759:
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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.
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1012:. 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.
582:, 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
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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
948:
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
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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
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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
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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
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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
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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
925:. 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
1653:
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
4637:
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".
1801:
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
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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
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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
1769:, 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
3282:
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".
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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
1256:. 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
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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
661:
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
1303:
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
1637:. 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.
735:
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.
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1989:
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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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".
1177:. 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
3822:
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
1214:(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
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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
949:
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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728:. 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).
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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.
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Chapman, Clark R.; Ryan, Eileen V.; Merline, William J.; Neukum, Gerhard; Wagner, Roland; Thomas, Peter C.; Veverka, Joseph; Sullivan, Robert J. (March 1996).
4237:
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).
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Geissler, Paul E.; Petit, Jean-Marc; Greenberg, Richard (1996). "Ejecta Reaccretion on Rapidly Rotating Asteroids: Implications for 243 Ida and 433 Eros".
4003:
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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Greenberg, Richard; Bottke, William F.; Nolan, Michael; Geissler, Paul E.; Petit, Jean-Marc; Durda, Daniel D.; Asphaug, Erik; Head, James (March 1996).
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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.
4778:
750:. 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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exposed parts of the surface resembled that of OC meteorites, but the older regions matched the spectra of S-type asteroids.
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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.
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The Standard American Encyclopedia of Arts, Sciences, History, Biography, Geography, Statistics, and General Knowledge
2909:). 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.
670:. These improved the measurement of Ida's orbit around the Sun and reduced the uncertainty of its position during the
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4856:
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Chapman, Clark R. (September 1995). "Galileo Observations of Gaspra, Ida, and Dactyl: Implications for Meteoritics".
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1123:, 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
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Several major structures mark Ida's surface. The asteroid appears to be split into two halves, here referred to as
62:
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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 ...
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898:. Ida's relatively large surface exhibited a diverse range of geological features. The discovery of Ida's moon
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asteroids. Ida orbits the Sun at an average distance of 2.862 AU (428.1 Gm), between the orbits of
1041:, loose debris that obscures the solid rock beneath. The largest, boulder-sized, debris fragments are called
5192:
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flybys, but was interpreted to be either of two minerals found in meteorites that had fallen to the Earth:
1092:. Because of this process, older regolith appears more red in color compared to freshly exposed material.
5061:
553:, the most numerous type in the inner asteroid belt. On 28 August 1993, Ida was visited by the uncrewed
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Region 1 of Ida contains two major structures. One is a prominent 40 km (25 mi) ridge named
563:. It was the second asteroid visited by a spacecraft and the first found to have a natural satellite.
5197:
3010:
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filling the gap between them. However, no such debris was seen in high-resolution images captured by
902:, 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
650:, who proposed in 1918 that the group comprised the remnants of a destroyed precursor body.
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742:. 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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2014:
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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
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Byrnes, Dennis V.; D'Amario, Louis A.; Galileo Navigation Team (December 1994).
3789:"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
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trajectory to approach Ida required that it consume 34 kg (75 lb) of
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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
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4463:. Cambridge Planetary Science. Vol. 11. Cambridge University Press.
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3400:"Galileo's Encounter with 243 Ida: An Overview of the Imaging Experiment"
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4600:"Idiosyncrasies of Ida—asteroid 243 Ida's irregular gravitational field"
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Chapman, Clark R. (1994). "The Galileo Encounters with Gaspra and Ida".
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4342:. Translated by Jones, W. H. S.; Omerod, H. A. Loeb Classical Library.
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1972:
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1238:. The mineral content appears to be homogeneous throughout its extent.
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3931:"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
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Mining the Sky: Untold Riches from the Asteroids, Comets, and Planets
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4694:"Discovery of Ida's Moon Indicates Possible "Families" of Asteroids"
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1967:
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4729:"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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2629:
2548:
2423:
2369:
2045:
936:
1285:
1219:
1081:
895:
792:
691:
560:
402:
4636:
4002:
2935:
2859:
2847:
2756:
2701:
2647:
2569:
2567:
2565:
2563:
2393:
2300:
2284:
2282:
2171:
2036:
2034:
2032:
2030:
2028:
1065:
and redistributed across Ida's surface by geological processes.
1020:
991:
Ida's mass is between 3.65 and 4.99 × 10 kg. Its
537:. It was discovered on 29 September 1884 by Austrian astronomer
1694:
1191:
1178:
1005:
866:
717:
606:
Ida was discovered on 29 September 1884 by Austrian astronomer
598:
meteorites, the most common type found on the Earth's surface.
33:
3579:
1268:
Orbit and positions of Ida and five planets as of 9 March 2009
860:
Trajectory of Galileo from launch to Jupiter orbital insertion
188:
4394:"Catalogue of Minor Planet Names and Discovery Circumstances"
3440:
3353:"An Overview of the Asteroids: The Asteroids III Perspective"
2560:
2411:
2279:
2267:
2255:
2224:
2025:
1976:
1798:
1168:
820:
806:
747:
635:
631:
627:
4640:
Abstracts of the 25th Lunar and Planetary Science Conference
4566:
Abstracts of the 25th Lunar and Planetary Science Conference
4091:"The vector alignments of asteroid spins by thermal torques"
3896:"Astrometry for the Galileo mission. 1: Asteroid encounters"
3735:
3350:
3247:
2966:
2832:
2607:
2399:
2200:
1264:
1088:. Its appearance changes over time through a process called
4860:
3821:
3663:
3508:
3161:
3142:
3140:
2871:
2718:
2686:
2671:
2635:
2554:
2542:
1749:
1726:
1504:
1501:
1281:
1227:
639:
567:
390:
191:
179:
128:
122:
5118:
4563:
4156:
Wilson, Lionel; Keil, Klaus; Love, Stanley J. (May 1999).
4088:
4053:
3963:
3259:
3235:
3223:
3211:
3199:
3054:
2530:
2429:
2378:
2056:
2040:
1708:
The two largest imaged craters on Dactyl were named Acmon
1331:
1102:
image of a 150 m (490 ft) block at 24.8°S, 2.8°E
2972:
2882:
2880:
2473:
2471:
2469:
2467:
2465:
2090:
2088:
2086:
2084:
1988:
1758:
1717:
1495:
1483:
1422:
1413:
3666:"Erosion and Ejecta Reaccretion on 243 Ida and Its Moon"
3312:
Asphaug, Erik; Ryan, Eileen V.; Zuber, Maria T. (2003).
3137:
1299:
of 4.63 hours (roughly 5 hours). The calculated maximum
894:
asteroid mission, permitted the first study of asteroid
2739:
19:
This article is about an asteroid. For other uses, see
3714:
3626:
2877:
2782:
2573:
2462:
2417:
2288:
2273:
2261:
2230:
2081:
1047:, several of which have been observed on the surface.
913:. The composition of S-types was uncertain before the
549:. Later telescopic observations categorized Ida as an
5095:
4452:
Thomas, Peter C.; Prockter, Louise M. (28 May 2004).
2984:
2914:
2814:
2767:
2765:
2319:
minutes before Galileo's closest approach on Aug. 28.
1761:
1746:
1729:
1720:
1507:
1486:
1434:
1416:
771:
trajectory from 19 October 1989 to 30 September 2003
194:
4502:
Belton, Michael J. S.; Carlson, R. (12 March 1994).
4198:
4158:"The internal structures and densities of asteroids"
3067:
3065:
3063:
2212:
2206:
2189:
2177:
1823:
100 million years ago, which reduced its size.
1752:
1498:
1492:
1480:
1425:
1419:
1410:
185:
125:
4757:
3893:
3787:Hurford, Terry A.; Greenberg, Richard (June 2000).
3167:
2788:
2745:
2405:
2359:
1755:
1743:
1723:
1714:
1693:Dactyl shares many characteristics with Ida. Their
1489:
1407:
1336:Highest-resolution image of Dactyl, recorded while
182:
119:
4767:33rd Annual Lunar and Planetary Science Conference
4538:
4290:
3110:
3108:
3003:
2762:
2729:
2727:
2586:
2584:
2582:
2514:
2512:
2510:
2508:
2506:
2504:
2502:
2489:
2487:
2485:
2477:
2452:
2450:
2448:
2446:
2444:
2442:
2440:
2438:
2357:
2355:
2353:
2351:
2349:
2347:
2345:
2343:
2341:
2339:
2245:
2243:
2241:
2239:
2161:
2159:
2157:
1909:
1785:Dactyl's orbit around Ida is not precisely known.
928:The Galileo images also led to the discovery that
4431:(Thesis). Massachusetts Institute of Technology.
3824:"Ejecta Blocks on 243 Ida and on Other Asteroids"
3060:
1833:List of geological features on 243 Ida and Dactyl
1288:. Ida takes 4.84089 years to complete one orbit.
657:was measured on 16 September 1980 by astronomers
5169:
3786:
3311:
3146:
3081:
3079:
3002:
2978:
2843:
2841:
1781:Diagram of potential orbits of Dactyl around Ida
746:of the asteroid at a resolution of 31–38 m/
674:flyby from 78 to 60 km (48 to 37 mi).
4429:Spin-Axis Alignment of Koronis Family Asteroids
3875:Journal of the British Astronomical Association
3105:
2724:
2653:
2579:
2499:
2482:
2435:
2336:
2324:
2236:
2154:
2112:
2100:
2071:
2069:
2067:
2065:
1908:
1234:. Olivine and pyroxene were detected on Ida by
622:, a Viennese brewer and amateur astronomer. In
4541:"Solving for Dactyl's Orbit and Ida's Density"
4451:
4155:
3873:Mason, John W. (June 1994). "Ida's new moon".
2941:
2920:
2886:
2771:
2124:
2094:
1872:A Practical Dictionary of the English Language
1163:Ida's major craters are named after caves and
614:. It was his 45th asteroid discovery. Ida was
5046:
4861:National Aeronautics and Space Administration
4839:. Jet Propulsion Laboratory. 25 August 2008.
4501:
4297:. Cambridge, UK: Cambridge University Press.
4288:
4270:Carroll, Bradley W.; Ostlie, Dale A. (1996).
4269:
4243:. Cambridge, UK: Cambridge University Press.
3929:Owen, W. M. Jr.; Yeomans, D. K. (June 1994).
3397:
3076:
3071:
2990:
2838:
2820:
2306:
1962:
1680:
601:
4692:Holm, Jeanne (June 1994). Jones, Jan (ed.).
4289:Greeley, Ronald; Batson, Raymond M. (2001).
3717:Completing the Inventory of the Solar System
3120:
3096:
3094:
2892:
2620:
2618:
2616:
2062:
1028:3.5 minutes before its closest approach
5060:
4758:Sárneczky, K; Kereszturi, Á. (March 2002).
4609:. Vol. 147, no. 15. p. 207.
4585:. Vol. 144, no. 14. p. 215.
3928:
3443:"Asteroid Density, Porosity, and Structure"
3285:Celestial Mechanics and Dynamical Astronomy
2218:
2145:
2143:
2141:
2139:
1628:. It was discovered in images taken by the
956:
5053:
5039:
4974:
4881:"Gazetteer of Planetary Nomenclature: Ida"
4837:"JPL Small-Body Database Browser: 243 Ida"
4400:. IAU commission. Vol. 20. Springer.
4335:
4293:The Compact NASA Atlas of the Solar System
4240:Business and Politics in Europe, 1900–1970
3738:"Collisional and Dynamical History of Ida"
3126:
1893:
1891:
1889:
1887:
1885:
1883:
1881:
1879:
1855:
1853:
1340:was about 3,900 km away from the moon
1330:
32:
4736:Meeting on Asteroids and Comets in Europe
4655:Green, Daniel W. E. (26 September 1994).
4181:
4079:
3985:
3954:
3919:
3812:
3605:
3423:
3091:
2613:
1982:
1956:
1947:
1945:
1943:
1941:
1939:
4391:
3114:
2136:
2118:
2057:Vokrouhlicky, Nesvorny & Bottke 2003
1776:
1645:Dactyl was found on 17 February 1994 by
1263:
1154:
1094:
1019:
935:
888:flybys of Gaspra and Ida, and the later
642:. Ida was recognized as a member of the
5223:Astronomical objects discovered in 1884
5178:Minor planet object articles (numbered)
4914:, Robert Johnston, johnstonsarchive.net
4799:"Reflections on the Geology of 243 Ida"
4368:
3550:
3529:
3487:
3038:"The Argonautica" of Apollonius Rhodius
2805:
2803:
2794:
2659:
2590:
2518:
2493:
2456:
2363:
2330:
2249:
2165:
2106:
1876:
1850:
5170:
4891:from the original on 23 September 2006
4857:"Images of Asteroids Ida & Dactyl"
4796:
4426:
4272:An Introduction to Modern Astrophysics
4236:
3475:from the original on 17 September 2003
2947:
2733:
2130:
1936:
1604:200 K (−73 °C; −100 °F)
5034:
4657:"1993 (243) 1 = (243) Ida I (Dactyl)"
4654:
4597:
4580:
4427:Slivan, Stephen Michael (June 1995).
4356:from the original on 18 November 2019
4311:
4274:. Addison-Wesley Publishing Company.
3872:
3100:
3085:
2898:
2624:
2312:
1259:
566:Ida's orbit lies between the planets
328:Longitude of ascending node
4855:
4784:from the original on 26 January 2005
4726:
4691:
4679:from the original on 1 February 2019
4526:from the original on 1 February 2019
3024:participating institution membership
2800:
2783:Geissler, Petit & Greenberg 1996
2574:Geissler, Petit & Greenberg 1996
2418:Geissler, Petit & Greenberg 1996
2149:
2076:Archinal, Acton, A'Hearn et al. 2018
1930:participating institution membership
1897:
1859:
5203:Minor planets visited by spacecraft
4835:
4162:Meteoritics & Planetary Science
3338:from the original on 30 August 2021
3274:
1951:
1624:named Dactyl, official designation
1015:
984:Successive images of a rotating Ida
13:
4843:from the original on 7 August 2011
4806:Lunar and Planetary Science XXVIII
4760:"'Global' Tectonism on Asteroids?"
4183:10.1111/j.1945-5100.1999.tb01355.x
3702:from the original on 20 March 2009
3573:10.1111/j.1945-5100.1996.tb02107.x
2207:Zellner, Tholen & Tedesco 1985
2190:Zellner, Tholen & Tedesco 1985
2178:Zellner, Tholen & Tedesco 1985
1665:1993 (243) 1. It was named by the
1076:Ida's regolith is composed of the
700:. Its encounters of the asteroids
14:
5234:
4905:
4823:from the original on 4 March 2009
4414:from the original on 15 June 2024
4379:from the original on 15 June 2024
4257:from the original on 15 June 2024
3614:from the original on 11 June 2019
3385:from the original on 11 June 2019
1817:
664:US Naval Observatory in Flagstaff
5153:
5141:
5129:
5117:
5105:
4922:AstDyS-2, Asteroids—Dynamic Site
4879:
4863:. 23 August 2005. Archived from
4398:Dictionary of minor planet names
4143:from the original on 11 May 2008
3774:from the original on 5 June 2019
2809:
2289:D'Amario, Bright & Wolf 1992
2274:D'Amario, Bright & Wolf 1992
2262:D'Amario, Bright & Wolf 1992
2231:D'Amario, Bright & Wolf 1992
1739:
1710:
1667:International Astronomical Union
1476:
1403:
977:
965:
865:
853:
757:
682:
175:
115:
4887:Astrogeology Research Program.
4885:United States Geological Survey
4321:. Reading, MA: Addison-Wesley.
3030:
2996:
2865:
2853:
2826:
2776:
2746:Sárneczky & Kereszturi 2002
2183:
709:was launched into orbit by the
690:Ida was visited in 1993 by the
286:1,767.644 days (4.83955 a)
3147:Asphaug, Ryan & Zuber 2003
1902:
1864:
1669:in 1994, for the mythological
1201:
1032:Ida's surface appears heavily
879:
677:
1:
3269:
1138:a set opposite Vienna Regio.
1110:
1024:Mosaic of images recorded by
720:on 18 October 1989. Changing
559:spacecraft while en route to
5188:Discoveries by Johann Palisa
4369:Ridpath, John Clark (1897).
4221:10.1016/0019-1035(85)90133-2
3793:Geophysical Research Letters
2979:Hurford & Greenberg 2000
2887:Wilson, Keil & Love 1999
2095:Wilson, Keil & Love 1999
1640:
1069:observed evidence of recent
547:a nymph from Greek mythology
7:
4598:Cowen, Ron (1 April 1995).
4454:"Tectonics of Small Bodies"
4375:. Encyclopedia Publishing.
1826:
1658:made its closest approach.
1071:downslope regolith movement
1050:
884:The data returned from the
340:Argument of perihelion
48:
10:
5239:
4392:Schmadel, Lutz D. (2003).
3490:Asteroids, Comets, Meteors
2921:Thomas & Prockter 2004
2772:Thomas & Prockter 2004
2478:Byrnes & D'Amario 1994
1613:
1533:90 km at time of discovery
1141:
911:spectroscopic measurements
602:Discovery and observations
373:59.8 × 25.4 × 18.6 km
154:Minor planet category
18:
5213:S-type asteroids (Tholen)
5068:
4912:Asteroids with Satellites
3305:10.1007/s10569-017-9805-5
3175:"Planetary Names: Dactyl"
3072:Belton & Carlson 1994
3011:Oxford English Dictionary
2991:Carroll & Ostlie 1996
2821:Greeley & Batson 2001
1917:Oxford English Dictionary
1608:
1598:
1586:
1576:
1569:
1559:
1549:
1540:Orbital period (sidereal)
1537:
1525:
1518:
1468:
1456:
1444:
1398:
1386:
1381:
1373:
1360:
1350:
1345:
1329:
1319:
1310:
1206:Ida was classified as an
585:The images returned from
578:. It was named after the
516:
501:
487:
477:
465:
452:
437:
433:4.63 hours (0.193 d)
425:
412:
399:
389:
377:
367:
360:
349:
337:
325:
315:
303:
290:
281:Orbital period (sidereal)
278:
268:
252:
238:
224:
212:
205:
167:
151:
139:
110:
98:
93:
85:
73:
61:
56:
31:
5218:S-type asteroids (SMASS)
4494:
4229:
3935:The Astronomical Journal
3900:The Astronomical Journal
3036:Edward Coleridge (1990)
1843:
1772:
1681:Physical characteristics
1677:on the island of Crete.
1571:Physical characteristics
1459:Alternative designations
957:Physical characteristics
905:Ida is classified as an
504:Absolute magnitude
483:200 K (−73 °C)
362:Physical characteristics
5062:Minor planets navigator
4971:JPL Small-Body Database
4174:1999M&PS...34..479W
3565:1996M&PS...31..699C
3466:10.2307/j.ctv1v7zdn4.37
3016:Oxford University Press
2219:Owen & Yeomans 1994
1922:Oxford University Press
1589:Synodic rotation period
1520:Orbital characteristics
1272:Ida is a member of the
1000:the asteroid entirely.
940:Polished section of an
428:Synodic rotation period
207:Orbital characteristics
4935:Observation prediction
4797:Stooke, P. J. (1997).
4727:Raab, Herbert (2002).
4081:10.1006/icar.1996.0033
4032:10.1006/icar.1996.0041
3996:10.1006/icar.1997.5788
3851:10.1006/icar.1996.0039
3765:10.1006/icar.1996.0040
3693:10.1006/icar.1996.0042
3607:10.1006/icar.1996.0038
3425:10.1006/icar.1996.0032
3376:10.2307/j.ctv1v7zdn4.7
3134:
2911:
2321:
2197:
1808:Hubble Space Telescope
1782:
1269:
1160:
1103:
1029:
945:
909:based on ground-based
4720:6 August 2019 at the
4698:The Galileo Messenger
4545:The Galileo Messenger
4339:Description of Greece
3629:Space Science Reviews
3248:Greenberg et al. 1996
3177:. IAU. Archived from
3129:
3127:Pausanias & 5.7.6
2967:Greenberg et al. 1996
2902:
2316:
2193:
1838:List of minor planets
1780:
1661:Dactyl was initially
1267:
1158:
1098:
1023:
939:
668:Oak Ridge Observatory
395:4.2 ± 0.6 ×10 kg
4700:(34). Archived from
4547:(35). Archived from
4005:"Geology of 243 Ida"
3814:10.1029/1999GL010956
3314:"Asteroid Interiors"
2936:Sullivan et al. 1996
2872:Geissler et al. 1996
2860:Sullivan et al. 1996
2848:Sullivan et al. 1996
2757:Sullivan et al. 1996
2702:Sullivan et al. 1996
2687:Geissler et al. 1996
2543:Geissler et al. 1996
2301:Sullivan et al. 1996
1870:Noah Webster (1884)
1389:MPC designation
1293:retrograde direction
1171:, also known as the
416:surface gravity
260:2.861 AU (4.280
244:2.743 AU (4.103
230:2.979 AU (4.457
101:MPC designation
21:Ida (disambiguation)
5193:Named minor planets
5022:Physical parameters
4814:1997LPI....28.1385S
4775:2002LPI....33.1381S
4673:1994IAUC.6082....2G
4648:1994LPI....25..469G
4574:1994LPI....25..237C
4520:1994IAUC.5948....2B
4461:Planetary Tectonics
4213:1985Icar...61..355Z
4118:10.1038/nature01948
4110:2003Natur.425..147V
4072:1996Icar..120...20T
4024:1996Icar..120..119S
3978:1997Icar..130..177P
3947:1994AJ....107.2295O
3912:1994AJ....107.2290M
3887:1994JBAA..104..108M
3843:1996Icar..120...87L
3805:2000GeoRL..27.1595H
3757:1996Icar..120..106G
3729:1996ASPC..107...57G
3685:1996Icar..120..140G
3641:1992SSRv...60...23D
3598:1996Icar..120...77C
3544:1995Metic..30R.496C
3523:1994Metic..29..455C
3502:1994IAUS..160..357C
3458:2002aste.book..485B
3416:1996Icar..120....1B
3368:2002aste.book....3B
3329:2002aste.book..463A
3297:2018CeMDA.130...22A
3162:Chapman et al. 1994
3014:(Online ed.).
2648:Greeley et al. 1994
2430:Chapman et al. 1994
2394:Greeley et al. 1994
2379:Chapman et al. 1994
2180:, pp. 357, 373
2003:1995Natur.374..785B
1920:(Online ed.).
1374:Discovery date
1362:Discovery site
1326:
1291:Ida rotates in the
993:gravitational field
694:-bound space probe
655:reflection spectrum
638:who raised the god
408:2.6 ± 0.5 g/cm
146:Ida (nurse of Zeus)
86:Discovery date
75:Discovery site
28:
4959:Observational info
4867:on 21 October 2008
4745:on 30 October 2008
4336:Pausanias (1916).
4056:"The shape of Ida"
3649:10.1007/BF00216849
3582:"Cratering on Ida"
2833:Bottke et al. 2002
2797:, pp. 707–708
2608:Bottke et al. 2002
2533:, pp. 179–180
2078:, p. 6, 15–16
2041:Thomas et al. 1996
1963:Belton et al. 1996
1783:
1626:(243) Ida I Dactyl
1545:prograde, ca. 20 h
1394:(243) Ida I Dactyl
1352:Discovered by
1324:
1270:
1260:Orbit and rotation
1212:ordinary chondrite
1161:
1104:
1030:
946:
942:ordinary chondrite
919:ordinary chondrite
648:Kiyotsugu Hirayama
612:Vienna Observatory
596:ordinary chondrite
543:Vienna Observatory
89:September 29, 1884
80:Vienna Observatory
63:Discovered by
43:image of 243 Ida.
26:
16:Main-belt asteroid
5183:Koronis asteroids
5093:
5092:
4551:on 5 January 1997
4470:978-0-521-76573-2
4407:978-3-540-00238-3
4349:978-0-674-99104-0
4328:978-0-201-47959-1
4304:978-0-521-80633-6
4281:978-0-201-54730-6
4250:978-0-521-82344-9
4104:(6954): 147–151.
3799:(11): 1595–1598.
3260:Petit et al. 1997
3236:Petit et al. 1997
3224:Petit et al. 1997
3212:Petit et al. 1997
3200:Petit et al. 1997
3055:Petit et al. 1997
3022:(Subscription or
2531:Petit et al. 1997
2406:Monet et al. 1994
1997:(6525): 785–788.
1977:Britt et al. 2002
1928:(Subscription or
1612:
1611:
1561:Satellite of
1301:moment of inertia
740:high-gain antenna
620:Moriz von Kuffner
520:
519:
421:0.3–1.1 cm/s
5230:
5198:Binary asteroids
5158:
5157:
5156:
5146:
5145:
5144:
5134:
5133:
5132:
5122:
5121:
5110:
5109:
5108:
5101:
5055:
5048:
5041:
5032:
5031:
5014:Orbital elements
4978:
4900:
4898:
4896:
4876:
4874:
4872:
4852:
4850:
4848:
4832:
4830:
4828:
4822:
4803:
4793:
4791:
4789:
4783:
4764:
4754:
4752:
4750:
4744:
4738:. Archived from
4733:
4713:
4711:
4709:
4688:
4686:
4684:
4651:
4633:
4631:
4629:
4624:on 27 March 2012
4623:
4617:. Archived from
4604:
4594:
4577:
4560:
4558:
4556:
4535:
4533:
4531:
4489:
4487:
4485:
4479:
4473:. Archived from
4458:
4448:
4423:
4421:
4419:
4388:
4386:
4384:
4365:
4363:
4361:
4332:
4308:
4296:
4285:
4266:
4264:
4262:
4224:
4195:
4185:
4152:
4150:
4148:
4142:
4095:
4085:
4083:
4050:
4048:
4046:
4040:
4034:. Archived from
4009:
3999:
3989:
3960:
3958:
3941:(6): 2295–2298.
3925:
3923:
3906:(6): 2290–2294.
3890:
3869:
3867:
3865:
3859:
3853:. Archived from
3828:
3818:
3816:
3783:
3781:
3779:
3773:
3742:
3732:
3711:
3709:
3707:
3701:
3670:
3660:
3623:
3621:
3619:
3609:
3576:
3547:
3526:
3505:
3484:
3482:
3480:
3474:
3447:
3437:
3427:
3394:
3392:
3390:
3384:
3357:
3347:
3345:
3343:
3337:
3318:
3308:
3275:Journal articles
3263:
3257:
3251:
3245:
3239:
3233:
3227:
3221:
3215:
3209:
3203:
3197:
3191:
3190:
3188:
3186:
3171:
3165:
3159:
3150:
3144:
3135:
3124:
3118:
3112:
3103:
3098:
3089:
3083:
3074:
3069:
3058:
3052:
3041:
3034:
3028:
3027:
3019:
3007:
3000:
2994:
2988:
2982:
2976:
2970:
2964:
2951:
2945:
2939:
2933:
2924:
2918:
2912:
2896:
2890:
2884:
2875:
2869:
2863:
2857:
2851:
2845:
2836:
2830:
2824:
2818:
2812:
2807:
2798:
2792:
2786:
2785:, pp. 57–58
2780:
2774:
2769:
2760:
2754:
2748:
2743:
2737:
2731:
2722:
2716:
2705:
2699:
2690:
2684:
2675:
2669:
2663:
2657:
2651:
2645:
2639:
2633:
2627:
2622:
2611:
2605:
2594:
2588:
2577:
2571:
2558:
2552:
2546:
2540:
2534:
2528:
2522:
2516:
2497:
2491:
2480:
2475:
2460:
2454:
2433:
2427:
2421:
2415:
2409:
2403:
2397:
2391:
2382:
2376:
2367:
2361:
2334:
2328:
2322:
2310:
2304:
2298:
2292:
2286:
2277:
2271:
2265:
2259:
2253:
2247:
2234:
2228:
2222:
2216:
2210:
2204:
2198:
2187:
2181:
2175:
2169:
2163:
2152:
2147:
2134:
2128:
2122:
2116:
2110:
2104:
2098:
2092:
2079:
2073:
2060:
2054:
2043:
2038:
2023:
2022:
2011:10.1038/374785a0
1986:
1980:
1974:
1965:
1960:
1954:
1949:
1934:
1933:
1925:
1913:
1906:
1900:
1895:
1874:
1868:
1862:
1857:
1768:
1767:
1764:
1763:
1760:
1757:
1754:
1751:
1748:
1745:
1736:
1735:
1732:
1731:
1728:
1725:
1722:
1719:
1716:
1514:
1513:
1510:
1509:
1506:
1503:
1500:
1497:
1494:
1491:
1488:
1485:
1482:
1437:
1432:
1431:
1428:
1427:
1424:
1421:
1418:
1415:
1412:
1409:
1377:17 February 1994
1334:
1327:
1323:
1090:space weathering
1016:Surface features
981:
969:
930:space weathering
869:
857:
848:
846:
837:
832:
823:
818:
809:
804:
795:
790:
781:
776:
770:
761:
545:and named after
468:Geometric albedo
454:North pole
444:
439:North pole
263:
247:
233:
201:
200:
197:
196:
193:
190:
187:
184:
181:
135:
134:
131:
130:
127:
124:
121:
36:
29:
25:
5238:
5237:
5233:
5232:
5231:
5229:
5228:
5227:
5208:Galileo program
5168:
5167:
5164:
5154:
5152:
5142:
5140:
5130:
5128:
5116:
5106:
5104:
5096:
5094:
5089:
5064:
5059:
4951:Proper elements
4908:
4903:
4894:
4892:
4870:
4868:
4846:
4844:
4826:
4824:
4820:
4801:
4787:
4785:
4781:
4762:
4748:
4746:
4742:
4731:
4722:Wayback Machine
4707:
4705:
4704:on 24 June 2010
4682:
4680:
4627:
4625:
4621:
4602:
4554:
4552:
4529:
4527:
4497:
4492:
4483:
4481:
4480:on 4 March 2009
4477:
4471:
4456:
4417:
4415:
4408:
4382:
4380:
4359:
4357:
4350:
4329:
4305:
4282:
4260:
4258:
4251:
4232:
4227:
4146:
4144:
4140:
4093:
4044:
4042:
4041:on 12 June 2016
4038:
4007:
3987:10.1.1.693.8814
3863:
3861:
3860:on 12 June 2016
3857:
3826:
3777:
3775:
3771:
3740:
3705:
3703:
3699:
3668:
3617:
3615:
3478:
3476:
3472:
3445:
3388:
3386:
3382:
3355:
3341:
3339:
3335:
3316:
3277:
3272:
3267:
3266:
3258:
3254:
3246:
3242:
3234:
3230:
3222:
3218:
3210:
3206:
3198:
3194:
3184:
3182:
3173:
3172:
3168:
3160:
3153:
3145:
3138:
3125:
3121:
3113:
3106:
3099:
3092:
3084:
3077:
3070:
3061:
3053:
3044:
3035:
3031:
3021:
3001:
2997:
2989:
2985:
2977:
2973:
2965:
2954:
2946:
2942:
2934:
2927:
2919:
2915:
2897:
2893:
2885:
2878:
2870:
2866:
2858:
2854:
2846:
2839:
2831:
2827:
2819:
2815:
2808:
2801:
2793:
2789:
2781:
2777:
2770:
2763:
2755:
2751:
2744:
2740:
2732:
2725:
2719:Lee et al. 1996
2717:
2708:
2700:
2693:
2685:
2678:
2672:Lee et al. 1996
2670:
2666:
2658:
2654:
2646:
2642:
2636:Lee et al. 1996
2634:
2630:
2623:
2614:
2606:
2597:
2589:
2580:
2572:
2561:
2555:Lee et al. 1996
2553:
2549:
2541:
2537:
2529:
2525:
2517:
2500:
2492:
2483:
2476:
2463:
2455:
2436:
2428:
2424:
2416:
2412:
2404:
2400:
2392:
2385:
2377:
2370:
2362:
2337:
2329:
2325:
2311:
2307:
2299:
2295:
2287:
2280:
2272:
2268:
2260:
2256:
2248:
2237:
2229:
2225:
2217:
2213:
2205:
2201:
2188:
2184:
2176:
2172:
2164:
2155:
2148:
2137:
2129:
2125:
2117:
2113:
2105:
2101:
2093:
2082:
2074:
2063:
2055:
2046:
2039:
2026:
1987:
1983:
1975:
1968:
1961:
1957:
1950:
1937:
1927:
1907:
1903:
1896:
1877:
1869:
1865:
1858:
1851:
1846:
1829:
1820:
1775:
1742:
1738:
1713:
1709:
1697:and reflection
1683:
1643:
1618:
1591:
1542:
1530:
1528:Semi-major axis
1479:
1475:
1461:
1447:
1435:
1406:
1402:
1391:
1341:
1322:
1313:
1297:rotation period
1262:
1208:S-type asteroid
1204:
1196:Ejecta blankets
1144:
1128:Townsend Dorsum
1113:
1053:
1018:
989:
988:
987:
986:
985:
982:
974:
973:
970:
959:
907:S-type asteroid
882:
877:
876:
875:
874:
873:
870:
862:
861:
858:
850:
849:
844:
843:
830:
829:
816:
815:
802:
801:
788:
787:
774:
773:
772:
768:
762:
688:
680:
659:David J. Tholen
624:Greek mythology
604:
551:S-type asteroid
509:
492:
470:
458:
445:
442:right ascension
440:
430:
418:
405:
382:
342:
330:
308:
296:
283:
261:
257:
255:Semi-major axis
245:
231:
178:
174:
156:
142:
118:
114:
103:
52:
24:
17:
12:
11:
5:
5236:
5226:
5225:
5220:
5215:
5210:
5205:
5200:
5195:
5190:
5185:
5180:
5163:
5162:
5150:
5138:
5126:
5114:
5091:
5090:
5088:
5087:
5082:
5075:
5073:242 Kriemhild
5069:
5066:
5065:
5058:
5057:
5050:
5043:
5035:
5027:
5026:
5025:
5024:
4982:Close approach
4963:
4962:
4961:
4915:
4907:
4906:External links
4904:
4902:
4901:
4877:
4853:
4833:
4794:
4755:
4724:
4689:
4652:
4634:
4595:
4578:
4561:
4536:
4504:"1993 (243) 1"
4498:
4496:
4493:
4491:
4490:
4469:
4449:
4424:
4406:
4389:
4366:
4348:
4333:
4327:
4313:Lewis, John S.
4309:
4303:
4286:
4280:
4267:
4249:
4233:
4231:
4228:
4226:
4225:
4207:(3): 355–416.
4196:
4168:(3): 479–483.
4153:
4086:
4051:
4018:(1): 119–139.
4000:
3972:(1): 177–197.
3961:
3956:10.1086/117037
3926:
3921:10.1086/117036
3891:
3870:
3819:
3784:
3751:(1): 106–118.
3733:
3712:
3679:(1): 140–157.
3661:
3635:(1–4): 23–78.
3624:
3577:
3559:(6): 699–725.
3548:
3527:
3506:
3485:
3438:
3395:
3348:
3309:
3278:
3276:
3273:
3271:
3268:
3265:
3264:
3252:
3240:
3228:
3216:
3204:
3192:
3181:on 1 July 2015
3166:
3151:
3136:
3119:
3104:
3090:
3075:
3059:
3042:
3029:
2995:
2983:
2981:, p. 1595
2971:
2952:
2940:
2925:
2913:
2891:
2876:
2864:
2852:
2837:
2825:
2813:
2799:
2787:
2775:
2761:
2749:
2738:
2736:, p. 1385
2723:
2706:
2691:
2676:
2664:
2652:
2640:
2628:
2612:
2595:
2578:
2559:
2547:
2535:
2523:
2498:
2481:
2461:
2434:
2422:
2410:
2408:, p. 2293
2398:
2383:
2368:
2335:
2323:
2315:, p. 215
2305:
2293:
2278:
2266:
2254:
2235:
2223:
2221:, p. 2295
2211:
2199:
2192:, p. 404
2182:
2170:
2153:
2135:
2123:
2111:
2099:
2080:
2061:
2044:
2024:
1981:
1966:
1955:
1935:
1901:
1875:
1863:
1848:
1847:
1845:
1842:
1841:
1840:
1835:
1828:
1825:
1819:
1818:Age and origin
1816:
1774:
1771:
1682:
1679:
1673:who inhabited
1642:
1639:
1635:prograde orbit
1614:Main article:
1610:
1609:
1606:
1605:
1602:
1596:
1595:
1592:
1587:
1584:
1583:
1582:1.6×1.4×1.2 km
1580:
1574:
1573:
1567:
1566:
1563:
1557:
1556:
1553:
1547:
1546:
1543:
1538:
1535:
1534:
1531:
1526:
1523:
1522:
1516:
1515:
1472:
1466:
1465:
1462:
1457:
1454:
1453:
1448:
1445:
1442:
1441:
1400:
1396:
1395:
1392:
1387:
1384:
1383:
1379:
1378:
1375:
1371:
1370:
1364:
1358:
1357:
1354:
1348:
1347:
1343:
1342:
1335:
1321:
1318:
1312:
1309:
1274:Koronis family
1261:
1258:
1203:
1200:
1184:prime meridian
1149:Koronis family
1143:
1140:
1112:
1109:
1052:
1049:
1017:
1014:
983:
976:
975:
971:
964:
963:
962:
961:
960:
958:
955:
891:NEAR Shoemaker
881:
878:
871:
864:
863:
859:
852:
851:
763:
756:
755:
754:
753:
752:
711:Space Shuttle
687:
681:
679:
676:
644:Koronis family
603:
600:
531:Koronis family
518:
517:
514:
513:
510:
502:
499:
498:
493:
488:
485:
484:
481:
475:
474:
471:
466:
463:
462:
459:
453:
450:
449:
446:
438:
435:
434:
431:
426:
423:
422:
419:
413:
410:
409:
406:
400:
397:
396:
393:
387:
386:
383:
378:
375:
374:
371:
365:
364:
358:
357:
354:
347:
346:
343:
338:
335:
334:
331:
326:
323:
322:
319:
313:
312:
309:
304:
301:
300:
297:
291:
288:
287:
284:
279:
276:
275:
272:
266:
265:
258:
253:
250:
249:
242:
236:
235:
228:
222:
221:
216:31 July 2016 (
210:
209:
203:
202:
173:Idean (Idæan)
171:
165:
164:
161:Koronis family
157:
152:
149:
148:
143:
140:
137:
136:
112:
108:
107:
104:
99:
96:
95:
91:
90:
87:
83:
82:
77:
71:
70:
65:
59:
58:
54:
53:
37:
15:
9:
6:
4:
3:
2:
5235:
5224:
5221:
5219:
5216:
5214:
5211:
5209:
5206:
5204:
5201:
5199:
5196:
5194:
5191:
5189:
5186:
5184:
5181:
5179:
5176:
5175:
5173:
5166:
5161:
5151:
5149:
5139:
5137:
5127:
5125:
5120:
5115:
5113:
5103:
5102:
5099:
5086:
5083:
5081:
5080:
5076:
5074:
5071:
5070:
5067:
5063:
5056:
5051:
5049:
5044:
5042:
5037:
5036:
5033:
5029:
5023:
5019:
5015:
5011:
5007:
5006:Orbit diagram
5003:
4999:
4995:
4991:
4987:
4983:
4980:
4979:
4977:
4973:
4972:
4967:
4964:
4960:
4956:
4952:
4948:
4944:
4940:
4936:
4932:
4928:
4925:
4924:
4923:
4919:
4916:
4913:
4910:
4909:
4890:
4886:
4882:
4878:
4866:
4862:
4858:
4854:
4842:
4838:
4834:
4819:
4815:
4811:
4808:: 1385–1386.
4807:
4800:
4795:
4780:
4776:
4772:
4768:
4761:
4756:
4741:
4737:
4730:
4725:
4723:
4719:
4716:
4703:
4699:
4695:
4690:
4678:
4674:
4670:
4666:
4662:
4658:
4653:
4649:
4645:
4641:
4635:
4620:
4616:
4612:
4608:
4601:
4596:
4592:
4588:
4584:
4579:
4575:
4571:
4567:
4562:
4550:
4546:
4542:
4537:
4525:
4521:
4517:
4513:
4509:
4505:
4500:
4499:
4476:
4472:
4466:
4462:
4455:
4450:
4446:
4442:
4438:
4434:
4430:
4425:
4413:
4409:
4403:
4399:
4395:
4390:
4378:
4374:
4373:
4367:
4355:
4351:
4345:
4341:
4340:
4334:
4330:
4324:
4320:
4319:
4314:
4310:
4306:
4300:
4295:
4294:
4287:
4283:
4277:
4273:
4268:
4256:
4252:
4246:
4242:
4241:
4235:
4234:
4222:
4218:
4214:
4210:
4206:
4202:
4197:
4193:
4189:
4184:
4179:
4175:
4171:
4167:
4163:
4159:
4154:
4139:
4135:
4131:
4127:
4123:
4119:
4115:
4111:
4107:
4103:
4099:
4092:
4087:
4082:
4077:
4073:
4069:
4065:
4061:
4057:
4052:
4037:
4033:
4029:
4025:
4021:
4017:
4013:
4006:
4001:
3997:
3993:
3988:
3983:
3979:
3975:
3971:
3967:
3962:
3957:
3952:
3948:
3944:
3940:
3936:
3932:
3927:
3922:
3917:
3913:
3909:
3905:
3901:
3897:
3892:
3888:
3884:
3880:
3876:
3871:
3856:
3852:
3848:
3844:
3840:
3837:(1): 87–105.
3836:
3832:
3825:
3820:
3815:
3810:
3806:
3802:
3798:
3794:
3790:
3785:
3770:
3766:
3762:
3758:
3754:
3750:
3746:
3739:
3734:
3730:
3726:
3722:
3718:
3713:
3698:
3694:
3690:
3686:
3682:
3678:
3674:
3667:
3662:
3658:
3654:
3650:
3646:
3642:
3638:
3634:
3630:
3625:
3613:
3608:
3603:
3599:
3595:
3591:
3587:
3583:
3578:
3574:
3570:
3566:
3562:
3558:
3554:
3549:
3545:
3541:
3537:
3533:
3528:
3524:
3520:
3516:
3512:
3507:
3503:
3499:
3495:
3491:
3486:
3471:
3467:
3463:
3459:
3455:
3451:
3450:Asteroids III
3444:
3439:
3435:
3431:
3426:
3421:
3417:
3413:
3409:
3405:
3401:
3396:
3381:
3377:
3373:
3369:
3365:
3361:
3360:Asteroids III
3354:
3349:
3334:
3330:
3326:
3322:
3321:Asteroids III
3315:
3310:
3306:
3302:
3298:
3294:
3290:
3286:
3280:
3279:
3262:, p. 182
3261:
3256:
3250:, p. 116
3249:
3244:
3238:, p. 193
3237:
3232:
3226:, p. 188
3225:
3220:
3214:, p. 195
3213:
3208:
3202:, p. 179
3201:
3196:
3180:
3176:
3170:
3164:, p. 455
3163:
3158:
3156:
3149:, p. 463
3148:
3143:
3141:
3133:
3128:
3123:
3116:
3115:Schmadel 2003
3111:
3109:
3102:
3097:
3095:
3088:, p. 108
3087:
3082:
3080:
3073:
3068:
3066:
3064:
3057:, p. 177
3056:
3051:
3049:
3047:
3039:
3033:
3025:
3017:
3013:
3012:
3006:
2999:
2993:, p. 878
2992:
2987:
2980:
2975:
2969:, p. 117
2968:
2963:
2961:
2959:
2957:
2950:, p. 134
2949:
2944:
2938:, p. 135
2937:
2932:
2930:
2922:
2917:
2910:
2908:
2901:, p. 89
2900:
2895:
2889:, p. 480
2888:
2883:
2881:
2874:, p. 155
2873:
2868:
2862:, p. 128
2861:
2856:
2850:, p. 124
2849:
2844:
2842:
2834:
2829:
2823:, p. 393
2822:
2817:
2811:
2806:
2804:
2796:
2791:
2784:
2779:
2773:
2768:
2766:
2759:, p. 131
2758:
2753:
2747:
2742:
2735:
2730:
2728:
2720:
2715:
2713:
2711:
2704:, p. 132
2703:
2698:
2696:
2689:, p. 141
2688:
2683:
2681:
2673:
2668:
2662:, p. 701
2661:
2656:
2650:, p. 470
2649:
2644:
2637:
2632:
2626:
2621:
2619:
2617:
2609:
2604:
2602:
2600:
2593:, p. 363
2592:
2587:
2585:
2583:
2575:
2570:
2568:
2566:
2564:
2556:
2551:
2545:, p. 142
2544:
2539:
2532:
2527:
2521:, p. 496
2520:
2515:
2513:
2511:
2509:
2507:
2505:
2503:
2496:, p. 710
2495:
2490:
2488:
2486:
2479:
2474:
2472:
2470:
2468:
2466:
2459:, p. 709
2458:
2453:
2451:
2449:
2447:
2445:
2443:
2441:
2439:
2432:, p. 238
2431:
2426:
2419:
2414:
2407:
2402:
2396:, p. 469
2395:
2390:
2388:
2381:, p. 237
2380:
2375:
2373:
2366:, p. 707
2365:
2360:
2358:
2356:
2354:
2352:
2350:
2348:
2346:
2344:
2342:
2340:
2333:, p. 358
2332:
2327:
2320:
2314:
2309:
2303:, p. 120
2302:
2297:
2290:
2285:
2283:
2275:
2270:
2263:
2258:
2252:, p. 699
2251:
2246:
2244:
2242:
2240:
2232:
2227:
2220:
2215:
2209:, p. 410
2208:
2203:
2196:
2191:
2186:
2179:
2174:
2168:, p. 700
2167:
2162:
2160:
2158:
2151:
2146:
2144:
2142:
2140:
2133:, p. 241
2132:
2127:
2120:
2119:Schmadel 2003
2115:
2109:, p. 206
2108:
2103:
2097:, p. 479
2096:
2091:
2089:
2087:
2085:
2077:
2072:
2070:
2068:
2066:
2059:, p. 147
2058:
2053:
2051:
2049:
2042:
2037:
2035:
2033:
2031:
2029:
2020:
2016:
2012:
2008:
2004:
2000:
1996:
1992:
1985:
1979:, p. 486
1978:
1973:
1971:
1964:
1959:
1953:
1948:
1946:
1944:
1942:
1940:
1931:
1923:
1919:
1918:
1912:
1905:
1899:
1894:
1892:
1890:
1888:
1886:
1884:
1882:
1880:
1873:
1867:
1861:
1856:
1854:
1849:
1839:
1836:
1834:
1831:
1830:
1824:
1815:
1811:
1809:
1805:
1800:
1796:
1792:
1788:
1779:
1770:
1766:
1734:
1706:
1704:
1700:
1696:
1691:
1689:
1678:
1676:
1672:
1668:
1664:
1659:
1657:
1652:
1648:
1638:
1636:
1631:
1627:
1623:
1617:
1616:Dactyl (moon)
1607:
1603:
1601:
1597:
1593:
1590:
1585:
1581:
1579:
1575:
1572:
1568:
1564:
1562:
1558:
1554:
1552:
1548:
1544:
1541:
1536:
1532:
1529:
1524:
1521:
1517:
1512:
1473:
1471:
1467:
1463:
1460:
1455:
1452:
1449:
1443:
1440:
1439:
1430:
1401:
1399:Pronunciation
1397:
1393:
1390:
1385:
1380:
1376:
1372:
1368:
1365:
1363:
1359:
1355:
1353:
1349:
1344:
1339:
1333:
1328:
1317:
1308:
1306:
1302:
1298:
1294:
1289:
1287:
1283:
1279:
1278:asteroid-belt
1275:
1266:
1257:
1255:
1254:
1248:
1246:
1241:
1237:
1233:
1229:
1225:
1221:
1217:
1213:
1209:
1199:
1197:
1193:
1187:
1185:
1180:
1176:
1175:
1170:
1166:
1157:
1153:
1150:
1139:
1135:
1133:
1129:
1124:
1122:
1118:
1108:
1101:
1097:
1093:
1091:
1087:
1083:
1079:
1074:
1072:
1068:
1064:
1063:impact events
1060:
1059:
1048:
1046:
1045:
1044:ejecta blocks
1040:
1035:
1027:
1022:
1013:
1011:
1007:
1001:
999:
994:
980:
968:
954:
952:
943:
938:
934:
931:
926:
924:
920:
916:
912:
908:
903:
901:
897:
893:
892:
887:
868:
856:
847: 243 Ida
841:
836:
827:
822:
813:
808:
799:
794:
785:
780:
767:
764:Animation of
760:
751:
749:
745:
741:
736:
733:
729:
727:
723:
719:
715:
714:
708:
703:
699:
698:
693:
685:
675:
673:
669:
665:
660:
656:
651:
649:
645:
641:
637:
633:
629:
625:
621:
617:
613:
609:
608:Johann Palisa
599:
597:
592:
588:
583:
581:
577:
572:
569:
564:
562:
558:
557:
552:
548:
544:
540:
539:Johann Palisa
536:
535:asteroid belt
532:
528:
524:
515:
511:
508:
507:
500:
497:
494:
491:
490:Spectral type
486:
482:
480:
476:
472:
469:
464:
460:
457:
451:
447:
443:
436:
432:
429:
424:
420:
417:
411:
407:
404:
398:
394:
392:
388:
384:
381:
376:
372:
370:
366:
363:
359:
355:
353:
348:
344:
341:
336:
332:
329:
324:
320:
318:
314:
310:
307:
302:
298:
295:
294:orbital speed
289:
285:
282:
277:
273:
271:
267:
259:
256:
251:
243:
241:
237:
229:
227:
223:
219:
215:
211:
208:
204:
199:
172:
170:
166:
162:
158:
155:
150:
147:
144:
138:
133:
113:
111:Pronunciation
109:
105:
102:
97:
92:
88:
84:
81:
78:
76:
72:
69:
68:Johann Palisa
66:
64:
60:
55:
50:
46:
42:
41:
35:
30:
22:
5165:
5160:Solar System
5077:
5028:
5017:
5009:
5001:
4993:
4985:
4969:
4954:
4946:
4943:Orbital info
4938:
4930:
4921:
4893:. Retrieved
4869:. Retrieved
4865:the original
4845:. Retrieved
4825:. Retrieved
4805:
4786:. Retrieved
4766:
4747:. Retrieved
4740:the original
4735:
4706:. Retrieved
4702:the original
4697:
4681:. Retrieved
4664:
4661:IAU Circular
4660:
4639:
4626:. Retrieved
4619:the original
4607:Science News
4606:
4583:Science News
4582:
4565:
4553:. Retrieved
4549:the original
4544:
4528:. Retrieved
4511:
4508:IAU Circular
4507:
4482:. Retrieved
4475:the original
4460:
4437:1721.1/11867
4428:
4416:. Retrieved
4397:
4381:. Retrieved
4371:
4358:. Retrieved
4338:
4317:
4292:
4271:
4259:. Retrieved
4239:
4204:
4200:
4165:
4161:
4145:. Retrieved
4101:
4097:
4066:(1): 20–32.
4063:
4059:
4043:. Retrieved
4036:the original
4015:
4011:
3969:
3965:
3938:
3934:
3903:
3899:
3878:
3874:
3862:. Retrieved
3855:the original
3834:
3830:
3796:
3792:
3776:. Retrieved
3748:
3744:
3720:
3716:
3704:. Retrieved
3676:
3672:
3632:
3628:
3616:. Retrieved
3592:(1): 77–86.
3589:
3585:
3556:
3552:
3535:
3531:
3514:
3510:
3493:
3489:
3477:. Retrieved
3449:
3407:
3403:
3387:. Retrieved
3359:
3340:. Retrieved
3320:
3288:
3284:
3255:
3243:
3231:
3219:
3207:
3195:
3183:. Retrieved
3179:the original
3169:
3130:
3122:
3117:, p. 37
3037:
3032:
3009:
2998:
2986:
2974:
2943:
2923:, p. 21
2916:
2903:
2894:
2867:
2855:
2828:
2816:
2795:Chapman 1996
2790:
2778:
2752:
2741:
2721:, p. 97
2674:, p. 90
2667:
2660:Chapman 1996
2655:
2643:
2638:, p. 96
2631:
2610:, p. 10
2591:Chapman 1994
2576:, p. 58
2557:, p. 99
2550:
2538:
2526:
2519:Chapman 1995
2494:Chapman 1996
2457:Chapman 1996
2425:
2420:, p. 57
2413:
2401:
2364:Chapman 1996
2331:Chapman 1994
2326:
2317:
2308:
2296:
2291:, p. 36
2276:, p. 72
2269:
2264:, p. 24
2257:
2250:Chapman 1996
2233:, p. 26
2226:
2214:
2202:
2194:
2185:
2173:
2166:Chapman 1996
2126:
2121:, p. 36
2114:
2107:Ridpath 1897
2102:
1994:
1990:
1984:
1958:
1915:
1904:
1871:
1866:
1821:
1812:
1803:
1786:
1784:
1707:
1692:
1684:
1660:
1655:
1650:
1646:
1644:
1629:
1625:
1619:
1464:1993 (243) 1
1382:Designations
1366:
1337:
1314:
1290:
1271:
1253:megaregolith
1251:
1249:
1239:
1235:
1216:bulk density
1205:
1188:
1172:
1162:
1145:
1136:
1132:Vienna Regio
1131:
1127:
1125:
1120:
1116:
1114:
1105:
1099:
1075:
1066:
1056:
1054:
1042:
1031:
1025:
1009:
1002:
990:
950:
947:
927:
914:
904:
889:
885:
883:
839:
825:
811:
797:
783:
778:
765:
737:
731:
730:
721:
712:
706:
695:
689:
683:
671:
652:
605:
590:
586:
584:
575:
573:
565:
554:
522:
521:
505:
385:15.7 km
306:Mean anomaly
270:Eccentricity
94:Designations
38:
5148:Outer space
5136:Spaceflight
4827:29 November
4667:(6082): 2.
4642:: 469–470.
4568:: 237–238.
4514:(5948): 2.
4484:29 November
4360:28 February
3553:Meteoritics
3532:Meteoritics
3511:Meteoritics
3496:: 357–365.
3452:: 485–500.
3410:(1): 1–19.
3323:: 463–484.
2948:Slivan 1995
2835:, p. 9
2734:Stooke 1997
2131:Berger 2003
1789:was in the
1737:and Celmis
1600:Temperature
1594:synchronous
1551:Inclination
1446:Named after
1247:of 11–42%.
1202:Composition
1174:Blue Grotto
880:Discoveries
678:Exploration
479:Temperature
456:declination
414:Equatorial
380:Mean radius
317:Inclination
159:Main belt (
141:Named after
5172:Categories
4871:4 December
4847:24 October
4788:22 October
4749:23 October
4708:23 October
4555:23 October
4418:23 October
4147:23 October
4045:27 October
3881:(3): 108.
3864:27 October
3778:23 October
3618:27 October
3538:(5): 496.
3479:27 October
3389:23 October
3270:References
3101:Green 1994
3086:Mason 1994
3026:required.)
2899:Lewis 1996
2625:Cowen 1995
2313:Cowen 1993
1932:required.)
1799:pericenter
1688:spheroidal
1663:designated
1620:Ida has a
1578:Dimensions
1474:Dactylian
1470:Adjectives
1369:spacecraft
1165:lava tubes
1111:Structures
923:stony-iron
835:951 Gaspra
726:propellant
369:Dimensions
352:satellites
264:10 m)
248:10 m)
240:Perihelion
234:10 m)
220:2457600.5)
169:Adjectives
45:Pola Regio
5112:Astronomy
4998:Ephemeris
4990:Discovery
4927:Ephemeris
4615:0036-8423
4591:0036-8423
4192:129231326
3982:CiteSeerX
3723:: 57–67.
3657:122388506
3342:4 January
3291:(3): 46.
2150:NASA 2005
1898:Holm 1994
1860:Raab 2002
1675:Mount Ida
1641:Discovery
1356:Ann Harch
1346:Discovery
1305:precesses
1080:minerals
944:meteorite
921:(OC) and
732:Galileo's
722:Galileo's
299:0.2036°/d
106:(243) Ida
57:Discovery
5085:244 Sita
4895:15 April
4889:Archived
4841:Archived
4818:Archived
4779:Archived
4769:: 1381.
4718:Archived
4677:Archived
4628:26 March
4524:Archived
4445:32907677
4412:Archived
4377:Archived
4354:Archived
4315:(1996).
4255:Archived
4138:Archived
4126:12968171
3769:Archived
3706:26 March
3697:Archived
3612:Archived
3470:Archived
3434:51885221
3380:Archived
3362:: 3–15.
3333:Archived
3005:"dactyl"
2907:troilite
1952:JPL 2008
1827:See also
1795:prograde
1703:regolith
1245:porosity
1232:feldspar
1224:pyroxene
1121:region 2
1117:region 1
1086:pyroxene
1078:silicate
1058:regolith
1051:Regolith
1039:regolith
1034:cratered
716:mission
713:Atlantis
666:and the
527:asteroid
345:110.961°
333:324.016°
292:Average
226:Aphelion
5098:Portals
5079:243 Ida
4968:at the
4966:243 Ida
4918:243 Ida
4810:Bibcode
4771:Bibcode
4715:Alt URL
4669:Bibcode
4644:Bibcode
4570:Bibcode
4516:Bibcode
4209:Bibcode
4170:Bibcode
4134:4367378
4106:Bibcode
4068:Bibcode
4020:Bibcode
3974:Bibcode
3943:Bibcode
3908:Bibcode
3883:Bibcode
3839:Bibcode
3801:Bibcode
3753:Bibcode
3725:Bibcode
3681:Bibcode
3637:Bibcode
3594:Bibcode
3561:Bibcode
3540:Bibcode
3519:Bibcode
3517:: 455.
3498:Bibcode
3454:Bibcode
3412:Bibcode
3364:Bibcode
3325:Bibcode
3293:Bibcode
3185:18 July
3040:, p. 42
2019:4333634
1999:Bibcode
1911:"Idæan"
1804:Galileo
1787:Galileo
1699:spectra
1695:albedos
1671:dactyls
1656:Galileo
1651:Galileo
1647:Galileo
1630:Galileo
1451:Dactyls
1367:Galileo
1338:Galileo
1295:with a
1286:Jupiter
1240:Galileo
1236:Galileo
1220:olivine
1142:Craters
1100:Galileo
1082:olivine
1067:Galileo
1026:Galileo
1010:Galileo
951:Galileo
915:Galileo
896:geology
886:Galileo
819:
793:Jupiter
779:Galileo
766:Galileo
707:Galileo
697:Galileo
692:Jupiter
684:Galileo
672:Galileo
610:at the
591:Galileo
587:Galileo
580:Dactyls
576:Galileo
561:Jupiter
556:Galileo
533:of the
529:in the
523:243 Ida
461:−87.12°
448:168.76°
403:density
311:38.707°
40:Galileo
5018:·
5016:
5010:·
5008:
5002:·
5000:
4994:·
4992:
4986:·
4984:
4955:·
4953:
4947:·
4945:
4939:·
4937:
4931:·
4929:
4683:5 July
4613:
4589:
4530:5 July
4467:
4443:
4404:
4383:3 June
4346:
4325:
4301:
4278:
4261:3 June
4247:
4201:Icarus
4190:
4132:
4124:
4098:Nature
4060:Icarus
4012:Icarus
3984:
3966:Icarus
3831:Icarus
3745:Icarus
3673:Icarus
3655:
3586:Icarus
3432:
3404:Icarus
2017:
1991:Nature
1555:ca. 8°
1325:Dactyl
1320:Dactyl
1311:Origin
1230:, and
1192:ejecta
1179:albedo
1006:debris
998:escape
900:Dactyl
845:
840:·
838:
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