On 7 July 2021, 2005 QN173 was found to be active by the Asteroid Terrestrial-impact Last Alert System survey.[6] Archival imagery showed it had been active during a previous perihelion passage,[8] dated 22 July 2016.[9] This indicates the activity is due to the sublimation of icy volatiles,[6] as is common with comets.[9] At the time that activity was identified, the object displayed a long, dusty tail, much like a comet. Follow up observations found this tail extended more than 9′ along its orbital plane.[7] By 14 August 2021, the coma around the nucleus was fading, while the brightness of the tail remained roughly constant.[6]
This asteroid has a mean diameter of 3.6±0.2 km, with a low visual albedo of 0.054±0.012. Its colors are consistent with a dark C-typecarbonaceous asteroid taxonomic classification, which is a class more commonly found in the outer main belt. Dust particles ejected from the object had very low velocities of about 1 m/s. This suggests that the dust emission may have been assisted by rapid spin of the asteroid, which would lower the escape velocity.[3]
The asteroid will make its next perihelion passage on 3 September 2026, and it may become active by February 2026.[3]
^ abHsieh, Henry; et al. (October 2021), "The Nucleus and Dust Tail of Active Asteroid (248370) 2005 QN173", Bulletin of the American Astronomical Society, 53 (7), Bibcode:2021DPS....5311004H, 2021n7i110p04.
^Chandler, C. O.; et al. (26 July 2021), Green, Daniel W. E. (ed.), "(248370) 2005 QN_173", Central Bureau for Astronomical Telegrams, 5005, retrieved 17 February 2023.
Olason, Mike (8 October 2021), "Comet 433P", Sky & Telescope, AAS Sky Publishing, LLC, retrieved 19 February 2023.
Ivanova, Oleksandra; et al. (September 2022), "Dust environment of active asteroid (248370) 2005 QN173", 16th Europlanet Science Congress 2022, held 18–23 September 2022 at Palacio de Congresos de Granada, Spain, Bibcode:2022EPSC...16..203I, doi:10.5194/epsc2022-203, EPSC2022-203.