504 Cora, provisional designation1902 LK, is a metallicasteroid from the middle region of theasteroid belt, approximately 30 kilometers in diameter. It was discovered by American astronomerSolon Bailey atHarvard'sBoyden Station in Arequipa, Peru, on 30 June 1902.[15] It was later named after Cora, a figure inInca mythology.[2]
Cora orbits the Sun in themiddle main-belt at a distance of 2.1–3.3 AU once every 4 years and 6 months (1,640 days). Its orbit has aneccentricity of 0.22 and aninclination of 13° with respect to theecliptic.[1] The body'sobservation arc begins 4 years after its discovery with the first used observation made atHeidelberg in 1906.[15]
Mineralogic observations in the near-infrared with theNASA IRTF telescope using itsSpeX spectrograph, showed that its surface is that of anX-type asteroid, with absorption features indicating the presence ofpyroxene minerals.[13] In 2004, the body's spectrum was also obtained in the SMASSII survey at the U.S.MDM Observatory, Kitt Peak, Arizona.[16]
Several rotationallightcurves ofCora were obtained for this asteroid by astronomersMaria A. Barucci,David Higgins,Axel Martin, and thePalomar Transient Factory. With one exception,[12] they all gave arotation period close to 7.59 hours.[11][10] Among these, David Higgins' observation made in September 2010, at the Hunters Hill Observatory (E14) in Ngunnawal, Australia – gave the best rated lightcurve with a period of7.588±0.003 hours and a brightness variation of 0.20magnitude (U=3-).[9]
According to the space-based surveys carried out by the Infrared Astronomical SatelliteIRAS, the JapaneseAkari satellite, and NASA's WISE telescope with its subsequent NEOWISE mission,Cora's surface has a highalbedo between 0.239 and 0.341. Combined with their respective absolute magnitudes, this results in a diameter estimate of 27.2 to 35.0 kilometers.[3][5][6][7][8] In contrast, theCollaborative Asteroid Lightcurve Link derives a much lower albedo of 0.19 and a diameter of 29.1 kilometers, based on anabsolute magnitude of 10.1.[4]