Eros (minor planet designation: (433)Eros), provisional designation 1898 DQ, is a stony asteroid of the Amor group and the first discovered and second-largest near-Earth object with an elongated shape and a mean diameter of approximately 16.8 kilometers (10.4 miles). Visited by the NEAR Shoemaker space probe in 1998, it became the first asteroid ever studied from orbit around the asteroid.
Near-Earth asteroid
This article is about the asteroid. For the dwarf planet, see Eris (dwarf planet).
433 Eros
Eros – composite image of the north polar region, with the craters Psyche above and Himeros below. The long ridge Hinks Dorsum, believed to be a thrust fault, can be seen snaking diagonally between them. The smaller crater in the foreground is Narcissus Watters, (2011)
The asteroid was discovered by German astronomer C.G. Witt at the Berlin Observatory on 13August 1898 in an eccentric orbit between Mars and Earth. It was later named after Eros, a god from Greek mythology, the son of Aphrodite. He is identified with the planet Venus.[3]
Eros is named after the Greek god of love, Erōs. It is pronounced /ˈɛrɒs/ERR-os or sometimes /ˈɪərɒs/EER-os. The rarely used adjectival form of the name is Erotian/ɪˈroʊʃən/.[9][3]
Eros was the first minor planet to be given a male name,[3] on account of its orbit (it was the first near-Earth asteroid discovered).
Later studies
During the approach (opposition) of 1900–1901, a worldwide program was launched to make parallax measurements of Eros to determine the solar parallax (or distance to the Sun), with the results published in 1910 by A. Hinks of Cambridge[10] and C.D. Perrine of the Lick Observatory, University of California.[11] Perrine published progress reports in 1906[12] and 1908.[13] He took 965photographs with the Crossley Reflector and selected 525 for measurement.[14] A similar program was then carried out, during a closer approach, in 1930–1931 by H.S. Jones.[15] The value of the Astronomical Unit (roughly the Earth-Sun distance) obtained by this program was considered definitive until 1968, when radar and dynamical parallax methods started producing more precise measurements.
Eros was one of the first asteroids visited by a spacecraft, the first one orbited, and the first one soft-landed on. NASA spacecraft NEAR Shoemaker entered orbit around Eros in 2000, and landed in 2001.
Mars-crosser
Eros is a Mars-crosser asteroid, the first known to come within the orbit of Mars. Objects in such an orbit can remain there for only a few hundred million years before the orbit is perturbed by gravitational interactions. Dynamical integrations suggest that Eros may evolve into an Earth-crosser within as short an interval as two million years, and has a roughly 50% chance of doing so over a time scale of 108~109years.[18] It is a potential Earth impactor,[18] about five times larger than the impactor that created Chicxulub crater and led to the extinction of the non-avian dinosaurs.[lower-alpha 1]
NEAR Shoemaker survey and landing
The NEAR Shoemaker probe visited Eros twice, first with a brief flyby in 1998, and then by orbiting it in 2000, when it extensively photographed its surface. On 12February 2001, at the end of its mission, it landed on the asteroid's surface using its maneuvering jets.
This was the first time a Near Earth asteroid was closely visited by a spacecraft.[19]
Animation of NEAR Shoemaker trajectory from 19 February 1996 to 12 February 2001.
Animation of NEAR Shoemaker's trajectory around 433 Eros from 1 April 2000 to 12 February 2001. NEAR Shoemaker·433 Eros
Physical characteristics
Surface gravity depends on the distance from a spot on the surface to the center of a body's mass. Eros's surface gravity varies greatly because Eros is not a sphere but an elongated peanut-shaped object. The daytime temperature on Eros can reach about 100°C (373K) at perihelion. Nighttime measurements fall near −150°C (123K). Eros's density is 2.67g/cm3, about the same as the density of Earth's crust. It rotates once every 5.27hours.
NEAR scientists have found that most of the larger rocks strewn across Eros were ejected from a single crater in an impact approximately 1billion years ago.[20] (The crater involved was proposed to be named "Shoemaker", but is not recognized as such by the International Astronomical Union (IAU), and has been formally designated Charlois Regio.) This event may also be responsible for the 40percent of the Erotian surface that is devoid of craters smaller than 0.5kilometers across. It was originally thought that the debris thrown up by the collision filled in the smaller craters. An analysis of crater densities over the surface indicates that the areas with lower crater density are within 9 kilometers of the impact point. Some of the lower density areas were found on the opposite side of the asteroid but still within 9kilometers.[21]
It is theorized that seismic shockwaves propagate through the asteroid, shaking smaller craters into rubble. Since Eros is irregularly shaped, parts of the surface antipodal to the point of impact can be within 9kilometres of the impact point (measured in a straight line through the asteroid) even though some intervening parts of the surface are more than 9kilometres away in straight-line distance. A suitable analogy would be the distance from the top centre of a bun to the bottom centre as compared to the distance from the top centre to a point on the bun's circumference: top-to-bottom is a longer distance than top-to-periphery when measured along the surface but shorter than it in direct straight-line terms.[21]
Compression from the same impact is believed to have created the thrust fault Hinks Dorsum.[22]
Data from the Near Earth Asteroid Rendezvous spacecraft collected on Eros in December 1998 suggests that it could contain 20 billion tonnes of aluminum and similar amounts of metals that are rare on Earth, such as gold and platinum.[23]
Visibility from Earth
Path in sky during opposition 2011/2012
On 31 January 2012, Eros passed Earth at 0.17867AU (26,729,000km; 16,608,000mi),[24][25] about 70times the distance to the Moon, with a visual magnitude of +8.1.[26] During rare oppositions, every 81 years, such as in 1975 and 2056, Eros can reach a magnitude of +7.0,[6] which is brighter than Neptune and brighter than any main-belt asteroid except 1 Ceres, 4 Vesta and, rarely, 2 Pallas and 7 Iris. Under this condition, the asteroid actually appears to stop, but unlike the normal condition for a body in heliocentric conjunction with Earth, its retrograde motion is very small. For example, in January and February 2137, it moves retrograde only 34minutes in right ascension.[1]
In popular culture
In the novel and television series The Expanse, a catastrophic science experiment is unleashed on a civilian population living within tunnels cut through Eros. This so-called "Eros Incident" ends with the asteroid mysteriously breaking its usual orbit and crashing into Venus.[27]
It makes an appearance in the novel Ender's Game by Orson Scott Card, serving as a base for humanity.[28]
Gallery
Animation of the rotation of Eros
View from one end of Eros across the gouge on its side towards the opposite end
First mosaic image of Eros taken from an orbiting spacecraft
Mosaic image of Eros
At 4.8km (3.0mi) across, the crater Psyche is Eros's second largest.
Regolith of Eros, seen during NEAR's descent; area shown is about 12 meters (40 feet) across
Orbital diagram of Eros with locations on 7 May 2013
Orbital diagram of Eros with locations on 1 January 2018
Schmadel, Lutz D. (2007). "(433)Eros". Dictionary of Minor Planet Names. Springer Berlin Heidelberg. p.50. doi:10.1007/978-3-540-29925-7_434. ISBN978-3-540-00238-3.
Scholl, Hans; Schmadel, Lutz D. (2002). "Discovery circumstances of the first near-Earth asteroid (433)Eros". Acta Historica Astronomiae. 15: 210–220. Bibcode:2002AcHA...15..210S.
Perrine, Charles D. (1910). Determination of the solar parallax from photographs of Eros made with the Crossley reflector of the Lick Observatory, University of California (Report). Washington, DC: Carnegie Institution of Washington. pp.1–104.
Jones, H.S. (1941). "The solar parallax and the mass of the Moon from observations of Eros at the opposition of 1931". Memoirs of the Royal Astronomical Society. 66: 11–66.
Michel, Patrick; Farinella, Paolo; Froeschlé, Christiane (25 April 1996). "The orbital evolution of the asteroid Eros and implications for collision with the Earth". Nature. 380 (6576): 689–691. Bibcode:1996Natur.380..689M. doi:10.1038/380689a0. S2CID4354612.
Thomas, P.C.; Veverka, J.; Robinson, M.S.; Murchie, S. (27 September 2001). "Shoemaker crater as the source of most ejecta blocks on the asteroid 433Eros". Nature. 413 (6854): 394–396. Bibcode:2001Natur.413..394T. doi:10.1038/35096513. ISSN0028-0836. PMID11574880. S2CID4325299.
Thomas, P.C.; Robinson, M.S. (21 July 2005). "Seismic resurfacing by a single impact on the asteroid 433Eros". Nature. 436 (7049): 366–369. Bibcode:2005Natur.436..366T. doi:10.1038/nature03855. PMID16034412. S2CID4425770.
433Eros (1898DQ) (last obs). JPL Close-Approach Data. 13 November 2011. Retrieved 14 November 2011.
"NEODyS-2 close approaches for (433)Eros". NEODyS-2 Near Earth Objects. European Space Agency / University of Pisa / Space Dynamics Service S.R.L. Retrieved 14 November 2011.
Ender's Game and Philosophy: The Logic Gate is Down. John Wiley & Sons. 2013. p.117.
Further reading
Clark, C.S.; Clark, P.E. (13–17 March 2006). Using boundary-based mapping projections to reveal patterns in depositional and erosional features on 433Eros. 37th Annual Lunar and Planetary Science Conference. League City, Texas. p.1189. Bibcode:2006LPI....37.1189C. Abstract no.1189.
Riner, M. A.; etal. (November 2008). "Global survey of color variations on 433Eros: Implications for regolith processes and asteroid environments". Icarus. 198 (1): 67–76. Bibcode:2008Icar..198...67R. doi:10.1016/j.icarus.2008.07.007.
External links
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Wikimedia Commons has media related to (433) Eros.
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