190:the original
3180:
3141:
3133:
3128:, p. 37
3048:
3043:
3020:
3009:
2997:
2985:
2954:
2934:, p. 21
2927:
2914:
2905:
2878:
2866:
2839:
2827:
2806:Chapman 1996
2801:
2789:
2763:
2752:
2732:, p. 97
2685:, p. 90
2678:
2671:Chapman 1996
2666:
2654:
2649:, p. 96
2642:
2621:, p. 10
2602:Chapman 1994
2587:, p. 58
2568:, p. 99
2561:
2549:
2537:
2530:Chapman 1995
2505:Chapman 1996
2468:Chapman 1996
2436:
2431:, p. 57
2424:
2412:
2375:Chapman 1996
2342:Chapman 1994
2337:
2328:
2319:
2307:
2302:, p. 36
2287:, p. 72
2280:
2275:, p. 24
2268:
2261:Chapman 1996
2244:, p. 26
2237:
2225:
2213:
2205:
2196:
2184:
2177:Chapman 1996
2137:
2132:, p. 36
2125:
2118:Ridpath 1897
2113:
2005:
2001:
1995:
1969:
1926:
1915:
1882:
1877:
1832:
1823:
1814:
1797:
1795:
1718:
1703:
1695:
1671:
1666:
1661:
1657:
1655:
1640:
1636:
1630:
1475:1993 (243) 1
1393:Designations
1377:
1348:
1325:
1301:
1282:
1264:megaregolith
1262:
1260:
1250:
1246:
1227:bulk density
1216:
1199:
1183:
1173:
1156:
1147:
1143:Vienna Regio
1142:
1138:
1136:
1131:
1127:
1125:
1116:
1110:
1086:
1077:
1067:
1065:
1053:
1042:
1036:
1020:
1013:
1001:
961:
958:
938:
925:
915:
900:
896:
894:
850:
836:
822:
808:
794:
789:
776:
748:
742:
741:
732:
723:
717:
706:
700:
694:
682:
663:
616:
601:
597:
595:
586:
584:
576:
565:
533:
532:
516:
396:15.7 km
317:Mean anomaly
281:Eccentricity
105:Designations
49:
5159:Outer space
5147:Spaceflight
4838:29 November
4678:(6082): 2.
4653:: 469–470.
4579:: 237–238.
4525:(5948): 2.
4495:29 November
4371:28 February
3564:Meteoritics
3543:Meteoritics
3522:Meteoritics
3507:: 357–365.
3463:: 485–500.
3421:(1): 1–19.
3334:: 463–484.
2959:Slivan 1995
2846:, p. 9
2745:Stooke 1997
2142:Berger 2003
1800:was in the
1748:and Celmis
1611:Temperature
1605:synchronous
1562:Inclination
1457:Named after
1258:of 11–42%.
1213:Composition
1185:Blue Grotto
891:Discoveries
689:Exploration
490:Temperature
467:declination
425:Equatorial
391:Mean radius
328:Inclination
170:Main belt (
152:Named after
5183:Categories
4882:4 December
4858:24 October
4799:22 October
4760:23 October
4719:23 October
4566:23 October
4429:23 October
4158:23 October
4056:27 October
3892:(3): 108.
3875:27 October
3789:23 October
3629:27 October
3549:(5): 496.
3490:27 October
3400:23 October
3281:References
3112:Green 1994
3097:Mason 1994
3037:required.)
2910:Lewis 1996
2636:Cowen 1995
2324:Cowen 1993
1943:required.)
1810:pericenter
1699:spheroidal
1674:designated
1631:Ida has a
1589:Dimensions
1485:Dactylian
1481:Adjectives
1380:spacecraft
1176:lava tubes
1122:Structures
934:stony-iron
846:951 Gaspra
737:propellant
380:Dimensions
363:satellites
275:10 m)
259:10 m)
251:Perihelion
245:10 m)
231:2457600.5)
180:Adjectives
56:Pola Regio
5123:Astronomy
5009:Ephemeris
5001:Discovery
4938:Ephemeris
4626:0036-8423
4602:0036-8423
4203:129231326
3993:CiteSeerX
3734:: 57–67.
3668:122388506
3353:4 January
3302:(3): 46.
2161:NASA 2005
1909:Holm 1994
1871:Raab 2002
1686:Mount Ida
1652:Discovery
1367:Ann Harch
1357:Discovery
1316:precesses
1091:minerals
955:meteorite
932:(OC) and
743:Galileo's
733:Galileo's
310:0.2036°/d
117:(243) Ida
68:Discovery
5096:244 Sita
4906:15 April
4900:Archived
4852:Archived
4829:Archived
4790:Archived
4780:: 1381.
4729:Archived
4688:Archived
4639:26 March
4535:Archived
4456:32907677
4423:Archived
4388:Archived
4365:Archived
4326:(1996).
4266:Archived
4149:Archived
4137:12968171
3780:Archived
3717:26 March
3708:Archived
3623:Archived
3481:Archived
3445:51885221
3391:Archived
3373:: 3–15.
3344:Archived
3016:"dactyl"
2918:troilite
1963:JPL 2008
1838:See also
1806:prograde
1714:regolith
1256:porosity
1243:feldspar
1235:pyroxene
1132:region 2
1128:region 1
1097:pyroxene
1089:silicate
1069:regolith
1062:Regolith
1050:regolith
1045:cratered
727:mission
724:Atlantis
677:and the
538:asteroid
356:110.961°
344:324.016°
303:Average
237:Aphelion
5109:Portals
5090:243 Ida
4979:at the
4977:243 Ida
4929:243 Ida
4821:Bibcode
4782:Bibcode
4726:Alt URL
4680:Bibcode
4655:Bibcode
4581:Bibcode
4527:Bibcode
4220:Bibcode
4181:Bibcode
4145:4367378
4117:Bibcode
4079:Bibcode
4031:Bibcode
3985:Bibcode
3954:Bibcode
3919:Bibcode
3894:Bibcode
3850:Bibcode
3812:Bibcode
3764:Bibcode
3736:Bibcode
3692:Bibcode
3648:Bibcode
3605:Bibcode
3572:Bibcode
3551:Bibcode
3530:Bibcode
3528:: 455.
3509:Bibcode
3465:Bibcode
3423:Bibcode
3375:Bibcode
3336:Bibcode
3304:Bibcode
3196:18 July
3051:, p. 42
2030:4333634
2010:Bibcode
1922:"Idæan"
1815:Galileo
1798:Galileo
1710:spectra
1706:albedos
1682:dactyls
1667:Galileo
1662:Galileo
1658:Galileo
1641:Galileo
1462:Dactyls
1378:Galileo
1349:Galileo
1306:with a
1297:Jupiter
1251:Galileo
1247:Galileo
1231:olivine
1153:Craters
1111:Galileo
1093:olivine
1078:Galileo
1037:Galileo
1021:Galileo
962:Galileo
926:Galileo
907:geology
897:Galileo
830:
804:Jupiter
790:Galileo
777:Galileo
718:Galileo
708:Galileo
703:Jupiter
695:Galileo
683:Galileo
621:at the
602:Galileo
598:Galileo
591:Dactyls
587:Galileo
572:Jupiter
567:Galileo
544:of the
540:in the
534:243 Ida
472:−87.12°
459:168.76°
414:density
322:38.707°
51:Galileo
5029:·
5027:
5021:·
5019:
5013:·
5011:
5005:·
5003:
4997:·
4995:
4966:·
4964:
4958:·
4956:
4950:·
4948:
4942:·
4940:
4694:5 July
4624:
4600:
4541:5 July
4478:
4454:
4415:
4394:3 June
4357:
4336:
4312:
4289:
4272:3 June
4258:
4212:Icarus
4201:
4143:
4135:
4109:Nature
4071:Icarus
4023:Icarus
3995:
3977:Icarus
3842:Icarus
3756:Icarus
3684:Icarus
3666:
3597:Icarus
3443:
3415:Icarus
2028:
2002:Nature
1566:ca. 8°
1336:Dactyl
1331:Dactyl
1322:Origin
1241:, and
1203:ejecta
1190:albedo
1017:debris
1009:escape
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664:Ida's
641:was a
536:is an
484:0.2383
367:Dactyl
361:Known
332:1.132°
285:0.0411
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5135:Stars
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5007:
4999:
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4908:2009
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4696:2011
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4641:2009
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4452:OCLC
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3402:2008
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3198:2015
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